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Calcareous Nannofossils from Simla Hills, (Himalaya, India) with a Discussion of their Age in the Tectono-Stratigraphic Column


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1 Wadia Institute of Himalayan Geology, Delhi, India
     

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The nannofossils and related coccolithophorids in the green shale of Krol B horizon playa significant role in removing the serious hanclicap of the absence of macrofossils for evaluating the stratigraphic status of Krol series. With the help of light and electron microscope the following forms were identified.

Tergestiella margereli (Noel) Rein, Microrhabdulus orbitosus Shumenko, Micula Staurophora (Vekshina) Gardet, Stradner, Zygolithus concinnus Martini, Tetralithus cf. gothicus Deflandre, Lucianorhabdus cayeuxi Deflandre, Lithraphidites carniolensis Deflandre, Discorhabdus sp, Deflandrius sp. and ex gr. Nannoconus. Most of these forms which also occur in other parts of the world indicate an age of Upper Jurassic to Upper Cretaceous to the Krol B horizon of Simla area.


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  • Calcareous Nannofossils from Simla Hills, (Himalaya, India) with a Discussion of their Age in the Tectono-Stratigraphic Column

Abstract Views: 207  |  PDF Views: 2

Authors

Anshu K. Sinha
Wadia Institute of Himalayan Geology, Delhi, India

Abstract


The nannofossils and related coccolithophorids in the green shale of Krol B horizon playa significant role in removing the serious hanclicap of the absence of macrofossils for evaluating the stratigraphic status of Krol series. With the help of light and electron microscope the following forms were identified.

Tergestiella margereli (Noel) Rein, Microrhabdulus orbitosus Shumenko, Micula Staurophora (Vekshina) Gardet, Stradner, Zygolithus concinnus Martini, Tetralithus cf. gothicus Deflandre, Lucianorhabdus cayeuxi Deflandre, Lithraphidites carniolensis Deflandre, Discorhabdus sp, Deflandrius sp. and ex gr. Nannoconus. Most of these forms which also occur in other parts of the world indicate an age of Upper Jurassic to Upper Cretaceous to the Krol B horizon of Simla area.