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峡东陡山沱组丝状蓝藻化石的新资料
引用本文:张忠英.峡东陡山沱组丝状蓝藻化石的新资料[J].地质科学,1986,0(1):30-37.
作者姓名:张忠英
作者单位:南京大学地质系
摘    要:三峡东部震旦系广泛分布于黄陵背斜两翼,发育良好,是研究我国震旦系的典型地区。本区震旦系自下而上分为下统莲沱组和南沱组,上统陡山沱组和灯影组。

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收稿时间:1983-12-31
修稿时间:1983-12-31;

NEW MATERIAL OF FILAMENTOUS FOSSIL CYANOPHYTES FROM THE DOUSHANTUO FORMATION (LATE SINIAN) IN THE EASTERN YANGTZE GORGE
Zhang Zhongying.NEW MATERIAL OF FILAMENTOUS FOSSIL CYANOPHYTES FROM THE DOUSHANTUO FORMATION (LATE SINIAN) IN THE EASTERN YANGTZE GORGE[J].Chinese Journal of Geology,1986,0(1):30-37.
Authors:Zhang Zhongying
Institution:Department of Geology, Nanjing University
Abstract:This paper deals with some filamentous mierofossils of oscillatoriaeean cyanophyte affinity discovered recently in petrographic thin sections of the c. 700 Ma old Doushan-tuo Formation (Late Sinian) in the Eastern Yangtze Gorge, Hubei Province, China. They are assigned to the taxa Siphonophyciis sinensis sp. nov., Siphonophycus inornatum Y. Zhang, Oscillatoriopsis maxima (Y. Zhang) comb. nov. (referred to as Palaeolyngbya sp. in Zhang Zhongying (1982)), Oscillatoriopsis sp., Salome hubeiensis sp. nov., and Salome svalbardcnsis Knoll. These newly discovered filaments supplement our understanding of the Doushantuo microflora.
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