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Holocene Paleoclimates of India

Published online by Cambridge University Press:  20 January 2017

Sushma Prasad  and
Yehouda Enzel
Sushma Prasad*
Affiliation:
Climate Dynamics and Sediments, GeoForschungsZentrum, Telegrafenberg, D 14473 Potsdam, Germany
Yehouda Enzel
Affiliation:
Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, 91904, Israel
*
*Corresponding author. E-mail addresses:[email protected] (S. Prasad), [email protected] (Y. Enzel).
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Abstract

We present a comprehensive summary of the available palaeoclimate records from India and compare the results from different proxies. The results indicate (i) fluctuating lake levels during the early Holocene. The period of relatively higher lake levels from increased precipitation efficiency was reached only ∼7.2–6.0 cal kyr BP, possibly due to increased contribution from winter rainfall; (ii) the onset of aridity in NW India could have begun as early as ∼5.3 cal kyr BP. Subsequently, there were multiple wet events but of shorter duration and smaller magnitude than during the mid Holocene; (iii) there is evidence of several short term climate events in the proxy record. However, in the absence of a rigorous chronological framework a detailed regional correlation is not possible at this stage. Finally, a comparison between marine and terrestrial records indicates that episodes of strongest and weakest monsoon winds were not always associated with wettest and driest episodes respectively in the NW Indian lakes.

Keywords

IndiaLakesHolocenePollensDunesPalaeoclimateEventsIndus valley civilisation
Type
Special Issue Articles
Information
Quaternary Research , Volume 66 , Issue 3 , November 2006 , pp. 442 - 453
Copyright
University of Washington

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