A Monograph of the Trilobites of North America: with Coloured Models of the SpeciesGreen, Jacob
Science
A Monograph of the Trilobites of North America: with Coloured Models of the Species
Green, Jacob
Paleontology -- North America; Trilobites -- North America
Some geologists imagine that the order of creation is registered in
the rocks which compose the external crust of the earth, and that they
can there clearly read a progressive development of organic life; in
other words, that a succession of more perfect animals may be traced in
ascending from the lower strata to the upper or more recent formations;
that there is a gradual approach to the present system of things, and
a succession of destructions and creations; worlds of living beings
alternating with worlds of desolation and death, antecedent to the
existence of man.
Others, again, contend that there is often a wide and palpable
discrepancy between the nature of the rock, and the fossils which it
contains, and, therefore, that such inquiries afford no clue, whatever,
to the order of creation.[1] We propose not to enter the field of
controversy. Fossils are undoubtedly historic medallions of remote
periods in the natural history of our earth, and our design is, merely
to illustrate with them a neglected department of ancient zoology, by
describing a few which have recently fallen under our own observation.
[Footnote 1: Nothing can be more opposed to true science, than to
pronounce on the priority of formation, or the comparative age of
rocks, from either their structure, or the organic remains they
present. M. Alexandre Brongniart thus propounds his opinion: "In those
cases where characters derived from the nature of the rocks are opposed
to those which we derive from organic remains, I should give the
preponderance to the latter." This seems to us to imply an admission,
that nothing definite can be inferred from the _nature of the rocks_;
moreover, that between the nature of the rock, and the organic remains,
there may be a palpable discrepancy; and that these may be even at
complete antipodes with each other. The event has proved, from what we
have already mentioned, that no evidence as to priority can be obtained
from the nature of the fossil remains displayed in particular strata.
In addition to what has been said on this subject, we may further
state, that _encrinites_, _entrochites_, and _pentacrinites_ are found
in clay slate, grauwacke, transition limestone, alpine limestone,
lias, muschelkalk, and chalk. It may be reasonably asked how these
three species of fossils could indicate any particular formation, when
they are found in so many types and structures of rocks altogether
different? If they would go to prove any thing at all, it would be that
of a _contemporaneous_ formation; but certainly not distinct epochas.
_See Eclectic Review, July, 1832._]
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