Woolly mammoth δ13C and δ15N values remained amazingly stable throughout the last ∼50,000 years in north-eastern Siberia

Author:

Kuitems M.,van Kolfschoten T.ORCID,Tikhonov A.N.,van der Plicht J.

Funder

Netherlands Organisation for Scientific Research

NWO

Publisher

Elsevier BV

Subject

Earth-Surface Processes

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3. Vegetation and climate history in the Laptev Sea region (Arctic Siberia) during Late Quaternary inferred from pollen records

4. Pleistocene graminoid-dominated ecosystems in the Arctic;Blinnikov;Quat. Sci. Rev.,2011

5. Isotopic biogeochemistry and the paleoecology of the mammoth steppe fauna;Bocherens,2003

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