Dissolved organic matter sources in large Arctic rivers

Publication: Research - peer-reviewJournal article – Annual report year: 2012

Without internal affiliation

  • Author: Amon, R.M.W.

    Texas A&M University, United States

  • Author: Rinehart, A.J.

    Texas A&M University, United States

  • Author: Duan, S.

    Texas A&M University, United States

  • Author: Louchouarn, P.

    Texas A&M University, United States

  • Author: Prokushkin, A.

    Russian Academy of Sciences, Russian Federation

  • Author: Guggenberger, G.

    Leibniz Universität Hannover, Germany

  • Author: Bauch, D.

    University of Kiel, Germany

  • Author: Stedmon, Colin

    Aarhus University

  • Author: Raymond, P.A.

    Yale University, United States

  • Author: Holmes, R.M.

    Woods Hole Research Center, United States

  • Author: McClelland, J.W.

    University of Texas, United States

  • Author: Peterson, B.J.

    Marine Biological Laboratory, United States

  • Author: Walker, S.A.

    Texas A&M University, United States

  • Author: Zhulidov, A.V.

    South Russian Regional Centre for Preparation and Implementation of International Projects, Russian Federation

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The biomarker composition of dissolvedorganic carbon (DOC) of the six largestArcticrivers was studied between 2003 and 2007 as part of the PARTNERS Project. Samples were collected over seasonal cycles relatively close to the river mouths. Here we report the lignin phenol and p-hydroxybenzene composition of Arcticriver DOC in order to identify major sources of carbon. Arcticriver DOC represents an important carbon conduit linking the large pools of organic carbon in the Arctic/Subarctic watersheds to the Arctic Ocean. Most of the annual lignin discharge (>75%) occurs during the two month of spring freshet with extremely high lignin concentrations and a lignin phenol composition indicative of fresh vegetation from boreal forests. The three large Siberian rivers, Lena, Yenisei, and Ob, which also have the highest proportion of forests within their watersheds, contribute about 90% of the total lignin discharge to the Arctic Ocean. The composition of river DOC is also characterized by elevated levels of p-hydroxybenzenes, particularly during the low flow season, which indicates a larger contribution from mosses and peat bogs. The lignin composition was strongly related to the average 14C-age of DOC supporting the abundance of young, boreal-vegetation-derived leachates during spring flood, and older, soil-, peat-, and wetland-derived DOC during groundwater dominated low flow conditions, particularly in the Ob and Yukon Rivers. We observed significant differences in DOC concentration and composition between the rivers over the seasonal cycles with the Mackenzie River being the most unique, the Lena River being similar to the Yenisei, and the Yukon being most similar to the Ob. The observed relationship between the lignin phenol composition and watershed characteristics suggests that DOC discharge from these rivers could increase in a warmer climate under otherwise undisturbed conditions
Original languageEnglish
JournalGeochimica et Cosmochimica Acta
Pages (from-to)217-237
StatePublished - 2012
Externally publishedYes
CitationsWeb of Science® Times Cited: 88
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ID: 10732067