Sedimentological and pollen studies of Lake Priyadarshini, Eastern Antarctica

Authors

  • Chhaya Sharma Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226007, India
  • Rajiv Sinha Department of Civil Engineering. Indian Institute of Technology, Kanpur 208016, India
  • M.S. Chauhan Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226007, India

DOI:

https://doi.org/10.54991/jop.2000.126

Keywords:

Holocene, Antarctica, Lake, Sedimentology, Pollen, Palaeoclimate

Abstract

A shallow sediment core from a freshwater Antarctic Lake-Priyadarshini, in Schirmacher Oasis, Eastern Antarctica has been studied for grain size, mineralogy and pollen assemblage. The silty clayey sediments from the lake bed have a simple clay mineral assemblage consisting of illite and chlorite with dominant quartz and feldspar in clay-size fraction. A low-hydrolyzing, periglacial depositional environment is reflected from this assemblage. The pollen analysis identifies three pollen zones based on the fluctuations in the retrieved palynomorphs which apparently manifest palaeoclimatic oscillations during Holocene.

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Published

2000-12-31

How to Cite

Sharma, C., Sinha, R., & Chauhan, M. (2000). Sedimentological and pollen studies of Lake Priyadarshini, Eastern Antarctica. Journal of Palaeosciences, 49((1-3), 1–8. https://doi.org/10.54991/jop.2000.126

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Section

Research Articles

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