B. Basak et al., LATE QUATERNARY ENVIRONMENT, PALEONTOLOGY AND CULTURE OF TARAFENI VALLEY, MIDNAPUR DISTRICT, WEST-BENGAL - A PRELIMINARY-STUDY, Journal of the Geological Society of India, 51(6), 1998, pp. 731-740
The authors present an integrated data on the Quaternary studies carri
ed out during the 1993-95 field seasons in a lesser known area, the Ta
rafeni 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 nodula
r calcrete of pedogenic origin. Occurrence of several vertebrate fossi
ls on the surface of the calcrete at Dhuliapur indicates Late Pleistoc
ene age of the artefact bearing colluvial deposits. The formation of p
edogenic calcrete in a sub-humid environment, with an average annual r
ainfall of 1600 - 2000 mm, suggests the presence of semi-aridity in La
te/Terminal Pleistocene period.