RECORD: Darwin, C. R. 1851. A monograph on the fossil Lepadidæ, or pedunculated cirripedes of Great Britain. London: Palæontographical Society.

REVISION HISTORY: Transcribed for John van Wyhe 2002. Proofread and corrected by Sue Asscher 6.2006. RN1

NOTE: See Marsha Richmond's introduction Darwin's Study of the Cirripedia.

See bibliographical introduction by R. B. Freeman.

The copy scanned was kindly provided by The Earth Sciences Library Cambridge.


[page i]

THE

PALÆONTOGRAPHICAL SOCIETY.

INSTITUTED MDCCCXLVII.

MDCCLI.

[page ii]

[page iii]

A MONOGRAPH

ON THE

FOSSIL LEPADIDÆ,

OR,

PEDUNCULATED CIRRIPEDES OF GREAT BRITAIN.

BY

CHARLES DARWIN, F.R.S., F.G.S.

LONDON:

PRINTED FOR THE PALÆONTOGRAPHICAL SOCIETY.

1851.

[page iv]

C. AND J. ADLARD, PRINTERS, BARTHOLOMEW CLOSE.

[page v]

PREFACE.

I HAVE great pleasure in returning my most sincere thanks to various naturalists, both for intrusting to me their collections of Fossil Cirripedia, and for allowing me, whenever it was advisable, to clear the specimens from their matrix. Although an entire stranger to many of the gentlemen to whom I applied, I have in every instance received the most courteous acquiescence to my demands. To Mr. Fitch, of Norwich, I here beg to return my thanks, for having allowed me to keep, during several months, his unrivalled collection of Cirripedia from the Upper Chalk of Norwich,—the fruit of twenty years' labour. Mr. Bowerbank has given me the freest use of his fine collection, rich in specimens from the Gault. Mr. Wetherell placed in my hands his beautiful and unique specimen of Loricula pulchella, and other species. Professor Buckman sent me, of his own accord, a fine series of the valves of Pollicipes ooliticus, the most ancient Cirripede as yet known, discovered and named by him. To Messrs. Flower, Searles Wood, F. Edwards, Harris, S. Woodward, Tennant, and other gentlemen, I owe the examination of several species new to me. Mr. Morris and Professor E. Forbes have, in their usual kind manner, supplied me with much valuable information, and with the loan of many specimens. To Mr. James de C. Sowerby I must express my thanks for the valuable aid rendered to me by the loan of the original specimens figured in the 'Mineral Conchology;' and for the pains exhibited in the drawings here published.

Professor Forchhammer, of Copenhagen, not only placed at my disposal many valuable specimens deposited in the Geological Museum of the University, but applied to Professor Steenstrup, who, in the most generous manner, sent me the collection in the Zoological department, including the highly valuable original specimens of his excellent Memoir on the Fossil Cirripedia of Denmark and Scania. Subsequently, Professor Steenstrup sent me a second large collection, the fruit of the indefatigable labours of M. Angelin, in

[page] vi PREFACE.

Scania: all these northern specimens have been of the greatest use to me in illustrating the British species. Having applied to Professor W. Dunker of Cassel, for some of the species described by various German authors, he not only sent me many specimens out of his own collection, but procured from Messrs. Roemer, Koch, and Philippi, other specimens of great value; and to these most distinguished naturalists I beg to return my very sincere thanks. Lastly, I may be permitted to state, that I hope very soon to have another and more appropriate opportunity of publicly expressing my gratitude to various gentlemen, who for many months together have left in my hands their large and valuable collections of recent Cirripedia, and who have assisted me in every possible way. I will here only state, that it was owing to the suggestion and encouragement of Mr. J. E. Gray, of the British Museum, that I was first induced to take up the systematic description of the Cirripedia, having originally intended only to study their anatomy. To all the foregoing gentlemen, I shall ever feel under the deepest obligations.

[page] 1

INTRODUCTION.

————————

THE CIRRIPEDIA, both recent and fossil, have been much neglected by systematic naturalists: the fossil species have, however, been more attended to than the recent. Professor Steenstrup has published1 an excellent monograph on the Danish and Scanian Cretaceous species: Mr. J. de Carle Sowerby has given good plates of several British valves in the Mineral Conchology; and F. Roemer2 has illustrated, by rather indifferent figures, though clear descriptions, various German forms. Other less important notices have appeared by several authors. As yet, however, no monograph has been produced on the whole group. The present volume is confined to the Lepadidæ or Pedunculated Cirripedia; and it so happens that the introduction, under the form of notes, of a few foreign species (which are necessary to illustrate the British species), serves to render this Monograph tolerably complete; that is, as far as the specimens collected on the Continent (judging from published accounts) serve for this end,—for we shall immediately see that certain valves are requisite in each genus.

It is unfortunate how rarely all the valves of the same species have been found coembedded; it is evident that, with the exception of some few species, the membrane which held the valves together, decayed very easily, as it does in recent Pedunculated Cirripedes. Hence, in the great majority of cases, the several valves have been found separate. Hitherto it has been the practice of naturalists to attach specific names indifferently to all the valves; and as in each species there are from three to five or six different kinds of valve, there would have been, had not the whole group been much neglected, so many names attached to each species. On the other hand, it has occurred in several instances, that many valves belonging to quite different species have been grouped together under the same name. To avoid these great evils, I have fixed on the most characteristic valves, one in each of the two main genera, and taking them as

1 Naturhistorisk Tidsskrift, af H. Kröyer, 1837 and 1839.          

2 Die Versteinerungen des Norddeutschen Kreidegebirges, 1841.

a

[page] 2 FOSSIL CIRRIPEDIA.

typical, have never, except in one instance where several valves were known all to belong to the same individual, and in another instance in which a valve was very remarkable, attached a specific name to any other one. I have, however, in two cases retained names already given to certain other valves, as they presented remarkable characters, and were almost certainly distinct. In Scalpellum I have taken the Carina or Keel-valve (i. e. dorsal valve of most authors) as typical; and in Pollicipes, the Scuta (i. e. the inferior lateral valves of most authors): it would have been desirable to have taken the same valve in both genera; but it so happened that the Carina has been much more frequently collected than any other valve in Scalpellum, in which genus it is highly characteristic; whereas in Pollicipes, it is apt to present less striking characters than the Scuta, which are, moreover, commoner in most collections. In almost all the Lepadidæ the Terga (i. e. the upper or posterior lateral valves) are not characteristic, and are particularly liable to variation. Although only certain valves in each genus thus receive specific names, yet from the conditions of embedment, several of the other valves can often be safely attributed to the same species.

Much confusion in nomenclature will, I think, be avoided by the plan here adopted; but the study of Fossil Cirripedia must, I fear, owing to the variability of the valves, as seen in some fossil species, and as inferred from what so commonly occurs with recent species, ever remain difficult. In very many of those recent species, of which large series have passed through my hands, several of the valves have varied so much, that had I seen only certain specimens from the opposite poles of the series, I should unhesitatingly have ranked them as quite distinct species: on the other hand there are some recent forms—for instance, some species of Lepas, and again Pollicipes cornucopia, and elegans of Lesson—which are perfectly distinct, but which it would be hopeless to attempt discriminating when fossilized, without quite perfect specimens. It should be borne in mind, that the recognition of the Fossil Pedunculated Cirripedes by the whole of their valves and peduncle, is identical with recognising a Crustacean by its carapace, without the organs of sense, the mouth, the legs, or abdomen: to name a Cirripede by a single valve is equivalent to doing this in a Crustacean by a single definite portion of the carapace, without the great advantage of its having received the impress of the viscera of the included animal's body: knowing this, and yet often having the power to identify with ease and certainty a Cirripede by one of its valves, or even by a fragment of a valve, adds one more to the many known proofs of the exhaustless fertility of Nature in the production of diversified yet constant forms.

I must allude to one more unfortunate cause of doubt in the classification of the extinct Lepadidæ, namely, the difficulty in attributing the separated valves to the two main genera of Scalpellum and Pollicipes; for the chief distinction between these two close genera in the recent state, lies in the number of the valves, and this can very rarely be ascertained in fossil specimens. At first I determined to follow those authors who have united both genera under Pollicipes; but reflecting that I had twelve recent and

[page] 3 INTRODUCTION.

above thirty-seven fossil species, with almost the certainty—as we shall presently see—of very many more being discovered, this plan seemed to me too inconvenient to be followed. There are six recent species which I intend, in a future work, to include under Scalpellum. Four of them have been raised by Dr. Leach and Mr. Gray to the rank of genera; two other unnamed species have certainly equal, if not stronger, claims to the same rank; so again the six recent species of Pollicipes have similar claims to be divided into three genera, thus making nine genera for the twelve recent species of Scalpellum and Pollicipes. In the majority of cases it would be eminently difficult to allocate the fossil species in these nine genera; nevertheless, taking the characters necessarily used for the generic divisions of all the other recent Pedunculated Cirripedes, there can be no doubt that the formation of the above nine genera might be justified, that is, if we are allowed to neglect mere classificatory utility as an element in the decision, and further, if we are invariably bound to make as far as possible all genera of exactly the same value. As far as utility in classification is concerned, it appears to me clear that the institution of so many genera, until many more species are discovered, is highly disadvantageous: with respect to making all genera of exactly equal value, this, though eminently desirable, appears to me almost hopeless; I know not how to weigh the value of slight differences in different valves; or whether a difference in the maxillæ or mandibles be the more important: anyhow, in this particular case, if we raised the six recent species of Scalpellum into six genera, they assuredly would not be distinct to an exactly equal degree. Under these circumstances I have followed a middle term, and kept Scalpellum and Pollicipes distinct,—genera easy to be recognised in a recent state,—which renders the classification of the fossil species, though always difficult and liable to many errors, somewhat easier than if both genera were united into one, and much easier than if the above nine genera were admitted.

APTYCHUS.

Before passing to more general considerations, I must offer a few remarks on the genus Aptychus, or Trigonellites, inasmuch as quite lately a distinguished naturalist, M. D'Orbigny,1 has adopted, and with much ingenuity supported, the view that these anomalous bodies are Pedunculated Cirripedia. It cannot be denied that the general form and lines of growth closely resemble those of the Scuta or lateral inferior valves in Lepas or Anatifa: nor can it be denied, from what we know of recent species, that the Terga (upper lateral valves) and Carina (dorsal valve), which on M. D'Orbigny's view must be considered as absent, are the most likely valves to disappear from abortion. But there are points of difference which, as it appears to me, are of far greater importance than the

1 Cours Élémentaire de Paléontologie, 1849, vol. i, p. 254.

[page] 4 FOSSIL CIRRIPEDIA.

resemblance in mere outline. The peculiar cancellated structure, which is almost visible on the external surface even to the naked eye, is wholly unlike anything known amongst Cirripedia; a thin polished slice of the valves of Lepas and of Aptychus, viewed under a high power, are as unlike as anything can well be.1 In Aptychus the lines of growth are conspicuous on the inner or concave surface, and indistinguishable or not plain on the outer surface; whereas in Lepas exactly the reverse holds good. Again, in some specimens it appears, that additions are made to the shell on the exterior edge of the growing margin, instead of on the inner edge, as in Cirripedia. In Aptychus latus, there is a rather deep internal fold along the whole of that margin, through which the cirri are supposed to have been protruded, and this is unlike anything which I have met with in Cirripedes. In all the species of Aptychus, the two valves are much the most frequently, though not invariably, found widely opened, and attached together, either exactly or nearly so, by the two margins through which the cirri must have been protruded. Now in all true fossil pedunculated Cirripedes, the valves are found either separate, which is the commonest case, or when held together, those on the opposite sides almost exactly cover each other, for there is nothing in the structure of Cirripedia tending to open the valves like the ligament in bivalve shells. How comes it, then, that the specimens of Aptychus, even those found within the protected chambers of Ammonites, thus generally have their valves widely gaping? Even if we pass over this difficulty, is it not strange that the valves should always have been held together by that margin, which in the recent condition is supposed to have been open for a considerable portion of its length, for the exsertion of the cirri; whereas, in not one single instance, as far as I have seen, are the two valves held together by the opposite margin, which in the recent state, on the idea of Aptychus having been a Cirripede, must have been continuously united by membrane.

There is another argument against Aptychus having been a Cirripede, which will have weight, perhaps, with only a few persons: in Pollicipes, the main growth of all the valves is downwards; in Lepas or Anatifa, as well as in most of the allied genera, the main growth of the Scuta and of the Carina (i. e. lower lateral, and dorsal, or valves,) is in a directly reversed direction, or upwards. Now Pollicipes is the oldest known genus of Cirripedes, having been found in the Lower Oolite, whereas hitherto Lepas is not certainly known to have been discovered even in the newest Tertiary formation. So again within the limits of the genus Scalpellum, I know of only two cretaceous species in which the Scuta grow upwards and downwards, and only one case in which the Carina has this double direction of growth; whereas in the recent and one Miocene species, these valves usually grow both upwards and downwards. Hence it would appear that there is some relation between the age of fossil Lepadidæ and the upward or downward direction of

1 When I had the slices made, I did not know of H. von Meyer's paper on Aptychus, in the 'Acta Acad. Cæs. Leop. Car.,' vol. xv, Oct. 1829, tab. lviii and lix, fig. 13, in which perfectly accurate sections are given of the microscopical structure of Aptychus lævis.

[page] 5 INTRODUCTION.

the lines of growth in their valves. Aptychus, according to M. D'Orbigny, existed during the Carboniferous system, at a period vastly anterior to the oldest known Pollicipes, yet on the idea of its having been a Cirripede, the growth of its valves (Scuta) must have been upwards, as in the most recent forms; and it was allied to Lepas, that genus which, in the order of creation, and in the manner of growth, stands at the opposite end of the series from Pollicipes. From the several reasons now given, it does not appear to me that Aptychus, until weightier evidence is adduced, can be safely admitted as a Cirripede.

Geological History.— No true Sessile Cirripede1 has hitherto been found in any Secondary formation; considering that at the present time many species are attached to oceanic floating objects, that many others live in deep water in congregated masses, that their shells are not subject to decay, and that they are not likely to be overlooked when fossilized, this seems one of the cases in which negative evidence is of considerable value. Mr. Samuel Stuchbury, moreover, (to whom I am deeply indebted for much information, and the loan of his beautiful collection of recent species,) has assured me that vast numbers of fossil secondary corals have passed through his hands, and that he has carefully looked without success for those genera which commonly inhabit living corals. Sessile Cirripedes are first found in Eocene deposits, and subsequently, often in abundance, in the later Tertiary formations. These Cirripedes now abound so under every zone, all over the world, that the present period will hereafter apparently have as good a claim to be called the age of Cirripedes, as the Palæozoic period has to be called the age of Trilobites. There is one apparent exception to the rule that Sessile Cirripedes are not found in Secondary formations, for I am enabled to announce that Mr. J. de C. Sowerby has in his collection a Verruca (= Clysia, Clytia, Creusia, Ochthosia) from our English chalk: but this genus, though hitherto included amongst the Sessile Cirripedes, must, when its whole organisation is taken into consideration, be ranked in a distinct family of equal value with the Balanidæ and Lepadidæ, but perhaps more nearly related to the latter than to the Sessile Cirripedes. Hence the presence of Verruca in the Chalk is no real exception to the rule that Sessile Cirripedes do not occur in Secondary formations; on the contrary, it harmonises with the law, that there is some relation between serial affinities of animals, and their first appearance on this earth.

The oldest known pedunculated Cirripede is a Pollicipes, discovered by Professor Buckman in the Stonesfield Slate in the Lower Oolite: two species of the same genus have been described by Mr. Morris from the Oxford Clay, in the middle Oolite. I have

1 Dr. Petzholdt has described and figured (Jahrbuch, 1842, p. 403, tab. x), a Balanus carbonaria from the carboniferous system; but as neither the operculum, the structure of the shell, the number of the valves, nor their manner of growth, can be made out or are described, the evidence appears quite insufficient to admit the existence of this genus at so immensely a remote epoch. Bronn, in the 'Index Palæontologicus,' gives, under Tubicinella, a cretaceous species; I have unfortunately not been able to consult the original work cited.

[page] 6 FOSSIL CIRRIPEDIA.

not heard of any Cirripede having been as yet discovered in the Upper Oolite, or in the Wealden formation. During the deposition of the great Cretaceous System, the Lepadidæ arrived at their culminant point; there were then three genera, and at least thirty-two species, some occurring in every stage of this system. Besides the thirty-two certainly known cretaceous forms, and several other doubtful ones, I believe that very many more will yet be discovered; I infer this from the fact, that in almost every collection lent to me for examination, although very small, I have found some new species. I have three or four species from the Gault; from five to eight in the Lower Chalk, and from nine to twelve species in the Upper Chalk (not including the Faxoe, Scanian, and Maëstricht stage); and of these nine to twelve species, five have been found by one collector, Mr. Fitch, in one locality, namely near Norwich. In Scania M. Angelin has found no less than nine or ten species, all belonging to the upper or Maëstricht stage of the Chalk. These fossils, judging from the habits of recent species of the same genera, were probably attached to fixed, or nearly fixed, objects at the bottom of the sea. Now at the present day, of attached Pedunculata (reckoning even Crustacea and Echinidæ as fixed objects), the whole Mediterranean and New Zealand can boast each only of three species, in both cases including Alepas, which is destitute of calcified valves and therefore not likely to be fossilized; Australia has three species; Madeira has four species, including one with very small and imperfectly calcified valves; the great Phillipine Archipelago, however, has afforded, owing to the labours of Mr. Cuming, as many as five species, though including one with horny valves, and a Lithotrya which lives embedded on the beach. Therefore since we already have nine or ten fossil species from one locality, and from the same stage of the chalk, we may admit that the pedunculated Cirripedes arrived during the upper part of the Cretaceous system at their culminant point.

Although, for this family, the number of species were considerable during the Cretaceous period, the individuals were mostly rare. I infer this from the small number of specimens in all collections; for instance, Mr. Fitch, who has assiduously collected for twenty years in the chalk near Norwich, possesses in his entire collection only nine keel-valves of Scalpellum maximum, and six of S. fossula; he has two Scuta (and with regard to these valves, it must be remembered, that each individual had two) of Pollicipes striatus, two of P. fallax, and four of P. Angelini. This occasional want of a relation, within the same region, between the number of the species in any given genus, and of the individuals appertaining to such species, is a singular fact, and has been strongly insisted on by Dr. Hooker, in regard to the Coniferous trees of the southern hemisphere: one would naturally have expected, that where circumstances favoured the existence of numerous species of a genus, they would likewise have favoured the multiplication of the individuals in all or most of such species; but this, as we here see, has not always been the case.

In the Eocene, Miocene, and Pliocene Tertiary deposits, I know only of two species of Scalpellum, and two of Pollicipes, with indications of two or three other species, all distinct

[page] 7 INTRODUCTION.

from recent forms. It is a rather singular fact, considering the present wide distribution of the genus Lepas or Anatifa, and the frequency of the individuals, that not a single valve known certainly1 to belong to this genus, or to any of the closely-allied genera, has hitherto been found fossil.

The oldest known cirripede is, as we have seen, a Pollicipes from the lower Oolite, and it does not differ conspicuously from some of the recent species of the same genus; so, again, the cretaceous Scalpellum fossula, and the eocene S. quadratum are certainly very nearly related to the recent S. rutilum (nov. spec.). Loricula alone is a genus perfectly distinct from all living Cirripedia; and I may here add that of the Tertiary Sessile Cirripedes, I have hitherto not seen a single new generic form. This persistence of the same genera is somewhat remarkable, considering that amongst ordinary Crustacea nearly all the Secondary species belong to extinct genera;2 it should, however, be borne in mind that Limulus has survived from the Palæozoic period to the present day. The Oolitic, Cretaceous, Tertiary, and recent species of Lepadidæ are all different from each other. By looking at the annexed Table, and putting out of question the species of which the age is uncertain, we have five common to two stages of the chalk; that is assuming for the present that the classification of the stages of the chalk commonly used and here followed, is correct. Pollicipes glaber is common to three, and, I believe, to four stages. Scalpellum arcuatum occurs in the Chalk-marl, and upper Greensand, and therefore this species also extends through three stages; but there is a slight difference between the specimens from the upper and lower stages, which some authors might perhaps consider specific. If fossil cirripedia had, like most recent species, very wide horizontal or geographical ranges, then, in accordance with a law now generally admitted, a considerable vertical range in some of the species is not improbable.

I may here observe that I am assured by Professors Forchammer and Steenstrup, that the formations of Scania and Westphalia are equivalent to that of Faxoe; and hence to that of Maëstricht. I have called these formations the " Maestricht formation," to distinguish them from the common upper or white Chalk.

1 In a mere catalogue, published without descriptions, in the 'Jahrbuch' for 1831, p. 155, by Hoenninghaus, Anatifa cancellata is given as a tertiary species: Mr. G. B. Sowerby has stated, in his ' Genera of Shells,' that he has seen a Tertiary specimen of this genus, but he cannot remember which valve it was.

2 Pictet, Traité Élémentaire de Paléontologie, tom. iv. p. 4.

[page] 8 FOSSIL CIRRIPEDIA.

TABLE OF THE DISTRIBUTION OF THE SPECIES.

 

Tertiary.

Faxoe, Scania, Maëstricht.

Upper Chalk.

Lower Chalk.

Chalk Marl.

Upper Greensand.

Gault.

Lower Greensand.

Middle Oolite.

Lower Oolite.

Scalpellum magnum...
*









— quadratum.. *









— fossula.... *







— maximum... *
*







— lineatum... *






— hastatum... *





— angustum... *? *? *?




— quadricarinatum. *





— triliniatum.. *





— simplex... *


— arcuatum... *
*



— tuberculatum.. *? *? *?




— solidulum ... *








— semiporcatum. *








— (?) cretæ.... *







Pollicipes concinnus...
*

— ooliticus... *
— Nilssonii... *








— Hausmanni.. *


— politus .... *?



— elongatus... *







— acuminatus.. *






— Angelini... *
*







— reflexus... *









— carinatus... *









— glaber.... *?
*
*
*





— unguis.... *
*


— validus.... *








— gracilis.... *
*






— dorsatus... *








— striatus.... *







— semilatus... *?
*?
*?





— rigidus.... *



— fallax.... *
*







— elegans.... *








— Bronnii.... *




— planulatus... *

Loricula pulchella.... *







————————————————————————————————————————————
Total 38....

4

9—10

9—12

5—8

5—8

1

3—4

3

2

1

[page] 9 INTRODUCTION.

NOMENCLATURE OF THE VALVES.

Figure I.

CAPITULUM.

PEDUNCLE.

————————

N.B.—In the Carina of Scalpellum, A is the tectum; B the parietes; C the intra-parietes.

Figure II.

Scutum of POLLICIPES.

Figure III.

Tergum of POLLICIPES.


Whoever will refer to the published descriptions of recent and fossil Cirripedia, will find the utmost confusion in the names given to the several valves; thus, the valve named in the above woodcut, the Scutum, has been designated by various well-known naturalists as the " ventral," the " anterior," the " inferior," the " ante-lateral," and the " latero-inferior" valve; the first two of these titles have, moreover, been applied to the rostrum or rostral valve of Sessile Cirripedes. The Tergum has been called the " dorsal," the " posterior," the " superior," the " central," the " terminal," the " postero-lateral," and the " latero-superior" valve. The Carina has received the first two of these identical epithets, viz. the " dorsal" and the " posterior;" and likewise has been called the " keel-valve." The confusion, however, becomes far worse, when any individual valve is described, for the very same margin which is anterior or inferior in the eyes of one author, is the posterior or superior in those of another; it has often happened to me that I have been quite unable even to conjecture to which margin or part of a valve an author was referring. Moreover, the length of these double titles is inconvenient.

Hence, as I intend to describe all the recent and fossil species, I have thought myself

b             

[page] 10 FOSSIL CIRRIPEDIA.

justified in giving short names to each of the more important valves, these being common to the Pedunculated and Sessile Cirripedes.

The title of peduncle, which is either naked or squamiferous, requires no explanation; the scales and lower valves are arranged in whorls, which I have called by the botanical term of Verticillus. The part supported by the peduncle, and which is generally, though not always, in recent species protected by valves, I have designated the Capitulum.

I have applied the term Scutum to the most important and persistent of the valves, and which can almost always be recognised by the hollow giving attachment to the adductor scutorum muscle, from the resemblance which the two valves taken together bear to a shield, and from their office of protecting the front side of the body. From the protection afforded by the two Terga to the dorso-lateral surface of the animal, these valves have been thus called. The term Carina is a mere translation of the name already used by some authors, of Keel-Valve: in the genus Scalpellum, in which this valve is taken as typical, I have found it quite necessary, with fossil specimens, to distinguish the roof (see Woodcut, I,) or exterior surface, as the tectum (A); the inflected sides, as the parietes (B); and in several species in the upper half of the valve, the intra-parietes (C): the expressions of apex, basal margin, and inner margin, as applied to the Carina, require no explanation. The rostrum has been so called from its relative position to the Carina or keel. There is often a sub-carina and a sub-rostrum.

The remaining valves have been called Latera; there is always one large upper one inserted between the lower halves of the Scuta and Terga, and this I have named the Upper Latus or Latera; the other Latera in Pollicipes are numerous, and require no special names; in Scalpellum, where there are at most only three pair beneath the Upper Latera, it is convenient to speak of them (vide Woodcut, I,) as the Carinal, Infra-median, and Rostral Latera.

As each valve, especially amongst the fossil species, requires a distinct description, I have found it indispensable to give names to each margin. These have mostly been taken from the name of the adjoining valve, (See Woodcut, I.) In Pollicipes the margin of the Scutum adjoining the Tergum and Upper Latus, is not divided (Woodcut, II,) into two distinct lines, as in Scalpellum, and is therefore called the tergo-lateral margin; a narrow portion or slip along this side of the valve may be seen (Woodcut, II,) to be formed of upturned lines of growth; this is often of service in classification, and I have called it the tergo-lateral slip or segmentum tergo-laterale. In Scalpellum (Woodcut, I,) these two margins are separately named Tergal and Lateral. The angle formed by the meeting of the basal and lateral or tergo-lateral margins, I call the baso-lateral angle; that formed by the basal and occludent margins, I call, from its closeness to the Rostrum, the rostral angle. In Pollicipes the Carinal margin of the Tergum (Woodcut, III,) can be divided into an upper and lower carinal margin.

That margin in the Scuta and Terga which opens and shuts for the exsertion and retraction of the cirri, I have called the Occludent margin.

[page] 11 INTRODUCTION.

During the periodical growth of the valves, especially when they are thick and massive, it happens in several species that the underlying corium deserts their upper ends or umbones, which consequently become marked by lines or ridges of growth, as I have called them, though perhaps lines of recession would have been more strictly correct. Such valves, consequently, have their upper ends projecting from and beyond the capitulum, and are said to project freely or liberè; this is often more especially the case with the Carina in Pollicipes, and in a lesser degree with the Terga.

From the peculiar curved position which the animal's body occupies within the capitulum, I have found it far more convenient (not to mention the confusion of nomenclature already existing) to apply the term Rostral instead of ventral, and Carinal instead of dorsal, to almost all the external and internal parts of the animal. Cirripedes have generally been figured with their surfaces of attachment downwards, hence I have termed the lower margins and angles the Basal, and those pointing in an opposite direction the Upper; strictly speaking, the exact centre of the usually broad and flat surface of attachment is the anterior end of the animal, and the upper tips of the Terga, the posterior end of that part of the animal which is externally visible; but in some cases, for instance in Coronula, where the base is deeply concave, and where the width of the shell far exceeds the depth, it seemed almost ridiculous to call this, the anterior extremity; as likewise does it in Balanus to call the united tips of the Terga, lying deeply within the shell, the most posterior point of the animal as seen externally.

[page 12]

CLASS—CRUSTACEA. SUB-CLASS—CIRRIPEDIA.

Family—LEPADIDÆ.

Cirripedia pedunculo flexili, musculis instructo: Scutis1 musculo adductore solummodô instructis: valvis cæteris, siquæ adsunt, in annulum immobilem haud conjunctis.

Cirripedia having a peduncle, flexible, and provided with muscles. Scuta1 furnished only with an adductor muscle: other valves, when present, not united into an immovable ring.

Besides the brief characters here given others might have been added, drawn from the softer parts of the animals, but as this Volume treats only of Fossil species, they would have been in this place superfluous. Nor have I thought it advisable to give here any definition of the Sub-class Cirripedia, or of the Order which contains both the Lepadidæ and Balanidæ, that is the Pedunculated and Sessile Cirripedes; for the characters would likewise have had to be derived almost entirely from the softer parts of the animal. It may, however, be worth stating, that by following the metamorphoses of the Cirripedia, it can be clearly shown that the capitulum together with the peduncle, in the Pedunculated Cirripedes, and that the shell together with the operculum in the Sessile Cirripedes, that is the whole of what is externally visible, consists simply of the first three segments of the head. In many Crustacea the carapace, formed by the backward production of the three anterior rings of the head, covers the dorsal surface of the thorax, and in some it encloses the limbs and mouth. This is likewise the case with the Cirripedia, and it is only the wonderful elongation of the anterior part of the head, its fixed condition, and the absence of external eyes and antennæ, which gives to the Cirripedia their peculiar character, and has hitherto prevented the homologies of these parts from having been recognised.2

1 The meaning of this and all other terms is given in the Introduction at page 9.

2 Nevertheless, in some Stomapoda, more especially in Leucifer of Vaughan Thompson, the anterior part of the head is only a little less elongated, compared with the rest of the body, than in the Cirripedia. That accomplished naturalist, M. J. D. Dana (Silliman's 'American Journal,' March, 1846,) has stated that " the pedicel of Anatifa corresponds to a pair of antennæ in the young:" although the peduncle or pedicel is undoubtedly thus terminated, this view cannot, I think, be admitted. In the larva, the part anterior to the mouth is as large, in proportion to the rest of the body, as in some mature Cirripedia: this anterior part supports only the eyes, antennæ, and two small cavities furnished with large nerves, which I

[page] 13 SCALPELLUM.

I may further state, that in the several Orders of Cirripedia such important differences of structure are presented, that there is scarcely more than one great character by which all Cirripedia may be distinguished from other Crustacea: this character is, that they are attached to some foreign object by a tissue or secretion (for at present I hardly know which to call it), which debouches, in the first instance, through the prehensile antennæ of the larva, the antennæ being thus embedded and preserved in the centre of the basis. The cementing substance is brought to its point of debouchement by a duct, leading from a gland, which (and this is perhaps the most remarkable point in the natural history of the Class) is part of and continuous with the branching ovaria. When we look at a Cirripede, we, in fact, see only a Crustacean, with the first three segments of its head much developed and enclosing the rest of the body, and with the anterior end of this metamorphosed head fixed by a most peculiar substance, homologically connected with the generative system, to a rock or other surface of attachment.

Genus—SCALPELLUM.

SCALPELLUM. Leach. Journ. de Physique, t. lxxxv, July, 1817.

LEPAS.  Linn. Systema Naturæ, 1767.

POLLICIPES. Lamarck. Animaux sans Vertebres.

POLYLEPAS.  De Blainville. Dict. des Sc. Nat., 1824.

SMILIUM (pars generis). Leach. Zoolog. Journal, Vol. 2, July, 1825.

CALANTICA (pars generis). J. E. Gray. Annals of Philosophy, vol. x, (2d series,) Aug. 1825.

THALIELLA (pars generis). J. E. Gray. Proc. Zoolog. Soc., 1848.

