POC, Colville River, Beaufort Sea, permafrost thaw, radiocarbon, ramped-temperature pyrolysis
Digital Object Identifier (DOI)
Burial of organic carbon (OC) in marine sediments is one of the most important linkages between the short-term biologic carbon cycle and the long-term geologic carbon cycle. Yet much is still unknown about the fate of terrigenous OC in marine coastal margins. Here the delivery of particulate OC (POC) to the Colville River deltaic region in the Alaskan Beaufort Sea by particulates of varying densities is studied through the use of ramped temperature pyrolysis and radiocarbon analyses. The Colville River is the largest river in North America whose watershed is underlain completely by high Arctic permafrost tundra. A variety of sources of POC are considered, including terrestrial soils, Pleistocene-aged yedoma-like sediments, coastal peat erosion, and marine POC. We provide the first evidence that riverine POC from the Colville River contains old (Pleistocene-sourced) OC, suggesting ongoing thaw and mobilization of yedoma-like permafrost OC from this northern Alaskan watershed. Additionally, much of this OC appears to be fairly labile and therefore could be readily oxidized and returned to the atmosphere.
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Citation / Publisher Attribution
Geophysical Research Letters, v. 41, issue 9, p. 3117-3126
©2014. American Geophysical Union. All Rights Reserved.
Scholar Commons Citation
Schreiner, Kathryn M.; Bianchi, Thomas S.; and Rosenheim, Brad E., "Evidence for Permafrost Thaw and Transport from an Alaskan North Slope Watershed" (2014). Marine Science Faculty Publications. 2436.