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...
Main Authors: | , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
European Geosciences Union
2020
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Subjects: | |
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/ |
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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