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From:Biogeosciences (Vol. 19, Issue 7) Peer-ReviewedBoreal upland forests are generally considered methane (CH.sub.4) sinks due to the predominance of CH.sub.4 oxidizing bacteria over the methanogenic archaea. However, boreal upland forests can temporarily act as CH.sub.4...
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From:Biogeosciences (Vol. 18, Issue 3) Peer-ReviewedThe patterned microtopography of subarctic mires generates a variety of environmental conditions, and carbon dioxide (CO.sub.2) and methane (CH.sub.4) dynamics vary spatially among different plant community types (PCTs)....
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From:Biogeosciences (Vol. 17, Issue 23) Peer-Reviewed
Water flow controls the spatial variability of methane emissions in a northern valley fen ecosystem.
Northern 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:Canadian Journal of Forest Research (Vol. 42, Issue 2) Peer-ReviewedPeatland forests constitute a significant timber resource in several boreal countries. In Finland, peatlands have been intensively managed with large-scale drainage operations to enhance growth of the stands. In...