Fossil organic carbon in Siberian Yedoma and thermokarst deposits
During the late Quaternary, a large pool of organic carbon accumulated in the ice-rich syngenetic frozen deposits and soils preserved in the arctic and subarctic permafrost zone. Because of the potential release of organic carbon from degrading permafrost, the organic-matter (OM) inventory in Yedoma...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2011
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Online Access: | https://epic.awi.de/id/eprint/31117/ https://epic.awi.de/id/eprint/31117/1/StraussAGU2011.pdf https://hdl.handle.net/10013/epic.39972 https://hdl.handle.net/10013/epic.39972.d001 |