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Reworked Permian palynofossils from Bhuban Formation (Early Miocene) of Tripura, India

机译:印度特里普拉邦布班组(中新世早期)的二叠纪古化石

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Palynological investigations were carried out from the sediments of Bhuban Formation, Amarpur area, located on the southern part of Tripura. The assemblage consists of a large number of marker pollen/spores of Miocene age, comprising pteridophytic spores, angiosperm and gymnosperm pollen and fungal remains. Besides these, an abundance of reworked Permian palynomorphs of Gondwanan affinity have been recorded which include Acanthotriletes, Jayantisporites, Barakarites, Parasaccites, Plicatipollenites, Densipollenites, Scheuringipollenites, Faunipollenites, Alisporites, Primuspollenites, Klausipollenites, etc. The recovered palynoassemblage is dominated by Parasaccites and subdominated by Plicatipollenites. From bottom to top, the monosaccates appear to decline and the striate and non-striate disaccates become dominant. The Gondwana sediments were eroded, transported and redeposited within the Miocene sediments in a shallow sea adjacent to a densely vegetated land mass. The implications of the reworked Permian palynofossils in the Miocene sediments ofTripura has been discussed.
机译:对位于特里普拉南部的阿马尔普尔地区布班组的沉积物进行了孢粉学调查。该组合由中新世时代的大量标志花粉/孢子组成,包括蕨类植物的孢子,被子植物和裸子植物的花粉以及真菌残留物。除此之外,还记录了大量的冈瓦南亲和力的二叠纪重晶石化形态,包括棘刺毛虫,Jayantisporites,Barakarites,伞石,Plicatipollenites,Densipollenites,Scheuringipollenites,Faunipollenites,Alisporites,Primuspollenites,亚科孢子虫,Klausipolage。由Plicatipollenites。从底部到顶部,单锯齿状显示下降,而纹状和非纹状不显示变化占主导。冈瓦纳的沉积物在与茂密的植被相邻的浅海中新世沉积物中被侵蚀,运输和重新沉积。讨论了特里普拉(Tripura)中新世沉积物中重制的二叠纪古化石的意义。

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