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

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...

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Bibliographic Details
Main Authors: Kostrova, Svetlana, Meyer, Hanno, Pestryakova, Luidmila, Biskaborn, Boris K., Fernandoy, Francisco, Baumer, Marlene
Format: Conference Object
Language:unknown
Published: European Geosciences Union 2020
Subjects:
Verkhoyansk
permafrost
Siberia
Online Access:https://epic.awi.de/id/eprint/51881/
https://epic.awi.de/id/eprint/51881/1/Kostrova_et_al_2020_EGU2020_8574_print.pdf
https://hdl.handle.net/10013/epic.e0593a29-35fa-4854-bb78-569ce872019f
https://hdl.handle.net/
Description
Summary: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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