ANATIFA. Quoy et Gaimard, Voyage de l'Astrolabe, 1826-34.

XIPHIDIUM (pars generis). Dixon. Geology of Suffolk, 1850.

Valvis 12 ad 15: Lateribus verticelli inferioris quatuor val sex, lineis incrementi plerumque convergentibus; Subrostrum rarissime adest: Pedunculo squamifero, rarissime nudo.

suspect to be auditory organs; this part, therefore, I think, must unquestionably consist of the first two or three segments of the head: within it, even before the larva moults, the incipient striæless muscles and ovaria of the peduncle can be distinctly traced: immediately after the moult, we see this anterior part converted into a perfect peduncle; and for some time afterwards certain coloured marks, indicating the former position of the (so called) olfactory cavities and of the cast-off compound eyes, are still preserved. The prehensile antennæ are not cast off, for they are fastened down by the cementing substance, and are thus preserved in a functionless condition, with their muscles absorbed; after a time even the corium is withdrawn from within them. From the above and other coloured marks, and from the antennæ being preserved, it is easy to point out, in the peduncle of a young though perfect Lepas, the exact point which each part occupied in the head of the natatory larva.

Since the above was written, I find that Lovén has taken the same view of the homologies of the external parts of the Cirripedia: in his description of his Alepas squalicola, (Ofversigt of Kongl. Vetens., &c., Stockholm, 1844, pp. 192-4,) he uses the following words: " Capitis reliquæ partes, ut in Lepadibus semper, in pedunculum mutatæ et involucrum," &c.; his involucrum is the same as the Capitulum of this work.

[page] 14 FOSSIL CIRRIPEDIA.

CHARACTERES VALVARUM IN SPECIEBUS FOSSILIBUS.

Carina angusta, introrsùm arcuata, ab apice ad marginem basalem paululum dilatata; parietes valde inflexi, costis manifestis a tecto plerumque disjuncti; in multis speciebus intra-parietibus instructi: intra-parietes nonnumquam supernè producti ultra Umbonem, qui fit inde subcentralis: parietum lineæ incrementi perobliquæ. Scuta plerumque subconvexa et tenuia, trapezoidea; marginibus tergalibus lateralibusque angulo insigni disjunctis.

Sect. †. Subcarina adest (solummodò species recentes).

Sect. ††. Subcarina deest.

A. Valvæ quatuordecim: Carinæ umbone subcentrali.

B. Valvæ duodecim: Carinæ umbone ad apicem posito.

Valves 12 to 15 in number. Latera of the lower whorl, four or six, with their lines of growth generally directed towards each other. Sub-rostrum1 very rarely present. Peduncle squamiferous, most rarely naked.

CHARACTERS OF THE VALVES IN FOSSIL SPECIES.

Carina narrow, bowed inwards, widening but little from the apex to the basal margin, having parietes much inflected, and generally separated by distinct ridges from the tectum, and having in many species intra-parietes, which are sometimes produced upwards beyond the umbo, so as to make it sub-central; lines of growth on the parietes very oblique. Scuta generally only slightly convex and thin, four-sided, the tergal and lateral margins distinctly separated by an angle.

Sect. †. Subcarina present. (This section includes only recent species.)

Sect. ††. Subcarina absent.

A. Valves fourteen in number; Carina with the umbo subcentral.

B. Valves twelve; Carina with the umbo at the apex.

The first of the above two paragraphs contains the true Generic description (here leaving out the softer parts), as applicable to recent and, as far as known, to fossil species: the second paragraph has been drawn up to aid any one in classifying the characteristic valves, when found separated, as is most frequently the case with all fossil Pedunculata. The first or proper Generic characters would have been more precise, had it not been for the existence of one recent species, the S. villosum (Pollicipes villosus, Leach, Calentica Homii, J. E. Gray,) which leads into the next genus Pollicipes. I mention this species in order to confess, that had the valves been found separately, and their number unknown, they would certainly have been included by me under Pollicipes, although, taking the whole organisation into consideration, I have determined to include this species under Scalpellum. I need not

1 The meaning of this and all other special terms is given in the Introduction at p. 9.

[page] 15 SCALPELLUM.

here repeat the remarks made in the Introduction on the great difficulties in classifying the recent species, and still more the fossil species of Scalpellum. I may, however, here state that should the S. vulgare be hereafter kept distinct in a genus to itself, S. magnum would have to go with it. Should a recent species, which in a future work I shall describe under the name of S. rutilum, be generically separated, it will probably have to bear the name of Xiphidium, from its alliance to the Eocene X. quadratum of Sowerby, to which species the cretaceous S. fossula and several other forms are apparently closely allied. These latter species, however, are likewise closely allied to the Scalpellum ornatum, which Mr. Gray has already raised to the rank of a genus under the name of Thaliella. There are some fossil species, as S. arcuatum, and simplex and solidulum, which I cannot rank particularly near any recent forms. Mr. Sowerby founded the genus Xiphidium on the umbo in the Carina being situated at the apex, and on its growth being consequently exclusively downwards. This is likewise the case with the recent S. rutilum; but I shall have occasion to show, under S. magnum, that the upward growth of the Carina in that and other species of the genus, depends merely on the intra-parietes, which are present in many species, meeting each other and being thus produced upwards. Moreover, in the recent S. ornatum, the position of the umbo is variable, according to the age of the specimen; in half-grown individuals being seated at the apex, and in large specimens being sub-central, as in S. vulgare, magnum, and other species. I should have been very glad to have retained the genus Xiphidium, but taking into consideration the whole organisation of the six recent species, I can only repeat that we must either make six genera of them, or leave them altogether, and this latter has appeared to me the most advisable course.

Sexual Peculiarities.—For reasons stated in the Introduction, I have kept the genera Scalpellum and Pollicipes distinct; but I may mention, in order to call attention to a point of structure which may hereafter be discovered in some fossil species, that I was much influenced in this decision by some truly extraordinary sexual peculiarities in all six recent species of Scalpellum. Scalpellum ornatum is bisexual; the individual forming the ordinary shell, is female; each female has two males (a case of Diandria monogynia), which are lodged in small transverse depressions, one on each side, hollowed out, on the inner sides of the Scuta, close above the slight depressions for the adductor scutorum muscle; in S. rutilum (nov. spec.) two males are lodged in the same place on each side, but rather in concavities in the valve, than in distinct depressions. As these are the two recent species most nearly related to several Cretaceous and Eocene forms, we might expect to find similar depressions in some fossil species; but as yet I have not succeeded in distinctly finding such. The male cirripedes are very singular bodies; they are minute, of the same size as the full-grown larva; they are sack-formed, with four bead-like rudimental valves at their upper ends; they have a conspicuous internal eye; they are absolutely destitute of a mouth, or stomach, or anus: the cirri are rudimental and furnished

Inside view of the scutum in Scalpellum ornatum. (A) is the depression for the adductor muscle.

[page] 16 FOSSIL CIRRIPEDIA.

with straight spines, serving, apparently, to protect the entrance of the sack: the whole animal is attached, like ordinary cirripedes, first by the prehensile antennæ, and afterwards by the cementing substance; the whole animal may be said to consist of one great sperm-receptacle, charged with spermatazoa; as soon as these are discharged, the animal dies.

A far more singular fact remains to be told: Scalpellum vulgare is like ordinary cirripedes, hermaphrodite, but the male organs are somewhat less developed than is usual; and, as if in compensation, several short-lived males are almost invariably attached on the occludent margin of both Scuta, at a spot marked by a fold (not thus caused), as may be seen on the inside view of this valve in the fossil S. magnum, which, in all probability, was furnished with them. I have called these beings complemental males, to signify that they are complemental to an hermaphrodite, and that they do not pair like ordinary males with simple females. In Scalpellum vulgare, the complemental male presents only slight specific differences from the male of S. ornatum. It would be foreign to the purpose of this volume here to enter on further details; nor should I have touched on the subject, had I not wished specially to call attention to the presence of cavities on the under sides of the Scuta above the pits for the adductor muscle. I will only add, that in the other species of Scalpellum, the complemental males are more highly organised, and are furnished with a mouth and prehensile cirri; the valves are more or less rudimental in the different species; these complemental males are not always present, and are never attached to young hermaphrodites; when present, they adhere in such a position, that they can discharge their spermatozoa into the sack of the hermaphrodite: their attachment does not affect the form of the valves.1

Description of Valves.—It will, I think, be most convenient to confine the following description to the fossil species of the genus. No one specimen has been found quite perfect; but, judging from analogy, the capitulum was probably formed of fourteen valves in S. magnum, and of twelve in the remaining species. These valves are commonly smooth,

1 Exactly analogous facts are presented, though more conspicuously, by the two species of the genus Ibla. Before examining this genus, I had noticed the complemental males on Scalpellum vulgare, but had not imagined even that they were Cirripedia. Ibla Cumingii (as I propose to call a new species collected by Mr. Cuming, at the Philippines) is bisexual; one or two males being parasitic near the bottom of the sack of the female. These males are small, are supported on a long peduncle, but are not enclosed in a capitulum (such protection being here unnecessary), are furnished with a mouth, ordinary trophi, stomach, and anus: there are only two pair of cirri, and these are distorted, useless and rudimentary; the whole thorax is extremely small; there is no penis, but a mere orifice beneath the anus for the emission of semen; hence Ibla Cumingii is exactly analogous to Scalpellum ornatum. On the other hand, the closely allied Australian Ibla Cuvierii, like Scalpellum vulgare, is hermaphrodite, but has, in every specimen opened by me, a complemental male attached to near the bottom of the sack; this complemental male differs only about as much from the male of Ibla Cumingii, as the female J. Cumingii differs from the hermaphrodite form of I. Cuvierii. I intend hereafter to give detailed anatomical descriptions and drawings of the males and complemental males of Ibla and Scalpellum.

[page] 17 SCALPELLUM.

but in two or three species are marked with longitudinal ridges; they are generally rather thin; this, however, is a character which is variable even in the same species.

Carina narrow, widening but little from the apex downwards, slightly or considerably curved inwards, with the umbo seated at the uppermost point: S. magnum, however, must be excepted, for in it the umbo is sub-central, and the valve almost angularly bent, as will be described in detail under that species. The apex rarely projects freely; but this is a variable point in the same species; the basal margin is either pointed, rounded, or rarely truncated. The chief character by which this valve can be recognised, as belonging to the genus Scalpellum, is the distinct separation by an angle, (see woodcut, Fig. 1, in the Introduction,) often surmounted by a prominent ridge, of the tectum or roof, from the parietes, which are either steeply or rectangularly inflected; the lines of growth on these parietes are oblique. A still more conspicuous character is afforded by the part (when present), which I have called the intra-parietes; these give to the valve a pieced appearance, and seem let in, to fill up a vacuity between the upper part of the carina and the terga, and this is their real office; they are separated from the true parietes by a ridge, which evidently marks the normal outline of the valve. These intra-parietes are flat, and they have a striated appearance rather different from the rest of the valve; and the lines of growth on them are extremely oblique, almost parallel to the inner margins of the valve.

Scuta very slightly convex; four-sided; the tergal and lateral margins being divided by a slightly projecting point or angle; and this is the chief character by which the scuta of this genus can be distinguished from those of Pollicipes. The umbo is seated at the uppermost point, except in S. magnum, and in S. (?) cretæ (Tab. I, fig. 1 c, and fig. 11 c), in which species the lines of growth, instead of terminating at the angle separating the lateral and tergal margins, are produced upwards, so that the valve is added to above the original umbo. In S. tuberculatum (fig. 10 d), the scuta present an intermediate character between that in ordinary fossil species, for instance in S. fossula (fig. 4 a), and in S. magnum and cretæ. The occludent margin is nearly straight, or slightly curved; both it and the lateral margin form nearly rectangles with the basal margin, which is nearly straight. Internally the depression for the adductor scutorum is generally, but not always, very plain; sometimes the valve is filled up and rendered solid in the upper part above the adductor muscle. The apex sometimes projects freely, and is internally marked with lines of growth. The internal occludent margin, or edge, is also often marked by lines of growth, and the part thus marked, close above the adductor muscle, sometimes becomes suddenly wider; this is caused by some slight change in the position of the animal's body during growth.

Terga flat, either trigonal or rhomboidal, and, in the former case, sometimes so much elongated, with the carinal margin so much hollowed out, as to become almost crescent-shaped; a slight furrow often runs from the upper to the basal angle. Internally, in the upper part, there is in some species a little group of small longitudinal ridges, unlike anything I have seen in recent species, and serving, I apprehend, to give firmer attachment to the corium.

c            

[page] 18 FOSSIL CIRRIPEDIA.

Rostrum unknown in any fossil species; but judging from recent species, it probably existed in all.

Upper latera known only in three species; in S. magnum it is irregularly oval, with the umbo central: in S. quadratum and fossula, five-sided, with the umbo at the upper angle: in the eocene S. quadratum, however, an inner ledge very slightly projects beyond the two upper sides, and first indicates a tendency to upward growth. Rostral latera, known only in S. magnum and quadratum, they are transversely elongated, narrow, and small. Infra-median latera unknown; they probably existed only in S. magnum. Carinal latera, known in S. magnum, quadratum, fossula, solidulum, and maximum; in the first species they are transversely elongated; in the three latter, of an irregular curved shape, and flat. In the fossil and recent species, the rostral and carinal latera grow chiefly in a direction towards each other; so that their umbones are close to, or even seated exteriorly to, the carinal and rostral ends of the capitulum. Peduncle, calcified scales are known only in one species, the S. quadratum; but they probably existed in all : the naked peduncle, however, of the recent S. Peronii must make us cautious on this head.

[A] Valvæ quatuordecem: Carinæ umbone sub-centrali.

1. SCALPELLUM MAGNUM.1 Tab. I, Fig. 1.

S. Laterum carinalium et rostralium umbonibus liberè (sicut cornua) prominentibus, dimidiam seu tertiam partem longitudinis valvarum æquantibus.

Carinal and rostral latera, with their umbones projecting freely like horns, and equalling one half or one third of the entire length of these valves.

Coralline Crag (lower part). Sutton, Gedgrave, Sudbourne. Mus. S. Wood and Lyell.

From the close affinity between this species and the recent Scalpellum vulgare, we may confidently infer that the capitulum consisted of fourteen valves, which are all preserved in Mr. Wood's collection, with the exception of the infra-median latera and of the rostrum. This latter valve would, no doubt, be rudimentary, and it has been overlooked by naturalists even in the recent species. The chief difference, excepting size, between these two species, is in the form of the rostral and carinal latera, but unfortunately these valves are extremely variable. It might even be maintained, with some degree of probability, that S. magnum was only a variety of S. vulgare. The valves of S. magnum are all thicker, stronger, more rugged, and considerably larger than in S. vulgare. Taking

1 I have followed Mr. Morris in his Catalogue, in adopting this name from the MS. of Mr. Searles Wood, to whose kindness I am greatly indebted for having placed in my hands the whole of his large series of valves of this species.

[page] 19 SCALPELLUM.

the largest scutum, tergum, carina and upper latera in Mr. Wood's collection, they are very nearly double the size of the same valves in the largest specimen of S. vulgare seen by me, namely from near Naples, which had a capitulum eight tenths of an inch in length; and they are more than double the size of the same valves in any British specimen. Scalpellum magnum probably had a capitulum one inch and a half in length.

Carina (Tab. I, fig. 1 b and f) abruptly, almost rectangularly bent, with the umbo of growth seated just above the bend, at about one third or one fourth of the entire length of the valve from the upper point; form linear, with the lower part slightly wider than the upper. Exteriorly the surface is rounded with no central ridge, excepting near the umbo, where the narrowness of the whole valve gives it a carinated appearance; basal margin rounded. From the umbo two faint ridges run to each corner of the basal margin, separating the steeply-inclined parietes from the roof,—a character of some importance in the cretaceous species of this genus: outside of these two ridges there are other two ridges, not extending down to the basal margin, and separating the parietes from the intra-parietes, which latter being united at their upper ends, and produced upwards, form that part of the carina which is above the umbo. By comparing the lateral views of the carina of the cretaceous S. fossula (fig. 4 c), and of this species, it will be seen, that the apparently great difference of the umbo of growth being either at the apex, or, as in this species, sub-central, simply results from the lines of growth of the intra-parietes meeting each other, the valve being thus added to at its upper end. The carina of S. magnum, examined internally, is found often to be narrower under the umbo than either above or below it, a character I have not seen in the recent S. vulgare. The lateral width or depth of the valve (measured from the umbo to the inner edge) is also greater than in S. vulgare: this portion is internally filled up and solidified. No part of the apex of the valve projected freely. The longest perfect specimen which I have seen, is half an inch in length; but I have noticed fragments indicating even a greater size.

Scuta (fig. 1 c) much elongated, trapezoidal, slightly convex; umbo placed on the occludent margin at about one fourth of the entire length of the valve from the apex, so that the valve grows upwards and downwards. Occludent margin straight, slightly hollowed out above the umbo, forming rather less than a right angle with the basal margin, which latter is at right angles to the lateral margin. The tergal margin is separated from the lateral by a slight projection (beneath which the margin is a little hollowed out), and from this projection there runs a ridge, often very conspicuous, to the umbo. The part above the ridge, stands at rather a lower level than that below it, and the lines of growth on it are generally less distinct. This is connected with the fact, as ascertained in S. vulgare, that the valve, during its earliest stage, grows only downwards, the ridge thus indicating the original form of the valve and tendency of the lines of growth. On comparing that part of the scuta beneath the umbo and ridge, in the present species (Tab. I, fig. 1 c), with the whole valve in some other species, for instance in S. fossula (fig. 4 a), in which the umbo is seated at the apex, as it was in the first commencement of growth in S. vulgare and magnum, it

[page] 20 FOSSIL CIRRIPEDIA.

will be seen how closely the two valves resemble each other. The scutum of S. tuberculatum (fig. 10 d) is intermediate in its manner of growth between those of S. magnum and fossula. Internally, the impression for the adductor muscle is deep: on the occludent margin, close to the umbo, there is a deep fold, which is connected with the growth of the upper part of the valve being subsequent to that of the lower part. There is very little difference between this valve and that of S. vulgare; the upper part, however, appears to be always thicker. Length of largest specimen one eighth of an inch.

Terga (fig. 1 d) triangular, sometimes approaching to crescent-shaped; flat and thin, though the thickness of the valve varies. Carinal margin straight, or very slightly hollowed out; in its upper part there is a barely perceptible prominence marking the limit of the upward extension of the carina. Basal angle blunt, rounded; from it a line, formed by the convergence of the zones of growth, runs near and parallel to the carinal margin, up to the apex. Occludent margin about equal in length to the scutal; parallel to the former, a slip of the valve is rounded and slightly protuberant, and this portion projects a little on the scutal margin. A very small portion, or none, of the apex of the valve projected freely. This valve is somewhat narrower, and the scutal margin straighter, than in S. vulgare.

Rostrum unknown, no doubt rudimentary, probably quadrangular.

Upper latera (fig. 1 e) flat, oval, with the upper half a little pointed; the lower margin shows traces in a varying degree consisting of three sides. The surface, but chiefly of the lower half, is faintly marked with striæ radiating from the centre. The umbo lies in the middle, and from it two slight ridges, first bending down, diverge on each side. In Scalpellum vulgare this valve (which is very similar in shape to that of S. magnum) at the first commencement of its growth, as with the scuta, is added to only downwards; and thus the two diverging ridges mark the form which the valve originally tended to assume: bearing in mind that the basal margin tends to be three sided, if we remove that part of the valve above the ridges which have been superadded to the original form, we shall have a five-sided valve, essentially like that in the S. quadratum and S. fossula (fig. 3 e, and fig. 4 d).

Rostral latera (fig. 1, g to k) elongated, widening gradually from the umbo to the opposite end, which is equably rounded: umbonal half free, curling outwards; the internal surface of the other half (h) is nearly flat and regularly oval, with its end towards the umbo pointed; the freely projecting portion varies from nearly one half to one third of the entire length of the valve; but in one distorted specimen it was only one sixth of this length. The width, also, of the valve varies (g and h), compared to its length. This valve, compared with its homologue in S. vulgare, differs more than any of the preceding valves; it is proportionally larger, and the internal or growing surface is oval, instead of being oblong and almost quadrangular; and the umbonal or freely projecting portion in S. vulgare is only one sixth or one seventh of the entire length of the valve.

Infra-median latera unknown.

Carinal latera (fig. 1, l to n) narrow, thick, much elongated, widening gradually from the umbo to the opposite end, which is rounded and obliquely truncated. Surface, exteriorly

[page] 21 SCALPELLUM.

flat; internally convex. The umbonal, freely projecting portion is sometimes more than half, sometimes only about one third, of the entire length of the valve. This portion curls outwards and likewise upwards. The degree of curvature and the width (m and n), in proportion to the length, varies. The upper and lower margins are approximately parallel to each other; the umbonal end of the growing surface is bluntly pointed. This valve differs from its homologue in S. vulgare, in being larger, much narrower in proportion to its length, more massive, and with a far larger portion of the umbonal end freely projecting; also in the approximate parallelism of the upper and lower margins, and in the umbonal end of the growing surface being pointed instead of square. In S. vulgare the upper margin is much more curled upwards than the lower, and the freely projecting portion is only one fifth of the entire length of the valve.

Taking the largest specimens in Mr. Wood's collection, the freely projecting portions of the carinal latera must have stuck out like horns, curling from each other and a little upwards, for a length of a quarter of an inch. So again, the much flattened horns of the rostral latera, curving from each other, but not upwards, must have projected half an inch beyond the probably rudimentary rostrum. The capitulum must have presented a singular appearance, represented in the imaginary restored figure (fig. 1 a), with its pair of projecting horns at both ends.

Peduncle; calcareous scales unknown, but undoubtedly they existed.

Varieties: the variation in the rostral and carinal latera has already been pointed out. In Mr. Wood's collection there are numerous scuta, terga, carinæ, and carinal latera, from Sutton; and these are all smaller than those above described, which come from Sudbourne, and than some others in Sir C. Lyell's collection from Gedgrave. All these places, however, belong (as I am informed by Mr. Wood) to the same stage of the Coralline Crag. In the Sutton specimens the carinal latera show the same character as in those from Sudbourne, but the carina apparently is not internally so much narrowed in under the umbo; this, however, is a character which is conspicuous only in the larger Sudbourne specimens, and anyhow cannot be considered as sufficient to be specific.

I may take this opportunity of stating, that in Mr. Harris's collection of organic remains from the chalk detritus, at Charing, in Kent, I have found the upper part of a carina of a very young and minute Scalpellum, which cannot be distinguished from this species; but considering the state of the specimen, it would be extremely rash to believe in their identity. All the known cretaceous species have the umbo at the apex, so that the Charing specimen differs remarkably from its cretaceous congeners.

[page] 22 FOSSIL CIRRIPEDIA.

[B] Valvæ duodecem: Carinæ umbone ad apicem posito.

2. SCALPELLUM QUADRATUM. Tab. I, fig. 3.

XIPHIDIUM QUADRATUM. Dixon, in Sowerby's Mineral. Conch., Tab. 648; Geology of Suffolk, Tab. xiv, figs. 3 and 4.

POLLICIPES     —    ? J. Sowerby. Geolog. Trans., 2d series, vol. v, pl. 8, fig. 5.

S. tecto parietibusque carinæ planis, lævibus, simplicibus, margine basali feré rotundato; Lateribus superioribus quinque-lateralibus, lævibus.

Carina, with its tectum and parietes flat, smooth, and simple; basal margin almost rounded. Upper latera five-sided, smooth.

Eocene Tertiary. Bognor; Hampstead. Mus. S. Wood, F. Edwards, N. Wetherell.

My materials consist of a slab of rock, belonging to Mr. S. Wood, almost made up of the valves of this species, of two beautiful specimens in Mr. F. Edwards's collection, and of some excellent drawings from Mr. Dixon's specimens by Mr. James de C. Sowerby, in the Mineral Conchology.1 The valves in several of these specimens are nearly in their proper positions, though there is not one in which they have not slipped a little. Their relative positions are given, I believe nearly correctly, in Pl. I, fig. 3 a. Their number I have little doubt was twelve. This, however, includes a rostrum, probably almost rudimentary, the existence of which I infer only from the analogy of all recent species. Mr. J. Sowerby supposed that there were, as in S. vulgare, four pair of latera (and therefore fourteen valves in all), but I conclude, without hesitation, that there were only three pair, as in the recent S. rutilum (nov. spec.), to which the S. quadratum is much more nearly allied than to S. vulgare.

Capitulum: elongated, probably composed of twelve valves. Carina (fig. 3, d, i, k), rather narrow, slightly and regularly bowed and widening from the apex to the basal margin, which latter is bluntly pointed, or almost rounded; internally deeply concave; externally with the tectum and parietes flat, and at right angles to each other;—hence the carina is square-edged, and its specific name has been given to it. Scuta (fig. 3, b, h) oblong, occludent margin slightly arched, forming with the basal rather less than a right angle; tergal margin separated by a just perceptibly projecting point from the lateral margin, which latter is very slightly hollowed out; whole valve slightly convex, with a trace of a ridge running from the apex to the baso-lateral angle. Internally (h), there is a large pit for the adductor scutorum, above which there is a slight depression or fold marked with c urved lines of growth, and in this depression on each side complemental males

1 Some small fragments were found by Mr. Wetherell, and are noticed in his Paper in the fifth volume of the 'Geolog. Transactions,' entitled " Observations on a Well dug on the south side of Hampstead Heath."

[page] 23 SCALPELLUM.

were probably attached. Terga (fig. 3 c) triangular, large, flat, basal angle bluntly pointed; apex slightly projecting, as a solid horn; occludent margin very slightly arched. Rostrum unknown; judging from the narrowness of the umbones of the rostral latera, it was probably minute or rudimentary. Upper latera (fig. 3 e) large compared with the lower valves, flat, five-sided, with the two upper sides the longest; of the three lower sides, that corresponding with the end of the rostral latera is generally (especially in young specimens) the shortest. Umbo seated at the uppermost angle; but in full-sized specimens, a narrow ledge has been added, during the thickening and growth of the valve, along the two upper margins, and consequently round the apex. Rostral latera (fig. 3 f) extremely narrow, three or four times as long as wide; considerably arched, extending parallel to the basal margin of the scuta; widening gradually from the umbo to the opposite end, which is obliquely truncated in a line (as I believe) corresponding with the shortest side of the upper latera; inner surface smoothly arched; during growth, the narrow rostral half of the valve becomes much thickened, and at the same time added to along its upper margin, thus producing a solid, sloping, projecting edge; umbo slightly projecting. Carinal latera (fig. 3 g) almost flat, not elongated, of a shape difficult to be described; approaching to a triangle, with curved sides, and one angle protuberant.

Peduncle. The calified scales are apparently large in proportion to the valves of the capitulum; transversely elongated, pointed at both ends, and more or less crescent shaped.

Affinities. This species was generically separated from Scalpellum by Mr. Dixon, as I am informed by Mr. James Sowerby, solely owing to the umbo of growth in the carina being at the apex, instead of being sub-central, as in S. vulgare; but I need not here repeat the reasons already assigned for at present keeping all the recent and fossil species under the same genus. In the umbo of growth, in the carina and scuta being seated at their upper ends, in the square form of the carina, in there being only three pair of latera, and in the large size of the upper latera, this eocene species is much more closely allied to S. rutilum (nov. spec., of which the habitat is unfortunately not known,) than to any other recent species. In some respects, however, I may remark, S. rutilum is even more closely related to certain cretaceous forms. To S. ornatum, the nearest recent congener of S. rutilum, the present species is allied by the narrowness of the rostral latera, and by the large size and peculiar shape of the scales on the peduncle : the carinal latera perhaps rather more resemble those of S. vulgare than of any other recent species. Certainly, all the affinities in S. quadratum point to S. rutilum, ornatum, and vulgare, and these three recent species are characterised by having males or complemental males attached to the sides of the orifice of the sack, whereas, in the other species, they are elsewhere attached; hence it is that I believe that males were probably lodged in the slight depressions described on the inner sides of the scuta; but the depression is not here nearly so distinctly developed as it is in the recent S. ornatum, and more resembles the fold on the occludent edge of the valve in S. vulgare: I must add that folds of this nature do not necessarily imply the presence of males.

[page] 24 FOSSIL CIRRIPEDIA.

3. SCALPELLUM FOSSULA. Tab. I, fig. 4.

POLLICIPES MAXIMUS. J. Sowerby. Min. Conch., tab. 606 (a tergum), fig. 3.

S. carinâ inter-parietibus instructâ; tecto utrinque costis magnis, tumidis, superne planatis, marginato; margine basali obtusè acuminato. Lateribus superioribus quinquelateralibus; costis duabus modicis ab apice ad marginem basalem continuatis.

Carina, having intra-parietes, with the tectum bordered on each side by large, protuberant, flat-topped ridges; basal margin bluntly pointed; upper latera five sided, with two slight ridges extending from the apex to the basal margin.

Upper Chalk. Norwich; Northfleet, Kent. Mus. Fitch, J. de C. Sowerby, Wetherell.

General Remarks. My materials consist of two specimens, belonging to Mr. Fitch, most kindly lent me for examination; in which, taken together, the scuta, terga, carina, upper and carinal latera, are seen almost in their proper places. In Mr. J. Sowerby's collection there is a single scutum, also, from Norwich. From analogy with the eocene S. quadratum and the recent S. rutilum, I have little doubt that there were only three pair of latera; and that, probably, there was a rostrum. With respect to the exact position of the carinal latera, there is, as also in the case of the S. quadratum, some little doubt.

Capitulum narrow, elongated, probably composed of 12 valves, which are moderately strong, and apparently closely locked together. The length of the capitulum in the largest specimen was 1.1 of an inch.

Carina (fig. 4, c, g, h) strong, moderately bowed, extending far up between the terga, almost to their upper ends; rather narrow throughout, gradually widening from the apex to the base; lines of growth plain; no portion projects freely. The tectum or central portion is slightly arched, subcarinated, and bounded on each side by flat-topped, protuberant ridges: the tectum terminates downwards in a blunt point (the two margins forming an angle of rather above 90°), which projects beyond the bounding ridges; the tectum and the two bounding ridges all widen gradually from the apex towards the base. The parietes are channelled or concave; they do not extend so far down as the ridges bounding the tectum. In the upper half of the carina, we here first see the additional parietes, or intra-parietes, which appear as if formed subsequently to the other parts, and let in between the ordinary parietes of the carina, and the terga. It has been already shown, under S. magnum, that it is the intra-parietes produced upwards, which causes in that and some other species the umbo of the valve to be sub-central.

