Iron Redistribution Upon Thermokarst Processes in the Yedoma Domain
Ice-rich permafrost has been subject to abrupt thaw and thermokarst formation in the past and is vulnerable to current global warming. The ice-rich permafrost domain includes Yedoma sediments that have never thawed since deposition during the late Pleistocene and Alas sediments that were formed by p...
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Published in | Frontiers in earth science (Lausanne) Vol. 9 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Frontiers Media S.A
23.07.2021
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Subjects | |
Online Access | Get full text |
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