The Elements of Geology eBook

This eBook from the Gutenberg Project consists of approximately 384 pages of information about The Elements of Geology.

The Elements of Geology eBook

This eBook from the Gutenberg Project consists of approximately 384 pages of information about The Elements of Geology.

Snakes are found for the first time in the early Tertiary.  These limbless reptiles, evolved by degeneration from lizardlike ancestors, appeared in nonpoisonous types scarcely to be distinguished from those of the present day.

Mammals of the early tertiary.  The fossils of continental deposits of the earliest Eocene show that a marked advance had now been made in the evolution of the Mammalia.  The higher mammals had appeared, and henceforth the lower mammals—­the monotremes and the marsupials—­are reduced to a subordinate place.

These first true mammals were archaic and generalized in structure.  Their feet were of the primitive type, with five toes of about equal length.  They were also PLANTIGRADES,—­that is, they touched the ground with the sole of the entire foot from toe to heel.  No foot had yet become adapted to swift running by a decrease in the number of digits and by lifting the heel and sole so that only the toes touch the ground,—­a tread called digitigrade.  Nor was there yet any foot like that of the cats, with sharp retractile claws adapted to seizing and tearing the prey.  The forearm and the lower leg each had still two separate bones (ulna and radius, fibula and tibia), neither pair having been replaced with a single strong bone, as in the leg of the horse.  The teeth also were primitive in type and of full number.  The complex heavy grinders of the horse and elephant, the sharp cutting teeth of the carnivores, and the cropping teeth of the grass eaters were all still to come.

Phenacodus is a characteristic genus of the early Eocene, whose species varied in size from that of a bulldog to that of an animal a little larger than a sheep.  Its feet were primitive, and their five toes bore nails intermediate in form between a claw and a hoof.  The archaic type of teeth indicates that the animal was omnivorous in diet.  A cast of the brain cavity shows that, like its associates of the time, its brain was extremely small and nearly smooth, having little more than traces of convolutions.

The long ages of the Eocene and the following epochs of the Tertiary were times of comparatively rapid evolution among the Mammalia.  The earliest forms evolved along diverging lines toward the various specialized types of hoofed mammals, rodents, carnivores, proboscidians, the primates, and the other mammalian orders as we know them now.  We must describe the Tertiary mammals very briefly, tracing the lines of descent of only a few of the more familiar mammals of the present.

The horse.  The pedigree of the horse runs back into the early Eocene through many genera and species to a five-toed, [Footnote:  Or, more accurately, with four perfect toes and a rudimentary fifth corresponding to the thumb.] short-legged ancestor little bigger than a cat.  Its descendants gradually increased in stature and became better and better adapted to swift running to escape their foes. 

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The Elements of Geology from Project Gutenberg. Public domain.