Carbon inventory of 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 thawing permafrost, the organic-matter (OM) inventory in Yedoma d...
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/25317/ https://epic.awi.de/id/eprint/25317/1/AK_Permafrost2011_Strauss.pdf https://hdl.handle.net/10013/epic.38402 https://hdl.handle.net/10013/epic.38402.d001 |