Scuta (fig. 4, a, f) oblong, the basal margin only slightly exceeding half the entire length of the valve; valve strong, rather plainly marked with lines of growth; basal margin at nearly right angles to the occludent margin; tergal margin separated by a slightly-projecting

[page] 25 SCALPELLUM.

point from the lateral margin, which in the lower half is slightly protuberant; tergal margin straight, with the edge thickened and slightly reflexed. A distinct, square-edged ridge (therefore formed by two angles) runs from the umbo to the baso-lateral angle, which is itself obliquely truncated. Internally (f), there is a large and deep pit for the adductor scutorum. Terga (fig. 4 b) triangular, flat, large, fully one third longer than the scuta; basal half much produced; basal angle pointed; from it to the apex or umbo there runs a narrow, almost straight furrow, at which the lines of growth converge—it runs at about one third of the entire width of the tergum (in its broadest part) from the carinal margin. Parallel to the occludent margin, and at a little distance from it, there runs a wide, very shallow depression up to the apex. The scutal margin is not quite straight, about a third part, above a slight bend corresponding with the apex of the upper latera, being slightly hollowed: from the above bend a very faint ridge runs to the apex of the valve. Upper latera (fig. 4 d) large, flat, with five sides, of which the two upper are much the longest; the basal side is next in length, and the scutal side much the shortest. As far as I can judge of the positions of the lower valves, with respect to the upper latus, I believe, that the rostral latera, probably, abutted against the shortest of the three lower sides; that the carina ran along the one next in length, and the carinal latera along the middle basal side, which I suppose extended in an oblique line, and not parallel to the base of the capitulum: the two upper long sides no doubt touched the scuta and terga. The umbo of growth is at the apex; there is, however, a trace of a projecting ledge added round the upper margins during the thickening of this upper part of the valve. Two slight ridges run from the apex to the two corners of the middle of the three lower sides. Carinal latera (fig. 4 e) : these are not quite perfectly seen: the umbo forms a sharp point, whence the valve rapidly expands and curves apparently downwards and towards the upper latera. Near one margin there is a very narrow furrow, and on the other a wide depression, both running and widening from the umbo to the opposite end, which is slightly sinuous. I imagine these carinal latera occupied a nearly triangular space between the middle of the three lower sides of the upper latera and the basal portion of the carina. Rostral latera, rostrum and peduncle unknown; the rostral latera must have been very narrow.

Affinities.—In the shape and manner of growth of the scuta, and more especially of the upper latera, this species is certainly more closely allied to the eocene S. quadratum, than to any other species; but in the peculiar characters of the carina, it is nearer to the recent S. rutilum; we have previously seen that the nearest congener to S. quadratum is this same S. rutilum. The most conspicuous diagnostic character of this species is derived from the peculiar form of the carina,—its tectum being bounded by a rounded ridge on each side. This square-edged ridge running from the apex to the baso-lateral angle of the scuta is a trifling, but I believe, a diagnostic character. If I am right in placing S. rutilum in the genus Scalpellum, and I think there can be no doubt of this, considering the characters of its complemental male, then there can be no question that the present species belongs to the same genus.

d         

[page] 26 FOSSIL CIRRIPEDIA.

4. SCALPELLUM MAXIMUM, Tab. II. fig. 1-10.

POLLICIPES MAXIMUS. J. Sowerby. Min. Conch., tab. 606, solummodo, fig. 4 et fig. 6. N. B.—Fig. 3 est Tergum S. fossulæ, et fig. 5 alia species ignota.

 — MAXIMUS. Steenstrup. Kroyer Tidsskrift, b. ii, pl. v, figs. 17, 18.

 — MEDIUS. Steenstrup. Kroyer Tidsskrift, b. ii, pl. v, figs. 13, 13*, 33.

 — SULCATUS. J. Sowerby. Min. Conch., pl. 606, fig. 2, sed non fig. 1 et 7.

S. carinâ intra-parietibus instructâ; tecto subangulari vel subcarinato; margine basali rectangulariter acuto; totâ valvâ plus minusve introrsùm arcuatâ, sed margine interno ferè-recto; tecto1 transversè plus minusve convexo; superficie pænè lævi, striis paucis obsoletis longitudinalibus elevatis; tectum, parietes, et intra-parietes inter se separantur costis plus minusve prominentibus.

Carina having intra-parietes, with the tectum slightly angular or subcarinated, basal margin rectangularly pointed: whole valve more or less bowed inwards, but with the inner margin nearly straight; tectum, in a transverse line, more or less convex; surface nearly smooth, with a few faint longitudinal raised striæ; more or less prominent ridges separate the tectum, parietes, and intra-parietes from each other.

Upper Chalk, Norwich (common), Mus. Fitch. Northfleet (single spec.), Kent, Mus. J. Sowerby. Upper Chalk, Charing, Kent, Mus. Harris. Scania, and Quedlingburg in Westphalia, Mus. University, Copenhagen. Cyply bei Mons, Belgium, Mus. Brit. Gehrden Hanover, oberer Kreidemergel, Mus. Dunker and Roemer.

I have had far more difficulty in making up my mind regarding this the commonest cretaceous species, than with all the other fossil pedunculated cirripedes. From reasons previously stated, I have in this genus, when only separate valves have been found, taken the carina as typical. Comparing ordinary specimens of the carina of Scalpellum maximum and var. sulcatum, such as those figured in the 'Mineral Conchology,' I should certainly have considered them quite distinct, had not an examination of Mr. Fitch's fine collection from Norwich, together with several other specimens, shown me that there are intermediate forms which it is scarcely possible to class. Again, had I not seen a particular carina of S. maximum var. cylindraceum, in which the upper part displays a different character from the lower in the same individual valve, I should have unhesitatingly received it as a species, instead of, as I now do with certainty, as a mere variety. I feel, moreover, very great doubts whether the S. lineatum be a species, or merely another variety of S. maximum;

1 For an explanation of this and all other terms, see the remarks on nomenclature and woodcuts in the Introduction, page 9 and 10.

[page] 27 SCALPELLUM.

its distinctive characters are extremely slight; but they do not blend away by any intermediate forms hitherto seen by me. Looking only thus far, it would have been natural to have classed, without any doubt, all the carinæ as varieties of S. maximum, but in the same Norwich beds, from which Mr. Fitch obtained his fine series of carinæ, there are scuta and terga, which undoubtedly belonged to the genus Scalpellum, and which, from being of equally large size, nearly equally numerous, and having a similar state of surface with the above carinæ, I believe belonged to them: but both the terga and scuta present a more remarkable range of variation than do even the carinæ. In the case of the terga, at one extreme of the series, I did not even at first recognise the valve to be a tergum! yet the forms so blend together with very short intervals, that I cannot specifically separate them. Terga of the two extreme forms come, also, from the same localities in Scania. In the case of the scuta there are three distinct forms in Mr. Fitch's collection, which I should certainly have considered as specifically distinct, had I not been led from studying the carinæ and terga to believe that this species varies much: moreover, the chief point of variation in the scuta, namely, in the character of the under surface of the upper part, I conceive to be, in some degree, in connection with one chief peculiarity in the terga, namely the varying prominence of their occludent margins. Although I have not seen any other instance of so much variation in the scuta: yet I believe that I have taken the most prudent and correct course in describing them as mere varieties. From the more frequent coincidence of the carina, described as that of the true maximum, with the Varieties I of the scuta and terga, I believe that these valves belonged to the same individuals: with respect to the two other varieties, I have hardly any grounds for conjecturing which belonged to which. It is most unfortunate that not a single specimen of this species seems, hitherto, to have been found with all, or even a few, of its valves embedded together.

In giving names to the varieties, as judged of by the Carinæ, there is a difficulty in nomenclature; for the carina of S. maximum and of S. maximum, var. sulcatum, are apparently almost equally numerous in the Norwich beds; and might either be taken as typical of the species; I have chosen the former name, simply as having been more commonly used, and from this form having been apparently most widely distributed. I have described under it the original carina of Pollicipes maximus of J. Sowerby, and all the other valves, which I have reason to suppose belonged to this species. The other carinæ, however, as being in this genus the typical valve, are described under separate subordinate headings; the description of S. maximum, var. sulcatum, being given from Mr. Sowerby's original specimen. Under the typical S. maximum, I indicate as far as able, to which carinæ the varieties of the scuta and terga, there described, probably belonged.

[page] 28 FOSSIL CIRRIPEDIA.

SCALPELLUM MAXIMUM, var. typicum. Tab. II, figs. 1, 4, 5, 8.

S. carinâ introrsùm leviter arcuatâ, latitudine valvæ altitudinem superante; tecto transversè leniter arcuato; parietibus intra-parietibusque angustis, superficie pænè lævi.

Carina slightly bowed inwards; width of valve greater than the depth; tectum flatly arched transversely; parietes and intra-parietes narrow; surface nearly smooth.

Carina, Tab. II, fig. 1. In this, the typical variety, the carina is very slightly bowed inwards, widening gradually downwards from the apex, of which no part projected freely; walls rather thin; tectum very flatly arched, not sub-carinated; basal margin rectangularly or rather more acutely pointed; parietes very slightly concave, splaying outwards, narrower than one side of the tectum, separated from it and from the intra-parietes by rounded ridges; intra-parietes narrow, not extending baseward so far as the basal margin of the parietes; width of valve measured from marginal edge to edge, considerably greater than the depth, measured in the same place from the central crest to either marginal edge; but the width compared with the depth varies a little: inner margin of valve nearly straight. Length of longest specimen (Mus. Fitch) nearly 1½ inch. This variety in the Norwich beds seems about equally common with var. sulcatum, but the former alone is found in Hanover and in Scania, excepting that in the latter country some specimens indicate a passage to the var. cylindraceum.

Scutum, Tab. II, fig. 8. In Mr. Fitch's collection there are three left-hand valves of a Scalpellum, which, from their size and smoothness, I have no doubt belonged to this species, and from their thinness, probably to the variety of carina considered as typical under the simple name of S. maximum: valve unusually thin and little convex; trapezoidal, with the apex less produced than is usual in the genus; broad in proportion to its length, the basal margin being .66, and the occludent margin .98 in length, therefore the breadth equals two thirds of the length. Basal margin (just perceptibly hollowed out) forming less than a right angle with the (just perceptibly outwardly arched) occludent margin, and forming an almost exact rectangle with the lateral margin; the latter meets the tergal margin at an angle of about 135°. The edge of the tergal margin is thickened and slightly reflexed; the upper part of the lateral margin is in some specimens a little bowed inwards. The baso-lateral angle is rounded and just perceptibly protuberant; no ridge or furrow runs from it to the apex. Internally the depression for the adductor muscle is singularly shallow (fig. 8 c); a very small portion of the upper part of the valve projected freely; the internal surface of the valve, above the pit for the adductor muscle, has not been thickened, and is therefore slightly concave or almost flat. The internal occludent edge in the upper part is only a very little widened, and is flat; on the tergal margin,

[page] 29 SCALPELLUM.

a narrow ledge of about equal width with the occludent edge, marked likewise with lines of growth, must have overlapped the tergum. Largest specimen 1.15 in length.

Scutum, Var. II, Tab. II, fig. 9. This valve is narrow, moderately convex, with the upper portion much acuminated; the tergal margin is somewhat hollowed out, and is bordered by a narrow smooth slip, (as in the scutum of S. arcuatum,) which is simply formed by the thickening from within of the upper part of the valve; this slip does not reach to the uppermost point. The occludent margin is somewhat arched, at nearly right angles to the basal margin; lateral margin forming an angle a very little above a right angle with the basal margin. A conspicuous, curved, angular ridge runs from the apex to the baso-lateral angle, (which is not at all protuberant,) and divides the valve obliquely into two almost equal halves. Surface just perceptibly striated, finely and longitudinally. Internally there is a deep pit for the adductor scutorum, which is situate low down in the valve; the inner occludent edge in the upper part of the valve (b), above the adductor scutorum, widens suddenly, and is formed into a furrow, which, however, I do not believe to have had any functional importance; the central internal surface of the valve, above the pit for the adductor muscle, is somewhat prominent; and a quite small, almost flat, portion of the tergal side is marked by lines of growth, showing where it overlapped the tergum. Altogether there is a considerable resemblance between this valve, both externally, and more especially internally, and that of the Pollicipes Angelini. From the valve being acuminated, with the upper part rather solid, and from the surface being just perceptibly striated, it more probably belonged to var. sulcatum than to the typical S. maximum.

Scutum, Var. III, Tab. II, fig. 10. This third variety, of which the specimen is a fine large one, is about intermediate in outline or acumination between the first and second varieties: the tergal margin is thickened and reflexed as in the first, and is not bordered by a smooth narrow slip as in the second variety. There is no distinct angular ridge, as in the second variety, running from the apex to the baso-lateral angle. Internally the differences are more conspicuous; the depression for the adductor muscle is pretty well developed; a large portion of the upper part of the valve projected freely; the internal occludent edge, above the adductor-depression, becomes greatly widened and deeply hollowed out, but yet the furrow I believe, as in Var. II, to be of little or no functional importance, and merely a consequence of the internal thickening of the central upper part of the valve; on the tergal side a wide ledge shows the extent to which that margin overlapped the tergum. The internal surface of the valve, above the adductor-depression, is filled up solid and is exceedingly prominent, as is the ridge extending from it to the apex; this ridge, from the unusual width of the internal occludent edge, is pushed over to the tergal side of the valve.

Professor Steenstrup has sent me two small scuta, collected by M. Angelin at Kopinge and Balsberg, in Scania, which come near to the Third variety; the internal furrow, however, along the occludent margin, is much narrower, deeper, and oblique, so that it is partly

[page] 30 FOSSIL CIRRIPEDIA.

covered by a lateral projection of the central portion: a tolerably distinct ridge runs from the apex to the baso-lateral angle. Amongst the several specimens from Hanover sent me by Drs. Dunker and Roemer, the scuta all belong to the First variety.

I believe all these differences in the scuta of the three varieties ensue partly from the varying acumination of the upper part, and consequently of the extent to which the apex projected freely, but chiefly from the degree to which the upper part of the valve above the adductor muscle has been internally thickened. In the first variety the upper part is simply concave, and the pit for the adductor very shallow; in the third variety, the same upper part is highly prominent, and apparently as a consequence the internal occludent edge is deeply furrowed; the pit for the adductor muscle is deepest in the second variety.

The above differences would perhaps affect the outline of the terga, but I am not able to follow the precise manner; nor should I have thought them sufficient to have produced the amount of variation presently to be described in the terga; but possibly other scuta may vary still more. At first I concluded that the upper part of the inner occludent edge, which in Var. III is deeply furrowed, received in it the occludent edge of the tergum (as the furrow on the tergal side of the apex of the scutum receives the edge of the tergum in the recent Pollicipes mitella), but this on consideration I do not think can possibly be the case, although it would amply account for the variation in the terga.

Terga. I have seen great numbers of these valves; eight specimens are in Mr. Fitch's collection from Norwich; one is figured by Mr. J. Sowerby in the 'Min. Conch.,' (Pl. 606, fig. 6,) and they are numerous in the collection from Scania and Hanover. These valves, which, as stated in the preliminary remarks, present a most remarkable amount of variation, will be best described under three distinct heads.

Variety I. Tab. II, fig. 5. This valve, from its greater width and smoothness, compared with the other varieties, perhaps belongs to the typical S. maximum. Surface smooth, with a mere trace of some longitudinal striæ, sub-rhomboidal, elongated, with the apex much produced and curled towards the carina; nearly flat; the occludent margin arched, nearly equal in length to the scutal margin; upper carinal margin hollowed out, about half the length of the lower carinal margin; the occludent and upper carinal margins meet each other at a very small angle, making the apex almost horn-like; from it to the bluntly pointed basal angle, a slight rounded ridge, and on the carinal side of it a slight furrow, (both becoming less plain towards the lower part of the valve,) extends. As seen internally, the thickness of the valve, in its upper part, varies; a rather large upper part projects freely. A rim along the occludent margin is rounded and slightly protuberant, with a slight depression in the valve parallel to it. Length of the largest specimen 1.2 of an inch.

This variety is found commonly near Norwich, in Scania, and Hanover.

Tergum. Variety II. Tab. II, fig. 6. The valve in this variety (from near Norwich) is much elongated, sub-triangular, approaching to crescent-shaped; lines of growth conspicuous, with a few very faint longitudinal striæ. Carinal margin not (or

[page] 31 SCALPELLUM.

barely) distinguishable into an upper and lower portion; the whole being nearly straight, or very slightly concave. Apex extremely produced, narrow, and horn-like; curled towards the carina; apparently (for the apex is broken) a considerable portion was thickened, and must have projected freely. Occludent margin slightly arched, about equal in length to the scutal margin, which latter in the lowest part is curved and projects a little. Basal angle bluntly pointed. A rounded ridge (with a mere trace of a furrow on its carinal side), almost disappearing in the lower part of the valve, runs from the apex to the basal angle in a slightly curved course, strictly parallel to the carinal margin. The rim of the valve along the occludent margin is rounded and strongly protuberant, and, parallel to it, the surface is considerably depressed. Length of valve, when perfect, 1.2 of an inch. This variety differs from the first in the much greater straightness of the carinal margin, in the occludent rim being more protuberant, and in the scutal margin not being quite straight. One specimen presented a decidedly intermediate form, though rather nearer to the first than to the second variety.

Tergum. Var. III. Tab. II, fig. 7. The valves of this variety, of which I have seen five specimens, were for a long time quite unintelligible to me, and I at first even thought that perhaps they were rostral latera, but I now find that in outline, though not in general appearance, owing to their great thickness, they closely resemble the terga of S. magnum. One of the four specimens is almost exactly intermediate between the variety last named and that now to be described; hence there can be no doubt that they are really terga. The chief characteristic of the valves of this variety is their narrowness, and the solidity of their upper ends, which, together with a point of structure presently to be mentioned, makes me think it likely that they belonged to the individuals which possessed a carina, hereafter to be described under the name of S. maximum, var. cylindraceum. Valve smooth but with the lines of growth plain, extremely narrow, almost crescent-shaped; carinal margin considerably more concave than in Var. II, with a barely perceptible prominence in the upper part, marking the commencement of the freely projecting portion, and probably the point of upward extension of the carina. The occludent margin is arched, and is equal in length to the straight scutal margin. From the apex there runs a fine furrow (instead of a ridge and furrow, as in Vars. I and II,) to the basal angle, nearly parallel to the carinal margin, but almost blending with it in the lower part of the valve. The upper freely projecting portion is much thickened, and rendered almost horn-like, but to a variable extent; owing to this the width of the valve in the upper part also varies. In the specimens most characteristic of the present variety, the rim of the valve along the occludent margin is not at all, or barely, protuberant, nor is there any plain depression parallel to the occludent margin: in the intermediate specimen, however, above alluded to, the rim is protuberant and there is a plain depression, though both much less conspicuous than in the tergum of Var. II. On the internal surface of the upper freely projecting part, (marked with lines of growth,) there can be observed in two specimens a slight and variable longitudinal depression; judging from what occurs in the recent genus

[page] 32 FOSSIL CIRRIPEDIA.

Lithotrya, and from what may be faintly seen in the tertiary Pollicipes carinatus, and even in some specimens of P. mitella, I believe that this structure indicates that the upper freely projecting portion of the carina had its inside filled up and rendered prominent, which we shall see is the case with the carina of the variety cylindraceum. Length of largest specimen, eight tenths of an inch.

This variety is found at Norwich, in Scania, and at Cyply bei Mons, in Belgium.

Amongst the Scanian specimens from Kopinge (where the carina of the true S. maximum is commonly found) there are some terga differing from the variety just described, only in having the lower part of the valve less produced; and more especially in having on the internal surface of the upper part a smooth prominent ridge, lying rather nearer to the occludent than to the carinal margin, and therefore in exactly the same position in which a little group of small, sharp, longitudinal ridges occurs in the terga of S. arcuatum and of some other species. I am surprised at such a point being variable, but I cannot doubt that this valve belongs to the same species. I may add that it was this trifling point of structure, which first led me to suspect that these singular crescent-shaped valves were really terga. Finally, I may remark, that when all the ten terga now described are placed in a row, it is scarcely possible to doubt that they form merely varieties of the same species.

Carinal latus, Tab. II, fig. 4. This is the only valve which remains to be described, for neither the rostrum nor rostral latera are as yet known. It was found at Kopinge, in Scania, where the carina of the true S. maximum occurs abundantly; it was sent to me by Professor Steenstrup, who attributed it to this species. I have also seen a specimen from Hanover, where the carina of the true S. maximum is also found, and another small specimen from Charing, in Kent. Valve thin, of an irregular shape, sub-triangular; flat, except at the umbo, which projects outwards, owing to a ledge formed beneath and round it; carinal margin very slightly convex, with a linear furrow parallel to it, between which and the edge the lines of growth are abruptly upturned; lower margin considerably convex; upper margin slightly concave, with a slight depression parallel to it, between which and the edge the lines of growth are rectangularly reflexed towards the umbo. The two Scanian specimens differed slightly in outline; chiefly with respect to the projection of the ledge round the umbo. Width of largest specimen one quarter of an inch. This valve unmistakeably resembles the homologous valves in S. quadratum and fossula, but can be distinguished from both; the end opposite the umbo is much less produced than in S. quadratum; the whole valve is wider, and the furrows much less developed, than in S. fossula, to which it comes nearest.

Affinities. Before describing the several varieties as characterised by their carinæ, I will offer a few remarks on the affinities of this, the most common and widely distributed species of all the cretaceous pedunculated cirripedes. Mr. James Sowerby at first naturally described it as a Pollicipes; quite lately in Mr. Dixon's work he has considered it as belonging to the same genus with his eocene Xiphidium quadratum and our Scalpellum

[page] 33 SCALPELLUM.

quadratum. Still closer is the affinity with the cretaceous S. fossula; the carinæ of both have intra-parietes; the tectum is distinct from the parietes, which latter are either channelled or concave; the trapeziform scuta of S. quadratum, fossula, and maximum, are unmistakeably alike, and even more striking is the resemblance of the carinal latera; there can be no doubt of these three species belonging to the same genus, and having the same number of valves, namely, as I have shown under S. quadratum and fossula, probably twelve.

Geological History. This species, with its varieties cylindraceum and sulcatum, is very common in the Upper Chalk strata of Norwich; I have seen one specimen from the Upper Chalk of Northfleet, in Kent. It is common in the sandstone beds of Scania, which I am assured by Professor Forchhammer, are without doubt equivalent with the Faxoe beds, and therefore belonging to a stage above our flinty chalk. I have seen, also, one specimen, belonging, I believe, to this species, from the same stage in Westphalia; and another from Belgium; it is also common at Gehrden, in Hanover, in the 'Oberer Kreidemergel' of Roemer.

SCALPELLUM MAXIMUM, VAR. CYLINDRACEUM. Tab. II, fig. 2.

S. parte superiore carinæ liberè prominente, parte interiore intra-parietibus rotundatis, inflexis, itâ repletâ, ut pæne cylindrica fiat; superficie externâ lævi, tecto parietibusque pæne confluentibus.

Carina, with the upper portion projecting freely, and with the inside filled up by the rounded inflected intra-parietes, so as to be almost cylindrical; exterior surface smooth, with the tectum and parietes almost confluent.

Amongst the specimens from Norwich, two differed from the others in being a little more elongated and smoother, in the parietes becoming almost confluent, low down on the valve, with the tectum, and in the intra-parietes being very little developed. On the internal face this variety presents its most remarkable character; for a large upper portion of the valve must have projected freely, and the intra-parietes, instead of forming a thin wall on each side, are thickened, rounded, and turned inwards, so as almost to meet, and thus to fill up the original concavity of the valve. Hence a section (fig. 2, c) of the upper part, some way below the apex, is almost cylindrical, or more strictly oval with the longer axis in the longitudinal plane of the animal, with either a wedge-formed hollow, or a mere, almost closed, cleft on the under side, penetrating not quite to the centre of the solid valve. The two specimens differ, one in being in a transverse line exteriorly much depressed, the other highly arched or convex, and internally still more conspicuously in the degree to which the intra-parietes have filled up the upper part. In one of the specimens there is even a difference on the opposite sides of the same individual valve. Notwithstanding these varieties, I should have much hesitated to have ranked

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[page] 34 FOSSIL CIRRIPEDIA.

these peculiar carinæ under S. maximum, had not the upper part in one specimen actually retained all the usual characters of S. maximum, the precise line where the manner of growth had changed, being distinctly visible. It is represented in Plate II, fig. 2, a and b. Amongst the Scanian specimens, some make an approach to this variety.

SCALPELLUM MAXIMUM, VAR. SULCATUM. Tab. II, fig. 3.

POLLICIPES SULCATUS. J. Sowerby. Min. Conch., pl. 606, solummodo, fig. 2. Fig. 7 fortasse Carina P. Angelini. Fig. 1, Tergum fortasse P. striati.1

S. carinâ introrsùm valde arcuatâ, sub-carinatâ; valvæ latitudine circâ dimidium altitudinis æquante, tecto transversè præruptè arcuato; parietibus intra-parietibusque latiusculus. Apice solidè repleto, liberè paululùm prominente; superficie externâ striis paucis, rotundatis, ad alterum vel utrumque latus costarum duarum tectum et parietes separantium.

Carina considerably bowed inwards, subcarinated; width of valve about half of the depth; tectum in a transverse line, steeply arched; parietes and intra-parietes rather wide; apex filled up solid, and projecting freely a little; exterior surface with a few rounded striæ on either one or both sides of the two ridges which separate the tectum and parietes.

Having had the advantage of seeing Mr. J. Sowerby's original specimen, the valve now to be described is certainly that figured by him as Pollicipes sulcatus. As already stated, certain specimens of this variety differ strikingly from the carinæ typical of S. maximum; whereas others, from the same formation and locality, are so intermediate that they can, with difficulty, be arranged on either side: this is also the case with one from Cyply bei Mons, in Belgium. This variety is common in the Upper Chalk of Norwich.

In a well-marked specimen of this variety, the chief distinctive characters, as contrasted with the true S. maximum, consist in the tectum being more steeply arched, in the depth of the valve being much greater than the width, in the intra-parietes and parietes being more developed, in the whole valve being more bowed inwards, in the walls being thicker and apex filled up solid, in the surface having a few fine raised lines on each side of the ridge separating the tectum and parietes, and, lastly, in the tectum being sub-carinated.

1 If I am correct in considering the carina of P. sulcatus to be only a variety of that of S. maximum, the tergum figured by Mr. Sowerby as belonging to his P. sulcatus cannot so belong; for it does not at all resemble the homologous valve of S. maximum. I believe from the character of the ridge running from the apex to the basal angle, that it belonged to a Pollicipes, which must have been coarsely striated longitudinally, and therefore I have provisionally described it under Pollicipes striatus.

[page] 35 SCALPELLUM.

Carina moderately bowed inwards, widening gradually downwards from the apex, of which a small portion is filled up solid, and must have projected freely; walls moderately thick; the two sides of the tectum are rather steeply inclined to each other, and meet in a central line, which is subcarinated with a slightly prominent ridge; basal margin rectangularly pointed; parietes nearly flat, about as wide as the tecta, in some specimens perpendicular, so as not to be visible when the valve is viewed from a central dorsal point; in others, very steeply splayed outwards; separated from the intra-parietes by a conspicuous rounded ridge, and from the tectum by a nearly equally large ridge, which has generally one, two, or three fine, longitudinal, raised lines on either one or both sides of it: in one specimen the whole surface was thus coarsely and obscurely lined. The intra-parietes are rather wide, extending to the basal margin of the parietes. Depth of valve, measured from the central crest to either inner edge, is about equal to the entire width, as measured from inner edge to edge. The depth compared with the width, though the most conspicuous character, varies a little. Inner edge of valve nearly straight. Length of longest specimen (in Mus. Bowerbank) 1.6 of an inch. This is the largest carina I have seen in any fossil cirripede.

5. SCALPELLUM LINEATUM. Tab. II, figs. 11 and 12.

S. superficie totâ carinæ lineis tenuibus, rotundatis, longitudinalibus, proximis, microcoscopicis obtectâ; cristæ centralis costâ crassiore; costis duabus vel tribus tectum et parietes separantibus; latitudine valvæ circa dimidium altitudinis æquante; intra-parietibus latiusculis, nullâ costâ conspicuâ a parietibus separatis; apice solidè repleto, aliquantulum liberè prominente.

Carina with the whole exterior surface covered with fine, rounded, longitudinal lines, scarcely visible to the naked eye; with a thicker ridge on the central crest, and with two or three similar ones separating the tectum and parietes; width of valve about half of depth; subcarinated; inter-parietes rather wide, not separated by a conspicuous ridge from the parietes. Apex filled up, solid, and projecting freely a little.

Lower Chalk of Sussex, Mus. J. Morris; Mus. J. Sowerby.

I have seen two carinæ in the collections of Mr. Morris and Mr. J. Sowerby so exactly like each other, and having a somewhat different aspect from S. maximum, var. sulcatum, to which they come nearest, that they deserve to be described, whether or not they are really specifically distinct. I long hesitated whether to give them a specific name, and have been, in some degree, influenced in doing so, from the presence of scuta and terga in the Lower Chalk, which indicate a distinct but closely-allied species. The scutum is in Mr. Morris's collection, and came in the same lot with the carina from Sussex: the tergum

[page] 36 FOSSIL CIRRIPEDIA.

is in Mr. Bowerbank's collection from the Lower Chalk of Maidstone. These valves are marked with longitudinal raised striæ more plainly than is the carina.

Carina (fig. 12); moderately bowed inwards; inner margin nearly straight; widening very gradually downwards from the apex, of which a very small part is filled up solid, and must have projected freely; walls rather thin. Both tecta and parietes are regularly striated longitudinally, with raised, hair-like, fine lines scarcely visible to the naked eye; one central, and two or three on each side between the tectum and parietes, being about twice as large as the others, and visible to the naked eye. Tecta rather steeply inclined towards each other; central line sub-carinated; basal margin rectangularly pointed; parietes slightly concave, about as wide as half the tectum; steeply inclined outwards; separated from the intra-parietes on each side by a slight ridge. Intra-parietes set a little inwards, wider in the widest part than the adjoining parietes or tecta; extending baseward not as far as the basal margin of the parietes. Depth of valve measured from central crest to either inner edge, nearly equal to the entire width, as measured across from inner edge to edge. In many respects this carina is intermediate between those described under S. maximum and S. maximum, var. sulcatum; but comes nearest to the latter: the intra-parietes not extending so far baseward; and the delicately lineated exterior surface gives it, however, a somewhat different aspect.

Scutum (fig. 11); this valve, from the Lower Chalk of Sussex, resembles that of S. arcuatum; its surface is covered with raised striæ, which are further apart, and less plain than in the typical specimens of S. arcuatum from the Gault, but resemble those in the variety from the Grey Chalk of Dover. Outline trapezoidal: the baso-lateral angle is very broad, rounded, and protuberant; no ridge runs from it to the apex: the basal margin projects very slightly close to the rostral angle, and the tergal margin is not inflected as in S. arcuatum. The internal surface of the valve, along the tergal margin, is not furrowed or marked by lines of growth: I have no doubt that this valve is, at least, distinct from S. arcuatum.

Tergum. This valve, from the Lower Chalk of Maidstone, resembles that of S. arcuatum, var. from the Grey Chalk; it is, however, slightly more elongated: it further closely resembles a tergum, which I have provisionally attributed to Pollicipes striatus, differing from it in being less elongated, and more especially in the absence of a ridge, steep on the carinal side, which in that species runs from the apex to the basal angle.

Finally, I may remark, that these three valves, on the supposition that they have been rightly attributed to one species, indicate a form intermediate between Scalpellum maximum of the Upper Chalk, and S. arcuatum of the Grey Chalk and Gault.

[page] 37 SCALPELLUM.

6. SCALPELLUM HASTATUM. Tab. II, fig. 13.

S. carinâ intra-parietibus, intrà paululùm positis, instructâ; valvâ totâ introrsùm valdè arcuatâ, margine interno non recto; margine basali acuto, lanceolato; valvâ tenui, lævi, tecto transversè leniter arcuato; parietibus à tecto vix disjunctis.

Carina having intra-parietes set a little inwards; whole valve much bowed inwards, with the inner margin not straight; basal margin sharply pointed, spear-shaped; valve thin, smooth; tectum in a transverse line flatly arched; parietes barely separated from tectum.

