Reptiles are a Class of Animals which are Cold Blooded and lay eggs. Most of them are 'Tetrapods', meaning that they have four legs or leg-like appendages. They have a Bilateral Symmetry. Reptiles started evolving around 330 million years ago and dominated the Earth for over 200 million years. Reptiles include Lizards, Snakes, Crocodiles, Tortoise etc. There are about 8,200 extant Speciess of Reptiles of which almost half are Snakes. Lizards and Snakes are 'The Largest Group of Reptiles'. Of the 1,670 Reptile Species that have been evaluated on the IUCN Red List, almost 1 in 3 are threatened with extinction.
Crocodilia - These include Crocodiles, Gavials, Caimans and Alligators. There are about 23 Species of Crocodilia.
Sphenodontia - These include Tuataras from New Zealand. There are only 2 Species of Sphenodontia.
Squamata - These include Lizards, Snakes and Worm Lizards. There are approximately 7,900 Species of Squamata.
Testudines - These include Turtles and Tortoises. There are approximately 300 Species of Testudines.
Subclasses of Reptiles
Subclasses of Reptiles is based on the basis of Temporal Openings.
Anapsida - These are characterised with having no Temporal Opening like the Primitive Reptiles and Turtles.
Diapsida - These are charcterised by 2 Temporal openings. These include Snakes, Lizards, Crocodilians, Dinosaurs, Pterosaurs, Tuatara, Nothosaurs, Plesiosaurs and Icthyosaurs etc.
Euryapsida - These are characterised with one high Temporal Opening placed above the 'Postorbital' and 'Squamosal' (some of the bones in vertebrate skull. These include Protorosaurs (small, early lizard-like reptiles) and Sauropterygia (plesiosaurs and their relatives).
Synapsida - These are characterised by One low Temporal opening. These include Pelycosaurs, Therapsid Mammals such as Dicynodonts, Cynodonts and the ancestors of Mammals.
Parapsida - These are characterised by One Temporal Opening placed high up on the skull. These include extinct Species like Protosaurs, Nothosaurs and Placodonts.
Today’s Reptiles fall into only 2 of the 5 Subclasses.
History and Evolution of Reptiles
The origin of the Reptiles lies about 320–310 million years ago, in the steaming swamps of the late Carboniferous Period, when the first Reptiles evolved from advanced 'Reptiliomorph labyrinthodonts'. The oldest trace of Reptiles is a series of footprints from the fossil strata of 'Nova Scotia', dated to 315 million years ago. The tracks are attributed to 'Hylonomus', the oldest known Reptile in biological sense. It was a small, Lizard-like Animal, about 20 to 30 cm (8–12 in) long, with numerous sharp teeth indicating an Insectivorous diet. Other examples include 'Westlothiana' and 'Paleothyris', both of similar build and presumably similar habit. One of the best known early Reptiles is Mesosaurus, a genus from the early Permian Period that had returned to water, feeding on Fish. The earliest Reptiles were largely overshadowed by bigger Labyrinthodont Amphibians such as Cochleosaurus, and remained a small, inconspicuous part of the Fauna until after the small Ice Age at the end of the Carboniferous Period.
Ancient Reptiles
The first Reptiles were Anapsids, i.e. they had a solid Skull with holes for only nose, eyes, spinal cord, etc.
Very soon after the first Reptiles appeared, they split into two branches.
1. Synapsida - These type of Reptiles had two openings in the Skull roof behind the eyes. These included 'Mammal-like Reptiles' or 'Stem Mammals'
2. Diapsida - These type of Reptiles possessed a pair of holes in their Skulls behind the eyes, along with a second pair located higher on the Skull. The function of the holes in both groups was to lighten the skull and give room for the jaw muscles to move, allowing for a more powerful bite.
The Diapsids and later Anapsids are classed as the 'True Reptiles' also known as the 'Sauropsida'
Permian Period
With the close of the Carboniferous, Reptiles became the dominant Tetrapod Fauna. The Synapsids evolved the first Terrestrial Megafauna (giant animals) in the form of 'Pelycosaurs' such as 'Edaphosaurus' and the Carnivorous 'Dimetrodon'.
Early in the Premian Period, the Diapsid Reptiles split into two main lineages, the Archosaurs (forefathers of crocodiles and dinosaurs) and the Lepidosaurs (predecessors of modern snakes, lizards, and tuataras). Both groups remained Lizard-like and relatively small and inconspicuous during the Permian.
In the mid-Permian period the climate turned dryer, resulting in a change of fauna. The Primitive Pelycosaurs were replaced by the more advanced 'Therapsids' (earliest mammals). The Anapsid Reptiles, whose massive skull roofs had no post-orbital holes, continued and flourished throughout the Permian. The 'Pareiasaurs' reached giant proportions in the late Permian, eventually disappearing at the close of the period.
