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Discovery of silicified microfossils from the Khatpul formation, Shali group (Neoproterozoic), H.P., India

机译:印度H.P. Shali组(新生代)Khatpul组发现硅化微化石

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摘要

Well-developed organic walled microfossils of cyanobacterial affinity are recorded for the first time from the bedded and stromatolitic chert units of the Shall Group (Neoproterozoic). The present discovery enhances our knowledge of the palaeobiology of the Shall Belt which has so far yielded only stromatolites. The association of these silicified microfossils with columnar stromatolites signifies the close ecological relationship between the two. A correlation of the Shall Belt with adjacent belts of the Lesser Himalaya has been discussed in the light of the present discovery. [References: 17]
机译:首次从Shall小组(新生代)的层状和层状硅质石单元中记录了发达的,具有蓝细菌亲和力的有机壁微化石。本发现增强了我们对Shall带古生物学的认识,到目前为止,Shall带仅产生了叠层石。这些硅化的微化石与柱状叠层石的结合表明两者之间的紧密生态关系。根据目前的发现,已经讨论了Shall带与小喜马拉雅山脉的相邻带之间的关系。 [参考:17]

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