J. Earth Syst. Sci. (2021) 130:93 Ó Indian Academy of Sciences https://doi.org/10.1007/s12040-021-01586-2 (0123456789().,-volV)(0123456789().,-volV) Impact of climate on the evolution of vegetation in tectonically active Karewa basin, Kashmir Himalayas 1, 1 1 1 ANJUM FAROOQUI *, SURESH KPILLAI ,DEEPA AGNIHOTRI ,SALMAN KHAN , 1 1 1 1 RAJNI TEWARI ,SUNIL KSHUKLA ,SAJID ALI ,ANJALI TRIVEDI , 2 1 3 1 SKPANDITA ,KAMLESH KUMAR ,GDBHAT and RAJESH AGNIHOTRI 1Birbal Sahni Institute of Palaeosciences, 53, University Road, Lucknow 226 007, India. 2Department of Geology, University of Jammu, Jammu 180 006, India. 3Directorate of Geology and Mining, Jammu and Kashmir Government, Srinagar, India. *Corresponding author. e-mail: afarooqui˙
[email protected] MS received 8 September 2020; revised 19 January 2021; accepted 22 January 2021 The rise of the Himalayas governed the Indian Summer Monsoon in Karewa basin during Plio-Pleistocene. A palynological study is presented to delineate the climate-vegetation relationship using an 8.5-m thick Cuvio-lacustrine sequence of the Hirpur Formation (2.4–2.1 Ma). Our results suggest that the sediment sequence is mainly comprised of two units, namely, Unit 1 and Unit 2. Unit 1 shows the dominance of sub-tropical to broad-leaf temperate vegetation when mean annual temperature (MAT) was *17°C and mean annual precipitation (MAP) was 1025 mm. The subsequent increase in sand followed by a thin lignite layer with Trapa megafossil (fruits) demarcates Cuvial adjustments, suggesting a low altitude Cuvio-lacustrine ecosystem. Conversely, Unit 2 shows a decline in rainforest pollen with a steady increase in conifers.