Do stable isotope data from calcrete record late Pleistocene monsoonal climate variation in the Thar Desert of India?
In this paper, the AA. attempt to construct a detailed terrestrial late Pleistocene climatic record in India by studying oxygen and carbon stable isotopes in pedogenic calcrete from the Thar Desert. The nearly continuous calcrete record in eolian intervals and the chronology from thermoluminescence, infrared- and green-light-stimulated luminescence dates give a good opportunity to examine the isotopic data for paleoclimatic variability and relate this to other marine and terrestrial records
Article of periodic
published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV
Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)
Millesime : 1998, vol. 50, no3 [pp. 240-251]
Bibliographic references : 56 ref.
Collation : Illustration ;
INIST-CNRS, Cote INIST : 15739