Grey Chalk, Dover, Mus. Brit.

Carina smooth, narrow, furnished with intra-parietes, widening gradually from the apex downwards; extremely much arcuated, so that the uppermost part, of which none, or very little, projected freely, is at right angles to the basal part. Not only is the dorsal surface considerably arcuated, but so are the inner margins, which is much more important. Basal margin sharply pointed, with the two edges meeting each other at about an angle of 75°. Roof with the two sides continuously and flatly arched; parietes rather narrow, slightly concave, barely separated from the tecta: the concavity of the parietes, as seen on the basal margin, together with the sharpness of the central portion, makes the lower part of the valve spear-shaped. The intra-parietes are set a little within the parietes; they extend down to about two thirds of the entire length of the carina, and not to the basal margin of the parietes: they are widest at about only one fourth of the entire length of the carina from the apex, and here they equal in width the rest of the valve. Internally the valve is, in the upper part, owing to the wide intra-parietes, deeply concave; in the lower part, only slightly so.

Length of carina, measured along the chord of the arch, .75 of an inch.

Affinities. This species certainly comes very near to S. maximum; but I think it is distinct, and is its representative in the Grey Chalk. I have seen only a single specimen. The carina differs from the former varieties and species in its smoothness, thinness, in the acumination of the basal margin, in its much arcuated form, and more especially (for this, probably, would greatly influence the outline of the terga,) in the inner margins being also thus arcuated.

7. SCALPELLUM ANGUSTUM. Tab. I, fig. 2.

XIPHIDIUM ANGUSTUM. Dixon. Geology of Suffolk, tab. xxviii, fig. 9.

S. carinâ angustâ, introrsùm valdè arcuatâ; tecto à parietibus rectangulè inflexis costâ, (ut videtur) disjuncto; intra-parietibus usque ad dimidium valvæ pertinentibus, deinde obliquè et abruptè truncatis; margine basali acutè cuspidato.

[page] 38 FOSSIL CIRRIPEDIA.

Carina narrow, much bowed inwards; tectum apparently separated from the rectangularly-inflected parietes by a ridge; the intra-parietes extend down half the valve, and are there obliquely and abruptly truncated; basal margin sharply pointed.

Chalk.

I know this species only from the plate in Mr. Dixon's work. Being well aware of Mr. J. de C. Sowerby's great accuracy, I cannot doubt that the intra-parietes are at their lower end, abruptly and obliquely truncated in the manner represented in the Plate: this character, with its sharply-pointed basal margin, makes me believe this species to be new: it comes, I imagine, nearest to S. hastatum.1

9. SCALPELLUM TRILINEATUM. Tab. I, fig. 5.

S. carinæ tecto transversè leniter arcuato, subcarinato, costâ centrali et costis duabus lateralibus, rotundatis, tumidis; parietibus angustis leviter concavis, rectangulè inflexis.

Carina, with its tectum in a transverse line flatly arched, sub-carinated, with a central and two lateral, rounded protuberant ridges; parietes narrow, slightly concave, rectangularly inflected.

Grey Chalk, Dover, Mus. Brit., Flower. Chalk Detritus, Charing, Kent, Mus. Harris.

Carina (fig. 5, a-d); moderately arched, narrow, gradually widening from the apex to the base, plainly marked by lines of growth: no part apparently projected freely. The tectum is flatly arched, sub-carinated, with its central crest forming a rounded protuberant ridge; on each side, the tectum is bounded by similar, very slightly larger ridges, making

1 8. SCALPELLUM QUADRICARINATUM.

POLLICIPES QUADRICARINATUS, Reuss, Verstein. Bohmisch. Kreideformation (1846), Tab. xlii, fig. 18.

S. carinâ intra-parietibus latis (ut videtur) instructâ; tecto transversè plano, lævi, costâ prominente utrinque marginato; margine basali abruptè truncato.

Carina having apparently wide intra-parietes; tectum in a transverse line, flat and smooth, bordered on each side by a prominent ridge; basal margin abruptly truncated.

Bohemia. Untern Plänerkalke (Chalk-marl).

I know this species only from an imperfect plate, but good description of a carina, in Reuss' work: it is an interesting form, showing in its truncated basal margin and flat tectum a still closer affinity to the recent S. rutilum, even than does S. fossula; thus confirming the view I have taken of the affinities of these several species.

Carina; rather narrow, slightly bowed inwards: tectum quite flat and smooth, separated from the parietes by a smooth prominent ridge: parietes concave, rectangularly inflected: intra-parietes apparently well developed, separated from the parietes by a ridge: basal margin abruptly truncated.

[page] 39 SCALPELLUM.

together three ridges. The basal margin is bluntly pointed, with the two sides meeting each other at an angle of rather above 90°. Parietes rather narrow, rectangularly inflected, slightly concave: in the upper part there is no trace of intra-parietes.

Terga (fig. 5, e-i). In Mr. Flower's collection there is a tergum, (embedded in exactly the same matrix,) which, from a certain degree of resemblance in outline with that of S. arcuatum, the nearest congener to S. trilineatum, and from another point of resemblance with S. fossula, I believe belonged to this species.1 The valve is very smooth, with obscure traces of fine striæ radiating from the umbo; nearly flat; pointed oval, but with the scutal side much more protuberant than the carinal. Apex much acuminated, curled forwards; carinal margin much and regularly bowed from the upper to the basal point, which latter is blunt and square: from it to the apex there runs, in a curved line, nearly parallel to the carinal margin, a barely perceptible broad ridge. Occludent margin curved up towards the umbo, short compared to the scutal margin; parallel to it there runs a very wide and very shallow depression. Scutal margin, with a portion corresponding with the above depression, forming rather more than a third of the margin, not projecting so much as the lower two thirds, and separated from this lower part by a slight bend, probably marking the spot to which the apex of the upper latera extended.

Affinities. The carina obviously most resembles that of S. fossula and arcuatum; it differs plainly from both, in having a central rounded ridge: in the two well-developed boundary ridges of the tectum it comes nearest to the cretaceous S. fossula; but in the absence of the intra-parietes (and this I conceive is a more important character), it comes nearest to the S. arcuatum, from which, however, it can be at once distinguished by the absence of the longitudinal striæ. The tergum above described, which I believe belonged to this species, in the form of the scutal margin, comes nearest to that of S. fossula, though in general shape perhaps nearer to S. arcuatum. In S. fossula the carina has intraparietes, which are closely adjusted to the straight carinal margins of the terga: in S. trilineatum the intra-parietes are absent, but in their place the carinal margins of the two terga are themselves highly protuberant, so that in these two species, although the upper parts of the carinæ and terga are separately of very different shapes, they give, when combined together, a similar general outline.

10. SCALPELLUM SIMPLEX. Tab. I, fig. 9.

S. carinâ lævi; parietibus angustissimis, rectangulé inflexis; tecto subcarinato, transversè mediocriter arcuato; margine basali rectangulè acuminato.

1 It must however be added that the terga, at present unknown, of S. hastatum, a species occurring in the Grey Chalk of Dover, would probably have the same outline, and almost certainly would have a very smooth surface.

[page] 40 FOSSIL CIRRIPEDIA.

Carina smooth; parietes extremely narrow, rectangularly inflected; tectum sub-carinated, in a transverse line moderately arched; basal margin rectangularly pointed.

Lower Greensand, Maidstone. Mus. J. Morris.

I know this species only from a single carina, which is chiefly characterised by its simplicity: it is, I think, certainly distinct from all the others. In the sides of the carina being simple, that is in not being divided by a ridge into parietes and intra-parietes, it comes nearest to S. arcuatum and trilineatum, from the former of which it is readily distinguished by its smoothness; and from S. trilineatum by the absence of the three ridges. This species possesses some interest, as being the oldest cirripede, which I have ventured to attribute to the genus Scalpellum. Carina moderately tapering, slightly bowed towards the terga; sub-carinated, but with the central ridge smooth; transversely moderately arched; basal margin rectangularly pointed; the whole surface is smooth. Parietes extremely narrow, rectangularly inflected, set inwards, not extending down to the basal margin, with the lines of growth almost parallel to the inner edges of the valve.

11. SCALPELLUM ARCUATUM. Tab. I, fig. 7.

S. valvarum lineis angustis elevatis ab apice radiantibus: carinæ tecto transversè leniter arcuato, et parietibus rectangulè inflexis, leniter concavis, lævibus.

Valves with narrow elevated lines radiating from their apices. Carina with its tectum in a transverse line flatly arched, and with the parietes rectangularly inflected, slightly concave, smooth.

Gault, Folkstone, Mus. Bowerbank, J. Sowerby, Flower. Var. in Grey Chalk, Dover, Mus. Brit. Pläner (Chalk-marl) near Hildesheim. Mus. Roemer.

I have ranked this species under Scalpellum instead of Pollicipes, from the somewhat greater resemblance of its scuta and carina with the fossil species of Scalpellum, than with any known Pollicipes; though in some respects it appears rather intermediate. This species appears to come nearest to the Pollicipes radiatus of J. de C. Sowerby in 'Geol. Trans.,' vol. iv, 2d Series, Pl. XI, fig. 6, but besides that that species comes from the Lower greensand, the lower angle of its tergum is much more pointed; the upper figure of the two there given appears to be something wholly different. From the state of the specimens, I believe that the three following valves, all in Mr. Bowerbank's collection, belonged to the same species.

General Appearance. Carina, scuta, and terga plainly marked with prominent, very narrow, straight ridges, radiating from their apices; the interspaces between these ridges are

[page] 41 SCALPELLUM.

three or four times as wide as the ridges themselves; the lines of growth are very fine and narrow.

Carina (fig. 7, a, b, g); narrow, considerably arched: tectum flatly arched, obscurely subcarinated: parietes rectangularly inflected, somewhat concave, and not longitudinally ridged, like the tectum, about two thirds as wide as half the tectum: basal margin bluntly pointed, the two edges meeting each other at rather above a right-angle; a trace of a rounded ridge separates the tectum and parietes; in the upper part of the carina there is no trace of intra-parietes, therefore the section of the upper half of the carina is only four-sided, see fig. 7, g.

Scutum (fig. 7, f); moderately convex, with the apex acuminated: lateral margin nearly parallel to the slightly arched occludent margin, and at right angles to the straight basal margin; a distinct ridge runs from the apex to the baso-lateral angle, which is distinctly prominent and rather sharp. The valve, above a line running from the apex to the tergo-lateral angle, is inflected; and the narrow portion thus inflected, which cannot be seen when the valve is viewed from above, is destitute of the longitudinal ridges.

In a specimen from the Grey Chalk of Dover, in which the internal surface was visible, there was, above the well-marked depression for the adductor muscle, a prominent, central, slightly oblique ridge, with the inner occludent edge of the valve widened and slightly hollowed out on the one side, and with a trace of a furrow on the other or tergal side.

Terga (fig. 7, c, d); flat, oval, with the scutal angle rather protuberant; basal angle not sharply pointed, from it to the apex there runs an obscure furrow, which furrow in the lower part of the valve is central, but higher up is situated at about one third of the width of the widest part of the valve from the carinal margin; in the lower part of the valve, the lines of growth (and consequently the margins of the valve) make with this furrow, equal angles on its opposite sides. The valve is slightly depressed, parallel to the occludent margin. A small portion of the apex projected freely; internally, in the upper part, rather nearer to the occludent than to the carinal margin, the valve is prominent, and this part is marked with two or three little ridges (c) ending abruptly downwards.

Size of largest specimen,—length of carina, .85 of an inch; of scutum, from the apex to the basal margin, rather above .6; of terga, .55. I do not, however, know that these valves belonged to the same individual.

Variety. In the British Museum there is a scutum, and in Mr. Flower's collection there is a tergum, both from the Grey Chalk of Dover, which are most closely allied to, if not identical with, the above valve. The raised striæ on both are rather further apart and are less prominent. In all the other characters the scutum is identical. The tergum differs in its carinal margin, being rather more angularly bent, and in there being no furrow running from the apex to the basal angle; but these differences are trifling and insufficient for distinguishing a species. Amongst some specimens most kindly sent me by Roemer, there is a tergum from the Pläner of Sarstedt (Chalk-marl), which is identical with this.

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[page] 42 FOSSIL CIRRIPEDIA.

Affinities. This species is related to S. trilineatum, simplex, and solidulum, in the absence of intra-parietes; in the terga it comes closest to the latter species.1

1 12. SCALPELLUM SOLIDULUM. Tab. I, fig. 8.

POLLICIPES SOLIDULUS. Steenstrup in Kroyer's Tidsskrift, b. ii (1839), pl. v, fig. 14 et 14*.

  — UNDULATUS. Id. Id. Id. fig. 6.

S. valvarum lineis latiusculis elevatis ab apice radiantibus. Carinæ parte superiori liberè prominente, et cristâ centrali, internâ, longitudinali instructâ.

Valves with rather wide elevated lines radiating from their apices. Carina, with the upper part freely projecting, and internally urnished with a central prominent, longitudinal crest.

Scania (Kjuge). Mus. Univers. Copenhagen.

Professor Steenstrup has described under this name some carinæ, in so worn a condition, that I confess that I thought it quite impossible to characterise them; and under the name of P. undulatus, some well-preserved terga. Quite lately, M. Angelin has sent to Professor Steenstrup, from Kjuge in Scania, several of the same carinæ in a much better condition, a scutum, and some broken terga of P. undulatus, which, from the similarity of their longitudinally striated surfaces, M. Angelin believes belonged to the same species: I quite concur in the probability of this view. The better state of the carinæ proves the sagacity of Professor Steenstrup, in considering his worn specimens indicative of a distinct species. Had I seen these carinæ alone, I should have much hesitated in considering them as belonging to a Scalpellum: for they differ considerably from the same valve in all other species; the parietes, or rather the part answering to the parietes, being here so much inflected, that they fill up and render solid the upper part of the valve; but the scutum undoubtedly belonged to a Scalpellum, and the terga closely resemble the same valve in the S. arcuatum.

Carina (fig. 8, b, c, d); narrow, elongated, strong and solid; moderately bowed inwards; basal margin rectangularly pointed; surface covered with rather broad slight ribs, central one being apparently (for the best specimens are much worn) twice as broad as any of the others. In a transverse line, the tectum is considerably arched in the upper part of the valve, and only slightly arched in the lower part. A considerable length of the upper part must have projected freely; this portion being filled up solid, and having a central, largely prominent crest or ridge: it appears, for the specimens are in a much worn condition, as if the ridge had been formed by the inflection of the parieties on each side, and their perfect junction. In the peculiar and almost monstrous variety of S. maximum, called var. cylindraceum, we have nearly the same structure; a cleft, however, being left, marking the line of junction of the opposite parietes. In general appearance and proportions, this carina comes nearest to those of Scalpellum; but in the peculiar modification of the parietes (if they can be so called) into a central crest, and in the apparent (from worn state) absence of any distinct ridge separating the tectum and parietes, the valve departs from the general description of the carina in Scalpellum.

Scutum; of this valve, which undoubtedly belonged to a Scalpellum, there is one entire specimen, but with the angles so much rounded, that I can point out no distinguishing character from the same valve in S. arcuatum (fig. 7, g), of which a figure has been given, except that the longitudinal ridges are proportionally broader and further apart. The ridges closely resemble those on the above-described carina.

Terga (fig. 8, a); sub-triangular, flat, strong, and thick, with moderately wide, not quite straight ridges, radiating from the apex: the interspaces between the ridges are three or four times as wide as the ridges themselves; valve very slightly depressed, parallel to the occludent margin. A slight ridge, connecting the sharp basal apex, runs quite close to the carinal margin, even in the lower part of the valve : in

[page] 43 SCALPELLUM.

13. SCALPELLUM TUBERCULATUM. Tab. I, fig. 10.

S. valvarum lineis tenuibus, tuberculatis, elevatis, ab apice radiantibus : carinæ tecto transversè leniter arcuato, et parietibus striatis: scuti umbone prope in medio marginis occludentis posito, costis duobus ab umbone ad angulum basi-lateralem, et ad basalis marginis medium decurrentibus.

Valves, with fine, tuberculated, elevated lines, radiating from their apices: carina, with the roof in a transverse line, gently arched, and with the parietes striated: scutum, with the umbo placed nearly in the middle of the occludent margin, with two ridges running from the umbo to the baso-lateral angle and to the middle of the basal margin.

Chalk Detritus. Charing, Kent. Mus. Harris.

Through the kindness of Mr. Harris, I have examined several valves, which I believe to belong to the same species: the specimens were found in the chalk detritus, and, therefore, may have come from the Upper or Lower Chalk or Chalk-marl; but more probably from the Upper Chalk. With respect to the scuta and terga I have scarcely any doubt, from certain peculiarities, that they belonged to the same species; but with regard to the most important valve, the carina, I cannot feel quite so certain: when the latter is so held, that the parietes are not visible, it has a very close general resemblance to the same valve in Pollicipes rigidus. In the carina, the present species comes closer to S. arcuatum than to any other species; in the other valves, especially in the singular scuta, it departs widely from that and all other known fossil forms, with the exception of S. (?) cretæ, of Denmark. All the specimens which I have seen are small; the carina being .2 long, and the terga less than .15 of an inch in length, in the largest specimens.

consequence of this, the lines of growth make a different angle, on the opposite sides, with this ridge: as the valve has been somewhat worn, it is possible that the carinal margin may have been more abraded than is apparent. Internally, it is seen that a considerable portion of the upper part of the valve projected freely; beneath this, the inner surface is slightly convex, but smooth, and though the shell has been much worn, I doubt whether there ever existed ridges, as on the internal surface of the upper part of the terga in S. arcuatum, to which valve this presents a close general resemblance. Length of tergum (when perfect), 1.2 of an inch.

Carinal Latus (fig. 8, e, f); amongst the fossils from Kopinge (at which place the same species are found as at Kjuge), there is a valve, which I believe to be a carinal latus of a Scalpellum, and which, from its longitudinal ridges, more probably belonged to the present than to any other species: from its peculiarity it is in any case worthy of description. In form it is a segment, somewhat less than a quarter, of a circle; of this segment, nearly half (I believe the upper half) had its end or circumferential margin much hollowed out, and its surface smooth: the other half has its periodical growth-ridges very prominent, and these are crossed by a few slight longitudinal ridges. One of the lateral sides (the upper, I believe,) is reflexed so as to form a prominent ledge; the other side is slightly inflected.

[page] 44 FOSSIL CIRRIPEDIA.

The valves all have their surfaces plainly ribbed longitudinally; the ribs are narrow, and as they cross each zone of periodical growth they are tuberculated.

Carina (fig. 10, b, c); narrow, tapering, little bowed inwards; tectum in a transverse line, steeply arched, not carinated; basal margin bluntly pointed; in very young specimens, however, it is evident from the lines of growth, that the basal margin must have been rounded; the parietes are inflected, and rather narrow, being barely half the width of half the tectum; they are plainly marked by parallel lines of growth; internally the valve is rather deeply concave; no part of the apex projected freely.

Scuta (fig. 10, e); umbo of growth on the occludent margin, at about one third of the entire length of the valve from the apex; somewhat convex; four-sided, the margins consisting of the lateral, which is considerably longer than the other sides; the basal which forms nearly a right angle with the lower half of the occludent margin; and of an upper and lower occludent margin, meeting each other at about an angle of 135°: the margin which I have here called the upper occludent, homologically corresponds with the tergal margin of the other cretaceous species, and with the upper, nearly straight, portion of the occludent margin in the tertiary S. magnum and the recent S. vulgare,—a fact which has been mentioned under the head of Scalpellum. The edge of the upper occludent margin forms a strongly prominent ridge, with its apex forming a slight projection; a second less prominent ridge runs from the umbo to the baso-lateral angle, and a third faint ridge runs from the umbo to a point in the basal margin, nearer to the rostral than to the baso-lateral angle. Internally there is a rather deep hollow for the adductor muscle; along the under surface of the upper occludent margin there is a slightly prominent ridge, bordered by two slight depressions.

Terga (fig. 10, a); flat, elongated diamond-shape; close and parallel to the occludent margin there is a narrow, very prominent ridge or plait, the end of which forms a slight projection; a straight ridge runs from the apex to the sharp basal angle; the scutal and lower carinal margins are of equal length, and longer than the occludent and upper carinal margins, which latter are equal, and meet at an angle very slightly less than a rectangle. On the under surface there is a slight depression and ridge, close and parallel to the occludent margin. I have no doubt that the ridge along the upper occludent margin of the scuta, and that on the occludent margin of the terga, together with their projecting points, are related to each other, owing to the close contact of these valves.1

1 14. SCALPELLUM SEMIPORCATUM. Tab. I, fig. 6.

S. carinâ ignotâ: scuti costis duobus ab umbone ad angulum basi-lateralem et ad marginis basalis medium decurrentibus: superficie inter hanc costam et marginem occludentem lineis tenuibus, longitudinalibus, elevatis instructâ.

Carina unknown: scutum, with two ridges running from the umbo to the baso-lateral angle, and to

[page] 45 SCALPELLUM.

15. SCALPELLUM (?) CRETÆ. Tab. I, fig. 11.

ANATIFERA CRETÆ. Steenstrup. Kroyer's Tidsskrift, 1837 et 1839, b. ii, pl. v, figs. 1, 2, 3.

S. valvis lævibus tenuissimis: scuti umbone propè medium marginis occludentis posito; costis tribus obscuris ab umbone ad angulos tergo-lateralem et basi-lateralem, et ad medium marginis basalis decurrentibus: carinæ apice et margine basali acutis; distincti parietes absunt.

Valves smooth, extremely thin: scutum with the umbo placed nearly in the middle of the occludent margin, with three obscure ridges running from the umbo to the tergo-lateral and baso-lateral angles, and to the middle of the basal margin: carina with the apex and basal margin sharply pointed; without distinct parietes.

White Chalk, Denmark, Mus. Univers., Copenhagen. Chalk Detritus, Charing, Kent (?), Mus. Harris.

Preliminary Remarks. I owe to the kindness of Professor Steenstrup, as in so many former instances, an examination of several specimens of this fossil, which is of interest, as being extremely common and characteristic of the white chalk of Denmark. Amongst the numerous minute specimens from the chalk detritus of Charing in Kent, sent me by Mr. Harris, there are some carinæ so similar that I have ventured, with doubt, to rank this as a British species; the carina, however, in this species, are far from characteristic. I have felt much hesitation in admitting this species in the genus Scalpellum: Professor Steenstrup was originally inclined to believe that the capitulum was formed of only five valves; could this be proved, the species would very naturally rank with a small recent one from the Island of Madeira, which, owing to the upward growth of the scuta, and to certain peculiarities in the animal's body, I have felt myself compelled to raise to the rank of a genus, under the name of Oxynaspis. But as the valves of S. (?) cretæ have never been found united, and as the main ones are very small, fragile, and generally in a broken condition, the small lower ones might easily be overlooked. I have seen, indeed, in two instances,

the middle of the basal margin; the surface between the latter ridge and the occludent margin covered with fine longitudinal elevated lines.

Scania (Kopinge). Mus. Univers., Copenhagen.

I have in this one instance departed from my rule of never naming any other valve, except the carina in the genus Scalpellum; but the scutum here to be described almost certainly belongs to this genus, and is interesting in connection with the homologous valves in S. tuberculatum and S. (?) cretæ, to which species it is apparently allied, but yet differs greatly from them in the umbo being seated at the uppermost point of the valve.

Scutum, moderately elongated, slightly convex; a narrow, prominent, well-defined ridge runs from the apex to the baso-lateral angle, at which point it forms a narrow projection: a second ridge, not quite so prominent, runs from the apex to the basal margin, to a point rather nearer to the baso-lateral than to the rostral angle. That part of the valve between this second ridge and the occludent margin has four or five faint longitudinal ridges, whereas the rest of the valve is smooth. Internally there is a deep depression for the adductor muscle, above which the surface is simply concave up to the apex.

[page] 46 FOSSIL CIRRIPEDIA.

what appeared to be upper latera, but as I could not remove them so as to examine their under sides, I am far from sure that they were not broken, angular portions of scuta. If we look to the character of the separate valves, there is a striking and important resemblance between the scuta of S. cretæ and tuberculatum, in the umbo being seated in a nearly middle point of the occludent margin, and likewise in the two ridges running from the umbo to the baso-lateral angle, and to a central point of the basal margin; in which latter character of the ridges, this species also agrees with S. semiporcatum. These facts have determined me, provisionally, to rank the present species under Scalpellum. But on the other hand, if we look to the carina, which, according to our rule, is considered the characteristic valve in this genus, it rather resembles the homologous valve in Pollicipes; for the carina has not any parietes separated from the tectum by a distinct ridge. The terga seldom afford any serviceable generic characters; but as far as they go, they also rather resemble the terga in Pollicipes than in Scalpellum. Hence, it is obvious, that the generic position of S. (?) cretæ is at present very uncertain.

Valves small, smooth, extremely thin and brittle.

Scutum (fig. 11, c); trapezoidal, with the upper part of the valve produced into a sharp point, and with the rostral angle slightly and obliquely cut off. Umbo seated at a little above the middle of the occludent margin, which is straight. The tergal margin is longer than the lateral margin: the basal margin (on the carinal side of the truncated rostral end) forms a right angle both with the lateral and occludent margins. Valve somewhat convex near to the umbo, whence three obscure ridges radiate,—one to the angle between the tergal and lateral margins; a second to the baso-lateral angle, and a third to the bend in the basal margin; these ridges, however, seem to vary in strength, and in the largest specimens could hardly be distinguished: in most of the specimens, the narrow portion of the valve, which ends in the truncated rostral angle, is a little inflected. The lines of growth follow the basal and tergo-lateral margins, and can be traced just bending round the sharp apex, so that a very narrow ledge is added along the upper part of the occludent margin.

Tergum (fig. 21, a); sub-rhomboidal, nearly flat: the carinal margin consists of an upper larger portion, and of a lower, shorter portion: the occludent and scutal margins are nearly equal in length. The apex is a little curled towards the scuta, and is sharp; basal angle bluntly pointed. A faint curved ridge runs from the apex to the basal angle, at about one fourth of the entire width of the valve from the carinal margin.

The Carina (fig. 11, b) widens rapidly downwards from the extremely sharp apex; basal margin spear-shaped, sharply pointed, the two edges meeting each other at about an angle of 75°; exterior surface sub-carinated; in a transverse line the valve is slightly arched, and longitudinally, very slightly bowed inwards: with a lens, traces of longitudinal striæ are visible.

Dimensions. The species seems to have been always small: the largest scutum and tergum were each about a quarter of an inch in length. Probably the individuals were attached in groups to corallines at the bottom of the cretaceous sea.

[page] 47 POLLICIPES.

Genus—POLLICIPES.

POLLICIPES. Leach. Journal de Physique, tom. lxxxv, Julius, 1817.1

LEPAS. Linn. Systema Naturæ, 1767.

ANATIFA. Brugière. Encyclop. Méthod. (des Vers), 1792.

MITELLA. Oken. Lehrbuch der Naturgesch., 1815.

RAMPHIDIONA. Schumacher. Essai d'un Nouveau Syst. &c., 1817 (ante Julium).

POLYLEPAS. De Blainville. Dict. des Sc. Nat., 1824.

CAPITULUM (secundum Klein). J. E. Gray. Annals of Philos., tom. x, 2d series, Aug. 1825.

Valvæ ab octodium usque ad centum et amplius. Lateribus verticelli inferioris multis; lineis incrementi deorsùm ordinatis. Subrostrum semper adest. Pedunculus squamiferus.

CHARACTERES VALVARUM IN SPECIEBUS FOSSILIBUS.

Carina ab apice ad marginem basalem multum dilatata; apex plerumque liberè prominens; parietes à tecto non distincté separati; lineæ incrementi parietum parum obliquæ. Scuta plerumque subsolida, convexa, subtrigonalia, margine tergo-laterali plus minusve eminente, sed non angulo in margines duos discreto.

†. Scuta, aut lævia aut lineis tenuibus incrementi solùm notata.

A. Scuta, costâ ab apice ad centrum marginis basalis non decurrente.

B. Scuta, costâ, nonnunquam subobseletâ, ab apice ad centrum marginis basalis decurrente.

††. Scuta, aut longitudinaliter aut transversè (i. e. secundum lineas incrementi) costata.

Valves from eighteen to above one hundred in number. Latera of the lower whorl numerous, with their lines of growth directed downwards. Sub-rostrum always present. Peduncle squamiferous.

CHARACTERS OF THE VALVES IN FOSSIL SPECIES.

Carina; widening considerably from the apex, which projects freely, to the basal margin; parietes not distinctly separated from the tectum; lines of growth on the parietes but little oblique. Scuta generally somewhat massive, convex, sub-trigonal, with

1 This is one of the rare cases in which, after much deliberation and with the advice of several distinguished naturalists, I have departed from the rules of the British Association; for it will be seen that Mitella of Oken, and Ramphidiona of Schumacher, are both prior to Pollicipes of Leach; yet as the latter name is universally adopted throughout Europe and North America, and has been extensively used in geological works, it has appeared to me to be as useless as hopeless to attempt any change. It may be observed that the genus Pollicipes was originally proposed by Sir John Hill (' History of Animals,' vol. iii, p. 170), in 1752, but as this was before the discovery of the binomial system, by the Rules it is absolutely excluded as of any authority. In my opinion, under all these circumstances, it would be mere pedantry to go back to Oken's 'Lehrbuch der Naturgesch.' for the name Mitella,—a work little known, and displaying entire ignorance regarding the Cirripedia.

[page] 48 FOSSIL CIRRIPEDIA.

the tergo-lateral margin more or less protuberant, but not divided by an angle into two distinct margins.

† Scuta smooth, or marked only with fine lines of growth.

A. Scuta without any ridge proceeding from the apex to a nearly middle point of the basal margin.

B. Scuta with a ridge, sometimes faint, proceeding from the apex to a nearly middle point of the basal margin.

††. Scuta either longitudinally or transversely (that is in the direction of the lines of growth) ridged.

As with Scalpellum, the first of the above two paragraphs contains the true generic description, as applicable to recent and fossil species; the second paragraph has been drawn up as an aid in classifying separated valves. This, the most ancient genus of the Lepadidæ, seems also to be the stem of the genealogical tree; for Pollicipes leads, with hardly a break, by some of its species into Scalpellum villosum; and Scalpellum leads by Oxynaspis into Lepas and the allied genera: Pollicipes mitella, moreover, is nearer allied to the Sessile Cirripedes than is any other Pedunculated cirripede, except, perhaps, Lithotrya, which is also closely connected with Pollicipes. The six recent species of Pollicipes might be divided into three sub-genera: one containing the P. mitella; a second, P. cornucopia, elegans and polymerus; and the third, P. spinosus and serta (nov. spec.) Of the fossil species some, as P. carinatus, dorsatus, validus, &c., are related to the first section; others, as P. reflexus and concinnus, to the second section; and lastly, others, as P. glaber and unguis, perhaps form a distinct section, though more related to P. mitella than to other recent species. As, however, most species are known by only a few of their valves, it is scarcely possible to speak with certainty regarding their finer affinities.

Description: as in the case of Scalpellum, the following remarks are confined to the fossil species of the genus. In all full-grown recent species the number of valves in the capitulum is very large: this seems to have been the case with the Oolitic P. concinnus, and probably with most other species, but whether with all may be doubted; from the size of the carinal latera of the lower whorl in P. unguis, I suspect that the total number of its valves cannot have been great. The valves are either smooth or plainly marked by the lines of growth, or they rarely have longitudinal ridges, or transverse ridges corresponding to each periodical zone of growth: no recent Pollicipes has a surface of this latter kind. The valves in Pollicipes are often strong and massive, with their apices projecting freely from the capitulum.

