Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features

Introduction During the late Quaternary, a large pool of organic matter (OM) accumulated in the arctic permafrost zone. Because of the potential re-introduction into the biogeochemical cycle from degrading permafrost, the OC inventory of ice-rich permafrost deposits and its degradation features are...

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Bibliographic Details
Main Authors: Strauss, Jens, Schirrmeister, Lutz, Wetterich, Sebastian, Mangelsdorf, Kai
Format: Conference Object
Language:unknown
Published: The Fort Dialog-Iset Publisher 2012
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/30849/
https://epic.awi.de/id/eprint/30849/1/Strauss_abstract_TICOP.pdf
https://hdl.handle.net/10013/epic.39819
https://hdl.handle.net/10013/epic.39819.d001