The Earth Through Time, 8e

Eighth Edition
by Harold L. Levin


Chapter 12 - page 10

Life of the Paleozoic


Phylum Chordata

The Amniotic Egg

The next major evolutionary development in vertebrate history was the ability to reproduce without returning to water. This was accomplished with the amniotic egg.

The amniotic egg is the key feature in the development of the reptiles.

Characteristics of the amniotic egg:


The Reptiles

CLASS REPTILIA

Name: From "reptilis" meaning "creeping".

Chief characteristics: Two characteristics of the skull which can be used to distinguish reptiles from amphibians are:

  1. The reptile skull is high and narrow, compared with the low, broad amphibian skull.
  2. In reptiles, the roof of the mouth is arched, with small openings. In amphibians, it is flat with large openings.

Mode of life: Complete colonization of land was achieved by the reptiles, which can lay their eggs on dry land.

Geologic range: Pennsylvanian to Recent.

The oldest reptile fossils, genus Hylonomus, (300 m.y. old) are found in Nova Scotia inside fossilized hollow trees filled with sediment. These reptiles were about 24 cm (about 1 ft) long. They resemble modern insect-eating lizards.

Diadectes
Diadectes sp., from the Early Permian (280-250 m.y.) was a land-dwelling plant eater.
The skeletal anatomy is reptilian, but the skull resembles that of Seymouria, an amphibian.
Photo courtesy of Pamela Gore.

Dicynodon
Dicynodon, a Late Permian (250-230 m.y.), plant-eating reptile. From Cape Province, South Africa.
Photo courtesy of Pamela Gore.

Various groups of vertebrates can be distinguished on the basis of the position and number of openings behind the eye on the side of their skulls.

  1. Anapsida (no holes) - amphibians, the earliest known reptile (Hylonomus), and turtles
  2. Diapsida (two holes) - dinosaurs, flying reptiles, birds, and all groups of living reptiles except turtles
  3. Euryapsida (upper hole only) - extinct marine reptiles
  4. Synapsida (lower hole only) - pelycosaurs, therapsids, and mammals

Diagram showing the four reptile skull types Diagram showing the evolution and classification of reptiles
Diagram showing four vertebrate skull types.
Diagram showing the evolution of reptiles and synapsids.


The Synapsids

CLASS SYNAPSIDA

The synapsids had diverged from the reptiles by the Late Carboniferous. The synapsids were long considered to be a subclass of reptile, but more recent cladistic analysis shows that they diverged from ancestors completely different than Hylonomus and other true reptiles.

The synapsids were the dominant terrestrial vertebrate in the Permian.

This group was formerly called the "mammal-like reptiles", however the name has been abandoned because they are not really reptiles.

Synapsids include the pelycosaurs and the therapsids.

Pelycosaurs

Several species of pelycosaurs had fins or "sails" on their backs, supported by rod-like extensions of their vertebrae. These sails may have been used as temperature regulating mechanisms.

Two well known pelycosaurs, which evolved their sails independently were the carnivorous Dimetrodon, and the plant-eating Edaphosaurus.

Edaphosaurus
The Permian pelycosaur, Edaphosaurus.
Photo courtesy of Pamela Gore.

Dimetrodon has a larger skull and teeth than does Edaphosaurus, suggesting that Dimetrodon was a meat eater.

Pelycosaurs lived in the Carboniferous and Permian. The sail-backed forms are characteristic of the Permian.

Therapsids

Therapsids were small to moderate-sized animals with several mammalian skeletal characteristics, such as:

Mammal-like features are well developed in the therapsid, Cynognathus. (From "kynos" meaning "dog" and "gnathos" meaning "jaw" or "tooth.")
Examination of the bone on the snout portion of the skull reveals probable "whisker pits", suggesting that they had hair, which may have functioned to insulate the animal and slow the rate of heat loss.

Cynognathus
Cynognathus crateronotus, a therapsid from the Early Triassic (230-225 m.y.), Cape Province, South Africa.
Note the differentiated teeth. This animal was obviously a predator.
Photo courtesy of Pamela Gore.

Therapsids are found in Permian and Triassic rocks.


Previous Page | Next Page | Back to Index

1 2 3 4 5 6 7 8 9 10 11 12


Document created by: Pamela J. W. Gore
Georgia Perimeter College, Clarkston, GA

January 14, 2006