Scuta generally three-sided, but sometimes, from either the baso-lateral or rostral angles being truncated, there is an additional lower side. The tergo-lateral margin is either straight or generally more or less convex, but it is never (as far as I know) divided into two distinct margins, as is always the case with Scalpellum owing to the abrupt ending of the upturned lines of growth. The basal margin is either straight or formed

[page] 49 POLLICIPES.

of two lines meeting each other at a wide angle, or somewhat irregular. The angle which this basal margin makes with the occludent margin varies much. The occludent margin is slightly arched, and is sometimes exteriorly strengthened by a ledge or rim. A prominent ridge runs in several species from the apex of the valve to the baso-lateral angle; and in another set of species there is a second obscurer ridge running to a nearly middle point of the basal margin: in this latter set, the two ridges no doubt mark the extent to which the rostrum and upper latera overlapped the scutum. Internally there is almost always a deep pit for the adductor scutorum muscle: the upper part of the valve generally projects freely, and is internally marked by lines of growth; sometimes there is a furrow along the upper part either of the occludent or the tergal margin; in the latter case the furrow seems to receive the scuto-occludent angle of the adjoining tergum, and thus locks the two valves together, as in the recent P. mitella. In two species the occludent margin at the rostral angle is internally produced downwards into a depending tooth or projection.

Terga: nearly flat, rhomboidal or sub-rhomboidal; a line formed by the converging zones of growth, or a ridge, sometimes steep only on the carinal side, sometimes steep on both sides, runs from the apex to the basal angle. The basal angle is sometimes truncated.

Carina: is either bowed inwards or is straight: it widens from the apex downwards more rapidly than in Scalpellum; generally a considerable upper portion projects freely; this upper portion is always much less concave than the lower part: it is sometimes filled up flat, and sometimes has even a central prominent crest; the basal margin is either bluntly pointed, rounded, or truncated; the parietes are generally more or less inflected, but they are not separated by any defined ridge or angle from the roof or tectum; the lines of growth on the parietes are transverse, or generally only slightly oblique. These characters will, I believe, in nearly all cases serve to distinguish the carina of a Pollicipes from that of a Scalpellum.

Sub-carina: I know of the existence of this valve only in P. concinnus, but I cannot doubt that it existed in all, or nearly all, the species. I have sometimes suspected that it might possibly have been absent in P. unguis and glaber, in which the carinal latera are so large.

Rostrum and sub-rostrum: as these valves occur in P. unguis, I have little doubt that they are universal; they are apparently present in P. concinnus; the rostrum always resembles the carina, but is shorter and proportionally broader; a larger proportion, also, seems always to have projected freely, caused no doubt by the more abrupt flexure of this end of the capitulum: this latter character is the most certain one by which the rostrum may be distinguished from the carina. The sub-rostrum in P. unguis resembles the rostrum, but is smaller, and exteriorly is not carinated.

Upper latera: I know these only in P. unguis and glaber, in which they consist of a flat triangular plate, and in P. concinnus, in which they seem to be diamond-shaped. Lower latera, these in P. concinnus also seem to be diamond-shaped, as in P. cornucopia; in P. unguis and glaber the apices of these little valves do not project freely, and they

g           

[page] 50 FOSSIL CIRRIPEDIA.

have a different appearance from their homologues in any recent species: they are trigonal, with their basal margin rounded and one end produced, to which end a narrow well defined ridge runs obliquely from the apex of the valve.

The peduncle is known only in P. concinnus; in this species it is covered with minute quadrangular calcified scales.

†. Scuta, aut lævia aut lineis tenuibus incrementi solùm notata.

A. Scuta, costâ ab apice ad centrum marginis basalis non decurrente.

1. POLLICIPES CONCINNUS. Plate III, fig. 1.

POLLICIPES CONCINNUS. J. Morris. Annals of Nat. Hist., vol. xv, 1845, p. 30, pl. vi, fig. 1, et Mineral Conch., pl. 647, fig. 1.

P. scutis pæne quadratis, margine basali propè rostrum subconcavo, segmento tergo-laterali, è lineis incrimenti ut videtur reflexis formato, lato, rotundato et prominente: tergis latis, pæne quadratis: carinæ margine basali, ut videtur acuto.

Scuta, almost square, with the basal margin near the rostrum a little hollowed out; tergo-lateral slip, apparently formed by upturned lines of growth, broad, rounded, and protuberant. Terga broad, almost square. Carina, with the basal margin apparently pointed.

Oxford Clay, Middle Oolite, attached to an Ammonite. Mus. Pearce.

Although to my great regret the state of Mr. Pearce's health has prevented him allowing me to examine the specimens in his possession, yet I have thought it advisable to commence the genus with this species, as it is in a far better state of preservation than any other specimen hitherto discovered. We gain by a single glance the knowledge that at so remote a period as the Middle oolite a true Pollicipes existed. In no other instance that I have heard of, has the peduncle been perfectly preserved. Mr. Morris first named and briefly described this interesting species; subsequently Mr. James Sowerby has given enlarged drawings (without any description) of it in the 'Mineral Conchology;' and it is from these figures that I have drawn up my specific description, which, from this cause, is necessarily imperfect. The figures in this volume are copied from those in the 'Mineral Conchology,' which I may remark have evidently been executed with great care, and Mr. Sowerby's accuracy of observation is universally well known. The peduncle is several times longer than the capitulum: Mr. Morris describes the scales on the peduncle as being small, closely pressed together, somewhat quadrate in form, and each regularly marked by a transverse carinated ridge; this latter character I do not understand. The rostrum is not clearly figured by Mr. Sowerby, but I believe that I can see evidence of its existence. From these materials it would appear that the P. concinnus is more nearly related to the recent P. cornucopia, and its two nearest congeners, than to any other species of the genus.

[page] 51 POLLICIPES.

2. POLLICIPES OOLITICUS. Tab. III, fig. 2.

POLLICIPES OOLITICUS. Buckman. Outline of the Geology of Cheltenham, by Sir R. Murchison, new edit. by James Buckman and H. Strickland, 1845, Tab. iii, fig. 7.

P. scutis triangulis; superficie undulatâ; margine basali rectangulè ad marginem rectum tergo-lateralem posito; segmentum tergo-laterale à lineis reflexis incrementi formatum deest. Carinâ pæne rectâ, semicylindricâ, margine basali quadrato.

Scuta triangular; surface undulatory; basal margin at right angles to the straight tergo-lateral margin; there is no tergo-lateral segment formed by upturned lines of growth. Carina nearly straight, semicylindrical, with the basal margin square.

Stonesfield Slate, Lower Oolite: Eyeford. Mus. Buckman, and Geolog. Soc.

My materials consist of several scuta, terga, and carinæ, kindly lent me by Professor Buckman, and of another set (which includes the rostrum) presented by him to the Geological Society of London.

Valves: these have a smooth surface, but are undulatory in the direction of the lines of growth; at the cessation, apparently, of each zone of growth, there was a tendency to form a projecting ridge or plait, as takes place in a far more marked manner in some of the cretaceous species, namely, P. elegans and fallax. There are also excessively fine, longitudinal striæ, which can be seen only when the valves are held in particular lights; these seem to have been formed by the so-called epidermis, which we know in the recent P. mitella is longitudinally and finely ribbed. Scuta (fig. 2, c) but slightly convex; triangular; basal margin straight, forming a right angle with the tergo-lateral margin, and rather less than a right angle with the slightly arched occludent margin; the tergo-lateral margin is straight, and not at all protuberant: in the figure the left hand is, as usual, the occludent margin; I mention this because the valve has a reversed appearance, owing to the unusually small angle which the occludent makes with the basal margin. Terga (fig. 2, d) rhomboidal, slightly convex, with a rounded ridge, which is central, running from the apex to the broad, rounded basal angle; the upper carinal and occludent margins stand at right angles to each other, and are short compared to the scutal and lower carinal margins; there is no trace of a depression parallel to the occludent margin. Carina (fig. 2, a, b) elongated, triangular; scarcely at all bowed inwards; not even sub-carinated; basal margin rounded, not at all protuberant. The Rostrum differs from the carina only in its greater breadth compared to its length.

Dimensions. The largest scutum is .6 long, but as there is a broken tergum about 1.1 long, no doubt the species attained a rather large size; the longest carina is .7 in length.

Diagnostic characters. This species is best characterised by the straightness of the whole tergo-lateral and of the basal margin of the scuta; by the ridge being central on the terga; by the carina not being carinated; and by the sinuous state of the surface of the valves, intermediate between the smooth species and those with distinct ridges parallel to the zones

[page] 52 FOSSIL CIRRIPEDIA.

of growth. The remarkable straightness of the tergo-lateral margin of the scuta is like that in the recent P. spinosus and serta, and in Scalpellum villosum, in all which species, I may observe, the scuta and terga are separated by an interspace of membrane; in these three recent species, however, the basal margin is considerably protuberant. The present species differs apparently from the P. concinnus of the Oxford clay, in the basal and tergo-lateral margins of its scuta being straight; in the greater proportional length of the scutal and1

1 3. POLLICIPES NILSSONII. Tab. III, fig. 11.

POLLICIPES NILSSONII. Steenstrup. Kroyer, Naturhist. Tidsskrift, 1839, pl. v, figs. 20-23.

P. scutis triangulis, planis: margine basali cum margine occludente angulum pæne rectum, cum margine recto tergo-laterali, angulum aliquanto minorem formante. Deest segmentum tergo-laterale, lineis incrementi reflexis formatum. Carinâ introrsùs admodùm arcuatâ, crassâ; marginis basalis mucrone obtuso.

Scuta triangular, flat; basal margin forming nearly a rectangle with the occludent margin, and a somewhat lesser angle with the straight tergo-lateral margin. There is no tergo-lateral slip formed by upturned lines of growth. Carina much bowed inwards, massive, with the basal margin bluntly pointed.

Scania (Balsberg, Kopinge, Ffo., &c.) Mus. Univers. Copenhagen.

Professor Steenstrup has described, under the name of Pollicipes Nilssonii, a large carina, and apparently a sub-carina and rostrum, and he remarks that these perhaps belong to the same species with the terga, named by him P. undulatus. M. Angelin, however, believes that the latter belong to the species already described as Scalpellum solidulum. With the specimens of the present species, M. Angelin has lately found three small scuta, which he believes belonged to it. These scuta are so extremely worn, that I should not have ventured to have named them, had it not been advisable to give figures of the remarkable carina already named as P. Nilssonii. Should it hereafter be proved that the following scuta belong to some other carina, then a new name will have to be attached to them.

Scuta (fig. 11, a) flat, thick, triangular, not much acuminated; basal margin forming almost a rectangle with the occludent margin; tergo-lateral margin (in present condition) straight, forming a rather less angle with the basal than does the occludent margin. There is no trace of a slip or portion of valve along the tergo-lateral side, formed by upturned lines of growth. Internally, the pit for the adductor muscle is deep; the central portion of the apex above the pit is prominent; apparently there was no internal furrow. Length of longest specimen only .4 of an inch.

Carina (fig. 11, b, c) strong, with the upper part unusually massive; though in a worn condition, there are distinct traces of its having been longitudinally and slightly ribbed. Strongly carinated, the two arched sides meeting each other at about a rectangle; much bowed inwards, and widening much from the apex to the base; upper portion, about one fifth of the entire length of the carina, seems (for the worn condition prevents certainty) to have projected freely; beneath the upper freely projecting portion, the inner margins are nearly straight; the depth of the shell, measured from the central crest to the inner margin, is, in the lower half, remarkably great, and consequently the valve in the same part is internally concave to a remarkable depth; the upper freely projecting portion is only slightly concave, and is singularly massive, from having been filled up with solid shelly layers. The basal margin is bluntly pointed, the edges meeting each other at about a right angle; in the lower part of the valve the lines of growth are of course parallel to the basal edges, but higher up they meet at a more open angle, and consequently the carina of a young individual must have had its basal margin less projecting. When the sides of the carina are examined carefully, a portion, about one fourth of its entire depth, can be observed to lie a very little more inwardly inflected than the more central part, so as not to form quite a continuous surface with

[page] 53 POLLICIPES.

lower carinal margins compared with the upper carinal and occludent margins of the terga, and lastly in the basal margin of the carina being truncated; it differs from P. planulatus of the Oxford Clay, and therefore its other nearest relative in age, by the basal angle of the terga being rounded, instead of square as in that species.

the two broad arched roof-sides; and in these slips the lines of growth run almost parallel to the inner margin of the valve: in this respect the valve approaches in character to that of Scalpellum. The heels or baso-lateral angles apparently projected slightly, as I infer from a slight downward curvature in the lines of growth, along a line corresponding with the heel, and separating the roof-part from the inflected walls of the carina.

Sub-carina (fig. 11, d): in Professor Steenstrup's collection there are several worn valves which appear to have been sub-carinæ; in shape approximately semi-conical; the basal margin being almost semi-oval, with the two corners a little inflected; hence the valve is deeply concave to an unprecedented degree, and this is quite conformable with the singular sectional outline of the carina (c). About one fourth part of the length of the valve must have projected freely; the outer surface is longitudinally ribbed, and the lines of growth remarkably undulatory.

Rostrum (fig. 11, e): this valve which I believe to be the rostrum resembles the sub-carina, but is more open, less high, and with a larger proportion, namely half, of its entire height freely projecting; the semi-oval basal margin is slightly sinuous, the projecting points corresponding with the external longitudinal ribs.

Length of carina, 1.5; of the largest of the sub-carinæ, .6; of the largest rostrum, .45 of an inch.

4. POLLICIPES HAUSMANNI. Tab. III, fig. 3.

POLLICIPES HAUSMANNI. C. L. Koch and Dunker. Norddeutsch. Oolithgebilder, p. 52, Tab. vi, fig. 6.

— — F. A. Roemer. Versteinerung. Norddeutsch. Oolithengebirges, p. 211, Tab. iv, fig. 2.

P. scutis subtriangulis, angulo baso-laterali valde rotundato; apice producto; margine basali cum margine occludente angulum pæne rectum formante; internâ apicis superficie prominente, margineque tergali sulcato.

Scuta, subtriangular, with the baso-lateral corner much rounded, and with the apex produced; basal margin forming nearly a right angle with the occludent margin; apex with its internal surface prominent, and with the tergal edge furrowed.

Hilsthon, des Elligser Brinkes. (Lower Greensand, Germany.)

Messrs. Koch and Dunker have given a full and detailed account of this species, together with truly excellent figures, and I have nothing to add to their remarks, but will re-describe, for the sake of uniformity, the valves of this species, which, through the kindness of Professor Steenstrup and Professor Dunker, I have examined. The valves are slightly worn. The figures given in tab. III are not, I think, so good as most of the others.

Scuta (Tab. III, fig. 3, b, c) moderately convex, sub-triangular; apex much acuminated, slightly curved towards the terga; surface smooth, faintly marked with zones of growth, and, especially near the apex, with faint lines and furrows radiating from it. There is no distinct ridge proceeding from the apex to the baso-lateral angle, which is so much rounded that the basal margin blends into the tergo-lateral; it must, however, be remarked, that the specimens are worn. The occludent margin stands at right angles to the basal; and the lower part of the tergo-lateral margin forms rather above a right angle with it. Internally (c), there is a deep pit for the adductor scutorum, and in the upper part, close to the tergal margin, a deep furrow; the central portion is prominent; the occludent margin keeps nearly of the same thickness up to the apex of the valve.

Terga (Tab. III, fig. 3, d), nearly flat, sub-rhomboidal, or rather pointed oval, with the scutal half

[page] 54 FOSSIL CIRRIPEDIA.

5. POLLICIPES POLITUS. Tab. III, fig. 4.

P. scutis ferè rhombicis, lævissimis; margine basali cum margine occludente angulum recto majorem formante; margine occludente projecturâ parietali,1 lineari, minutâ instructo; internâ apicis superficie concavâ.

Scuta, almost rhomboidal, excessively smooth, basal margin forming above a right angle with the occludent margin, which latter is exteriorly furnished with a linear, minute, wall-sided ledge; apex with its internal surface concave.

Mus. Bowerbank. Locality and formation unknown; from the state of another specimen fastened on the same board, I think probably from the Gault; the colour of the substance in the cracks of the valve countenances this same opinion.

I have been unwilling to fix a specific name to a single, much broken scutum; but as even in its present state it can be clearly seen to be distinct, and as this is the typical valve in this genus, I have felt myself compelled to do so.

Scutum sub-rhomboidal, approaching to oval in outline: rather thin; surface excessively smooth; slightly convex, but with a narrow portion along the occludent margin, somewhat inflected: exteriorly close to this same margin, or rather almost forming it, (b) there is an extremely narrow, sharp, wall-sided, projecting ledge. The occludent margin is slightly arched, and forms, with the basal margin, an angle considerably above a right angle, so that the whole baso-lateral corner of the valve is much produced: the lower part of the tergo-lateral margin is at right angles to the basal margin. Baso-lateral angle smoothly rounded, with no trace of a ridge running from it to the apex, though this is the line of chief flexure of the valve. Internally, the valve has been much injured; the de-

protuberant; surface smooth, but near the pointed, slightly curled apex, it is marked by fine radiating lines; carinal margin regularly curved from the apex to the basal angle, which latter is not very sharp. A curved ridge (formed by the surface of the shell being lower on the carinal than on the other side) connects the upper and basal apices, running almost parallel to the carinal margin, and at about one-fourth of the entire width of the valve from the latter margin. Occludent margin shorter than the scutal; rounded, protuberant, with a depression parallel to it; the scutal margin, corresponding with this depression, being slightly hollowed out; a small portion of the apex projects freely. Internally, and nearer to the occludent than to the carinal margin, there are three or four short parallel longitudinal ridges or crests, as described in Scalpellum arcuatum.

Carina (Tab. III, fig. 3, a) moderately bowed inwards, widening gradually from the apex to the basal margin, which is rounded and protuberant, and with a trace of an angular bend in the middle; exteriorly the surface presents just a trace of being sub-carinated; roof convex; the upper part of the valve projects freely.

Rostrum: Koch and Dunker figure valves, which, from their general appearance, breadth, and apparently large proportional upper, freely-projecting portion, I have little doubt have been rightly considered by them as rostra; they are, however, longitudinally plicated or striated to a greater extent than the other valves.

1 Parietali, i. e. lateribus utrinque perpendicularibus.

[page] 55 POLLICIPES,

pression for the adductor scutorum does not appear to have been deep: the concavity of the valve extended to the apex, with the upper part not filled up solid; a considerable portion of the upper tergal margin is marked by lines of growth, and must have overlapped the tergum, but there is no trace in it of a recipient furrow.

Affinities. This species seems quite distinct from all others; and I can hardly say to which species it is most related; in some few respects it comes nearest to P. acuminatus.1

1 6. POLLICIPES ELONGATUS. Tab. III, fig. 5.

POLLICIPES ELONGATUS. Steenstrup. Kroyer's Tidsskrift, b. i, p. 361.

 — LÆVIS (Sowerby). Ib. Ib. b. ii, p. 409, pl. 5, figs. 9, 10.

P. scutis pæne quadratis; margine occludente et parte inferiori marginis tergo-lateralis rectangulè ad marginem basalem positis; apice obtuso.

Scuta almost square; occludent margin and the lower part of the tergo-lateral margin at right angles to the basal margin; apex blunt.

White Chalk, Denmark. Mus. Univers. Copenhagen.

General Remarks. Professor Steenstrup at first described this species as distinct, but subsequently considered it the same with P. lævis of Sowerby; this is not the case, and therefore I have retained the name first given, though very inappropriate to the more important valve. According to the practice here followed, the species is founded on the scutum, of which a mere fragment and impression exists, but it is sufficient to show that it is distinct. In the same chalk with this scutum, there are two terga which are different from any other seen by me, and which Professor Steenstrup has described as belonging to this species, a view which I have followed with some hesitation.

Scutum (fig. 5, c, b) nearly smooth, but with the growth-lines plain; thin, very slightly convex; oblong, almost rectangular, but with the upper lateral corner rounded off. Occludent and lower part of tergo-lateral margin both straight, and at right angles to the straight basal margin: upper part of tergo-lateral margin much arched and protuberant, which, together with the blunt apex given to the valve, it is almost rectangular, oblong outline. A trace of a ridge runs from the baso-lateral angle to the blunt apex. The figure given is a restoration; being guided by the outline impressed on the chalk, and the lines of growth as seen on the small baso-lateral preserved portion.

Tergum (fig. 5, a), convex, thick, elongated, sub-rhomboidal, or rather triangular, for the upper and lower carinal margins blend into each other with quite a uniform and gentle sweep: upper part of the carinal and occludent margins meet at an angle of about 45°; from the apex to the sharp basal angle, an angular, very slightly curved, conspicuous ridge runs at about one third of the entire width of valve from the carinal margin: the surface of the valve slopes rather steeply away on both sides from this ridge. Occludent and scutal margins about equal in length; parallel to the former, a rather wide space of the valve is slightly depressed, with a corresponding portion of the scutal margin slightly indented; the occludent margin itself is not rounded and protuberant, as if it had been received in a furrow in the scuta. A considerable portion of the upper part of the valve projected freely. This valve more resembles the homologous one in the Italian tertiary, P. carinatus, than that of any other species: as before stated, I assign it to this species on the excellent authority of Professor Steenstrup; I may, however, remark, that it appears much thicker and stronger than the scutum. The figure of the tergum (a) is not very good, and has been drawn on too small a scale.

[page] 56 FOSSIL CIRRIPEDIA.

7. POLLICIPES ACUMINATUS. Tab. III, fig. 6.

P. scutis elongatis, triangularis; margine basali cum margine occludente angulum recto longè minorem formante; internâ apicis superficie concavâ.

Scuta elongated, triangular; basal margin forming much less than a right angle with the occludent margin; apex, with its internal surface concave.

White Chalk. Mus. Flower, (believed to have come from the Lower Chalk of Stoke Ferry, Norfolk).

My materials consist only of a single left-hand scutum, and that with the whole of the basal margin broken off; nevertheless, there can be no question that it is quite distinct from all the species hitherto described.

Scutum: shell rather thin, surface extremely smooth; triangular, much elongated, with the upper part a little bent over towards the terga: slightly convex, but with the whole middle part of the valve remarkably flat; the convexity being caused by the inflection, in a slight degree, of the occludent margin, but chiefly of the tergo-lateral portion; hence, a smooth ridge of chief curvature runs from the apex to the baso-lateral angle. Occludent margin arched, forming less than a rectangle with the straight basal margin, with which the very slightly concave tergo-lateral margin forms an angle rather above a right angle: the tergo-lateral portion of the valve, formed by the upturned zones of growth, moderately wide, being in the upper part about one third of the entire width of the valve: rostral angle rounded. Internally (b) the valve is singular; the depression for the adductor scutorum muscle is extremely faint, and is situated unusually low down in the valve, though the exact relative position must at present remain unknown, as the basal margin has been broken off. But the most unusual character, at least in the cretaceous species of Pollicipes, is, that the concavity of the valve runs up to the apex, and must have been lined up to that point with corium; the flat internal occludent edge, marked by lines of growth, widens very little in the uppermost part.

8. POLLICIPES ANGELINI. Tab. III, fig. 7.

P. scutis elongatis, triangulis, margine basali propè angulum rostralem in prominentiam obliquè rotundatam producto: internâ apicis superficie prominente, margine occludente sulcato.

Scuta elongated, triangular, with the basal margin near to the rostral angle, produced into an obliquely rounded point; apex with its internal surface prominent, and with the occludent edge furrowed.

Upper Chalk, Norwich. Mus. Fitch. Kjuge, Scania. Mus. Univers. Copenhagen.

My materials consist of four scuta which, as usual, I take as typical, a pair of terga, and one or two carinæ which, for reasons to be given, perhaps belonged to this species; all

[page] 57 POLLICIPES.

in Mr. Fitch's Collection: also a single scutum sent me by Professor Steenstrup, and found by M. Angelin, after whose name I have called this well-marked and peculiar species.

Scuta (fig. 7, a, b); triangular, much elongated, considerably convex, apex extremely acuminated; basal margin at nearly right angles to the straight occludent margin, but near to the rostral angle, it is produced in a remarkable manner into a rounded, obliquely truncated broad point.1 The tergo-lateral portion of the valve, formed by the upturned lines of growth, is not much developed: the tergo-lateral margin, as seen externally, is obscurely divided into two lines, of which the upper, or tergal portion, has its edge reflexed; this same whole margin, however, seen internally, appears nearly straight, and this is essentially the case; the projecting angle being connected with the thickening of the valve during growth. The exterior surface is smooth, with some faint longitudinal striæ: a single ridge, or rather, line of flexure, runs from the apex to the baso-lateral angle. Seen internally, the uppermost part of the valve is found to be unusually thick and solid, with the pit for the adductor scutorum muscle well developed, and placed rather low down. The internal occludent edge (b), marked with lines of growth, becomes close above the adductor depression suddenly very wide, and forms a deep furrow, which I at first thought was formed to receive the occludent angle of the terga; but upon consideration, I feel pretty sure that this cannot have been the case, and I believe the furrow to be of no functional importance, but to result from the sharp apex of the still corium-covered portion of the valve having been greatly thickened: this same upper portion has, in most specimens, in its middle, a slight linear furrow. On the tergal margin of the internal surface there is a small portion, marked with lines of growth, which is obliquely truncated, owing to the valve having become very thick; and this must have overlapped the tergum. From these peculiarities in the internal surface of the apex of the scuta, it may be inferred, that the terga, owing to the probable close contact of the two valves, would present peculiarities of a corresponding nature. The largest British specimen is .8; and the Scanian specimen is .95 of an inch, in length.

Terga (fig. 7, c, d); in Mr. Fitch's collection there are, from the same formation in which the above scuta were found, two terga, remarkable from a very wide square-edged depression, running parallel to the occludent margin, which is itself rounded and protuberant: these valves probably belonged to the P. Angelini, and anyhow may be conveniently here described. Valve rhomboidal, not very flat, smooth, with a conspicuous ridge, wall-sided on its carinal aspect, running almost down the middle of the valve from the apex to the basal angle, which latter is not very sharp. The upper carinal and occludent margins meet each other at slightly less than a right angle; occludent margin a little longer than the scutal margin, with its edge thickened, rounded, and protuberant to an unusual degree; alongside the occludent margin an unusually broad and deep, square-sided depression runs, equalling in width about one third of the scutal margin; a

1 Amongst the Scanian fossils from Kopinge, there is a scutum with the whole upper part broken off, but which I think belonged to this species; if so, it differs from all the others in the rostral portion of the basal margin projecting very little.

h           

[page] 58 FOSSIL CIRRIPEDIA.

transverse section across the middle of the valve is given in fig. 7, d, exhibiting its peculiar outline.

Carina. In Mr. Fitch's collection there are two carinæ which probably belonged to this species, at least they do not belong to the only two other species of Pollicipes, (viz. P. fallax and striatus,) found by this gentleman in the chalk near Norwich. These carinæ are identical, as I know from examination, with that (also from Norwich) figured by Mr. Sowerby, (Min. Conch., Pl. 606, fig. 7,) as the anterior valve of his Pollicipes sulcatus, Scalpellum maximum, var. sulcatum of this work. These two carinæ differ a little from each other in the basal margin, being either rectangularly pointed or rather blunter and more arched; their surfaces are smooth, but in one specimen there are some obscure longitudinal striæ; in outline they are tapering, triangular, almost straight, transversely flatly arched, subcarinated, edge inflected, with the lines of growth bowed downwards, and consequently with the basal lateral angles or heels a little prominent. Finally, these carinæ cannot be strictly distinguished from the same valve in P. glaber and unguis, but as I believe neither of these species occur in the upper chalk near Norwich, they can hardly belong to them.

Affinities. The scuta in this species differ from all others in the projection of the basal margin, close to the rostral angle; a somewhat similar projection, I may remark, sometimes occurs in the scuta of the recent Lepas fascicularis, A. vitrea of Lamarck. Internally, the valve more resembles that of the second and third varieties of Scalpellum maximum than any other species. The terga can be distinguished from those of P. glaber only by the depression along the occludent margin being deeper, wider, and square-sided.

9. POLLICIPES REFLEXUS. Tab. III, fig. 8.

POLLICIPES REFLEXUS. J. Sowerby. Min. Conch., pl. 606, fig. 8.

P. scutis tenuibus, subovalibus; margine basali cum margine occludente angulum recto longè majorem formante; costâ obsoletâ rotundatâ ab apice ad angulum baso-lateralem decurrente, valvam in duas ferè æquales partes separante. Carinâ lineari, transversè abruptè arcuatâ; margine basali multum producto, apice truncato. Lateribus superioribus subpentagonis.

Scuta; thin, suboval, with the basal margin forming an angle much larger than a rectangle with the occludent margin; a faint rounded ridge runs from the apex to the baso-lateral angle, dividing the valve into two nearly equal halves. Carina linear, in a transverse line steeply arched; basal margin much produced, with its apex truncated. Upper Latera subpentagonal.

Upper Marine Eocene formation; Colville Bay, Isle of Wight. Mus. J. Sowerby, F. Edwards.

I owe to the kindness of Mr. Sowerby an examination of some of the original speci-

[page] 59 POLLICIPES.

mens, consisting of a scutum, terga, carinæ, and upper latera; and to Mr. F. E. Edwards the loan of several very perfect specimens.

Valves; smooth, rather thin. Scutum (fig. 8, e) elongated, very slightly convex, many-sided, almost oval, with its upper point produced, but apparently apt to be broken off. Occludent margin slightly arched; basal margin consists of two sides, of which the rostral side is extremely oblique to the other, the two sides together forming a very large angle with the occludent margin; the tergo-lateral margin also consists of two sides, meeting each other at a very open angle; the lower half forms above a rectangle with the basal margin; possibly this lower half corresponds with the widely-truncated baso-lateral angle in P. dorsatus, and with the smaller similar angle in the tertiary P. carinatus. A faint rounded ridge runs from the apex to the baso-lateral angle, and thus divides the valve into two nearly equal halves. Internally there is a deep pit for the adductor muscle; only a narrow internal edge along both sides of the apex is marked by lines of growth.

Terga (fig. 8, d); elongated, rhomboidal, flat and thin; carinal margin continuously curved; apex much produced; the occludent and upper carinal margins meet each other at much less than a right angle; occludent margin slightly longer than the scutal margin, which latter in the upper part is very slightly hollowed out; a faint, rather wide ridge, runs down the centre of the valve to the rectangularly-pointed basal angle; a small portion of the upper part of the terga projected freely.

Carina fig. 8, a, b, c); narrow, with the lower part somewhat spear-shaped; almost straight, transversely convex, with the central part forming a broad rounded crest; lateral margin a little inflected; basal margin extraordinarily produced, with its apex square; internally, the corium-covered surface is produced upwards into the sharpest apex; a small portion only of the uppermost part of the valve projected freely.

Upper Latera (fig. 8, f); flat, almost pentagonal, with the two upper margins considerably longer than the three lower ones; of these three, the carinal margin is the shortest, and the other two equal, with the rostral one considerably arched or convex; these three basal margins must have been in contact with the Latera of the lower whorl; the apex did not project freely. I have not seen any latera of the lower whorl, but Mr. Sowerby gives figures of some minute valves, which no doubt were such. Several of Mr. Edwards's specimens are tinged a pale-reddish purple.

