Chordata: Class Reptilia
Class Reptilia
The reptiles, which evolved from amphibians during the Carboniferous period, were the first vertebrate group to become entirely independent of water. This was made possible by the development of a scaly, water-resistant skin and of the terrestrial, or amniote, type of egg found in all higher land vertebrates. The amniote egg has an elaborate series of internal membranes (one of which is called the amnion) surrounding a pool of liquid in which the embryo develops; the membranes prevent desiccation and allow inward diffusion of oxygen. Reptilian eggs have porous shells and large amounts of yolk. Fertilization is internal. In most cases the eggs are laid unhatched; in a few species they are retained and hatched in the body. Reptiles, including such forms as turtles and sea snakes that have returned to an aquatic life, are air-breathing at all stages, and nearly all lay their eggs on land. Gill passages appear, as in birds and mammals, only in the embryo.
During the Mesozoic era, reptiles were exceedingly diverse and numerous. The reptilian dinosaurs included the largest terrestrial animals that have ever lived, as well as many smaller forms. There were also flying and aquatic reptiles. With the rise of the early mammals the decline of the reptiles began. The only large and successful modern group of reptiles is the order of lizards and snakes. Snakes are descended from lizards, but have lost their limbs. Reptiles, like fish and amphibians, are cold-blooded, that is, they have little ability to regulate their body temperature, which approaches that of the environment. The reptiles gave rise to the two warm-blooded vertebrate groups, the birds and the mammals.
Sections in this article:
- Introduction
- Class Mammalia
- Class Aves
- Class Reptilia
- Class Amphibia
- Class Sacropterygii
- Class Actinopterygii
- Class Chondrichthyes
- Class Placodermi
- Classes Myxini and Hyperoartia
- Subphylum Vertebrata
- Subphylum Cephalochordata
- Subphylum Urochordata
- Bibliography
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