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CO_2 fluxes at northern fens and bogs have opposite responses to inter-annual fluctuations in water table

机译:北部和沼泽的CO_2通量对地下水位年际波动具有相反的响应

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This study compares eddy-covariance measurements of carbon dioxide fluxes at six northern temperate and boreal peatland sites in Canada and the northern United States of America, representing both bogs and fens. The two peatland types had opposite responses of gross ecosystem photosynthesis (GEP) and ecosystem respiration (ER) to inter-annual fluctuations in water table level. At fens, wetter conditions were correlated with lower GEP and ER, while at bogs wetter conditions were correlated with higher GEP and ER. We hypothesize that these contrasting responses are due to differences in the relative contributions of vascular plants and mosses. The coherence of our results between sites representing a range of average environmental conditions indicates ecosystem-scale differences in resilience to hydrological changes that should be taken into account when considering the future of peatland ecosystem services such as carbon sequestration under changing environmental conditions.
机译:这项研究比较了加拿大和美利坚合众国北部的六个温带和寒带泥炭地站点的二氧化碳通量的涡动协方差测量值,分别代表沼泽和。两种泥炭地对地下水位年际波动的生态系统总光合作用(GEP)和生态系统呼吸(ER)具有相反的响应。在沼泽,较湿的条件与较低的GEP和ER相关,而在沼泽,较湿的条件与较高的GEP和ER相关。我们假设这些相反的反应是由于维管植物和苔藓的相对贡献的差异而引起的。代表一系列平均环境条件的站点之间的结果一致性表明,在考虑泥炭地生态系统服务的未来(例如在不断变化的环境条件下进行固碳)时,应考虑生态系统规模对水文变化适应力的差异。

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