Dimensions. The valves described are all rather small; the largest, a tergum, is a little more than a quarter of an inch in length.

Affinities. This species is more nearly related to the section of the genus containing the recent P. cornucopia, elegans, and polymerus, than to the other sections. Its affinity is closest to P. cornucopia, though in the form of the basal margin of the scuta there is more resemblance to P. polymerus. The scutum presents some points of resemblance to the cretaceous P. gracilis and dorsatus.

[page] 60 FOSSIL CIRRIPEDIA.

[B.] Scuta, costâ, nonnumquam subobsoletâ, ab apice ad centrum marginis basilis decurrente.1

1 10. POLLICIPES CARINATUS. Tab. III, fig. 9.

POLLICIPES CARINATUS. Phillippi. Enum. Mollusc. Siciliæ, 1836, Tab. xii, figs. 26, 28.

P. scutis crassiusculis ad formam trianguli æquianguli accedentibus; margine occludente externè costâ humuli firmato; costâ firmâ ab apice ad centrum marginis basalis decurrente; margine basali recto; angulo baso-laterali truncato, brevi; segmentum tergo-laterale ex lineis incrementi reflexis formatum, deest. Carinâ externè valdè carinatâ cum sulco laterali ad utrumque latus.

Scuta moderately thick, in shape nearly an equilateral triangle; occludent margin exteriorly strengthened by a slight ridge; a strong ridge runs from the apex to the middle of the basal margin; basal margin straight; baso-lateral angle truncated, short: the tergo-lateral portion, formed by upturned lines of growth, is absent. Carina, exteriorly, strongly carinated, with a lateral furrow on each side.

Tertiary; Messina, Sicily.

I owe to the great kindness of Dr. Phillippi an examination of an authentic series of specimens. Valves rather thick, with the lines of growth plain, and with a few fine striæ radiating from their apices: these striæ are sometimes so conspicuous, that I have doubted whether the species ought not to have been placed in the next section.

Scuta (fig. 9, d, e); triangular, with the apex slightly bowed over towards the terga; moderately convex; occludent margin slightly arched, about equal in length to the slightly hollowed-out tergo-lateral margin; basal margin nearly straight, though formed by two lines meeting each other, sometimes with the rostral half not descending so low as the other half; this margin forms equal angles with the other two margins. The baso-lateral angle is obliquely truncated: there is no tergo-lateral slip formed by upturned zones of growth. The occludent margin is exteriorly strengthened in a manner only just perceptible by a flattened rim. A strong, conspicuous, and prominent ridge runs, in a slightly curved course, from the apex to a point in the basal margin, rather nearer to the rostral than to the baso-lateral angle; this point just perceptibly projects beyond the rest of the basal margin: the ridge is either moderately sharp, or broad and flat-topped; it marks the line of chief curvature of the valve. Internally (e), the pit for the adductor muscle is not very strongly developed, and to a different degree in different specimens: the internal surface of the centre of the apex is prominent; on its tergal side there is no furrow, but a rectangular indentation formed by a remarkably wide, flat, smooth ledge, which runs down, narrowing, to the baso-lateral angle; hence the scuta along the whole of this side, especially in the upper part, must have widely overlapped the terga, in a manner and to a degree I have not seen equalled in any other Pollicipes; but the two valves cannot be said to have been articulated together. The internal occludent edge widens a little in the upper part, and is here divided by an oblique line, with the lines of growth apparently discontinuous on opposite sides of it, into two portions, of which the inner portion is slightly more prominent than the outer. I have already alluded to the fact, that in some specimens the scuta are strongly ribbed longitudinally, in some very faintly striated, and in others smooth.

Terga (fig. 9, a, b); sub-rhomboidal, elongated, exteriorly convex, internally very slightly concave: upper part very thick and solid, with a considerable portion freely projecting, and internally marked by lines of growth: along the middle of the portion thus marked, there is a slight longitudinal depression, which is worth remarking, inasmuch as (judging from a conspicuous and analogous character in certain recent species of Lithotrya) it was probably caused by the internal central crest of the upper part of the carina. Occludent margin slightly convex, very little shorter than the scutal margin; upper and lower carinal margins nearly equal in length; they meet each other at a very open angle: upper carinal and occludent margins meet each other at an angle of only a little above 50°. A prominent, strongly marked ridge, (with both sides of the

[page] 61 POLLICIPES.

11. POLLICIPES GLABER. Tab. III, fig. 10.

POLLICIPES GLABER. Roemer. Norddeutsch. Kreidegebirg. Tab. xvi, fig. 11.

XIPHIDIUM MAXIMUM. J. Sowerby. Dixon's Geology of Suffolk, Tab. xxviii, figs. 6-8.

P. scutis subtenuibus, latiusculis, ad formam trianguli æquianguli accedentibus; margine basali non prorsus recto; tergo-laterali segmento e zonis incrementi reflexis formato, ubi latissimo, reliquæ valvæ dimidium æquante: margine tergali apicis intùs sulcato. Carinæ margine basali obtusé acuminato. Lateribus superioribus triangulis, tertiam partem longitudinis tergorum æquantibus. Lateribus anticis inferioribus singulis costâ propè terminum marginis basalis decurrente.

valve sloping from it,) runs from the apex to the sharp basal angle: this ridge is very slightly curved in two directions, like the letter S, it runs at about one third of the entire width of the valve from the carinal margin.

Carina (fig. 9, e, f) strong and solid, with lines of growth conspicuous on its surface; very slightly arched inwards; triangular, moderately tapering; transversely moderately convex, very plainly carinated, with a slightly projecting rib; on each side, at a little distance from the lateral edges, there is a distinct and linear furrow, and these edges themselves are, partly in consequence, rounded and slightly protuberant: basal margin square, and not at all protuberant. Internally, the upper part, for about one third of the total length of the valve, must have projected freely, and has been filled up solid with a trace (f) of a central crest: the internal lateral edges are slightly scalloped out along the whole length of the valve.

Rostrum (fig. g, h, i); broad, triangular: apex curled inwards to a most remarkable extent, so as even to point a little downwards; basal margin just perceptibly protuberant, with a square projection formed by the end of a wall-sided, broad, flat-topped ridge, running down from the apex; Phillippi, however, states, that the form of the basal margin varies. Internally, a full upper half of the valve projected freely; the internal upper surface is smooth and concave, with just a trace of a fine central crest: the inwardly curled apex converts the upper part into a hood: the central basal projection is channelled, the channel running a little way up the valve, and being gradually lost: this channel, no doubt, allowed a filament of the corium to pass to the sub-rostrum.

Peduncle. Dr. Phillippi has sent for my inspection, a rare and interesting specimen of a peduncle, with the scales preserved, no doubt, belonging to this species. The scales, as usual, decrease downwards in size; they are rather broad; each has its upper end rounded; is marked transversely by lines of growth, and has a slight external, central, longitudinal crest: this crest is wedge-formed, being widest at the apex. I have not seen this latter character in the peduncular scales of any other Pollicipes; there are, however, traces of it in the small lower Latera in P. mitella; it is apparently caused by the lateral overlapping of the closely-packed scales, and chiefly when the specimen was young.

Affinities. The general form of the carina, with its lateral furrows and rounded protuberant margins,—its carinated central line;—the shortness, and great inward curvature of the rostrum, with its strong, central ridge, terminating in a channelled projection on its basal margin—show a clear affinity between this species and the recent P. mitella of the Eastern tropical seas. There are some points of resemblance in the scuta and terga to the same recent species; but in the scuta a closer affinity is shown to P. dorsatus; and in the terga to those described under P. elongatus: in the manner, moreover, in which the upper part of the carina is filled up and furnished with a central crest, there is a relationship to P. validus. The affinity of P. carinatus to P. mitella is interesting; because we may with some confidence infer from the relationship between P. carinatus, dorsatus, validus, and rigidus, that, in these several species, the valves, which hitherto have been found only separated, were united together to form the capitulum in a somewhat similar manner as in the well-known recent P. mitella.

[page] 62 FOSSIL CIRRIPEDIA.

Scuta moderately thin, rather broad, approaching to an equilateral triangle; basal margin not quite straight; the tergo-lateral portion, formed by the upturned zones of growth, where widest, half as wide as the rest of valve; apex internally furrowed on the tergal side. Carina with the basal margin bluntly pointed. Upper latera triangular, one third the length of the terga. Anterior lower latera, each with a ridge running to near one end of their basal margins.

Lower Chalk, Stoke Ferry, Norfolk. Lower Chalk, Hanover, according to Roemer. Pläner (Chalk-marl), Sarstedt, near Hildesheim, Mus. Roemer. Upper Chalk, Northfleet and Gravesend, Kent. Chalk Detritus, Charing, Kent. Maëstricht Formation, Scania ? Mus. Flower, Wetherell, Harris, Univers. Copenhagen, Geolog. Soc., and Bowerbank.

General remarks. My materials consist of several scuta, in Mr. Flower's collection from Stoke Ferry, together with some carinæ, and a rostrum of apparently the same species; of a single scutum from Northfleet, and of others from Charing, both in Kent; of some scuta, terga, and carinæ, sent me by the great kindness of Roemer, from Sarstedt, near Hildesheim, and therefore authentic specimens by him named; and lastly, of a valuable specimen from Gravesend, in Kent, in Mr. Bowerbank's collection (fig. 10, a), in which a carina, pair of terga, an upper latus, and two lower latera, were embedded in nearly their proper positions, together with a fragment of a scutum, which latter is sufficiently perfect to leave no doubt on my mind regarding its identity with the valves from Stoke Ferry, Northfleet, and Sarstedt. This appears to have been one of the commonest species of Pollicipes during the cretaceous period. Though found in the upper chalk of Northfleet and Gravesend, it is singular that not a single valve of this species has been collected by Mr. Fitch in the upper chalk of Norwich. Amongst the Scanian fossils, collected by M. Angelin at Kopinge, from a still higher stage of the chalk, and forwarded to me by Professor Steenstrup, there is an upper latus and tergum most closely allied, probably even identical with the present species. We have seen that it extends down even to the pläner or chalk marl.

Scuta (fig. 10, b, c, d). These valves are moderately thick and convex, so that in their upper halves they are almost semi-conical; the basal margin is not quite straight, it forms a rather larger angle with the lower part of the tergo-lateral margin, than with the occludent margin, both angles being less than right angles. From the apex two faint ridges run, one to the baso-lateral angle, and the second to a point in the basal margin, a little nearer to the rostral than to the baso-lateral angle. The valve is bent, so as to be convex, chiefly along these two ridges. The tergo-lateral portion formed by the upturned lines of growth is wide and protuberant. Outer surface of valve smooth, with the faintest striæ radiating from the apex. Viewed internally (d), a conspicuous furrow runs from the pit for the adductor scutorum muscle up to the apex; the internal occludent edge keeps the same width up to the apex. The Sarstedt specimen is the largest scutum which I have seen, and that is .6 of an inch in length.

One out of Mr. Flower's five specimens (believed all to have come from the lower chalk of Stoke Ferry) and another in Mr. Wetherell's collection from the upper chalk of

[page] 63 POLLICIPES.

Northfleet, present some slight differences, in the valve being flatter, in the tergo-lateral portion being more developed, and in the basal margin being straighter; but these differences are so very slight that it would be exceedingly rash to consider them as specific.

Terga (fig. 10, e, a); rhomboidal, flat, with a straight slight ridge running, at about one third of the entire width of the valve from the carinal angle, to the sharp basal angle; this ridge is steep on its carinal side, on which side the whole surface of the valve is somewhat depressed. The upper carinal margin meets the occludent margin at somewhat less than a right angle: the occludent margin slightly exceeds in length the scutal margin; the valve is widest nearly in its middle. A narrow rim along the occludent margin is slightly protuberant, within which there is a slight parallel depression. The scutal margin is not quite straight; the lower half (which probably was in contact with the upper latus) projecting a little.

Carina (fig. 10, f, g); triangular, tapering, moderately strong, with a smooth surface; almost straight or slightly curved inwards; transversely, flatly arched, sub-carinated. Lateral margins narrow, inflected, with the lines of growth first curved downwards (g), and then on the edge itself abruptly upturned; basal margin bluntly pointed, apparently in a variable degree. The two baso-lateral angles are slightly prominent, in conformity with the above-stated direction of the lines of growth along the margin. I may remind the reader that this valve, the terga, and the latera presently to be described, were all embedded together in their proper positions.

Rostrum (fig. 10, h, i): in Mr. Flower's collection, with the other loose valves from Stoke Ferry, there is one which I can hardly doubt is a rostrum: it is nearly an equilateral triangle; externally convex, sub-carinated, basal margin not protuberant. The upper part, for about one fourth of the entire length of the valve, must have projected freely; this part is remarkable, from having been filled up internally with a central crest, like the carina of P. validus and carinatus.

Upper latus (fig. 10, k, a); flat, almost an equilateral triangle, but with the two upper sides not exactly equal, and both a very little longer than the basal margin; umbo of growth at the uppermost point; length, one third of the terga; surface smooth, with no trace of a central longitudinal ridge; internally the edges are bevelled, and a very small portion of the apex must have projected freely.

Lower latera (fig. 10, l, a). There are two of these (one much broken) nearly resembling each other: from analogy with the latera of P. unguis, these are probably from the rostral end of the capitulum; they are slightly convex, and approximately form a transversely elongated triangle, with one corner cut off; the two upper sides are slightly unequal in length: umbo of growth at the apex, from this point a narrow well-defined ridge runs obliquely across the valve, to the most protuberant point of the basal margin, which is situated about one fourth of the entire width of valve from one end. These lower latera are wider than, but not so high as the upper latus: seen internally the edges are bevelled, and a very small portion of the apex must have projected freely.

As it is so very rare to find the valves of a Pollicipes united, it will be advisable to give

[page] 64 FOSSIL CIRRIPEDIA.

the measurements of the Gravesend specimen: the scutum is too much broken to be measured, and the breadth only of the basal margin of the carina can be given—it is .25 of an inch; the terga are nearly .8 long and fully .4 broad. The upper latus is .27 in height, basal margin .23 in length. Lower latus .2 in height and .26 in breadth. I imagine that the broken scutum belonging to this individual, was fully two thirds of the size of the largest scutum which I have seen, namely, that from Sarstedt, .6 of an inch in length.

Affinities. From the very close affinity of this species to the following one, P. unguis of the Gault, we may safely infer that it had not only a rostrum (of which a specimen found separately has been described), but also a sub-rostrum; whether it had a sub-carina, as is probable, must remain doubtful. The two faint ridges running from the umbo of each scutum to its basal margin, probably mark the extent to which this valve was overlapped, as in the case of the recent P. mitella, by the rostrum and upper latera; and the ridge on the terga, steep towards the carina, probably shows the extent to which this latter valve reached. It is also probable, as we shall see under the head of P. unguis, that there was only one whorl of valves under the upper latera, and that this included the sub-rostrum: the latera in this lower whorl were probably not very numerous, but large, and of very unequal sizes; their mutual overlapping no doubt caused the oblique ridges on their exterior surfaces.

12. POLLICIPES UNGUIS. Tab. IV, fig. 1.

POLLICIPES UNGUIS. J. Sowerby. Geolog. Transac. 2d series, vol. iv, t. xi, fig. 5*.

 — LÆVIS Ib. Ib. Ib. fig. 5 (sed non Tab. xvi, fig. 1,—alia species).

P. scutis incognitis, verisimiliter ut in P. glabro. Margine basali carinæ obtusè acuminato, sub-rotundato. Lateribus superioribus elongatis triangularibus, dimidium longitudinis tergorum superantibus. Lateribus anticis inferioribus costâ subcentrali instructis.

Scuta unknown, probably as in P. glaber. Carina, with the basal margin, bluntly pointed, somewhat rounded. Upper latera elongated, triangular, exceeding half the length of the terga. Anterior lower latera, each with a ridge, subcentral.

Gault; Folkstone, (common.) Burham, Eastweare Bay, Maidstone. Mus. Practical Geolog., Bowerbank, J. Sowerby, Brit. Mus., &c. In the Museum of Geolog. Soc. there is a tergum of this species, marked Lower Greensand, Maidstone.

General Remarks. This species comes very close to P. glaber, but can, I think, be safely distinguished from it, even with our present materials. A specimen most unusually perfect is in the Museum of Practical Geology; it consists of a carina and pair of terga, much mutilated, a rostrum, sub-rostrum, a pair of upper latera, a pair of latera of the lower whorl from the carinal end of the capitulum, and two other latera of this same

[page] 65 POLLICIPES.

whorl from one side of the rostral end of the capitulum. All these valves are magnified twice in fig. 1, Tab. IV; and as all, except (d), belonged to the same individual, we here have the rare advantage of learning their relative sizes. The largest of the lower latera has been mistaken for a scutum, and has been thus figured by Mr. Sowerby; the mistake was a very natural one, to be rectified only by examining the under side of the specimen. Although the scutum is, unfortunately, at present unknown, there can be scarcely any doubt that it would closely resemble that of P. glaber, and therefore I have not hesitated, in this instance, to break through my rule of exclusively taking the scutum as typical in Pollicipes: should, hereafter, a scutum be found in the Gault like that of P. glaber, it may, with considerable confidence, be named as belonging to this species.

I have felt considerable doubts regarding the nomenclature of this species: P. unguis is founded on one of the latera of the lower whorl, and on what apparently is a rostrum; these valves are at present, and will probably for very long remain insufficient for the foundation of a species. P. lævis is founded on a tergum and carina, and therefore on better grounds. The specimen immediately to be described, leads me to believe that all these valves belong to the same species; and therefore both names were open to me. Mr. Sowerby, however, has given in the same volume of the ' Geological Transactions,' the name of P. lævis to a carina and tergum from Blackdown, which, I cannot doubt, is distinct: Professor Steenstrup has also described a new form under the same name of lævis; such being the case, it has appeared to me advisable to take the name of P. unguis. I must add, that there is some considerable variation in the terga from the Gault, which renders it just possible, but not probable, that there may be a second closely allied form. It is very singular, considering how very frequent terga are in all collections, that I should not have seen a single scutum which could, as I believe, have belonged to this form.

Scutum unknown. Tergum (Tab. IV, fig. 1, b, c); this is a medium-sized specimen, .5 or .6 of an inch in length; it is rhomboidal, nearly flat, with a straight, slight ridge, running from the apex, at about one third of the entire width of the valve from the carinal angle, to the sharp basal angle: the ridge is steep on its carinal side, on which side the whole surface of the valve is somewhat depressed. The upper carinal margin meets the occludent margin at somewhat less than a right angle. Internally, a rather small portion of the apex is marked by lines of growth; and close along the upper carinal margin there is a narrow furrow (b), with a ridge parallel and exterior to it; both furrow and ridge are rather variable, and, no doubt, are produced by contact with the edge of the carina. The occludent margin very slightly exceeds in length the scutal margin; the valve is widest nearly across the middle. A slight depression, with just perceptibly angular sides, runs parallel to the occludent margin. The scutal margin is nearly straight; with the exception of this latter single character, scarcely any difference can be perceived between this valve and that of P. glaber.

I have seen several large terga, (d, natural size,) nearly an inch in length, from the Gault, which at first appeared so different, that I thought them specifically distinct; they

i            

[page] 66 FOSSIL CIRRIPEDIA.

form the variation above alluded to. But, after careful comparison of a large series, I feel convinced that the difference is caused solely by age: the chief difference consists in the occludent margin being considerably longer than the scutal margin, and consequently in the widest part of the valve lying below the middle point: that portion of the valve, moreover, which lies on the carinal side of the sub-central ridge is, in proportion, narrower than in the common form. Internally, in these large specimens, a considerable portion of the apex is marked by lines of growth: it follows from this, that if only the internal corium-covered surfaces of the large and small terga be compared, there is far less difference of outline than if they be compared externally. I repeat that I have no doubt that these valves all belonged to the same species.

Carina (Tab. 4, fig. 1a), closely like that of P. glaber, triangular, moderately tapering, very slightly bowed inwards; smooth, sub-carinated, transversely slightly convex; lateral margins very narrowly inflected, with the lines of growth curved downwards, and those on the edge itself upturned; there is in this specimen a narrow, slight, linear channel along the line where the lines of growth are upturned; a small portion of the apex must have projected freely; basal margin (and consequently lines of growth) rounded, less angularly protuberant than in P. glaber, with the two baso-lateral angles slightly prominent.

Rostrum (fig. 1e), triangular, rather more than half as wide and about half as long as the carina, therefore rather wider in proportion to its length; more bowed inwards; a very small portion of the apex, which is internally simply concave, projected freely; basal margin curved, slightly protuberant: exterior surface smooth, sub-carinated, like the carina; edges very thin. Sub-rostrum (f) about half as long, and two thirds as wide as the rostrum; apex rounded; basal margin not protuberant; internally, slightly concave, with thin lateral margins, widely overlapping the latera of the lower whorl; exterior surface not subcarinated, that is, destitute of a central ridge.

Upper Latera (g), elongated, triangular, flat, exteriorly smooth, except from the lines of growth; two upper sides almost exactly equal in length, and equalling once and a half of the length of the basal margin; entire valve rather exceeding half the length of the terga.

Lower Latera: these consist of two small valves (l, k), namely (judging from the position in which, overlapping each other, they were embedded), the first and second, or more probably the second and third right-hand rostral latera of the lower whorl; and a pair (h, i) (right-hand and left-hand) of latera, of about twice the size of the two anterior ones, which must have come from the carinal half of the whorl, but the exact position of which I cannot tell. These latter larger latera are thin, and considerably convex; they are transversely elongated, and, in their longer axis, are rather more than half the length of the terga of the same individual. In shape they may be almost compared to one valve of a Donax; being sub-trigonal, with the two upper sides unequal in length, and with the third side arched and protuberant at a point about one third of the entire length of the valve from the narrower end: to this protuberant point, a well-defined ridge runs from the apex

[page] 67 POLLICIPES.

of the valve; internally (i), the lines of growth round the upper margins show that the two upper sides and the apex overlapped freely the valves on each side of them. This valve, as stated in the preliminary remarks, has naturally been always mistaken for a scutum; but the manner in which it has overlapped other valves (as shown by the internal view), on both its upper margins, and the entire absence of all hollow for the adductor muscle prove that this view is quite erroneous.

The two rostral or anterior small latera resemble each other (the anterior one being a little the smallest), and likewise the largest carinal latera just described; the external ridge, however, here runs to a much more nearly central point of the basal margin; and the shorter and more pointed portion of the basal margin is just perceptibly hollowed out. The more pointed end is directed towards the carina. In the first latus this end abuts against (no doubt thus producing) the external ridge on the second latus, which it overlaps. Internally, under the apex, there is a central crest (l), exactly as in the latera of the lower whorl in large specimens of the recent P. mitella, caused likewise by the overlapping of the valves: in the above-described large carinal latera, however, this internal crest is absent, showing that the arrangement of these latter valves differed from that of the two anterior ones.

With respect to the number of valves in the whole capitulum, it is almost useless to speculate: we have two scuta, two terga, two upper latera, two rostra, and we may, perhaps, infer two carinæ, making ten valves, we know of three pair of lower latera, making sixteen valves: I believe there must have existed some other latera, but probably only a few more; for these valves, especially the carinal pair, are much larger, in proportion to the scuta and terga, than in any recent Pollicipes. Probably the lower latera, together with the sub-rostrum, and perhaps a sub-carina, formed only a single lower whorl.

Size: in the individual here described, the carina and terga, were equal in length to each other, and .65 of an inch long. In Mr. Bowerbank's collection there is a lower latus of nearly double the size of the same valve in this individual, which shows that this species attains large dimensions.

Affinities. As before remarked, this species is very closely related to the cretaceous P. glaber, of which it is evidently the representative in the Gault; the chief difference consisting in the more elongated form and greater size of the upper latera, which, in P. unguis, exceed half the length of the tergum, whereas in P. glaber they are only one third of its length. The carina, in the present species, has its basal margin, perhaps, less pointed, and has a narrow linear channel along its edges; but I am not at all sure that this latter character does not vary. Lastly, the anterior lower latera in P. unguis are thinner, and rather more convex, with the basal margin more arched and protuberant, with the external oblique ridge very much more central.

Considering the characters of both species taken together, namely, the two ridges proceeding from the umbo of the scuta to the baso-lateral angle and basal margin,—the triangular shape of the upper latera,—the considerable size of the rostrum, and the ridges

[page] 68 FOSSIL CIRRIPEDIA.

on the lower latera,—this species comes much nearer to P. mitella than to any other recent species; I believe, however, that it must have had much fewer valves.1 From the growth

1 13. POLLICIPES VALIDUS. Tab. IV, fig. 2.

POLLICIPES VALIDUS. Steenstrup. Kroyer's Tidsskrift, 1839, pl. v, figs. 28-32.

P. scutis crassissimis, angustis; margine occludente externè costâ rotundatâ forti firmato; intus prominentiâ rostrali infra marginem rectum basalem dependente; costâ ab apice ad marginem basalem propiùs ad rostralem quam ad basi-lateralem angulum accedente. Carinâ lævissimâ, transversè semicylindricâ; parte superiori liberè prominente, internè aut planâ aut cristâ centrali instructâ.

Scuta, extraordinarily thick, narrow; occludent margin exteriorly strengthened by a rounded, strong ridge; internally, at the rostral angle, a blunt tooth depends beneath the straight basal margin: the ridge running from the apex to the basal margin is nearer to the rostral than to the baso-lateral angle. Carina very smooth, transversely semi-cylindrical; upper freely projecting portion internally, either solid and flat, or with a central prominent crest.

Scania, Sweden. Mus. Univers. Copenhagen. Petersberg, near Maëstricht.

My materials consist of several scuta and carinæ, sent me by Professor Steenstrup as belonging to the same species, which is likewise the opinion of that able collector, M. Angelin, who has found this species in various localities in Scania. A very fine carina, from near Maestricht, has been sent to me by Krantz, of Bonn.

Valves, remarkably thick, massive, and strong. Scuta (fig. 2, e, f, g, nat. size) elongated, being twice as long as broad; slightly convex; whole upper part bent towards the terga; surface, in some specimens, with traces of longitudinal striæ. Basal margin formed obscurely (partly owing to the rubbed condition of all the specimens), by two lines meeting each other at a very open angle. Occludent margin much arched, forming with the basal margin, taken as a whole, an angle of about 60° : tergo-lateral margin nearly straight, forming a rectangle with the adjoining portion of the basal margin. That part of the valve formed by the upturned zones of growth is narrow, being, in the widest part, barely half the width of the other part of the valve. The occludent margin is strengthened by a rounded, strong, projecting ledge, running along its entire length; the basal end of this ledge, and consequently the lines of growth crossing it, are oblique, and slightly upturned. A slight ridge, or angle, runs from the apex to the baso-lateral angle, and a second, still slighter ridge, to a point in the basal margin rather nearer to the rostral than to the baso-lateral angle. Close to the rostral angle, the internal lamina of the shell is produced downwards into a strong, blunt tooth, which (when not too much worn) can be seen from the external side, depending beneath the basal margin : this is the most singular character of the species. The internal occludent edge is broad (and of nearly the same breadth throughout the whole upper part of the valve), flat, and marked by lines of growth: this striated internal edge is separated from the smooth, depending, rostral tooth, by a very oblique line. The pit for the adductor muscle is very deep: above this pit there does not appear to have been any furrow on either margin, or any marked central prominence.

Carina (fig. 2, a, b, c, d, nat. size), broad, extremely solid, much bowed inwards; the upper part, even more than half the valve in length, must have freely projected; exterior surface transversely semi-cylindrical, or rather steeper than a semi-cylinder, but not at all carinated: basal margin not at all protuberant; lateral angles, or heels, just perceptibly projecting below the central part of the basal margin: in the Maestricht specimen it appears that there was a very slight furrow near each exterior lateral margin, making them just perceptibly protuberant. The internal, smooth, corium-covered surface is concave, forming almost an equilateral triangle (b): above this, the inner freely projecting portion is either filled up flat, or forms a central prominent crest (d).

Affinities. We shall immediately see that this species appears to be most closely allied to P. gracilis, of Roemer: it is also allied to P. dorsatus, by the strength of the valves, by the occludent margin of the

[page] 69 POLLICIPES.

of all the valves, as far as is apparent, being downwards, and from their number, apparently exceeding 16, I have, without hesitation, ranked this species, (and consequently P. glaber,) under the genus Pollicipes.

scuta being exteriorly strengthened by a prominent ridge, and by the two angular ridges running down to the basal margin, and by the general character of the under surface of the apex: it differs widely from P. dorsatus, in the rostral, tooth-like process, and in the baso-lateral angle not being widely truncated. The carina of these two species also presents some points of similarity. In P. validus the centre of the upper freely projecting portion often, but not always, has a longitudinal crest or ridge: in the recent P. mitella, the degree of filling up of the upper part of the carina varies considerably, and sometimes even a central crest is formed in it.

14. POLLICIPES GRACILIS. Tab. IV, fig. 3.

POLLICIPES GRACILIS. Roemer. Norddeutsch. Kreidegebirges, 1841, Tab. xvi, fig. 14.

P. scutis tenuibus, angustis, margine occludente externè costâ rotundatâ firmato; intus prominentiâ rostrali infra marginem basalem dependente; costâ ab apice ad marginem basalem centrali: internè, sulco transverso super fossam musculi adductoris, excavato.

Scuta thin, narrow, occludent margin exteriorly strengthened by a rounded ridge; internally at the rostral angle a blunt tooth depends beneath the basal margin; the ridge running from the apex to the basal margin is central. Internally there is a transverse furrow above the hollow for the adductor muscle.

Unterer Kreidemergel (lower division of Lower Chalk), Hanover. Oberer Kreidemergel, Shaftricht. Mus. Roemer.

Roemer has most kindly sent me a beautifully preserved scutum, which he has fully described in the above quoted work. It is unfortunately rather young, being .6 of an inch in length. It resembles so closely the same valve in P. validus, that had it not already received a name I should not have affixed one; still I think it is perhaps a distinct species. It will be quite superfluous to do more than describe the few points of difference, of which the chief and most conspicuous one is the much greater thinness of the whole valve. I should, however, state that I have not seen any specimen of P. validus so small, the smallest being more than one third longer. The second chief difference is that the medial longitudinal ridge here runs to a central point of the basal margin instead of to a point nearer to the rostral angle. I think the basal margin is more conspicuously formed by two distinct lines, meeting each other at the above point. Internally the third and perhaps most important distinction is the presence of a moderately deep and large depression or fold, marked by lines of growth, extending inwards from the occludent margin, just above the pit for the adductor muscle, and as far inwards at the middle of the pit: this fold precisely resembles that which occurs in the same position in Scalpellum magnum, vulgare, and in some Pollicipes, as P. Angelini. The rostral tooth appears to have been larger. Owing to the thinness of the valve, the internal occludent edge does not here present a flat striated ledge.

I must again repeat that I doubt whether the differences here pointed out are specific: I have seen nearly all such peculiarities variable in other species. I am, however, in some degree strengthened in leaving the P. gracilis distinct, by the supposition that it is the representative species in the true Chalk of the P. validus of the uppermost stage.

15. POLLICIPES DORSATUS.

POLLICIPES DORSATUS. Steenstrup. Kroyer's Naturhist. Tidsskrift, 1839, b. ii, h. iv, pl. v, figs. 27 and 30.

