Organic matter characterisation along a river delta to shelf transect in eastern Siberia

• Published in: 29th International Meeting on Organic Geochemistry
• Main Authors: Jong, D. J., Bröder, L. M., Keskitalo, K. H., Tesi, T., Zimov, N., Davydova, A., Haghipour, N., Eglinton, T. I., Vonk, J. E.
• Format: Other Non-Article Part of Journal/Newspaper
• Language: English
• Published: European Association of Geoscientists and Engineers, EAGE 2019
• Subjects: Ambarchik; Arctic; Arctic Ocean; Cherskiy; East Siberian Sea; East Siberian Shelf; Kolyma; Ice; kolyma river; permafrost; Sea ice; Siberia
• Online Access: https://research.vu.nl/en/publications/985b7039-c427-44a4-a058-81986837e702; https://doi.org/10.3997/2214-4609.201902747; http://hdl.handle.net/1871.1/985b7039-c427-44a4-a058-81986837e702; http://www.scopus.com/inward/record.url?scp=85088771910&partnerID=8YFLogxK; http://www.scopus.com/inward/citedby.url?scp=85088771910&partnerID=8YFLogxK

The Arctic Ocean receives an estimated amount of 40 × 10 12 g organic carbon (OC) through inflow of rivers every year (Holmes et al., 2012; McClelland et al., 2016). A large part of the Arctic Ocean watershed is underlain by permafrost that experiences widescale warming exposing more OC to thaw and...