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Upper Jurassic Foraminiferal Zones and Position of the Jurassic-Cretaceous Boundary in Western Siberia

机译:西伯利亚西部侏罗腊山传染率的区域和侏罗纪 - 白垩纪边界的位置

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The biostratigraphy of Upper Jurassic deposits of Western Siberia is based on zones of foraminifera (hereafter abbreviated F-zones) with widespread foraminiferal assemblages. The description of F-zones corresponding to Oxfordian, Kimmeridgian and Volgian stages is given. The Upper Jurassic-Cretaceous boundary coincides with the top of the Upper Volgian F-zone Ammodiscus veteranus-Evolutinella volossatovi. The Volgian foraminiferal assemblages cannot be further subdivided; they differ systematically at the species level from the Early Berriasian faunas of the Early Cretaceous.
机译:西伯利亚的上侏罗纪沉积物的生物数据库基于具有广泛的传染孔组装的Foraminifera(以下缩写F区)的区域。给出了对应于牛车德,KimMeridgian和Volgian阶段的F区的描述。上侏罗纪 - 白垩纪边界与上Volgian F区Ammodiscus veteranus-Evolutinella volossatovi的顶部一致。 Volgian Foraminiferal集会不能进一步细分;它们在早期白垩纪早期的Berriasian群藻中系统地有系统地不同。

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