An inter-regional assessment of concentrations and b13C values of methane and dissolved inorganic carbon in small European lakes
An inter-regional assessment of concentrations and b13C values of methane and dissolved inorganic carbon in small European lakes
Methane (CH4) and carbon dioxide emissions from lakes are relevant for assessing the greenhouse gas output of wetlands. However, only few standardized datasets describe concentrations of these gases in lakes across different geographical regions. We studied concentrations and stable carbon isotopic composition (?13C) of CH4 and dissolved inorganic carbon (DIC) in 32 small lakes from Finland, Sweden, Germany, the Netherlands, and Switzerland in late summer. Higher concentrations and ?13C values of DIC were observed in calcareous lakes than in lakes on non-calcareous areas. In stratified lakes, ?13C values of DIC were generally lower in the hypolimnion due to the degradation of organic matter (OM). Unexpectedly, increased ?13C values of DIC were registered above the sediment in several lakes. This may reflect carbonate dissolution in calcareous lakes or methanogenesis in deepwater layers or in the sediments. Surface water CH4 concentrations were generally higher in western and central European lakes than in Fennoscandian lakes, possibly due to higher CH4 production in the littoral sediments and lateral transport, whereas CH4 concentrations in the hypolimnion did not differ significantly between the regions. The ?13C values of CH4 in the sediment suggest that ?13C values of biogenic CH4 are not necessarily linked to ?13C values of sedimentary OM but may be strongly influenced by OM quality and methanogenic pathway. Our study suggests that CH4 and DIC cycling in small lakes differ between geographical regions and that this should be taken into account when regional studies on greenhouse gas emissions are upscaled to inter-regional scales.
CH4, CO2, carbon cycling, greenhouse gas, stable carbon isotopes, lakes
667-680
Rinta, P.
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Bastviken, D.
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van Hardenbroek, M.
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Kankaala, P.
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Leuenberger, M.
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Schilder, J.
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Stötter, T.
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Heiri, O.
21199b62-05e6-48ca-ac1e-a4665e7e6801
October 2015
Rinta, P.
25bb576c-5b87-4aa9-a37f-4289d729c1ba
Bastviken, D.
e79b2d1f-5f5f-415a-894f-5259b7b51162
van Hardenbroek, M.
7ddff57e-78f7-444a-a3fc-946ef7f7bbfc
Kankaala, P.
d756fd0c-ec7b-4b85-8c50-2a7be2387ed9
Leuenberger, M.
34f2d997-e281-4d0a-8436-34f7c0987367
Schilder, J.
2bcce33e-a802-4faa-8084-b10987e7b553
Stötter, T.
3fcc25dd-67c4-4998-ab0f-04ccd40e81d1
Heiri, O.
21199b62-05e6-48ca-ac1e-a4665e7e6801
Rinta, P., Bastviken, D., van Hardenbroek, M., Kankaala, P., Leuenberger, M., Schilder, J., Stötter, T. and Heiri, O.
(2015)
An inter-regional assessment of concentrations and b13C values of methane and dissolved inorganic carbon in small European lakes.
Aquatic Sciences, 77 (4), .
(doi:10.1007/s00027-015-0410-y).
Abstract
Methane (CH4) and carbon dioxide emissions from lakes are relevant for assessing the greenhouse gas output of wetlands. However, only few standardized datasets describe concentrations of these gases in lakes across different geographical regions. We studied concentrations and stable carbon isotopic composition (?13C) of CH4 and dissolved inorganic carbon (DIC) in 32 small lakes from Finland, Sweden, Germany, the Netherlands, and Switzerland in late summer. Higher concentrations and ?13C values of DIC were observed in calcareous lakes than in lakes on non-calcareous areas. In stratified lakes, ?13C values of DIC were generally lower in the hypolimnion due to the degradation of organic matter (OM). Unexpectedly, increased ?13C values of DIC were registered above the sediment in several lakes. This may reflect carbonate dissolution in calcareous lakes or methanogenesis in deepwater layers or in the sediments. Surface water CH4 concentrations were generally higher in western and central European lakes than in Fennoscandian lakes, possibly due to higher CH4 production in the littoral sediments and lateral transport, whereas CH4 concentrations in the hypolimnion did not differ significantly between the regions. The ?13C values of CH4 in the sediment suggest that ?13C values of biogenic CH4 are not necessarily linked to ?13C values of sedimentary OM but may be strongly influenced by OM quality and methanogenic pathway. Our study suggests that CH4 and DIC cycling in small lakes differ between geographical regions and that this should be taken into account when regional studies on greenhouse gas emissions are upscaled to inter-regional scales.
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Accepted/In Press date: 31 July 2015
e-pub ahead of print date: 12 August 2015
Published date: October 2015
Keywords:
CH4, CO2, carbon cycling, greenhouse gas, stable carbon isotopes, lakes
Organisations:
Palaeoenvironment Laboratory (PLUS)
Identifiers
Local EPrints ID: 378302
URI: http://eprints.soton.ac.uk/id/eprint/378302
ISSN: 1015-1621
PURE UUID: cf2a78ab-c963-4546-a295-6d470b6d2573
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Date deposited: 30 Jun 2015 13:48
Last modified: 14 Mar 2024 20:20
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Contributors
Author:
P. Rinta
Author:
D. Bastviken
Author:
M. van Hardenbroek
Author:
P. Kankaala
Author:
M. Leuenberger
Author:
J. Schilder
Author:
T. Stötter
Author:
O. Heiri
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