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https://hdl.handle.net/2440/24133
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Type: | Journal article |
Title: | River response to Quaternary climatic fluctuations: evidence from the Son and Belan valleys, north-central India |
Author: | Williams, M. Pal, J. Jaiswal, M. Singhvi, A. |
Citation: | Quaternary Science Reviews: the international multidisciplinary research and review journal, 2006; 25(19-20):2619-2631 |
Publisher: | Pergamon-Elsevier Science Ltd |
Issue Date: | 2006 |
ISSN: | 0277-3791 |
Statement of Responsibility: | M.A.J. Williams, J.N. Pal, M. Jaiswal and A.K. Singhvi |
Abstract: | The last glacial period was cold and dry in peninsular India. In north-central India, the interval from 39±9 to 16±3 ka was associated with widespread and prolonged aggradation in the Son and Belan valleys. The aggradation ended with sustained vertical incision after 16±3 ka and reflects a return to warmer, wetter conditions. In this region, it would appear that terminal Pleistocene to Holocene river incision was broadly synchronous with a strong summer monsoon regime and higher levels of river discharge and the preceding river aggradation with lower discharge and a weaker or more variable summer monsoon regime. Two older phases of prolonged aggradation followed by vertical incision are evident in the Son and Belan valleys before ~39 ka. One of these phases is centred towards 73±4 ka when ash from the Toba mega-eruption in Sumatra was deposited across peninsular India. The following phase of aggradation has yielded infrared stimulated luminescence ages of 58±6 and 45±12 ka. The youngest phase of aggradation began towards ~5.5 ka and seems to mark a return to a weaker summer monsoon regime. |
DOI: | 10.1016/j.quascirev.2005.07.018 |
Description (link): | http://www.elsevier.com/wps/find/journaldescription.cws_home/636/description#description |
Published version: | http://dx.doi.org/10.1016/j.quascirev.2005.07.018 |
Appears in Collections: | Aurora harvest 6 Geography, Environment and Population publications |
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