Water flow controls the spatial variability of methane emissions in a northern valley fen ecosystem

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http://hdl.handle.net/10138/324021

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Zhang , H , Tuittila , E-S , Korrensalo , A , Rasänen , A , Virtanen , T , Aurela , M , Penttilä , T , Laurila , T , Gerin , S , Lindholm , V & Lohila , A 2020 , ' Water flow controls the spatial variability of methane emissions in a northern valley fen ecosystem ' , Biogeosciences , vol. 17 , no. 23 , pp. 6247-6270 . https://doi.org/10.5194/bg-17-6247-2020

Title: Water flow controls the spatial variability of methane emissions in a northern valley fen ecosystem
Author: Zhang, Hui; Tuittila, Eeva-Stiina; Korrensalo, Aino; Rasänen, Aleksi; Virtanen, Tarmo; Aurela, Mika; Penttilä, Timo; Laurila, Tuomas; Gerin, Stephanie; Lindholm, Viivi; Lohila, Annalea
Contributor organization: INAR Physics
Helsinki Institute of Sustainability Science (HELSUS)
Environmental Change Research Unit (ECRU)
Helsinki Institute of Urban and Regional Studies (Urbaria)
Urban Environmental Policy
Tarmo Virtanen / Principal Investigator
Ecosystems and Environment Research Programme
Organismal and Evolutionary Biology Research Programme
Institute for Atmospheric and Earth System Research (INAR)
Date: 2020-12-10
Language: eng
Number of pages: 24
Belongs to series: Biogeosciences
ISSN: 1726-4170
DOI: https://doi.org/10.5194/bg-17-6247-2020
URI: http://hdl.handle.net/10138/324021
Abstract: Northern peatlands are projected to be crucial in future atmospheric methane (CH4) budgets and have a positive feedback on global warming. Fens receive nutrients from catchments via inflowing water and are more sensitive than bogs to variations in their ecohydrology. Yet, due to a lack of data detailing the impacts of moving water on microhabitats and CH4 fluxes in fens, large uncertainties remain with respect to predicting CH4 emissions from these sites under climate changes. We measured CH4 fluxes with manual chambers over three growing seasons (2017-2019) at a northern boreal fen. To address the spatial variation at the site where a stream flows through the long and narrow valley fen, we established sample plots at varying distances from the stream. To link the variations in CH4 emissions to environmental controls, we quantified water levels, peat temperature, dissolved oxygen concentration, vegetation composition, and leaf area index in combination with flux measurements during the growing season in 2019. We found that due to the flowing water, there was a higher water level, cooler peat temperatures, and more oxygen in the peat close to the stream, which also had the highest total leaf area and gross primary production (GPP) values but the lowest CH4 emissions. CH4 emissions were highest at an intermediate distance from the stream where the oxygen concentration in the surface peat was low but GPP was still high. Further from the stream, the conditions were drier and produced low CH4 emissions. Our results emphasize the key role of ecohydrology in CH4 dynamics in fens and, for the first time, show how a stream controls CH4 emissions in a flow-through fen. As valley fens are common peatland ecosystems from the Arctic to the temperate zones, future projections of global CH4 budgets need to take flowing water features into account.
Subject: TABLE DRAWDOWN
BOREAL FEN
CARBON DYNAMICS
VASCULAR PLANTS
CLIMATE-CHANGE
VEGETATION
MIRE
RESPONSES
TEMPERATE
PEATLANDS
1172 Environmental sciences
1171 Geosciences
1181 Ecology, evolutionary biology
Peer reviewed: Yes
Rights: cc_by
Usage restriction: openAccess
Self-archived version: publishedVersion


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