A first book in organic evolutionShute, D. Kerfoot (Daniel Kerfoot)
Science
A first book in organic evolution
Shute, D. Kerfoot (Daniel Kerfoot)
Evolution
These plants of the coal period were remarkable, generalized types,
connecting classes now widely separated. During this period the insects
increase in variety and numbers along with the advancing vegetation.
It is interesting to find that as the highest flowering plants are not
yet in existence, so those highest orders of insects, the flower-loving
and honey-loving ones, such as bees, butterflies and moths, are not yet
in existence. Corals and Echinoderms, Molluscs and Crustaceans, etc.,
continue through the ages with ever shifting forms. Brachiopods have
greatly diminished. Foraminifera for the first time assume considerable
importance in the earth’s economy.
The Molluscan Goniatites continue through this age with changing forms
and advancing organization, and are very numerous. The Trilobites, which
are characteristic of Palæozoic times, continue under new forms through
this age, and then perish. In this age are introduced for the first time
typical Crustaceans of the long-tailed kind, such as shrimps.
Devonian fishes still prevail. The Elasmobranchii are numerous and
varied, and some of them are highly specialized. _Pleuracanthus_ is a
remarkable shark which has many features in common with the lung-fishes
(Dipnoi), such as the character of the pectoral fins, the shape of the
tail, the bones which form a roof for the skull, while the skin is naked.
The Dipnoi continue, though in diminished numbers.
The Crossopterygians are much less abundant. The Ganoidei increase in
numbers and varieties.
The fact of greatest interest concerning the Carboniferous period is the
_expansion of the true land-breathing, backboned animals, such as the_
=Amphibians=. _Their expansion marks a distinct step forward in the scale
of life._
The Carboniferous Amphibia all belong to the extinct order of
_Labyrinthodonts_ (_Stegocephala_), in which the skull is well covered
with a roof of sculptured bones. The Amphibia of the lower Carboniferous
rocks are of small or moderate size, not exceeding eight feet in length
and mostly much smaller. A great number of these Amphibians are known,
most of them like the Salamanders in shape, but some are snake-like
in form, being long and slender. An example of the Stegocephala is
_Archegosaurus_.
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