The Atlantic Monthly, Volume 12, No. 70, August, 1863: A Magazine of Literature, Art, and PoliticsVarious
History
The Atlantic Monthly, Volume 12, No. 70, August, 1863: A Magazine of Literature, Art, and Politics
Various
American periodicals
Take first the class of Fishes. We have seen that in the Jurassic
periods there were none of our common Fishes, none corresponding to our
Herring, Pickerel, Mackerel, and the like,--no Fishes, in short, with
thin membranous scales, but that the class was represented exclusively
by those with hard, flint-like scales. In the Cretaceous epoch, however,
we come suddenly upon a horde of Fishes corresponding to our smaller
common Fishes of the Pickerel and Herring tribes, but principally of the
kinds found now in tropical waters; there are none like our Cods,
Haddocks, etc., such as are found at present in the colder seas. The
Fishes of the Jurassic epoch corresponding to our Sharks and Skates and
Gar-Pikes still exist, but in much smaller proportion, while these more
modern kinds are very numerous. Indeed, a classification of the
Cretaceous Fishes would correspond very nearly to one founded on those
now living. Shall we, then, suppose that the large reptilian Fishes of
the Jurassic time began suddenly to lay numerous broods of these
smaller, more modern, scaly Fishes? And shall we account for the
diminution of the previous forms by supposing that in order to give a
fair chance to the new kinds they brought them forth in large numbers,
while they reproduced their own kind less abundantly? According to very
careful estimates, if we accept this view, the progeny of the Jurassic
Fishes must have borne a proportion of about ninety per cent, of
entirely new types to some ten per cent, of those resembling the
parents. One would like a fact or two on which to rest so very
extraordinary a reversal of all known physiological laws of
reproduction, but, unhappily, there is not one.
Still more unaccountable, upon any theory of development according to
ordinary laws of reproduction, are those unique, isolated types limited
to a single epoch, or sometimes even to a single period. There are some
very remarkable instances of this in the Cretaceous deposits. To make my
statement clearer, I will say a word of the sequence of these deposits
and their division into periods.
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