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Significance of cold-season respiration and photosynthesis in a subarctic heath ecosystem in Northern Sweden

机译:瑞典北部亚热带石南丛生生态系统冷季呼吸和光合作用的意义

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摘要

While substantial cold-season respiration has been documented in most arctic and alpine ecosystems in recent years, the significance of cold-season photosynthesis in these biomes is still believed to be small. In a mesic, subartic heath during both the cold and warm season, we measured in situ ecosystem respiration and photosynthesis with a chamber technique at ambient conditions and at artificially, increased frequency of freeze-thaw (FT) cycles during fall and spring. We fitted the measured ecosystem exchange rates to respiration and photosynthesis models with R-2-values ranging from 0.81 to 0.85. As expected, estimated cold-season (October, November, April and May) respiration was significant and accounted for at least 22% of the annual respiratory CO2 flux. More surprisingly, estimated photosynthesis during this period accounted for up to 19% of the annual gross CO2 uptake, suggesting that cold-season photosynthesis partly balanced the cold-season respiratory carbon losses and can be significant for the annual cycle of carbon. Still, during the full year the ecosystem was a significant net source of 120 +/- 12g Cm-2 to the atmosphere. Neither respiration nor photosynthetic rates were much affected by the extra FT cycles, although the mean rate of net ecosystem loss decreased slightly, but significantly, in May. The results suggest only a small response of net carbon fluxes to increased frequency of FT cycles in this ecosystem.
机译:尽管近年来已在大多数北极和高山生态系统中记录到大量的冷季呼吸作用,但据信在这些生物群落中冷季光合作用的重要性仍然很小。在寒冷和温暖季节的中亚亚热带荒地中,我们利用室内技术在环境条件下以及在秋季和春季增加了冻融(FT)周期频率的情况下,测量了原位生态系统的呼吸作用和光合作用。我们将测得的生态系统汇率拟合到呼吸和光合作用模型,其R-2-值介于0.81至0.85之间。正如预期的那样,估计的寒冷季节(10月,11月,4月和5月)呼吸作用很明显,至少占年度呼吸CO2通量的22%。更令人惊讶的是,在此期间,估计的光合作用占年度总CO2吸收量的19%,这表明冷季光合作用在一定程度上平衡了冷季呼吸碳损失,并且对于年度碳循环可能很重要。尽管如此,在整个一年中,生态系统还是大气中120 +/- 12g Cm-2的重要净来源。 FT额外的周期对呼吸和光合速率都没有很大的影响,尽管五月份的平均生态系统净损失率略有下降,但显着下降。结果表明,在该生态系统中,净碳通量对FT循环频率增加的响应很小。

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