Banerjee, M., Sen, P. and Dastidar, A.G. (1984) On the Depositional Condition of the Holocene Sediments of Bengal Basin with Remarks on Environmental Condition of the Soft Grey Clay Deposition in Calcutta. Proceedings of Indian Geotechnical Conference 1, Calcutta, 21-23 December 1984, Div. I, 63-69.

has been cited by the following article:

• TITLE: Holocene Biostratigraphic Zones Corresponding Litho-Chronostratigraphy, Environment of Deposition and Successive Changes in the Geomorphology of Bengal Basin, India during Last 10,000 Years

  AUTHORS: Prasanta Kumar Sen, Manju Banerjee

  KEYWORDS: Holocene, Biostratigraphy, Flandrian Transgression, Geomorphology, Bengal Basin

  JOURNAL NAME: International Journal of Geosciences, Vol.7 No.4, April 28, 2016

  ABSTRACT: Biostratigraphic Zones Bb. Bz. H. I-V distinguished in C14dated Peat, peaty clay sediments above arid, Barren zone have identified distinct environment of deposition as fresh water mixed brackish water to shallow marine to brackish water mangrove swamp, brackish water mixed fresh water swamp followed by colonization of non-littoral species to fresh water swamp during Holocene in the Bengal basin, India in chronological succession. The successive phases of depositional environment have identified the events of sea level rise, marine transgression and sea ward movement of the sea. The unique database has explored successive changes in the geomorphology of South Bengal from upland dry to marine deltaic environment to fresh water upland condition.