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Mesozoic

  The Mesozoic era began 251 mya ago, right after the Permian mass extinction. It's divided into three periods - Triassic, Jurassic and Cretaceous. Mesozoic is usually refered as the "Age of the Reptiles", though it's more accurate to say it was the "Age of the Archosaurs".

  Archosauria is group of diapsid amniotes that dominated Mesozoic terrestrial (and some aquatic) ecosystems, and is still playing important role in today's ecosystems. There are two main lineages, or branches, of archosaurs - crocodilian one and bird one. The croc-line archosaurs include modern crocodiles and alligators, along with their numerous extinct relatives, while the bird-line is represented by two major groups - the pterosaurs and the dinosaurs. The birds evolved sometime during the middle Jurassic, as a group of derived coelurosaurian theropod dinosaurs - the Avialae (or Aves, if you like). Although dinosaurs first appeared toward the end of the middle Triassic, they were not major part of the ecocsystems up until the Triassic-Jurassic boundary, when a mass extinction wiped out the dominant until then croc-line archosaurs. Since Jurassic times, dinosaurs are the most numerous group of tetrapod animals.

   Besides the archosaurs, there were many other group of animals living through the Mesozoic. Many groups of marine sauropsids lived in mesozoic seas and oceans - nothosaurs, placoderms, ichthyosaurs, plesiosaurs and mosasaurs among others. Invertebrate animals also flourished - countless species of ammonites, belemnites, bivalves, gastropods, echinoids, brachiopods, foraminifers, etc., evolved during this era. On land first mammals appeared. The plant life went through serious changes in the early Cretaceous, when flowering plants evolved. This led to co-evolution of many new insects, like butterflies and bees, whos way of life was tightly connected to the new plants.

  During the Triassic there was one supercontinent - Pangaea. The climates were warm and arid. Big parts of Pangaea were deserts where life hardly managed to survive. There were no ice caps on the poles, but the sea levels were the lowest since the Precambrian. The oxygen levels were also pretty low, an aftermath of the cataclysms that marked the end of the Paleozoic era.

   In the next period, the Jurassic, conditions on Earth stabilized. The climates were warm and the temperature gradient towards the poles was more gradual than today's. Also overal climates were moister than those in the Triassic. Sea levels rised, so did the oxygen levels. Plant life in different latitudes was more uniform than it's today. With the onset of the Jurassic, Pangaea started to break up. This led to the forming of two major continental masses - the northern Laurassia and the southern Gondwana. In middle Jurassic times the North Atlantic ocean started to open. Eastern from the newly forming Atlantic was the mesozoic Tethys ocean - a complex system of ocean and sea basins that existed from the late Paleozoic to the Cenozoic. 

  For the last 550 mya the highest sea leves were during the mid-Cretaceous times - back then oceans were 250 meters above the modern levels. At the same time the temperatures hit their maximum too - the mean global temperatures were well above 30 degrees celsius. This led to series of global anoxia (lack of oxygen) events in the oceans. There were no glaciers on the poles. But not all of the Cretaceous was like this. There were time intervals (like early Cretaceous China or maastrichtian North America) when the climates were more like todays though the temperatures were still somewhat higher. The levels of carbon dioxide were few times higher than todays. In the early Cretaceous the South Atlantic and Indian oceans started to open, due to the breaking up of Gondwana. The continents moved slowly to more familiar positions. Late Cretaceous was time of wide spread volcanism and magmatism.

 The Mesozoic era closed when 10 kilometers wide meteorite (asteroid or less likely a comet) hit the Earth and led to the most famous of all mass extinctions - Cretaceous-Paleogene mass extinction. The impact happened near what's now Yucatan peninsula, forming the Chixulub crater. The aftermaths of this collision, along with the intensive late Certaceous volcanism, wiped out big part of the life on Earth. The most notable victims of this cataclysm were the non-avian dinosaurs, followed by the pterosaurs. Many other groups like plesiosaurs, mosasaurs, ammonites, belemnites, etc., were also wiped out without leaving descendants. The stage for the beginning of Cenozoic era was set.

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