When the marine forms of life are spoken of 
 as | as 1859 1860 1861 1869 1872 |  | us 1866 |  
  
having changed simultaneously throughout the world, it must not be supposed that this expression relates to the same 
 thousandth | thousandth 1859 1860 1861 1866 1869 |  | year, 1872 |  
  
or 
 hundred-thousandth year, | hundred-thousandth year, 1859 1860 1861 1866 |  
| ten-thousandth year, 1869 |  
| to the same century, 1872 |  
  
or even that it has a very strict geological sense; for if all the marine animals 
 which live at the present day | which live at the present day 1859 1860 1861 1866 |  
| now living 1869 1872 |  
  
in Europe, and all those that lived in Europe during the pleistocene period 
 (an enormously | (an enormously 1859 1860 1861 1866 |  | (a very 1869 1872 |  
  
remote period as measured by years, including the whole glacial 
 epoch), | epoch), 1859 1860 1861 1866 |  | epoch) 1869 1872 |  
  
were 
 to be | to be 1859 1860 1861 1866 |  to be 1869 1872 |  
  
compared with those now 
 living | living 1859 1860 1861 1866 |  | existing 1869 1872 |  
  
in South America or in Australia, the most skilful naturalist would hardly be able to say whether the 
 existing | existing 1859 1860 1861 1866 |  | present 1869 1872 |  
  
or the pleistocene inhabitants of Europe resembled most closely those of the southern hemisphere.  So, again, several highly competent 
 observers | observers 1859 1860 1861 1869 1872 |  | observes 1866 |  
  
 believe | believe 1859 1860 1861 1866 |  | maintain 1869 1872 |  
  
that the existing productions of the United States are more closely related to those which lived in Europe during certain 
 later | later 1859 1860 1861 1866 |  | late 1869 1872 |  
  
tertiary stages, than to 
 those which now live here; | those which now live here; 1859 1860 1861 1866 |  
| the present inhabitants of Europe; 1869 1872 |  
  
and if this be so, it is evident that fossiliferous beds 
 deposited at the present day | deposited at the present day 1859 1860 1861 1866 |  
| now being deposited 1869 |  
| now deposited 1872 |  
  
on the shores of North America would hereafter be liable to be classed with somewhat older European beds.  Nevertheless, looking to a remotely future epoch, there 
 can, | can, 1859 1860 1861 1866 |  | can 1869 1872 |  
  
 I think, | I think, 1859 1860 1861 1866 |  I think, 1869 1872 |  
  
be little doubt that all the more modern 
marine 
formations, namely, the upper pliocene, the pleistocene and strictly modern beds, of Europe, North and South America, and Australia, from containing fossil remains in some degree allied, and from not including those forms which are 
 only found | only found 1859 1860 1861 1866 |  | found only 1869 1872 |  
  
in the older underlying deposits, would be correctly ranked as simultaneous in a geological sense.  |