Inventories and behavior of particulate organic carbon in the Laptev and East Siberian seas

• Published in: Global Biogeochemical Cycles
• Main Authors: Sánchez-García, Laura, Alling, Vanja, Pugach, Svetlana, Vonk, Jorien, Van Dongen, Bart, Humborg, Christoph, Dudarev, Oleg, Semiletov, Igor, Gustafsson, Örjan
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2011
• Subjects: Arctic; Arctic Ocean; Laptev Sea; laptev; permafrost
• Online Access: https://research.manchester.ac.uk/en/publications/abfc4bd2-d642-4fc2-841d-c9b1764c012e; https://doi.org/10.1029/2010GB003862

[1] Fluvial and erosional release processes in permafrost-dominated Eurasian Arctic cause transport of large amounts of particulate organic carbon (POC) to coastal waters. The marine fate of this terrestrial POC (terr-POC), water column degradation, burial in shelf sediments, or export to depth, impacts the potential for climate-carbon feedback. As part of the International Siberian Shelf Study (ISSS-08; August-September 2008), the POC distribution, inventory, and fate in the water column of the extensive yet poorly studied Eurasian Arctic Shelf seas were investigated. The POC concentration spanned 1-152 mM, with highest values in the SE Laptev Sea. The POC inventory was constrained for the Laptev (1.32 ± 0.09 Tg) and East Siberian seas (2.85 ± 0.20 Tg). A hydraulic residence time of 3.5 ± 2 years for these Siberian shelf seas yielded a combined annual terr-POC removal flux of 3.9 ± 1.4 Tg yr?1. Accounting for sediment burial and shelf-break exchange, the terr-POC water column degradation was ?2.5 ± 1.6 Tg yr?1, corresponding to a first-order terr-POC degradation rate constant of 1.4 ± 0.9 yr?1, which is 5-10 times faster than reported for terr-DOC degradation in the Arctic Ocean. This terr-POC degradation flux thus contributes substantially to the dissolved inorganic carbon excess of 10 Tg C observed during ISSS-08 for these waters. This evaluation suggests that extensive decay of terr-POC occurs already in the water column and contributes to outgassing of CO2. This process should be considered as a geographically dislocated carbon-climate coupling where thawing of vulnerable permafrost carbon on land is eventually adding CO2 above the ocean. Copyright 2011 by the American Geophysical Union.