Origin of Species Variorum

→ throughout the greater part of their thickness rich 1861

rich 1859 1860

throughout the greater part of their thickness rich 1866 1869 1872

↑ 2 blocks not present in 1861 1866 1869 1872; present in 1859 1860

Thus the geological record will almost necessarily be rendered intermittent. I feel much confidence in the truth of these views, for they are in strict accordance with the general principles inculcated by Sir C. Lyell; and E. Forbes independently arrived at a similar conclusion.

↑ 3 blocks not present in 1859 1860 1861 1866 1869 1872; present in

are →throughout the greater part of their thickness rich

fossils ,

fossils,

fossils,

have thus been formed during subsidence. Since publishing my views on this subject in 1845, I have watched the progress of Geology, and have been surprised to note how author after author, in treating of this or that great formation, has come to the conclusion that it was accumulated during subsidence. I may add, that the only ancient tertiary formation on the west coast of South America, which has been bulky enough to resist such degradation as it has as yet suffered, but which will hardly last to a distant geological age, was

~~certainly~~

certainly

deposited during a downward oscillation of level, and thus gained considerable thickness.

All geological facts tell us plainly that each area has undergone numerous slow oscillations of level, and apparently these oscillations have affected wide spaces.

Consequently,

Consequently

formations rich in fossils and sufficiently thick and extensive to resist subsequent degradation,

will

may

have been formed over wide spaces during periods of subsidence, but only where the supply of sediment was sufficient to keep the sea shallow and to embed and preserve the remains before they had time to decay. On the other hand, as long as the bed of the sea

remains

remained

stationary,

thick

thick

deposits

cannot

could not

have been accumulated in the shallow parts, which are the most favourable to life. Still less

can

could

this have happened during the alternate periods of elevation; or, to speak more accurately, the beds which were then accumulated will

have

generally have

been destroyed by being upraised and brought within the limits of the coast-action. ↑ ↑

These remarks apply chiefly to littoral and

sublittoral

sub-littoral

deposits. In the case of an extensive and shallow sea, such as that within a large part of the Malay Archipelago, where the depth varies from 30 or 40 to 60 fathoms, a widely extended formation might be formed