In the Late Permian, a volcanic region in India called the Deccan Traps formed, pumping large amounts of gases into Earth's atmosphere. These created a greenhouse effect, raising global temperatures. This is known as the End Permian Extinction. By the Permian-Triassic boundary, 250 million years ago, vast deserts covered the planet. Over 90 percent of all animal species on Earth had died out.
Pangaea existed from the Permian, about 299 million years ago, through the Triassic, and into the early Jurassic.There were very different animals in Pangaea during the Permian than there were in the Triassic because, at the end of the Permian, about 90% of species became extinct in the worst mass extinction in Earth's history.PermianInsects in Pangaea included beetles, dragonflies, and flies. Early in the Permian, large amphibians and pelycosaur reptiles, like the carnivorous, sail backed Demitrodon, or the herbivorous, sail backed Edaphosaurus. Later in the Permian the archosaurs evolved, which later gave rise to the dinosaurs, pterosaurs, and crocodillians. There were also therapsids, the reptillian ancestors of mammals. TriassicThe temnospndyli, which were large amphibians, and therapsids both survived the Permian extinction event. Archosaurs were the primary terrestrial vertebrates. There were herbivores such as Hyperodapedon, and carnivores like Postosuchus. The first dinosaurs were small meat eaters like Eoraptor, and small, long necked, herbivorous dinosaurs called prosauropods, evolved in Panagaea during the Triassic.
There is evidence to suggest that life on Earth first appeared around 3.8 billion years ago. However, there likely were periods of time when life faced significant challenges, such as during mass extinction events like the Permian-Triassic extinction around 252 million years ago.
Many of earth's marine invertebrates were extinct, and many other species that had evolved on earth were extinct as well, so basically the ecosystem was "rebuilding" after the Permian mass-extinction.
There were more. In the Permian, Triassic, and early Jurassic periods there were mammal-like reptiles from which true mammals evolved, some of which were likely warm blooded.
The major subdivisions are the Precambrian, Palaeozoic, Mesozoic and Cenozoic, which are subdivided into Archean and Proterozoic (Precambrian), Cambrian, Ordovician, Silurian, Devonian, Carboniferous (or Missisipian and Pennsylvanian in the US) and Permian (Palaeozoic), Triassic, Jurassic and Cretaceous (Mesozoic) and Tertiary and Quaternary (Cenozoic). For a graphical representation, see http://geomaps.wr.usgs.gov/socal/geology/geologic_history/images/geologic_time_scale.jpg
251 million years ago was the time of the Permian Extinction, the single largest extinction of biological life in the history of Earth. Before the extinction the dominant animals were probably therapsids, mammal like animals that were either mammals or the ancestors of mammals.
In the Permian Period, the land on Earth was a giant landmass called Pangaea. It was arid and desert-like. The creatures probably would have like a freshwater lake.?æ?æ
there were several groups of creatures on Pangaea. but for going the insects there where 4 major groups amphibians, anapsids diapsids and therapsids. the amphibians where remnants from the coniforus still large but not dominante on land anymore. anapsids accounted for a good chunk of life on land at this time. therapsids or so called mamal like reptials (eventualy evolved into mamals) where very common but the ones you know about are the diapsids. thees included crocidiles lizards and dinosaurs.
The Permian Period,248 million years ago, was the largest extinction period on Earth. Ninety to ninety-five percent of marine species were eliminated, including fusulinid foraminifera, trilobites, rugose and tabulate corals, blastoids, acanthodians, placoderms, and pelycosaurs. Numbers of sharks and bony fish were drastically reduced during this period.
The ages of Earth are like several stages of the Earth. If you research about each of the stages I have typed below you may get more information, I recommend Wikipedia (If it has it). It starts like this: Pre-Cambrian, Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian, Triassic, Jurassic, Cretaceous, Eocene, Oligocene, Miocene, Pliocene, Pleistocene and Holocene. Note: Some of the ages are named after particular places. Other sites might mention some other information or some ages between some of the ones I've given you.
Glossopteris: A large seed fern that dominated the flora of the Permian period, found in Gondwana. Cordaites: Tall, tree-like plants with needle-like leaves that were common in the late Paleozoic era, including the Permian. Sigillaria: An extinct tree-like plant with segmented trunks and scale-like leaves, characteristic of the Carboniferous and Permian periods.