Further palynological investigation of coaliferous sequences of Tura Formation of Nangwalbibra, East Garo Hills, Meghalaya: inferences on palaeovegetation and palaeoclimate

Priyanka Monga; Gaurav Srivastava; Madhav Kumar; R.C. Mehrotra

doi:10.54991/jop.2014.322

Authors

Priyanka Monga Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226007, India
Gaurav Srivastava Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226007, India
Madhav Kumar Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226007, India
R.C. Mehrotra Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226007, India

DOI:

https://doi.org/10.54991/jop.2014.322

Keywords:

Spore, Pollen, Tura Formation, Late Palaeocene, Garo Hills, Meghalaya

Abstract

The coal and carbonaceous shales collected from the Tura Formation (late Palaeocene) of Nangwalbibra, East Garo Hills, Meghalaya, have been analysed for palynological study to deduce palaeovegetation and palaeoclimate. The palynoflora represented by pteridophytic spores and angiospermic pollen grains shows similarity with other contemporaneous deposits of the Garo, Khasi and Jaintia Hills of Meghalaya. The palynoassemblage dominated by angiosperms depicts subtropical to tropical vegetation during the late Palaeocene in the region. The fossil pollen grains show their similarity with modern plants of various tropical angiosperm families, like Alangiaceae, Anacardiaceae, Annonaceae, Arecaceae, Bombacaceae, Clusiaceae and Gunneraceae, etc. which indicate the existence of tropical evergreen to moist deciduous forest. Some of the taxa resemble the floral elements growing near swamps in the tropical zone. The fossil palynoflora indicates warm and humid climate during the depositional period. The study is supported by plant megafossil data known from the same horizon.

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