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From:Biogeosciences (Vol. 18, Issue 16) Peer-ReviewedPristine boreal mires are known as substantial sinks of carbon dioxide (CO.sub.2) and net emitters of methane (CH.sub.4). Bogs constitute a major fraction of pristine boreal mires. However, the bog CO.sub.2 and CH.sub.4...
From:Biogeosciences (Vol. 16, Issue 11) Peer-Reviewed
We measured methane ebullition from a patterned boreal bog situated in the Siikaneva wetland complex in southern Finland. Measurements were conducted on water (W) and bare peat surfaces (BP) in three growing seasons...
From:Biogeosciences (Vol. 15, Issue 6) Peer-ReviewedByline: Aino Korrensalo, Elisa Mä,nnistö,, Pavel Alekseychik, Ivan Mammarella, Janne Rinne, Timo Vesala, Eeva-Stiina Tuittila To access, purchase, authenticate, or subscribe to the full-text of this article,...
From:Biogeosciences (Vol. 17, Issue 3) Peer-ReviewedVegetation and hydrology are important controlling factors in peatland methane dynamics. This study aimed at investigating the role of vegetation components, sedges, dwarf shrubs, and Sphagnum mosses, in methane fluxes...
From:Biogeosciences (Vol. 17, Issue 23) Peer-ReviewedNorthern peatlands are projected to be crucial in future atmospheric methane (CH.sub.4) budgets and have a positive feedback on global warming. Fens receive nutrients from catchments via inflowing water and are more...
From:Biogeosciences (Vol. 14, Issue 2) Peer-ReviewedIn boreal bogs plant species are low in number, but they differ greatly in their growth forms and photosynthetic properties. We assessed how ecosystem carbon (C) sink dynamics were affected by seasonal variations in the...
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