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Callovian and Upper Jurassic foraminiferal and ammonite biostratigraphy of the Shaim petroleum region (West Siberia)

机译:Shaim石油地区(西西伯利亚)的卡洛夫阶和上侏罗纪有孔虫和菊石生物地层

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摘要

The results of biostratigraphic analysis of foraminiferal assemblages were used to identify a nearly complete succesion of biostratigraphic units in the Callovian-Upper Jurassic section of the Shaim region. The finds of the ammonites from different parts of the Callovian-Volgian sections helped to correlate the identified foraminiferal biostratigraphic units to the General Stratigraphic Scale. Analysis of variations in the taxonomic composition and structure of foraminiferal assemblages allowed refinement of paleontological characteristics of the foraminiferal biostratigraphic units for different facies conditions in the southwest of the West Siberian Basin. (C) 2015, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
机译:有孔虫组合的生物地层学分析结果被用于确定谢伊姆地区卡洛夫-侏罗纪上侏罗统地区生物地层单元几乎完全成功。从卡洛夫-沃尔格断面的不同部分发现的铵铁矿有助于将已确定的有孔虫生物地层单位与一般地层范围联系起来。通过对有孔虫类群的分类学组成和结构的变化进行分析,可以对西西伯利亚盆地西南部不同相情况下有孔虫生物地层单元的古生物学特征进行细化。 (C)2015,V.S. Sobolev IGM,RAS的西伯利亚分公司。由Elsevier B.V.发布。保留所有权利。

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