The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic RemainsMantell, Gideon Algernon
Science
The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic Remains
Mantell, Gideon Algernon
Geology -- England -- Guidebooks; Paleontology
The scales of fishes, and the integuments of marine reptiles, are not
the only vestiges of the dermal coverings of vertebrated animals that
are preserved by mineralization. Traces of the wing-integument of
flying reptiles, and of the feathers of birds, are sometimes manifest:
and even when every atom of the original structure has perished, the
impression may remain, and afford satisfactory results. The footmarks
of unknown animals are often preserved in the rocks, and the imprints
of the feet of several species of bipeds, presumed to be birds of
colossal size, in tracks as distinct as if but recently made, have been
discovered in the New Red sandstone of North America; in the section on
fossil birds, this highly interesting subject will be fully explained.
The student, even from this brief review, will perceive how many
valuable facts may be unnoticed, and irretrievably lost, unless
attention be paid to the various circumstances under which fossil
remains are presented to his notice.
Of the invertebrated orders, the most durable, and consequently the
most numerous relics, are shells and corals. The integuments of the
eyes, antennæ, and wings of Insects occur; and the shelly coverings
of Crustaceans are not uncommon; those of the Echinoderms, the
Star-fishes, and of the Crinoidea or Lily-animals, are very abundant in
certain deposits. Instructions for the collection and arrangement of
these fossils will be given in the chapters in which they are severally
described.
PART II.
⎼⎼⎼⎼⎼◆⎼⎼⎼⎼⎼
CHAPTER IV.
FOSSIL BOTANY.
Fossil Vegetables.--The remains of the vegetable kingdom are presented
to the notice of the geologist in various conditions; in some instances
these relics are but little changed in their aspect, as, for example,
in the recent accumulations of mud and silt, at the bottoms of lakes
and rivers, and in morasses, and peat-bogs. In tufaceous incrustations,
the imprints of wood, and of leaves and stems, are often sharply
defined on the solid masses of concretionary and crystalline limestone.
Public-domain text, read in full here on John Shaqi.
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