To assess the pattern of climatic evolution during the late Miocene to early Pleistocene in the largest fluvio-deltaic sedimentary system on the Earth, the Bengal Basin (BB), a quantitative palaeoclimatic reconstruction was made, based on 20 fossil wood floras. Those floras show that moisture-loving taxa have decreased considerably since the Miocene, especially at the western margin of the basin. A quantitative reconstruction of climate parameters reveals that the late Miocene−early Pliocene was warmer and wetter than now, yet with spatial variability. Seasonality of temperature was low in the basin and subsequently increased during the late Pliocene−early Pleistocene. Monsoon intensity was weaker during the interval from the late Miocene to early Pleistocene than the present day. A comparison of the retrieved data with some earlier records from sites either influenced by Indian summer monsoon (ISM) or East Asian summer monsoon (EASM) or both, the two branches of the Asian summer monsoon (AM) provide insights into the temporal and spatial patterns of climate evolution in southern Asia during the late Neogene–Quaternary transition. In general, a drop in temperature and a weakening in ISM strength since the early Pleistocene correlate with the global cooling trend, though with spatial differences.
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RG acknowledges the Director, Birbal Sahni Institute of Palaeosciences, Lucknow, for her encouragement, support and permission to publish this work. SB, AB, IS and DKP acknowledge UGC-CAS, Phase VII, Department of Botany, University of Calcutta, for the infrastructural facilities. This work is a contribution to NECLIME (Neogene Climate Evolution in Eurasia) and the ROCEEH (The Role of Culture in Early Expansions of Humans) Research Centre of the Heidelberg Academy of Sciences and Humanities. We thank Professor Robert A. Spicer, The Open University, UK and an anonymous reviewer for their constructive suggestions on this manuscript which certainly have increased the merit of this work.
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This article is a contribution to the special issue “Palaeobotanical contributions in honour of Volker Mosbrugger”.
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Ghosh, R., Biswas, A., Bruch, A.A. et al. Palaeoclimate estimates based on the late Miocene to early Pleistocene wood flora of the Bengal Basin: an insight into the climatic evolution of southern Asia. Palaeobio Palaeoenv 101, 141–162 (2021). https://doi.org/10.1007/s12549-020-00467-8
- Late Miocene to early Pleistocene
- Bengal Basin
- Fossil woods