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Palynostratigraphy of the Lower-Middle Jurassic deposits, borehole section Vostok 4 (Southeast of West Siberia)

机译:下中侏罗统沉积层古地层,Vostok 4井段(西西伯利亚东南部)

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摘要

This work presents the results of palynological investigation of the Vostok 4 borehole section situated in the Azharma region of the Ob-Irtysh facies area, where drilling has penetrated through the Urmanskaya, Ilansk, Peshkovskaya, and Tyumen formations. Six palynoassemblages are distinguished in the section based on the analyzed distribution of spores, pollen of terrestrial plants, and microphytoplankton. According to their succession, the section is subdivided into biostratigraphic units ranked as beds with palynomorphs. Comparative analysis and correlation with the Siberian palynostratigraphic standard scale of the Lower-Middle Jurassic, where succession of palynoassemblages is coordinated with ammonite zones, substantiate the Pliensbachian-Bajocian age of the deposits studied. Diverse microphytoplankton (dinoflagellate cysts, acritarchs, prasinophytes, zignematacean and colonial algae) occurs throughout the section. The facies environment of sedimentation is reconstructed based on quantitative proportions of microphytoplankton taxa.
机译:这项工作介绍了位于Ob-Irtysh相区Azharma地区的Vostok 4井段的孢粉学调查结果,该区的钻探已穿过Urmanskaya,Ilansk,Peshkovskaya和秋明地层。本节根据孢子分布,陆生植物花粉和浮游植物的微细区分,区分出六个古生物组合。根据他们的继承,该部分被细分为生物地层单元,这些单元被划分为具有多形的床。与下中侏罗世的西伯利亚古地层标准规模进行比较分析,并与之相关联,其中古陆组合的连续性与亚铁矿带相协调,从而证实了所研究矿床的Pliensbachian-Bajocian年龄。整个切片中都出现了不同的微浮游植物(鞭毛藻囊肿,顶角纲,藻类植物,褐藻类和殖民藻类)。根据微浮游植物类群的定量比例,重建了沉积相环境。

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