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- W2390464737 abstract "This approach addresses the current research in palaeoecology which focuses on the early metazoan biotas in China during the Doushantuoan (Late Sinian). Two important categories have been classified for the Sinian biotas: Miaohe and Weng' an biotas on the Upper Yangtze platform. Of particular significance is why and how these biotas flourished and were preserved during geological time. The author contends that abundant SiO_2 and P_2O_5 supplied by the upwelling currents permitted the living organisms to get thriving on a larger scale on the margins of the platform. The steady increase in SiO_2 and P_2O_5 resulted in intense phosphatiza- tion and silicification; that is to say, the abundant organic remains were rapidly phosphatized and silicificated, and got out of oxidization and decomposition. It can be seen that mineraliza- tion (phosphatization, silicification and manganesation) may be interpreted as an important factor in the preservation of the organic remains as fossils, and that the Upper Yangtze area is a favourable region in China for the flourishing of organisms during the Doushantuoan (Late Sinian)." @default.
- W2390464737 created "2016-06-24" @default.
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- W2390464737 date "1999-01-01" @default.
- W2390464737 modified "2023-09-27" @default.
- W2390464737 title "Palaeoecology and fossil preservation of the early metazoan biotas during the Doushantuoan(Late Sinian)" @default.
- W2390464737 hasPublicationYear "1999" @default.
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