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    Author(s): Lutz Schirrmeister; Guido Grosse; Sebastian Wetterich; Pier Paul Overduin; Jens Straub; Edward A.G. Schuur; Hans-Wolfgang Hubberton
    Date: 2011
    Source: Journal of Geophysical Research. 116: G00M02. 16 p. doi:10.1029/2011JG001647.
    Publication Series: Scientific Journal (JRNL)
    Station: Pacific Northwest Research Station
    PDF: Download Publication  (1.68 MB)


    Permafrost deposits constitute a large organic carbon pool highly vulnerable to degradation and potential carbon release due to global warming. Permafrost sections along coastal and river bank exposures in NE Siberia were studied for organic matter (OM) characteristics and ice content. OM stored in Quaternary permafrost grew, accumulated, froze, partly decomposed, and refroze under different periglacial environments, reflected in specific biogeochemical and cryolithological features. OM in permafrost is represented by twigs, leaves, peat, grass roots, and plant detritus. The vertical distribution of total organic carbon (TOC) in exposures varies from 0.1 wt % of the dry sediment in fluvial deposits to 45 wt % in Holocene peats. Based on TOC data and updated information on bulk densities, we estimate average organic carbon inventories for ten different stratigraphic units in northeast Siberia, ranging from 7.2 kg C m-3 for Early Weichselian fluvial deposits, to 33.2 kg C m-3 for Middle Weichselian Ice Complex deposits, to 74.7 kg C m-3 for Holocene peaty deposits. The resulting landscape average is likely about 25% lower than previously published permafrost carbon inventories.

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    Schirrmeister, Lutz; Grosse, Guido; Wetterich, Sebastian; Overduin, Pier Paul; Straub, Jens; Schuur, Edward A.G.; Hubberton, Hans-Wolfgang. 2011. Fossil organic matter characteristics in permafrost deposits of the northeast Siberian Arctic. Journal of Geophysical Research. 116: G00M02. 16 p. doi:10.1029/2011JG001647.


    permafrost thaw, climate change, carbon

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