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The role of sediments in the carbon budget of a small boreal lake

Chmiel, Hannah Elisa, 1983- (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
Kokic, Jovana (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
Denfeld, Blaize Amber (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
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Einarsdóttir, Karólina (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
Wallin, Marcus (author)
Uppsala universitet,Limnologi,Luft-, vatten- och landskapslära,Uppsala University, Sweden
Köhler, Birgit (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
Isidorova, Anastasija (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
Bastviken, David (author)
Linköpings universitet,Tema Miljöförändring,Filosofiska fakulteten
Ferland, Marie-Ève (author)
Université du Québec à Montréal, Québec, Canada,Groupe de Recherche Interuniversitaire en Limnologie
Sobek, Sebastian (author)
Uppsala universitet,Limnologi,Uppsala University, Sweden
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 (creator_code:org_t)
2016-06-24
2016
English.
In: Limnology and Oceanography. - : Wiley. - 0024-3590 .- 1939-5590. ; 61:5, s. 1814-1825
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • We investigated the role of lake sediments as carbon (C) source and sink in the annual C budget of a small (0.07 km2), shallow (mean depth 3.4 m), and humic lake (mean DOC concentration 17 mg L-1) in boreal Sweden. Organic carbon (OC) burial and mineralization in sediments were quantified from 210Pb-dated sediment and laboratory sediment incubation experiments, respectively, and upscaled to the entire basin and to one whole year, by using sediment thickness derived sub-bottom profiling, basin morphometry, and water column monitoring data of temperature and oxygen concentration. Furthermore, catchment C import, open water metabolism, photochemical mineralization as well as carbon dioxide (CO2) and methane (CH4) emissions to the atmosphere, were quantified to relate sediment processes to other lake C fluxes. We found that on a whole-basin and annual scale, sediment OC mineralization was three times larger than OC burial, and contributed about 16% to the annual CO2 emission from the lake to the atmosphere. Remaining contributions to the CO2 emission were attributed to water column metabolism (31%), photochemical mineralization (6%), and catchment imports via inlet streams and inflow of shallow groundwater (47%). We conclude that on an annual and whole-basin scale 1) sediment OC mineralization dominated over OC burial, 2) water column OC mineralization contributed more than sediments to lake CO2 emission, and 3) catchment import of C to the lake was greater than lake-internal C cycling. 

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)

Keyword

mineralization
burial
carbon dioxide
methane
emission
photomineralization
Biologi med inriktning mot limnologi
Biology with specialization in Limnology

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ref (subject category)
art (subject category)

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