Late Oligocene climate and floristic diversity of Assam, Northeast India

Harshita Bhatia; Gaurav Srivastava; R.C. Mehrotra

doi:10.54991/jop.2020.32

Authors

Harshita Bhatia Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Gaurav Srivastava Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
R.C. Mehrotra Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India

DOI:

https://doi.org/10.54991/jop.2020.32

Keywords:

Fossils, CLAMP, Monsoon, Oligocene, Palaeoclimate

Abstract

Late Oligocene is considered as the last significant globally warm climate. In India, the Makum Coalfield has exposures of sediments which were deposited at a low latitude of 10–15° N during the late Oligocene. Here, we report a diverse assemblage of fossil leaves and fruits. The assemblage envelops 18 leaf and 9 fruit morphotypes. The floristic assemblage indicates a warm and humid climate during the deposition of the sediments. The quantitative palaeoclimate reconstruction indicates that the leaf morphological traits were dominantly adapted to Indonesian–Australian type of monsoon.

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