Spatial variation in CO2 exchange at a northern aapa mire

被引:0
作者
Liisa Maanavilja
Terhi Riutta
Mika Aurela
Minna Pulkkinen
Tuomas Laurila
Eeva-Stiina Tuittila
机构
[1] University of Helsinki,Department of Forest Sciences
[2] Finnish Meteorological Institute,Environmental Change Institute, School of Geography and the Environment
[3] University of Oxford,undefined
来源
Biogeochemistry | 2011年 / 104卷
关键词
Chamber; Eddy covariance; Functional diversity; Net ecosystem exchange; Peatland; Photosynthesis; Plant community; Respiration;
D O I
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中图分类号
学科分类号
摘要
We compared the CO2 exchange and its controls in the plant communities of a strongly patterned aapa mire, the Kaamanen fen in northern Finland. Based on a systematic vegetation inventory and an ordination analysis, four plant community types were chosen for the study: Ericales–Pleurozium string tops, Betula–Sphagnum string margins, Trichophorum tussock flarks and Carex–Scorpidium wet flarks. We measured plant community CO2 exchange with a closed chamber technique during the growing season of 2007 and early summer of 2008. Nonlinear regression models were used for simulating the CO2 exchange over the measurement period for different mire components and for the whole mire. The CO2 exchange dynamics distinguished two functional components in the mire: an ombrotrophic component (Ericales–Pleurozium string tops) and a minerotrophic component (other plant community types). Minerotrophic plant communities responded similarly to environmental controls, the most important of these being variation in leaf area and aerobic peat volume (water level). The ombrotrophic component dynamics were more obscure; frost and possibly peat moisture played a role. The minerotrophic communities functioned as effective CO2 sinks in the simulation, while the net CO2 exchange of the ombrotrophic community was close to zero. The smaller NEE of the ombrotrophic community was due to less efficient photosynthesis per unit leaf area in combination with high ecosystem respiration resulting from a large aerobic peat volume. Our study shows that a fen/bog functional dichotomy can also exist within one mire. Wet minerotrophic communities within northern mires can act as effective CO2 sinks.
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页码:325 / 345
页数:20
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共 213 条
  • [1] Ahti T(1968)Vegetation zones and their sections in northwestern Europe Ann Bot Fenn 5 169-211
  • [2] Hämet-Ahti L(1999)Carbon balance of a boreal bog during a year with an exceptionally dry summer Ecology 80 161-174
  • [3] Jalas J(2007)Methods for determining emission factors for the use of peat and peatlands—flux measurements and modelling Boreal Environ Res 12 85-100
  • [4] Alm J(1998)Carbon dioxide exchange in a subarctic peatland ecosystem in northern Europe measured by the eddy covariance technique J Geophys Res D: Atmos 103 11289-11301
  • [5] Schulman L(2001)Seasonal CO J Geophys Res D: Atmos 106 1623-1637
  • [6] Walden J(2002) balances of a subarctic mire J Geophys Res D: Atmos 107 4607-492
  • [7] Nykänen H(2004)Annual CO Geophys Res Lett 31 L16119-210
  • [8] Martikainen PJ(2008) balance of a subarctic fen in northern Europe: importance of the wintertime efflux J Geophys Res G: Biogeosci 113 G03026-46
  • [9] Silvola J(2003)The timing of snow melt controls the annual CO Global Change Biol 9 479-714
  • [10] Alm J(2003) balance in a subarctic fen Appl Soil Ecol 22 205-27692