Эволюция биосферы по палеонтологическим коллекциям В. М. Подобина, Т. Г. Ксенева, Л. Г. Пороховниченко
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ArticleOther title: Biosphaere evolution on the base paleontological collection [Parallel title]Subject(s): палеонтологические коллекции | эволюция биосферы | СибирьGenre/Form: статьи в сборниках Online resources: Click here to access online
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Эволюция жизни на Земле : материалы V Международного симпозиума, 12-16 ноября 2018 г С. 33-36Abstract: Different Paleontological collection from the Fanerozoic deposits keeping in Museum of Tomsk State University have
shown the Biosphaere evolution during this time. We can see the exhibits from the Protista organic (Nevlandien and other fauna)to gigantic Mammoth fauna across many shells and skeletons of Paleozoic, Mesozoic, Cainozoic Eras. The more impotent
exhibits in Museum are the first higher Plants-Riniofites, different fauna from Jurassic Zolengophen slantzes, Lower Cretaceous
skeletons of Dinosaurus – Psittacosaus, many other skeletons of bison, rhinoceros, mammoth and their remains. In museum are
different Plant imprints especially impotent from Carbonian, Jurassic a nd Neogenian deposits.
Different Paleontological collection from the Fanerozoic deposits keeping in Museum of Tomsk State University have
shown the Biosphaere evolution during this time. We can see the exhibits from the Protista organic (Nevlandien and other fauna)to gigantic Mammoth fauna across many shells and skeletons of Paleozoic, Mesozoic, Cainozoic Eras. The more impotent
exhibits in Museum are the first higher Plants-Riniofites, different fauna from Jurassic Zolengophen slantzes, Lower Cretaceous
skeletons of Dinosaurus – Psittacosaus, many other skeletons of bison, rhinoceros, mammoth and their remains. In museum are
different Plant imprints especially impotent from Carbonian, Jurassic a nd Neogenian deposits.
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