Journal of Paleolimnology

, Volume 13, Issue 2, pp 179–191

Radiometric dating of lake sediments from Signy Island (maritime Antarctic): evidence of recent climatic change

Authors

  • P. G. Appleby
    • Department of Applied Mathematics and Theoretical PhysicsUniversity of Liverpool
  • V. J. Jones
    • Environmental Change Research Centre, Department of GeographyUniversity College London
  • J. C. Ellis-Evans
    • British Antarctic Survey
Article

DOI: 10.1007/BF00678106

Cite this article as:
Appleby, P.G., Jones, V.J. & Ellis-Evans, J.C. J Paleolimnol (1995) 13: 179. doi:10.1007/BF00678106

Abstract

Sediment cores from three lakes (Moss, Sombre and Heywood) in the maritime Antarctic (Signy Island, South Orkney Islands) have been successfully dated radiometrically by210Pb and137Cs. The core inventories of both fallout radionuclides are an order of magnitude higher than that which can be supported by the direct atmospheric flux at this latitude. The elevated values may be explained by fallout onto the catchment during the winter being delivered directly to the lakes during the annual thaw. Two of the lakes (Sombre and Heywood) show marked increases in sediment accumulation afterc. 1950. This appears to be associated with a documented rise in temperature in the South Orkney Islands, which has caused extensive deglaciation at Signy Island.

Key words

maritime AntarcticSigny IslandlakessedimentsPb-210Cs-137radionuclide fluxesclimate change

Copyright information

© Kluwer Academic Publishers 1995