P. scutis crassis; ad formam trianguli æquianguli accedentibus; margine occludente externè costâ rotundatâ firmato; angulo baso-laterali latè truncato, dimidium longitudinis marginis basalis veri, æquante;

[page] 70 FOSSIL CIRRIPEDIA.

††. Scuta, aut longitudinaliter aut transversè (i. e. secundum lineas incrementi) costata.

16. POLLICIPES STRIATUS. Tab IV, fig. 5.

P. valvis longitudinaliter striatis: scutis sub-triangulis, margine tergo-laterali valdè arcuato et prominente; costâ obscurâ, rotundatâ, ab apice ad angulum baso-lateralem decurrente; internâ apicis superficie solidè repletâ, sulcus manifestus deest.

Valves longitudinally striated: scuta subtriangular, with the tergo-lateral margin much

tergo-laterali segmento ex lineis incrementi reflexis formato, angustissimo. Tergorum, costâ rectâ, latâ, proclivi ab apice ad angulum basalem decurrente; angulo basali scutum versùs, obliquè truncato.

Scuta thick, approaching to an equilateral triangle; occludent margin exteriorly strengthened by a rounded ridge; baso-lateral angle widely truncated, equalling half the length of the true basal margin; tergo-lateral segment formed by the upturned lines of growth, extremely narrow. Terga with a straight, broad, steep-sided ridge running from the apex to the basal angle, which latter on the scutal side is obliquely truncated.

Faxoe; Denmark. Mus. Univers., Copenhagen.

Professor Steenstrup has kindly sent for my examination a large series of scuta, terga, and carinæ, all from the same formation of Faxoe, and no doubt belonging to the same species.

All the valves are rather strong and thick; they are smooth, with the exception of the fine lines of growth. Scuta (fig. 4f, nat. size, in a reversed position compared with the other figures,) triangular, with the baso-lateral angle largely truncated; considerably convex; breadth, nearly equalling three fourths of length; apex acuminated, slightly curved towards the terga. Occludent margin nearly straight, forming an angle considerably less than a right angle with the basal margin; this latter is short and nearly straight; the tergo-lateral margin is just perceptibly concave; a very narrow slip is formed along this margin by upturned lines of growth; this margin, if produced, would meet the basal margin produced, at a less angle than the occludent margin does. The baso-lateral angle is so largely truncated that the side so formed is half the length of the proper basal margin, which it meets at a very large angle; it is doubtful whether it should be called part of the basal, or of the tergo-lateral margin; it touches, I suspect, exclusively the latera, but in comparison with the other valves of this genus I do not think it corresponds with the ordinary tergo-lateral margin. Externally there is a slightly depressed line running from the apex parallel and near to the occludent margin, causing this edge of the valve to appear convex and protuberant; two slight ridges also run from the apex—one to the angle uniting the basal and the above-described truncated margin, and the other line, which is rather fainter, runs down the valve half way between the first line and the occludent margin. Internally, there is a deep, upwardly pointed pit for the adductor muscle; the internal occludent edge keeps the same width up to the apex; the internal tergal margin has no furrow, but is slightly indented, and must have, to a certain extent, overlapped the thin edge of the terga, and thus partly locked the valves together.

Terga (fig. 4, d, e), rhomboidal, much elongated, almost flat; occludent and upper carinal margins (meeting each other at less than a right angle) much shorter than the lower carinal and scutal margins. From the apex to the basal angle, down almost exactly the middle of the valve, a flat-topped ridge, either absolutely straight or nearly so, runs, and widens considerably in its downward course; its carinal side is steep, its opposite side less so; the oblique end of this ridge forms the basal angle, which is nearly, but not exactly parallel to the upper carinal margin. There is no depression parallel to the occludent margin.

Carina (fig. 4, a, b, c) much elongated, very slightly bowed inwards; transversely, arched flatly; barely sub-carinated; basal margin almost rectangularly protuberant. Apparently, a full upper half of the carina projected freely; this part is filled up flat and solid (c); a rather wide inner margin of the carina extending

[page] 71 POLLICIPES.

arched and protuberant; an obscure rounded ridge runs from the apex to the baso-lateral angle; apex with the internal surface filled up solid, without any distinct furrow.

Upper Chalk, Norwich. Mus. Fitch.

My materials consist of two scuta, of which one is young; and of some terga and a carina which I provisionally here describe.

Scuta (fig. 5, c), broad, moderately convex; rather thick and strong; surface strongly ribbed from the apex to the basal margin; ribs rather broad: apex much acuminated; occludent margin nearly straight, at right angles to the basal margin, as is also the lower part of the tergo-lateral margin; the upper part of this latter margin is inflected. A broad, very slightly prominent ridge runs from the apex to the baso-lateral angle, which is broad and rounded, but not prominent. There is no second ridge from the apex to the basal margin, but along the line where such occurs in P. glaber, the valve is rather abruptly arched; and in the younger specimens, a distinct trace of a ridge can be seen. Internally, the pit for the adductor muscle is conspicuous; the whole upper part of the valve is filled up and rendered solid; the internal occludent edge does not widen above the adductor pit; on the tergal margin a wide internal ledge is marked by lines of growth, is slightly concave, irregular, but not furrowed; on its surface, however, in the larger specimens, there is, some little way below the apex, a small ridge and linear hollow, which probably affected, in some peculiar way, the shape of the terga; but I doubt whether this structure is constant. In general external aspect, this valve comes nearest to the Scalpellum arcuatum; but its tergo-lateral margin not being angularly bent, its baso-lateral angle not being prominent, and the greater width of the ridges easily serve to distinguish it.

Terga (fig. 5, b; in a reversed position compared to the other figures). Mr. Sowerby has figured a tergum in the ' Mineral Conchology,' Plate 606, fig. 1, under the name of P. sulcatus, from the Upper Chalk, and I have had given me by Mr. Woodward a second specimen from the Upper Chalk of Norwich. From reasons stated under my description of Scalpellum maximum, var. sulcatum, I do not think it can belong to that species; and from one trifling character, namely, the kind of ridge running from the apex to the basal angle, most likely it belonged to a Pollicipes; and as only one species in the Norwich beds is as yet known to be ribbed longitudinally, I believe that I have rightly attributed this valve to P. striatus.

almost to the base, is marked by lines of growth, showing that the valve rather widely overlapped the terga. Amongst the specimens there is one very narrow valve, curled a little laterally as well as inwards; I believe it to have belonged to a young and injured or monstrous individual.

Affinities. The P. dorsatus, though most readily distinguished from the P. elegans of the same Faxoe formation, by the absence of ridges on the valves parallel to the lines of growth, and likewise by the absence of a strong ridge, running from the apex to the baso-lateral angle of the scuta, certainly has a considerable affinity to it, as is particularly manifest in comparing the terga of the two species; in the scuta of P. elegans (fig. 9 c) the truncated end of the oblique wall-sided ridge is obviously analogous with the broad truncated baso-lateral angle in P. dorsatus. This species is also related, as we have seen, to P. validus, and P. gracilis; again, also, it is related to the tertiary P. carinatus, and through it remotely to the recent P. mitella.

[page] 72 FOSSIL CIRRIPEDIA.

Valve much elongated, sub-rhomboidal; whole surface rather plainly ribbed longitudinally. A larger rounded ridge, with the surface of the valve depressed on the carinal side of it, runs in a slightly curved line, at about one third of the entire width of the valve from the carinal margin, down to the sharp basal angle. Apex narrow, much produced: occludent margin about equal in length to the scutal margin: upper and lower carinal margins almost running into each other. Parallel to the occludent margin, the valve is depressed, with a raised plait in the middle of the depression. Except in the more elongated form, and in the character of the ridge running from the apex to the basal angle, this valve is barely distinguishable from the tergum of S. arcuatum (with its varieties) found in the Chalk Marl and Gault.

Carina (fig. 4, a). In Mr. Tennant's collection there is a carina from the Chalk of Kent, different from any other seen by me, and which, from being plainly ridged, or rather furrowed longitudinally, I provisionally describe here. Valve thin, triangular, moderately tapering; very slightly bowed inwards; transversely, very flatly arched; plainly subcarinated; lateral edges narrowly and much inflected; basal margin rectangularly pointed. A very small portion of the valve projected freely. The internal concavity of the valve is angular, instead of, as usual, being rounded. The whole exterior surface, except close on each side of the central ridge, is longitudinally furrowed.

17. POLLICIPES SEMILATUS. Tab. IV, fig. 6.

P. valvis longitudinaliter et transversè costatis: scutorum margine basali brevi, recto, cum margine occludente angulum rectum formante; costâ, parietali,1 tenuissimâ ab apice ad angulum prominentem basi-lateralem decurrente; hæc valvam in duas partes inæquales dividit, è quibus portio tergo-lateralis latior est.

Valves longitudinally and transversely ridged; scuta with the basal margin short, straight, forming a rectangle with the occludent margin; a very narrow wall-sided ridge runs from the apex to the prominent baso-lateral angle, and divides the valve into two unequal portions, of which the tergo-lateral portion is the broadest.

Chalk Detritus, Charing, Kent. Mus. Harris.

General Remarks. I know this species only from one minute broken scutum (.15 of an inch in length), with its surface somewhat disintegrated; but it is certainly distinct from the other species hitherto described. The Chalk detritus at Charing is derived from the upper and lower Chalk and Chalk Marl.

Scutum; the surface is marked by narrow, square-edged, longitudinal ridges, placed rather distant from each other; each zone of growth appears (for the surface is much disintegrated) to have had a prominent plait or ridge which, consequently, runs in lines transverse to the longitudinal ridges. The upper part of the valve is only moderately

1 Parietali, i. e. lateribus utrinque perpendicularibus.

[page] 73 POLLICIPES.

pointed: the basal margin is short and straight; it forms, with the occludent margin, a right angle, and with the lower part of the tergo-lateral margin, an angle rather above a right angle. A quite narrow ridge, having perpendicular sides, only about twice as wide as the other ridges, runs in a slightly curved course from the apex to the baso-lateral angle; at which angle the ridge, as it appears, must have formed a projection. The tergo-lateral portion of the valve, formed by the upturned zones of growth, is unusually broad, rather exceeding in width the rest of the valve; so that the ridge, running from the apex to the baso-lateral angle, divides the valve into two only slightly unequal portions, of which the tergo-lateral portion is the broadest. Internally, the upper part, above the pit for the adductor muscle, is along the middle, slightly prominent; on the tergal side, barely furrowed, and on the occludent side, slightly hollowed out. This species is allied to the three following species, and is, in some respects, intermediate between them and P. striatus.

18. POLLICIPES RIGIDUS. Tab. IV, fig. 7.

POLLICIPES RIGIDUS. J. Sowerby. Trans. Geolog. Soc., 2d series, vol. iv, 1836, pl. xi, fig. 6* (carina et scuta).

P. valvis transversè costatis: scutorum margine basali recto, cum margine occludente angulum recto majorem formante; costâ angustissimâ, parietali, ab apice ad angulum baso-lateralem decurrente: tergis, costâ curvâ, parietali, ad angulum basalem decurrente instructis; apice basali in prominentiam parvam terminante, lateribus prominentiæ parallelis.

Valves transversely ridged. Scuta with the basal margin straight, forming above a right angle with the occludent margin; a wall-sided, very narrow ridge runs from the apex to the baso-lateral angle. Terga with a curved, wall-sided ridge running to the basal angle, which latter terminates in a little, parallel-sided projection.

Gault: Folkstone and Maidstone, Kent. Eastweare Bay, Sussex. Mus. J. Sowerby, Bowerbank, Brit. Mus., J. Morris, Flower.

General remarks. This species appears rather common. I have scuta, terga, and carinæ, which I infer without hesitation belong to the same species, from the similarity of their peculiar surfaces, and from their having been found frequently at the same place and in the same formation.

Description. All the valves have their surfaces conspicuously marked with sharp, narrow, steep-sided prominent plaits parallel to the lines of growth; each periodical zone of growth seems to have been completed by the formation of one of these projecting plaits; the interspaces between the plaits, both on the scuta and carina, are either smooth, or more or less plainly fluted with fine longitudinal ridges; these apparently are in some instances

k         

[page] 74 FOSSIL CIRRIPEDIA.

only rendered visible or prominent by disintegration; the transverse plaits are also rendered more prominent by disintegration.

Scutum (Tab. IV, fig. 7, d, f) elongated, triangular, but with the baso-lateral corner produced; convex, with the upper part almost semi-conical; apex much pointed, and curved towards the carina; occludent margin considerably arched; basal margin short, forming, with the occludent margin, an angle considerably above a rectangle, and therefore causing the baso-lateral angle to be much produced. The tergo-lateral margin is in the upper part slightly concave, in the lower part rounded and protuberant. The baso-lateral angle is broad and rounded, but with a small, central, square-sided prominence, formed by the projection of the ridge running from this angle to the apex. This ridge is very conspicuous, it is narrow, being not above one third of the width of an average zone of growth, increasing very little in width downwards; it is wall-sided, that is, has its sides absolutely perpendicular; its summit is surmounted by transverse plaits, really continuous (but not at first appearing so) with those on the surface of the valve on both sides of it. This ridge runs in a curved line, nearly parallel to the occludent margin. Internally (f), the occludent edge is broad and flat, and is marked with lines of growth; it becomes wide at the apex; there is a rather deep furrow close to the tergal margin, but there is no trace of a central ridge; the pit for the adductor muscle lies quite close under the furrow and flat occludent edge; the nearest approach to this structure of the under side of the apex of the scuta, is in the P. glaber.

Terga (fig. 7, e). On this valve the plaits, in specimens which have not undergone any disintegration, are much less strongly pronounced than on the scuta and carina; in shape, sub-rhomboidal, not quite flat; a curved, wall-sided, narrow ridge (like that on the scutum) runs from the pointed, slightly curved apex to the sharp basal angle, and itself projects as a little point, with parallel sides; the growth-plaits extend across this ridge, which runs at about one third of the entire width of the valve from the carinal margin. The upper carinal margin is very slightly longer than the lower carinal margin, with which it is almost blended by a continuous curve. The occludent is shorter than the scutal margin; the edge of the shell close to the former is rounded and protuberant, and parallel to this rounded edge the valve is slightly depressed, and correspondingly slightly hollowed out on the scutal margin; internally there are lines of growth along the upper carinal and occludent margins. Carina (fig. 7, a, b, c) widening rather slowly from the apex to the base; almost semi-cylindrical; very slightly bowed inwards; not in the least carinated; basal margin not at all protuberant. The transverse plaits are, in the three specimens which I have seen of the carina, undulatory; on the very narrow lateral margins (b) the plaits are obliquely upturned. The upper part of the carina projected freely; this part, and both margins, are internally marked by lines of growth.

Dimensions. Most of the specimens are rather small, but I have seen one tergum seven-tenths of an inch in length.

Affinities. This species, with the two following P. fallax and elegans, form a little group

[page] 75 POLLICIPES.

closely related to each other, and in a far less degree to P. dorsatus. Some remarks on their diagnostic characters will be given under the two following species. All three species are remarkable by the peculiar form of their scuta, which have so much resemblance (especially in P. rigidus) to the terga of other cirripedes, that until I examined their under surfaces I was not sure which valves they were. The conspicuous ridges running obliquely downwards from the apices of the scuta and terga, I have little doubt were due to the carina and rostrum largely overlapping these valves, and to the presence of large upper latera, so that the lower angles of the scuta and terga were closely wedged between these valves.

19. POLLICIPES FALLAX. Tab. IV, fig. 8.

P. valvis transversè costatis: scutis, margine basali non recto, angulum pæne rectum cum margine occludente formante; costâ, parietibus obliquis, ab apice ad angulum baso-lateralem decurrente: tergis, costâ curvatâ, parietibus obliquis, ad angulum basalem latum, rotundatum, decurrente.

Valves transversely ridged. Scuta, with the basal margin not straight, forming nearly a right angle with the occludent margin; a ridge having sloping sides runs from the apex to the baso-lateral angle. Terga, with a curved ridge having sloping sides, runs to the broad, rounded basal angle.

Upper Chalk, Norwich. Mus. Fitch. Maëstricht Formation, Balsberg and Kopinge, Scania. Mus. Univ. Copenhagen. Oberer Kreidemergel (Upper Chalk), Gehrden in Hanover. Mus. Roemer.

The specimens which I have seen, consist of three right-hand scuta and one tergum, in the possession of Mr. Fitch, from Norwich; of two scuta and two terga collected by M. Angelin, in Scania, and forwarded to me by Professor Steenstrup, and of a scutum from Hanover, sent to me by Roemer, together with specimens of his P. uncinatus.

Description. The valves are moderately thick; they are conspicuously marked with rather wide prominent ridges, forming the basal edges of each zone of growth; they seem in both scuta and terga most strongly developed near the occludent margins.

Scuta (fig. 8, a) almost triangular, moderately convex; occludent margin considerably arched in the upper part, and bowed towards the terga; basal margin not straight, with a short portion close to the rostral angle forming a rectangle with the occludent margin; the remaining portion, if produced, would form a rather larger angle with it; hence the baso-lateral portion of the whole valve is somewhat protuberant. The tergo-lateral margin is in the upper part slightly hollowed out, and in the lower part almost straight. A very slightly curved ridge runs from the apex to the baso-lateral angle, which is broad, rounded, and not prominent; the ridge has sloping, not wall-like sides. Internally the structure of the upper part closely resembles that of P. rigidus. The furrow on the tergal side is rather

[page] 76 FOSSIL CIRRIPEDIA.

narrower, and a central portion of the inner occludent margin (marked with lines of growth) here forms a slightly prominent ridge. In one of the three specimens, the baso-lateral portion of the valve was considerably more produced than in the other two. Terga (fig. 8, b), rather broad, considerably convex; apex pointed, and much curled towards the scuta; upper carinal margin unusually arched, slightly longer than the lower carinal margin; there is a deep depression parallel to the occludent margin, which is itself rounded, protuberant, and considerably shorter than the scutal margin. A curved ridge, projecting up above the general surface of the valve, with sloping sides, runs from the apex to the basal angle, which latter is broad and rounded; the ridge runs down nearly the middle of the valve.

Dimensions. Length of longest scutum .65 of an inch.1

1 20. POLLICIPES ELEGANS. Tab. IV, fig. 9.

P. valvis longitudinaliter et transversè striatis: scutorum margine basali recto, cum margine occludente angulum recto paulo majorem formante; costâ parietali, latiore quam pro solitâ incrementorum latitudine, ab apice ad angulum baso-lateralem decurrente: tergorum costâ parietali, rectâ, ad apicem basalem, acuminatum decurrente.

Valves longitudinally and transversely striated. Scuta with the basal margin straight, forming an angle rather above a rectangle with the occludent margin; a wall-sided ridge, which is broader than the average width of the zones of growth, runs from the apex to the baso-lateral angle. Terga with a straight, wall-sided ridge running to the pointed basal angle.

Maestricht Formation, Faxoe, Denmark. Ignaberga, Scania.

I am indebted to Professor Steenstrup for an examination of three scuta, a tergum and two carinæ, firmly embedded in the fragmentary coral-rock of Faxoe, and of two very fine scuta from Scania, collected by M. Angelin. The valves have each zone of growth raised into a ridge like the roof of a house; the interspaces between these ridges are marked by longitudinal striæ. Length of largest scutum 1.1 of an inch.

Scuta (fig. 9, c), with the apex acuminated, much curved towards the terga; occludent margin either slightly or much arched; forming an angle rather above a right angle with the straight basal margin; tergo-lateral margin slightly (but to a variable degree) hollowed out in upper part, and nearly straight in the lower part, where it forms nearly a right angle with the basal margin. Baso-lateral angle generally very broad, rounded, almost obliquely truncated. From the apex to this angle a gently curved, broad, wall-sided ridge runs, which very perceptibly widens in its downward course; it is generally wider than the average width of each zone of growth. Internally the occludent margin is very wide, flat, and marked with ridges; the pit for the adductor muscle is deep.

Terga (fig. 9, d) broad, rhomboidal, slightly convex; basal angle apparently (for specimen is broken) blunt, and obliquely truncated; upper carinal and occludent margins nearly straight; shorter than lower carinal and scutal margins; valve considerably depressed in a line parallel with the occludent margin, close to which the margin itself is convex and arched. The wall-sided ridge which runs from the apex to the basal angle is straight, (not quite correctly represented at d), and widens considerably in its downward course: it is not so wide proportionally to the whole valve as the ridge on the scuta, for it is here only a little above half as wide as the average width of each zone of growth; it runs at about one third of the width of the entire valve from the carinal margin: the plaits cross its summit in a course not exactly corresponding with those on the valve on each side of it; probably this ridge projected and formed, as in P. rigidus, the basal point of the valve.

Carina (fig. 9, a, b) imperfect, elongated, that is, tapering gradually downwards from the apex; some-

[page] 77 POLLICIPES.

Species aliquot quas, scutis incognitis, auctores a valvis insignibus nominârunt, hìc pro tempore solummodo iterum describuntur.

Species named by authors from remarkable valves, but their scuta being unknown are here only provisionally re-described.

21. POLLICIPES BRONNII. Tab. IV, fig. 10.

POLLICIPES BRONNII. F. Roemer. Verstein. Norddeutschen Kreidegebirges, p. 103, Tab. xvi, fig. 8.

P. carinâ lævi, subcarinatâ, margine basali arcuato et turgido; totâ valvâ vel extrorsùm arcuatâ vel pæne rectâ; internè, costis duabus elevatis ad utrumque latus partis superioris liberè prominentis.

Carina smooth, subcarinated; basal margin arched and protuberant; whole valve either outwardly bowed or nearly straight. Internally, the upper, freely-projecting portion, has on each side a prominent ridge.

Upper Greensand, Warminster, England. Mus. J. Tennant. Hils-conglomerat bei Essen. Mus. Univers., Copenhagen.

My materials consist of some specimens lent me by the kindness of Professor Steenstrup; they consist, as well as those described by Roemer, only of the carina; their surfaces are considerably worn. The Hils-conglomerat of Essen is considered by Roemer as the equivalent of one of the lower beds of the Lower Greensand; but recently MM. Saemaan and Geinitz have shown that it really corresponds with the Upper Greensand. Professor Tennant has lent me a single broken carina from Warminster, which cannot, in our present state of knowledge, be specifically separated from the typical continental specimens, though, as we shall see, slightly differing from them.

I will first describe the foreign specimens.

Carina (Tab. IV, fig. 10) strong, massive, triangular, about twice as high as broad; but

what bowed inwards; basal margin not in the least protuberant; not carinated, but steeply convex, so that a section of the base (b) has steeper sides than a semi-circle.

Diagnostic characters. In comparing the scuta of P. rigidus, fallax, and elegans, the latter can be at once distinguished from P. fallax by the ridge running from the apex having perpendicular or wall-sides, and by the straightness of the basal margin; from P. rigidus, by the ridge being much broader; P. fallax differs from both, in the absence of longitudinal striæ. In the terga, P. elegans differs from both P. rigidus and fallax, in the ridge running from the apex to the basal angle being straight, and in its greater breadth, and likewise in the shortness of the upper carinal margin. The terga of P. fallax differ from the homologues of the other two species, in the ridge connecting the upper and lower points, not having perpendicular sides.

[page] 78 FOSSIL CIRRIPEDIA.

the breadth varies with respect to the height; sub-carinated, slightly bowed outwards or backwards, and therefore, in the opposite direction to what is usual; but the amount of curvature varies much: roof arched, inflected along the lateral edges; basal margin protuberant, formed of two curved lines meeting each other at an angle of above 90°. The lines of growth on the inflected lateral edges, curve slightly downwards (b), and then just perceptibly upwards; thus, no doubt, making the heels or two basal corners slightly prominent. Internally, within the lateral edges (having the lines of growth as just described), and separated from them by a distinct indentation, there is on each side (b) a narrow ridge, widest at about the middle of the upper half of the valve, and marked with longitudinal lines of growth; these internal lateral ridges have evidently been (as seen in the section) (d) formed during the filling up and thickening of the upper, solid, outwardly bowed part of the carina, which part, no doubt, projected freely. The lower part of the carina (c) is deeply concave. Roemer describes the exterior surface of the shell as marked with alternate finer and stronger concentric lines, and rarely along the edges alone with longitudinal lines.

The specimens from the Upper Greensand of Warminster differ from the foreign specimens, in being very slightly bowed inwards instead of outwards, and in having a more tapering form; but it is precisely in these two respects, that the four foreign specimens seen by me vary to a considerable extent; therefore, at present, the English specimens must be ranked under P. Bronnii.

These valves certainly differ considerably from any other known ones: the slight outward bowing of the carinæ from the Hils-conglomerat is their most conspicuous character, and was present in the four specimens seen by me, and I presume, from Roemer's description, is general. In recent species, however, the degree of curvature of the carina is often variable: in P. spinosus, I have seen some specimens with the upper part of the carina even outwardly bent, and others with it straight. The manner in which the upper part of the valve has been filled up, having two lateral, inwardly projecting ridges, is unlike any other species, and is the main specific character: the carinæ of Scalpellum solidulum and of the var. cylindraceum of S. maximum make the nearest approach to this structure. From such scanty materials I will not pretend to say to what species this is most closely allied.

22. POLLICIPES PLANULATUS. Tab. IV, fig. 11.

POLLICIPES PLANULATUS. J. Morris. Annals of Nat. Hist., vol. xv, 1845, pl. 6, fig. 2.

 — — J. Sowerby. Min. Conch., pl. 647, fig. 2.

P. tergis subrhombicis, latis, lævibus, apice basali latè truncato, latitudine dimidium longitudinis marginis occludentis æquante; apice basali truncato angulum rectum cum margine scutali formante; parte superiori marginis scutalis cuspidem latam, rotundatam, læviter prominentem formante.

[page] 79 POLLICIPES.

Terga subrhomboidal, broad, smooth, with the basal angle widely truncated, and equalling in breadth half the length of the occludent margin; the basal truncated side forms a right angle with the scutal margin: the uppermost part of the scutal margin forms a broad, rounded, slightly projecting point.

Oxford Clay; Christian Malford and Chippenham, Wilts. Mus. J. Morris.

This species has been named by Mr. Morris, as it appears to me, from the terga alone, which are well figured by him and by Mr. Sowerby: these valves (an inspection of two of which from Chippenham, I owe to the kindness of Mr. Morris,) are certainly quite distinct, in the extent to which the basal angle is truncated, and in the degree of projection of the uppermost part of the scutal margin, from any others which I have seen; but had they not been already named, according to the rule followed here, they would have been passed over.

Terga subrhomboidal, or strictly pentagonal, rather broad, very flat and thin; basal angle truncated, extraordinarily broad, equalling half the length of the occludent margin, at right angles to the scutal margin; no single distinct ridge, or furrow, runs from the apex to the broad basal angle: upper and lower carinal margins nearly equal in length: occludent and upper carinal margins meet each other at right angles: occludent margin rather shorter than the scutal margin; with the uppermost portion of the latter slightly projecting in a blunt, rounded point, which corresponds with a just perceptibly convex slip of valve, extending along the occludent margin in the manner so common in this genus. Internally, the surface is smooth; scarcely even the smallest part of the apex could have projected freely.

Largest specimen nearly a quarter of an inch in length.

[Published species of Lepadidæ of a doubtful nature, owing to valves, not typical, having been named, or from the specimens having been imperfect, or from the shortness of the descriptions.]

Anatifera turgida. Professor Steenstrup (in Kroyer's Tidsskrift, 2 B. (1839), Pl. V, figs. 4-5,) has thus named some valves from Scania: he states that the scuta resemble in their growth those of Cineras, or his Anatifera cretæ, that is the Scalpellum? cretæ of this work. Therefore, I conclude that these valves cannot properly be ranked under Anatifera or Lepas.

Anatifera convexa. Roemer, Norddeutsch. Kreidegebirges, Tab. XVI, fig. 7. I do not consider the evidence nearly sufficient to place the valve here described in the genus Anatifera; it might be one of the lower Latera of a species allied to Pollicipes glaber or unguis. Pictet (Traité Elementaire de Paléontologie, Tom. III, p. 438) states that the specimen in question is Aptychus cretaceus. Several vague notices of fossil species of Anatifera or Lepas have appeared at various times, but they hardly seem to deserve notice.

[page] 80 FOSSIL CIRRIPEDIA.

Pollicipes angustatus Geinitz (Die Verstein. von Kieslingswalde des Sächsisch-bohmischen, Kreidegebirges, 1843, Tab. IV, fig. 10) is almost certainly a Scalpellum, and probably a new species; the carina is narrow, bowed inwards, with the basal margin sharply pointed; tectum carinated, separated from the parietes by a line or ridge, which is said to be enclosed between two fine furrows; this latter seems to be its most singular character. I cannot make out whether it has intra-parietes; only a single view is given: found at Strehlen, Saxony, in Pläner-Kalke (chalk-marl), and, according to the same author, in his 'Das Quadersandsteingebirge" (p. 100); likewise in Greensand, at Essen, in Westphalia.

The Pollicipes lævis of J. Sowerby, figured in 'Geological Transactions,' 2d series (1836), Vol. IV. Pl. XI, fig. 5, I consider the same as his P. unguis, fig. 5*; but the P. lævis, from Blackdown, Pl. XVI, fig. 1, seems to be certainly a distinct species, and possibly a Scalpellum: no details are given. The P. radiatus of the same author, of the lower greensand (Pl. XI, fig. 6), is unknown to me; the tergum figured is like that of S. arcuatum; the upper valve, if a scutum, is very remarkable.

The name Pollicipes radiatus has been a favorite with authors; there is a tertiary species so called, but not described in 'Müller's Jahrbuch,' 1835. Koch and Dunker, also, (Norddeutsch. Oolithgebildes, 1837,) have given this name to a tergum found, according to Roemer, in the Hilsthon or Lower Greensand; I conceive it to be scarcely possible, and very inconvenient, to attach names to terga.

Michelotti has called, without any description ('Bulletin, Géolog. Societé,' tom. 10, p. 140), a tertiary Pollicipes from near Turin, P. antiquus,—a most infelicitous name for a miocene species.

Roemer in his 'Die Versteinerungen des Norddeutsch. Kreidegebirges,' 1841, has figured, Pl. 16, fig. 13, the above-mentioned P. radiatus, of Koch and Dunker; also, Pollicipes asper (Pl. 16, fig. 15), which is founded on a fragment of a carina, which I have been permitted to inspect by the great kindness of Roemer; it is not sufficiently perfect in the upper part to show whether it probably belonged to Scalpellum or Pollicipes, but apparently to the latter genus; it is almost certainly distinct from anything which I have seen; the tectum is very flatly arched, and the basal margin (as inferred from the lines of growth) scarcely at all protuberant; it was very slightly bowed inwards; its surface is covered with faint longitudinal ridges, and these are crossed by concentric, leaf-like, projecting lines of growth. The longitudinal ridges cause this valve to resemble that of Scalpellum solidulum from Scania, but the basal margin is much less protuberant, the tectum more steeply arched, and the whole valve thicker than in that species. The P. asper comes from the " Oberer Kreidemergel" (Upper Chalk) of Quedlinburg, in Westphalia.

Roemer has also described in the same work (Pl. XVI, fig. 10, a, b, c,) Pollicipes uncinatus from the Upper Chalk: the carina (b) has its roof sharply carinated; its parietes are quite flat, and I presume rectangularly inflected, which makes me suppose it may have belonged to a Scalpellum; basal margin rectangularly pointed. The valve, described as a tergum (c) I have had, through the kindness of Roemer, an opportunity of examining; it cannot, I conceive, be a tergum; it is unknown to me; it appears to be a carinal latus; if so, the valve ought to have been placed in the figure transversely to its present position.

