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Late Quaternary Environment, Palaeontology and Culture of Tarafeni Valley, Midnapur District, West Bengal - A Preliminary Study


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1 Deccan College Postgraduate and Research Institute, Pune 411 006, India
     

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The authors present an integrated data on the Quaternary studies carried out during the 1993-95 field seasons in a lesser known area, the Tarafeni Valley in Midnapur District, West Bengal. Microliths primarily made on chert, quartzite have been found in association with colluvial deposits formed more or less contemporaneously with underlying nodular calcrete of pedogenic Oligin. Occurrence of several vertebrate fossils on the surface of the calcrete at Dhuliapur indicates Late Pleistocene age of the artefact bearing colluvial deposits. The formation of pedogenic calcrete in a sub-humid environment, with an average annual rainfall of 1600 - 2000 mm, suggests the presence of semi-aridity in Late Terminal Pleistocene period.

Keywords

Palaeoenvironment, Tarafeni Valley, Late Quaternary, Vertebrate Fossils, West Bengal.
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  • Late Quaternary Environment, Palaeontology and Culture of Tarafeni Valley, Midnapur District, West Bengal - A Preliminary Study

Abstract Views: 204  |  PDF Views: 2

Authors

Bishnupriya Basak
Deccan College Postgraduate and Research Institute, Pune 411 006, India
G. L. Badam
Deccan College Postgraduate and Research Institute, Pune 411 006, India
Anupama Kshirsagar
Deccan College Postgraduate and Research Institute, Pune 411 006, India
S. N. Rajaguru
Deccan College Postgraduate and Research Institute, Pune 411 006, India

Abstract


The authors present an integrated data on the Quaternary studies carried out during the 1993-95 field seasons in a lesser known area, the Tarafeni Valley in Midnapur District, West Bengal. Microliths primarily made on chert, quartzite have been found in association with colluvial deposits formed more or less contemporaneously with underlying nodular calcrete of pedogenic Oligin. Occurrence of several vertebrate fossils on the surface of the calcrete at Dhuliapur indicates Late Pleistocene age of the artefact bearing colluvial deposits. The formation of pedogenic calcrete in a sub-humid environment, with an average annual rainfall of 1600 - 2000 mm, suggests the presence of semi-aridity in Late Terminal Pleistocene period.

Keywords


Palaeoenvironment, Tarafeni Valley, Late Quaternary, Vertebrate Fossils, West Bengal.