ssive forms of life, in the stages of the widely separated
palaeozoic and tertiary periods, would still be manifest, and the several
formations could be easily correlated.

These observations, however, relate to the marine inhabitants of distant
parts of the world: we have not sufficient data to judge whether the
productions of the land and of fresh water change at distant points in the
same parallel manner. We may doubt whether they have thus changed: if the
Megatherium, Mylodon, Macrauchenia, and Toxodon had been brought to Europe
from La Plata, without any information in regard to their geological
position, no one would have suspected that they had co-existed with still
living sea-shells; but as these anomalous monsters co-existed with the
{324} Mastodon and Horse, it might at least have been inferred that they
had lived during one of the later tertiary stages.

When the marine forms of life are spoken of as having changed
simultaneously throughout the world, it must not be supposed that this
expression relates to the same thousandth or hundred-thousandth year, or
even that it has a very strict geological sense; for if all the marine
animals which live at the present day in Europe, and all those that lived
in Europe during the pleistocene period (an enormously remote period as
measured by years, including the whole glacial epoch), were to be compared
with those now living in South America or in Australia, the most skilful
naturalist would hardly be able to say whether the existing or the
pleistocene inhabitants of Europe resembled most closely those of the
southern hemisphere. So, again, several highly competent observers believe
that the existing productions of the United States are more closely related
to those which lived in Europe during certain later tertiary stages, than
to those which now live here; and if this be so, it is evident that
fossiliferous beds deposited at the present day 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,
I think, 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 in the older underlying deposits, would be correctly ranked as
simu