Reuss in Die Verstein. der Bohmischen Kreideformation (1845) has figured (Tab. V, fig. 43) a carina, under the name of Pollicipes conicus, from the Chalk; I do not consider it to be recognisable. The P. glaber in this same work (Tab. V, fig. 45-49, and Tab. XIII, fig. 86-91) appears to consist of several species; on the other hand, P. radiatus (Tab. V, fig. 42) appears to be a scutum of the true P. glaber.

Dr. W. Dunker (Palæontographica: Beitrage zur Naturgeschichte, &c., der Vorwelt von Dr. W. Dunker,

[page] 81 LORICULA.

and H. Von Meyer, 1848, 1 Band, p. 180, Tab. XXV, fig. 14) has described and figured a valve of Pollicipes liasinus: he considers it as one of the great hinder lateral valves—that is, a tergum. This eminent palæontologist is well acquainted with the cirripedia, and is therefore probably right in his determination; but I am forced to say that the manner of growth seems to me, if I rightly understand the figure, unlike that of the terga in any known Pollicipes.

Müller (Aachen, p. 43, Tab. II, fig. 16,) has described Pollicipes ornatissimus; the valve figured is a carina, I believe, of Scalpellum maximum.

POLLICIPES ———. J. Sowerby. Geolog. Transact. 2d series, vol. v, pl. ix, fig. 2.

The specimens here figured by Mr. Sowerby, were found by Mr. Wetherell in a deep well in the London Clay, at Hampstead, together with portions of Scalpellum quadratum. The specimens are in a broken condition, and have been kindly lent me by Mr. Wetherell: they consist of some fragments of terga, and I believe of the basal portion of a scutum, of a carina, and of several latera. The species appears to have come near to the Eocene P. reflexus; but although thinking it distinct, I dare not, considering the imperfect state of the scutum, name it. The valves appear to have been much thicker and more rugged than those of P. reflexus; the basal angle of the terga sharper, and the rostral angle of the scutum more abruptly truncated. The latera are remarkable, and unlike anything which I have seen; they present several shapes; they are all more or less triangular, and their lateral edges are more or less distinctly bordered exteriorly by prominent ridges; one has a central exterior ridge, and its basal margin is protuberant; another has one of its sides at right angles to the basal margin, and the other side largely convex. Not having seen the lower latera of the P. reflexus, or indeed of any fossil Pollicipes except of P. glaber and unguis, I cannot use characters drawn from the latera as diagnostic. The specimens are extremely small.

Genus—LORICULA.

LORICULA PULCHELLA. Tab. V, figs. 1-4.

LORICULA PULCHELLA. G. B. Sowerby, jun. Annals of Nat. History, vol. xii, 1843, p. 260.

L. capitulo decem (fortasse) valvis instructo. Pedunculo seriebus decem squamarum lævium calcarearum instructo; sex lateralibus multum transversè elongatis; quatuor terminalibus angustis; secundùm pedunculi margines rostralem et carinalem decurrit sutura medialis recta, squamis non intersecantibus.

Capitulum with (perhaps) ten valves. Peduncle with ten rows of smooth calcareous scales, of which the six lateral rows are much elongated transversely, and the four end rows narrow; along the rostral and carinal margins of the peduncle there is a straight medial suture, with the scales not intersecting each other.

Lower Chalk, Cuxton, near Rochester, Kent. Mus. Wetherell.

I owe to the kindness of Mr. Wetherell an examination of this beautiful and unique specimen, well described and figured by Mr. G. B. Sowerby, Junr., in the 'Annals of

l        

[page] 82 FOSSIL CIRRIPEDIA.

Natural History.'1 I believe the specimen to be extremely incomplete; certainly only one side of the capitulum and peduncle is preserved; but on this subject I shall offer a few remarks after describing the specimen in its present state. The specimen was embedded outside the cast of an Ammonite: Mr. J. Morris informs me, that he has no doubt that the pit at Cuxton is worked in the Lower Chalk.

The Capitulum (Plate V, fig. 1, of nat. size,) consists of three left-hand valves, which are small compared to the size and width of the peduncle, making me believe that the greater part of the animal's body was lodged in the peduncle, as in the recent genera, Lithotrya and Ibla. Of the three valves, I believe from the general shape and direction of the lines of growth, that one (on the right-hand side of the figure) is the scutum; of the other two, I will at present call that nearest to the scutum the first latus, and the other the second latus. The three valves are of nearly equal size: they are very slightly convex, quite smooth, moderately thick, with the lines of growth fine and obscure.

Scutum (fig. 3) triangular, apex somewhat produced, and bowed over towards the latera: occludent margin slightly arched, forming an angle much less than a rectangle with the basal margin, which latter is at right angles with the margin, called in Pollicipes tergo-lateral. The lines of growth, in the lower part of the valve, are parallel to the tergo-lateral and basal margins; and as far as I could distinguish in the imperfect condition of of the valve, the valve is added to a little during the growth of the apex, so that the umbo is not situated at the uppermost point. In this important respect Loricula apparently resembles the Scalpellum magnum, tuberculatum and cretæ.

The first (so called) latus is nearly flat, triangular, with its apex on a level with that of the scutum; the scutal margin (lying close and rather over the edge of the scutum) is just perceptibly arched, and a very little longer than the other lateral margin: the basal margin is shorter than the two lateral margins; growth downwards.

The second (so called) latus (fig. 2) is triangular, of nearly the same shape with the last valve, with the inner basal angle a little produced; the outer margin is very slightly arched, and is shorter than the inner margin; the main growth is downwards, but the lines curl a little up and round the inner margin. The apex of the valve in its present position stands a little above the apices of the other two valves, and a wedge-formed open space separates the upper part of the two latera.

Peduncle: this has a most singular, elegant, loricated structure: it is wider than the capitulum in the present condition of the latter, and about four times as long. It is completely protected by large, smooth, calcareous scales, of which five rows are preserved; and I conceive there can be no doubt from the shape of the end rows, that there originally existed a corresponding series on the opposite side, making altogether ten rows. The base is sharply pointed, down to which the full complement of scales extends. In each row

1 Since Mr. Sowerby made his description, Mr. Wetherell has cleared away more of the Chalk, thus exposing a row of small scales at the carinal end of the peduncle, not seen by Mr. Sowerby.

[page] 83 LORICULA.

there are about twenty-one scales, their numbers obviously depending on the age and size of the individual. There is one more scale under the second latus (fig. 4, restored figure), than under the first latus, and one more under the first latus than under the scutum; hence the summit of the peduncle is obliquely truncated, being lowest at the rostral end: in this respect there is some resemblance to the genus Lithotrya. The scales in the three lateral rows resemble each other pretty closely in outline: they are transversely elongated, and are together about as wide as the three valves of the capitulum; they are much longer than the scales of either end row. The first row of these elongated scales lies directly under the scutum, and the other two under the two latera; so that the lines of junction of the three rows of peduncular scales, and of the three valves of the capitulum, correspond. The scales in the middle row are rather longer than those on either side of it, are pointed at both ends, and have their upper margin very flatly arched and almost square-edged. The scales in the row under the second latus are rather wider than it, projecting (which is important) beyond its outer edge; their upper margins are square-edged; their outer ends blunt and truncated; their inner ends pointed. The scales of the third row under the scutum are rather less wide than it, and do not reach so far as its outer or rostral angle; their upper margins are arched; their outer ends bluntly rounded, and their inner ends pointed.

The two end (that is, the rostral and carinal) rows of narrow scales remain to be described: those at the rostral end (fig. 3) are as high as the larger lateral scales, but only about one fourth as wide: in shape they are almost a rectangular oblong, with their upper ends a little rounded, and the outer (with respect to the longitudinal axis of the animal) basal angle a little produced; hence the two lateral margins of the scales of this rostral row do not quite match each other; consequently, to make the animal symmetrical, there must have been a corresponding approximate row of small scales on the other side of the medial line. The straight inner (both sides of the peduncle being supposed to be present) edges of the scales of the row just described, extend rather beyond the occludent margin of the scuta. The scales in the carinal row, at the opposite end of the peduncle, are not above half the width of those of the rostral row: they are of nearly the same shape, but their upper ends are more pointed, and their outer (with respect to the medial longitudinal axis of the animal) basal angles more produced; their straight inner margins projected considerably beyond the carinal edge of the second latera: it is more obvious in this case than in the rostral row, that there must have been a second adjoining row of small scales on the other side of the carinal medial line. The small scales of the carinal and rostral rows differ from the others in their inner (that is, close to the medial axis), basal angles, not crossing each other; so that the peduncle could have been divided in a medial rostro-carinal plane, without cutting through a single scale. Their outer basal angles, on the other hand, intersect the ends of the adjoining large lateral scales, like these latter intersect each other, the lines of intersection between them being straight and corresponding with the junctions (as already stated) of the scuta and

[page] 84 FOSSIL CIRRIPEDIA.

latera. The consequence of this arrangement is, that in the alternate whorls there are in one, four of the large lateral scales and none of the smaller end scales; and in the whorl, both above and below, only two of these large lateral scales, and four of the carinal and rostral scales; so that the alternate whorls (fig. 4) had an unequal number of scales, namely, four and six.

Growth.—New scales for the peduncle are formed round its upper edge, at the bases of the valves of the capitulum, the chief growth of which, as we have seen, is downwards: hence, we here have, as in other pedunculated Cirripedia, a principal line of growth round the summit of the peduncle. It can be seen that a new scale is first formed under the second latus, at the carinal end of the peduncle; and this agrees with the fact that there is one more scale in this row than in that next to it; and one more in the latter, than in the row under the scutum. I may mention, as in conformity with this fact, that in the development of the young of Scalpellum vulgare from the larval condition, the calcareous scales on the peduncle first appear under the carina.

Attachment.—With respect to the attachment, Mr. G. B. Sowerby seems to have felt great difficulty on account of the peduncle ending in so fine a point; but the peduncle of Scalpellum vulgare, when carefully dissected from the coralline to which it is attached, often ends in a much finer point, and is symmetrically attached to the branch by its narrow rostral margin. In Loricula, the attachment was probably by one lateral face of the lower part of the peduncle; for it is by no means unusual for the cement-stuff (even when proceeding only from the two original central orifices, where the prehensal antennæ of the larva may still be found) to encroach largely on the peduncle, and thus fix it down. The calcareous scales of Pollicipes, and the horny spines of Ibla, may often be found thus embedded and firmly fixed to the supporting rock; it is moreover possible, that in Loricula the cement was poured out of orifices, specially situated on one side of the peduncle, as takes place along the rostral margin in Scalpellum vulgare, and high up on both sides of the peduncle in Lepas fascicularis.

Dimensions.—Entire length of the specimen rather above one inch: width of widest part of the peduncle .6 of an inch.

On the probable condition of the Specimen when perfect.—I have already remarked that the three valves of the capitulum, and the five rows of scales on the peduncle, must have had an opposite series. I at first thought it extremely improbable that the animal should have been split so exactly down the middle; and I conceive, in most genera, as in the common Lepas, it would be quite impossible to effect this; but in removing the terga and scuta from one side of several specimens in Ibla and Lithotrya, it was difficult to prevent exactly half of the membrane of the peduncle (which in these genera is thin) being torn off with them. Mr. G. B. Sowerby, jun., also has remarked (Annals of Nat. Hist., 1843, p. 261), that, owing to the rostral and carinal rows of small scales not intersecting each other, the splitting of the specimen into halves along this plane would be much favoured. The inner edge of the so-called second latus could not have touched the inner edge of its

[page] 85 LORICULA.

fellow valve on the opposite side, inasmuch as two small peduncular scales were inserted between the ends of the larger peduncular scales, which of themselves projected beyond the edges of the second latera: to fill up this hiatus, I conceive there must have once existed a carina. For the same reason, I believe, but less strongly, that there also existed a rostrum. It may be observed that in the present condition of the specimen, the straight lines of intersection between the two outer large peduncular scales and the small rostral and carinal scales, do not correspond with junctions of any valves in the capitulum; but if, as in our imaginary figure (4), a carina and rostrum be added, the above two lines of intersection will correspond with junctions of valves in the capitulum; making altogether, on each side, in the capitulum four lines of junction, and in the peduncle four lines of intersection.

At present there is a wedge-formed open space between the first and second latera; and judging from the lifted up position (fig. 1) of the upper scales of the peduncle under the second latus, this interspace must originally have been a little larger. In order to complete the sack to receive and protect the animal's body, this interspace must have been closed either by a valve or by a membrane;—the latter supposition seems to me very improbable, considering the closely loricated condition of the whole exterior; consequently, I believe that on each side, a triangular valve with its apex downwards was wedged in between the two latera, and that these valves answered to the terga of other Cirripedes. On any other view, considering the high improbability of the entire abortion of the terga, we must conclude that either the first or second latus was a tergum, though of a totally different shape from that valve in every other pedunculated Cirripede; the other latus, moreover, would on such a view be a complete anomaly.

In the imaginary restored figure (fig. 4), the tergum has its normal shape and manner of growth. The first latus now answers to the upper latus in Scalpellum, but it is interposed to a quite unprecedented extent between the scutum and tergum. The second latus is on this view the carinal latus; and the rostral latus, always smaller than the carinal latus, and in S. quadratum and Peronii reduced to a very small size, is here quite aborted. A restoration, however, of this nature must always be very doubtful. Finally, I imagine that the Loricula was attached by the side of the lower part of its peduncle to some large shell or coral, and that a crab or some other animal tore off the upper side, and this subsequently being dropped, became embedded in the chalk; the corresponding valves with the addition of a carina, rostrum, and a pair of terga being left adhering to the surface of attachment.

Affinities.—In an animal so imperfectly known, it is useless to enter on this subject : I will only remark that the restored figure comes nearest to the genus Scalpellum; the recent S. ornatum has the scales on the peduncle even proportionally more elongated than in Loricula. The chief distinctive character of the genus, as at present imperfectly known, lies in the arrangement of the scales on the peduncle. In those species of Pollicipes, Scalpellum, and Lithotrya, in which the scales on the peduncle are symmetrically arranged,

[page] 86 FOSSIL CIRRIPEDIA.

each scale lies exactly between two scales in the whorls, both above and below: this is, in fact, the case with the large lateral scales in Loricula, but the ends of the scales in the same whorl, instead of, as is usual, quite or nearly touching each other, are here far removed from each other, so that each whorl is broken by wide open spaces. In the marked difference in size between the lateral scales and those in the two end rows;—in the latter scales not intersecting each other, but presenting a straight, medial, rostral and carinal suture;—and lastly, in each alternate whorl having a different number of scales, namely, four in one and six in the other, Loricula differs from every other known Cirripede.

[page 87]

INDEX.

[N.B.—The names in italics are either synonyms or doubtful species.]


Page
Alepas squalicola . . . . . .
13
Anatifa cancellata . . . . . 7
 " convexa . . . . . . 79
Anatifera cretæ . . . . . . 45
 " turgida . . . . . 79
Angelin, M., on fossils of Scania . . . 6
Antennæ prehensile of larva . . . . 13
Aptychus . . . . . . . 3
Attachment, manner of, in Cirripedes . . 13
Balanus carbonarius . . . . . 5
Calentica Homii . . . . . . 14
Carina, manner of growth of . . . 19
Clisia or Creusia, fossil . . . . 5
Corals, fossil, not inhabited by Cirripedes  . 5
Crustacea compared with Cirripedes . . 13
Dana, J. D., on the peduncle of Cirripedes . 12
Distribution of recent Cirripedes . . . 6
 " of fossil Cirripedes . . . 8
D'Orbigny, Alcide, on Aptychus . . . 3
Fitch, Mr., specimens collected by . .
6
Forchhammer, on the age of the beds of Scania . . 7
Gray, Mr. J. E., on the genus Scalpellum 3, 14
Homologies of the peduncle and capitulum .
13
Ibla, sex of . . . . . . . 16
Leach, Dr., on the genus Scalpellum .
3, 14
Lepadidæ . . . . . . . 12
Loricula pulchella . . . . . 81
Lovén, on the homologies of Cirripedia . . 13
Male Cirripedes . . . . . 15, 23
Meyer, on Aptychus . . . . . 4
Morren, on fossil Tubicinella . . . 5
Nomenclature of valves . . . . 9
Nomenclature, rules of . . . . . 47
Oken, on Mitella . . . . . . 47
Oxynaspis (genus recent) . . . . 45
Peduncle, homologies of . . . . 13
Petzholdt, on Balanus carbonarius . .
5
Pictet, on fossil Crustacea . . . . 7

Page
Pollicipes acuminatus . . . . . 56
   Angelini . . . . . 56
 " angustatus . . . . . 80
 " antiquus . . . . . 80
 " asper . . . . . . 80
 " Bronnii . . . . . 77
 " carinatus . . . . . 60
 " concinnus . . . . . 50
 " conicus . . . . . . 80
 " dorsatus . . . . . 69
 " elegans . . . . . 76
 " elongatus . . . . . 55
 " fallax . . . . . . 75
 " Genus of . . . . . 47
 " glaber . . . . . . 61
 " gracilis . . . . . 69
 " Hausmanni . . . . . 53
 " lævis . . . . 55, 65, 80
 " liasinus . . . . . 81
 " medius . . . . . . 26
 " maximus . . . 24, 26, 34
 " Nilssonii . . . . . 52
 " ooliticus . . . . . 51
 " ornatissimus . . . . . 81
 " planulatus . . . . . 78
 " politus . . . . . . 54
 " quadricarinatus . . . . 38
 " reflexus . . . . 58, 81
 " radiatus . . . . 40, 80
 " rigidus . . . . . . 73
 " semilatus . . . . . 72
 " solidulus . . . . . 42
 " striatus . . . . . 70
 " Sub-genera of . . . 3, 48
 " sulcatus . . . . . 26
 " uncinatus . . . . . 80
 " undulatus . . . . . 42
 " unguis . . . . . . 64
 " validus . . . . . . 68
 " villosus . . . . . . 14

[page] 88 INDEX.

  
Page
Roemer, work of . . . . . . 1
Rules of British Association . . . . 47
Scalpellum angustum . . . . . 37
 " arcuatum . . . . . 40
 " cretaceous species allied to S. magnum 21
 " (?) cretæ . . . . . 45
 " fossula . . . . . 24
 " Genus of . . . . . 13
 " hastatum . . . . . 37
 " lineatum . . . . . 35
 " magnum . . . . . 18
 " maximum . . . . . 26
 " maximum, var. cylindraceum .
33
 " maximum, var. sulcatum . .
34
 " ornatum . . . . 15, 23
 " quadratum . . . . . 22
 " quadricarinatum . . . . 38
 " rutilum . . . . 15, 23
 " semiporcatum . . . . 44
 " simplex . . . . . 39
 " solidulum . . . . . 42
 " Sub-genera of . . . 3, 15
 " trilineatum . . . . 38

Page
Scalpellum tuberculatum . . . . 43
 " villosum . . . . . 14
 " vulgare, sex of . . . . 16
Sexes, peculiarities of, in Scalpellum .
15, 23
Sowerby, G. B., on a fossil Anatifa . .
7
Sowerby, J. work of . . . . . 1
 " on the genus Xiphidium . .
15
Steenstrup, Professor, work of . . . 1
 " " on age of beds of Scania 7
 " " on P. solidulus . .
42
Stomapoda . . . . . . . 12
Stutchbury, Mr. on fossil Cirripedes . .
5
Thaliella . . . . . . . 15
Trigonellites . . . . . . 3
Tubicinella fossil . . . . . 5
Valves, nomenclature of . . . . 9
Verruca fossil in the chalk . . . . 5
Wetherell, Mr., on a well at Hampstead . .
22
Xiphidium, Genus . . . . . 15
 " angustum . . . . . 37
 " quadratum . . . . . 22
 " maximum . . . . . 61

[page break]

[page break]

TAB. I.

[In every case right-hand Scuta and Terga are figured; hence the occludent margins are always to the left-hand.]

Fig. 1. Scalpellum magnum:—fig. (a) natural size, the rest magnified twice.

(a) Imaginary restored figure, of natural size.

(b) Carina, dorsal view.

(c) Scutum.

(d) Tergum.

(e) Upper latus.

(f) Carina, lateral view.

(g) Rostral latus, narrow variety.

(h) Rostral latus, inside view of, broad variety.

(i) Ditto, outside view of, narrow variety.

(k) Ditto, seen in profile.

(l) Carinal latus, outside view.

(m) Ditto, inside view.

(n) Ditto, outside view, broad variety.

Fig. 2. Scalpellum angustum:—carina, dorsal and lateral views of, copied from Dixon's 'Geology and Fossils of Sussex,' Tab. xxviii, fig. 9.

Fig. 3. Scalpellum quadratum, fig. (a) natural size, the rest magnified twice.

(a) Specimen as found embedded, with the valves in nearly their natural positions; the end of the rostral latus ought to touch the short basal side of the upper latus.

(b) Scutum.

(c) Tergum.

(d) Carina, lateral view.

(e) Upper latus.

(f) Rostral latus.

(g) Carinal latus.

(h) Scutum, internal view.

(i) Carina, dorsal view.

(k) Ditto, section across middle of valve.

Fig. 4. Scalpellum fossula; all the figures magnified twice, except (h), which is four times the natural size.

(a) Scutum.

(b) Tergum.

(c) Carina, side view.

(d) Upper latus.

(e) Carinal latus.

(f) Scutum, internal view.

(g) Carina, dorsal view.

(h) Ditto, section across middle.

Fig. 5. Scalpellum trilineatum; all the figures magnified twice, except (c and d), which are four times the natural size.

(a) Carina, dorsal view.

(b) Ditto, lateral view.

(c) Ditto, section of, lower part.

(d) Carina, section of, near apex.

(e) Tergum.

Fig. 6. Scalpellum semiporcatum; scutum, magnified three times.

Fig. 7. Scalpellum arcuatum; all the figures magnified twice, except (g), which is four times the natural size.

(a) Carina, dorsal view.

(b) Ditto, lateral view.

(c) Tergum, inside view.

(d) Ditto, outside view.

(e) Surface of carina, much magnified.

(f) Scutum.

(g) Section across carina.

Fig. 8. Scalpellum solidulum; natural size, except (f).

(a) Tergum.

(b) Carina, dorsal view.

(c) Ditto, internal, almost lateral, view.

(d) Carina, section of upper part.

(e) Carinal latus, natural size.

(f) Ditto, much magnified.

Fig. 9. Scalpellum simplex; twice natural size.

(a) Carina, dorsal view.

(b) Carina, lateral view.

(c) Carina, section of.

Fig. 10. Scalpellum tuberculatum; largely magnified.

(a) Tergum.

(b) Carina, dorsal view.

(c) Ditto, lateral view.

(d) Scutum; (e) basal margin, (f) occludent margin; these two margins ought to form a rather larger angle.

Fig. 11. Scalpellum (?) cretæ; largely magnified.

(a) Tergum.

(b) Carina.

(c) Scutum.

[Tab. I]

Tab. I.

J.De C. Sowerby fecit.

[page break]

[page break]

[page break]

TAB. II.

[In every case right-hand Scuta and Terga are figured; hence the occludent margins are always to the left-hand.]

Fig. 1. Scalpellum maximum, var. typicum.

(a) Carina, twice natural size.

(b) Ditto, lateral view, natural size.

(c) Ditto, ditto, twice natural size.

(d) Section of carina across middle of valve, twice natural size.

(e) Section of carina across lower part of valve.

Fig. 2. Scalpellum maximum, var. cylindraceum; all the figures twice the natural size, except the sections.

(a) Carina.

(b) Ditto, lateral view.

(c) Section of carina, upper part.

(d) Ditto, ditto, lower part.

Fig. 3. Scalpellum maximum, var. sulcatum.

(a) Carina, twice natural size.

(b) Ditto, natural size.

(c) Ditto, lateral view.

(d) Section across the middle of carina, four times natural size.

Fig. 4. Scalpellum maximum; carinal latus, two varieties.

(a) Natural size.

(b) Magnified four times.

(c) Natural size.

(d) Magnified four times.

Fig. 5. Scalpellum maximum; Tergum, Var. I., natural size and twice magnified.

Fig. 6. Scalpellum maximum; Tergum, Var. II., natural size and twice magnified.

Fig. 7. Scalpellum maximum; Tergum, Var. III.

(a and a) Natural size, and twice magnified.

(b) Internal view, twice magnified.

Fig. 8. Scalpellum maximum; Var. I.

(a) Scutum, twice natural size; some longitudinal lines have been erroneously introduced in this engraving.

(b) Scutum, natural size.

(c) Ditto, internal view, twice natural size.

Fig. 9. Scalpellum maximum; Var. II.

(a) Scutum, outside view, twice natural size.

(b) Scutum, internal view, twice natural size.

(c) Scutum, outside view, natural size.

Fig. 10. Scalpellum maximum; Var. III. Scutum, inside view, natural size.

Fig. 11. Scalpellum lineatum.

(a) Scutum, natural size.

(b) Scutum, twice natural size.

Fig. 12. Scalpellum lineatum; Carina twice natural size.

Fig. 13. Scalpellum hastatum.

(a) Carina, twice natural size.

(b) Ditto, natural size, lateral view.

(c) Carina, lateral view, twice natural size.

(d) Ditto, section across middle of valve.

[Tab. II]

Tab. II.

J.De C. Sowerby fecit.

[page break]

[page break]

[page break]

TAB. III.

[In every case right-hand Scuta and Terga are figured; hence the occlu ent margins are always to the left-hand.]

Fig. 1. Pollicipes concinnus; copied from the Mineral Conchology, Pl. 647.

(a) Group of specimens as found adhering to an Ammonite, of the natural size.

(b) Capitulum enlarged.

(c) Scales of the peduncle magnified.

Fig. 2. Pollicipes ooliticus.

(a) Carina.

(b) Rostrum.

(c) Tergum.

(d) Scutum.

Fig. 3. Pollicipes Hausmanni.

(a) Carina.

(b) Scutum.

(c) Scutum, inside view of.

(d) Tergum.

Fig. 4. Pollicipes politus.

(a) Scutum.

(b) Small portion of the occludent margin, much magnified, to show the narrow prominent ledge.

Fig. 5. Pollicipes elongatus.

(a) Tergum, about half natural size.

(b) Scutum, much magnified; the impression on the chalk gives the general outline.

(c) Scutum, natural size.

Fig. 6. Pollicipes acuminatus.

(a) Scutum, outside view, figure restored.

(b) Inside view of actual specimen.

Fig. 7. Pollicipes Angelini.

(a) Scutum.

(b) Ditto, inside view of.

(c) Tergum.

(d) Section across the middle of the tergum, to show form of surface.

Fig. 8. Pollicipes reflexus.

(a) Carina, dorsal view.

(b) Ditto, lateral view.

(c) Ditto, section beneath the middle.

(d) Tergum.

(e) Scutum; the letter (e) stands close to the occludent margin.

(f) Upper latus.

Fig. 9. Pollicipes carinatus.

(a) Tergum.

(b) Ditto, internal view.

(c) Carina.

(d) Scutum.

(e) Scutum, inside view of.

(f) Carina, section of, near apex.

(g) Rostrum, inside view.

(h) Ditto, lateral view.

(i) Ditto, dorsal view.

Fig. 10. Pollicipes glaber.

(a) Tergum, broken carina, upper latus, and a latus of the lower whorl; all these valves belonged to the same individual, and show their relative natural sizes.

(b) Scutum, natural size, of another individual.

(c) Ditto, ditto, four times magnified.

(d) Ditto, inside view of upper part; the left-hand is the occludent margin.

(e) Tergum, four times magnified.

(f) Carina.

(g) Ditto, small portion of lateral margin, close above the basal margin, much enlarged.

(h) Rostrum, natural size.

(i) Ditto, four times magnified.

(k) Upper latus, three times magnified.

(l) Latus (probably from near the rostrum) of the lower whorl, three times magnified.

Fig. 11. Pollicipes Nilssonii.

(a) Scutum, from a small worn specimen.

(b) Carina, natural size, lateral view of.

(c) Ditto, section of, across the middle.

(d) Sub-carina, inside view, natural size.

(e) Rostrum, inside view, natural size.

[Tab. III]

Tab. III.

J.De C. Sowerby fecit.

[page break]

[page break]

[page break]

TAB. IV.

[N.B.—A left-hand scutum (fig. 4, f), and a left-hand tergum (fig. 5, b), have been accidentally figured instead of right-hand valves, as in all the other Figures and Plates; hence these two hold reversed positions, and in both the occludent margins are to the right, instead of to the left hand.]

Fig. 1. Pollicipes unguis; all the figures except (d) are from the same individual and are magnified twice: (d) is of the natural size.

(a) Carina.

(b) Tergum, inside view.

(c) Ditto, outside view.

(d) Ditto, ditto, (var., natural size.)

(e) Rostrum.

(f) Sub-rostrum.

(g) Upper latus.

(h) Latus of the lower whorl, probably adjoining the carina.

(i) Ditto, inside view.

(k) Latera of the lower whorl, probably the two adjoining the rostrum.

(l) Ditto, inside view of.

Fig. 2. Pollicipes validus; all figures natural size.

(a) Carina.

(b) Ditto, inside view.

(c) Ditto, lateral internal view of.

(d) Ditto, section of upper part.

(e) Scutum.

(f) Ditto, inside view of.

(g) Ditto, inside view of another specimen.

Fig. 3. Pollicipes gracilis.

(a) Scutum, natural size.

(b) Scutum, magnified, inside view.

Fig. 4. Pollicipes dorsatus; all figures natural size, except (d), magnified twice.

(a) Carina, inside view of.

(b) Ditto, outside view of.

(c) Ditto, section of upper part of.

(d) Tergum, magnified twice.

(e) Tergum, natural size.

(f) Scutum, left-hand valve (vide supra).

Fig. 5. Pollicipes striatus; figures natural size, and magnified twice.

(a) Carina.

(b) Tergum; a left-hand valve (vide supra).

(c) Scutum.

Fig. 6. Pollicipes semilatus; magnified about ten times.

Fig. 7. Pollicipes rigidus; all figures thrice natural size, except (f), which is twice.

(a) Carina.

(b) Ditto, side view.

(c) Ditto, section of lower part of.

(d) Scutum.

(e) Tergum.

(f) Scutum, inside view.

Fig. 8. Pollicipes fallax; figures twice natural size.

(a) Scutum.

(b) Tergum.

Fig. 9. Pollicipes elegans.

(a) Carina, thrice natural size.

(b) Ditto, section of.

(c) Scutum, twice natural size.

(d) Tergum, twice natural size.

Fig. 10. Pollicipes Bronnii; figures magnified twice.

(a) Carina.

(b) Ditto, lateral view of.

(c) Ditto, section of, near basis.

(d) Carina, section of, at one third of length from the apex.

Fig. 11. Pollicipes planulatus; Tergum, upper figure, natural size.

[Tab. IV]

Tab. IV.

J.De C. Sowerby fecit.

[page break]

[page break]

[page break]

TAB. V.

Fig.

1. Loricula pulchella; natural size, as found embedded.

2. Ditto Left-hand main valve, and scales of the peduncle, magnified three times.

3. Ditto Right-hand main valve (scutum), and scales of the peduncle, magnified three times.

4. Ditto Imaginary, restored figure.

[Tab. V]

Tab. V.

J.De C. Sowerby fecit.

[See Volume 2.]


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