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...
Main Authors: | , , , |
---|---|
Format: | Conference Object |
Language: | unknown |
Published: |
The Fort Dialog-Iset Publisher
2012
|
Subjects: | |
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 |