Эволюция биосферы по палеонтологическим коллекциям /В. М. Подобина, Т. Г. Ксенева, Л. Г. Пороховниченко

Подобина, Вера Михайловна 1934-
Электронный ресурс
Другой Автор
Ксенева, Татьяна Георгиевна
Пороховниченко, Любовь Георгиевна
Источник
Паралельное заглавие
Biosphaere evolution on the base paleontological collection
Аннотация
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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Резюме
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.