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Microfossils from loess of the Miaodao Islands, Bohai Sea

机译:渤海庙岛群岛黄土中的微化石

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Microfossils from the Malan Loess profiles, Miaodao Islands, have been quantitatively studied. The microfauna is composed mainly of benthic foraminifers together with a few planktonic foraminifers, ostracods, gastropods, bivalves and echinoid spines. With the exception of indigenous gastropods, benthic foraminifers, ostracods, bivalves and echinoid spines were transported from the north or northwest of the Bohai Sea in the glacial period by the prevailing winter monsoon, while planktonic foraminifers were probably driven from the Yellow Sea or even the northern East China Sea by southerly winds. The upward decrease of marine mjcrofossil abundance and diversity in the Malan Loess profiles shows that the microfossil transportation occurred mainly at the beginning of the regression.
机译:对苗岛马兰黄土剖面的微化石进行了定量研究。微型动物区系主要由底栖有孔虫和一些浮游有孔虫,成虫,腹足纲,双壳类和棘突类动物组成。除本地腹足动物外,盛行的冬季季风在冰河时期从渤海的北部或西北部运输了底栖有孔虫,成虫,双壳类和棘突类棘类动物,而浮游有孔虫可能是由黄海或什至是北半球带动的。东海北部受南风影响。马兰黄土剖面中海洋微化石丰度和多样性的下降表明,微化石的运输主要发生在回归开始时。

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