Spatial variation in concentration and sources of organic carbon in the Lena River, Siberia

• Published in: Journal of Geophysical Research: Biogeosciences
• Main Authors: Kutscher, Liselott, Mörth, Carl-Magnus, Porcelli, Don, Hirst, Catherine, Maximov, Trofim, Petrov, Roman, Andersson, Per
• Format: Article in Journal/Newspaper
• Language: English
• Published: Naturhistoriska riksmuseet, Enheten för geovetenskap 2017
• Subjects: DOC; POC Lena River; Geochemistry; Geokemi; Arctic Ocean; Global warming; lena river; permafrost; Siberia
• Online Access: http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-2462; https://doi.org/10.1002/2017JG003858

Global warming in permafrost areas is expected to change fluxes of riverine organic carbon (OC) 22 to the Arctic Ocean. Here OC concentrations, stable carbon isotope signatures (δ13C) and carbon-23 nitrogen ratios (C/N) are presented from 22 sampling stations in the Lena River and 40 of its 24 tributaries. Sampling was conducted during two expeditions: the first in July 2012 in the south 25 and southeastern region and the second in June 2013 in the northern region of the Lena basin. 26 The data showed significant spatial differences in concentrations and major sources of OC. Mean 27 sub-catchment slopes were correlated with OC concentrations, implying that mountainous areas 28 in general had lower concentrations than lowland areas. δ13C and C/N data from tributaries 29 originating in mountainous areas indicated that both dissolved and particulate OC (DOC and 30 POC) were mainly derived from soil organic matter (SOM). In contrast, tributaries originating in 31 lowland areas had larger contributions from fresh vegetation to DOC, while aquatically produced 32 OC was the major source of POC. We suggest that these differences in dominant sources 33 indicated differences in dominant flow pathways. Tributaries with larger influence of fresh 34 vegetation probably had surficial flow pathways, while tributaries with more SOM influence had 35 deeper water flow pathways. Thus, the future export of OC to the Arctic Ocean will likely be 36 controlled by changes in spatial patterns in hydroclimatology and the depth of the active layers 37 influencing the dominant water flow pathways in Arctic river basins.