Carbonate isotopes from high altitude Tso Moriri Lake (NW Himalayas) provide clues to late glacial and Holocene moisture source and atmospheric circulation changes-Reference-Cited by-同舟云学术

Carbonate isotopes from high altitude Tso Moriri Lake (NW Himalayas) provide clues to late glacial and Holocene moisture source and atmospheric circulation changes

Published:2015-05 Issue: Volume:425 Page:76-83
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Mishra Praveen K.,Prasad Sushma,Anoop A.,Plessen B.,Jehangir A.,Gaye B.,Menzel Philip,Weise S.M.,Yousuf A.R.

Funder

Deutsche Forschungsgemeinschaft

Deutsches GFZ Potsdam

Kashmir University

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference62 articles.

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3. Palaeoenvironmental implications of evaporative Gaylussite crystals from Lonar lake, Central India;Anoop;J. Quat. Sci.,2013

4. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion;Benn;J. Geol. Soc.,1998

5. Insolation values for the climate of the last 10millionyears;Berger;Quat. Sci. Rev.,1991

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