Mesozoic Period
The end of the Permian Period witnessed the 'Greatest Mass Extinction' known as the 'Permian–Triassic Extinction Event'. Most of the earlier Anapsid/Synapsid Megafauna became extinct. They were replaced by the 'Archosauromorph Diapsids'. The Archosaurs had elongated hind legs and an erect pose and the early forms looked somewhat like 'Long-Legged Crocodiles'. The Archosaurs became the dominant group during the Triassic period, developing into the well-known Dinosaurs and Pterosaurs, as well as Crocodiles and Phytosaurs. Some of the Dinosaurs developed into the 'Largest Land Animals' ever to have lived.
Many varieties of Reptiles evolved during this Period. The Lepidosauromorph Diapsids may have been ancestral to the Sea Reptiles. These Reptiles developed into the Sauropterygians in the early Triassic and the Ichthyosaurs during the Middle Triassic. The Mosasaurs also evolved in the Mesozoic era, emerging during the Cretaceous period. The Therapsids came under increasing pressure from the Dinosaurs in the early Mesozoic and developed into increasingly smaller and more nocturnal forms, the first Mammals being the only survivors of the line by the late Jurassic.
Cretaceous - Tertiary Extinction Event
The close of the Cretaceous Period witnessed mass extinction of Mesozoic era Reptilian Megafauna which is known as the 'Cretaceous–tertiary Extinction Event'. Of the large Marine Reptiles, only the Sea Turtles were left, and amongst Dinosaurs, only the small feathered Theropods survived in the form of Birds.
Kingdom - Animalia.
Phylum - Chordata.
Subphylum - Vertebrata.
(unranked) - Amniota.
Class - Reptilia.
Weight - The 'Largest Extant Reptile' weighs over 1,000 kg and the 'Smallest Reptile' weighs between 20-50 grams.
Size - The 'Largest Extant Reptile' reaches approximately 6 metres in length and the 'Smallest Extant Reptile' grows to only 1.6 cm (0.6 in).
Geographical Range and Habitat
Reptiles inhabit every Continent with the exception of Antarctica. Their Habitats include Deserts, Forests, Mountains etc.
Diet - Most Reptiles eat a variety of food but most are Carnivorous. But there are some Reptiles which are Omnivorous. A small number of Reptile Species eat only plants like some Species of Turtles, Chuckwalla and Desert Iguana. Some Reptiles eat only certain type of food such as the Striped Crayfish Snake, which eats only Crayfish. Their Diet includes a wide variety of Mammals, Birds, Insects, other Reptiles etc.
Almost all the Reptiles reproduce sexually, though some are capable of Asexual Reproduction. All reproductive activity occurs through the Cloaca, the single exit/entrance at the base of the tail where waste is also eliminated. Most Reptiles have Copulatory Organs, which are usually retracted or inverted and stored inside the body. In Turtles and Crocodilians, the Male has a single median penis, while Snakes and Lizards, possess a pair of 'Hemipenes'. Tuataras, however, lack copulatory organs, and so the Male and Female simply press their Cloacas together as the Male excretes sperm. Asexual reproduction has been identified in Squamates in six families of Lizards and one Snake. In some Species of Squamates, a population of Females is able to produce a 'Unisexual Diploid Clone' (organism having two sets of chromosomes) of the mother. This form of Asexual Reproduction is called Parthenogenesis. In Parthenogenesis an unfertilized egg develops into a new individual. It also occurs in several Species of Gecko and is particularly widespread in the Teiids (new world lizards especially Aspidocelis) and Lacertids (old world terrestrial lizard, Lacerta). In captivity, Komodo dragons (Varanidae) have reproduced by Parthenogenesis. Some Species among Chameleons, Agamids, Xantusiids and Typhlopids are also suspected of Parthenogenesis.
Most Reptiles lay amniotic eggs covered with leathery or calcareous shells. An amnion, chorion, and allantois are present during embryonic life. There are no larval stages of development. Viviparity and Ovoviviparity have evolved only in Squamates, and many Species, including all boas and most vipers, utilize this mode of reproduction. The degree of Viviparity varies: some Species simply retain the eggs until just before hatching, others provide maternal nourishment to supplement the yolk, and yet others lack any yolk and provide all nutrients via a structure similar to the mammalian placenta.Some Reptiles exhibit temperature-dependent sex determination (TDSD), in which the incubation temperature determines whether a particular egg hatches as Male or Female. TDSD is most common in Turtles and Crocodiles, but also occurs in Lizards and Tuataras.