Environmental and climate dynamics in northeastern Siberia according to diatom oxygen isotopes


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svetlana.kostrova [ at ] awi.de

Abstract

The sedimentary sequence from Lake Emanda (65°17′N; 135°45′E; 675 m a.s.l), one large freshwater body (33.1 km2) in the continuous permafrost of the Verkhoyansk Mountains, has been investigated within the German-Russian ‘Paleolimnological Transect’ (PLOT) project. It provided important insight into the environmental and climate dynamics in northeastern Siberia.



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Event Details
EGU General Assembly 2020, 04 May 2020 - 08 May 2020, Vienna (online).
Eprint ID
51881
Cite as
Kostrova, S. , Meyer, H. , Pestryakova, L. , Biskaborn, B. K. , Fernandoy, F. and Baumer, M. (2020): Environmental and climate dynamics in northeastern Siberia according to diatom oxygen isotopes , EGU General Assembly 2020, Vienna (online), 4 May 2020 - 8 May 2020 .


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