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Winter climate change affects growing-season soil microbial biomass and activity in northern hardwood forests

机译:冬季气候变化影响北部硬木森林生长季节土壤微生物的生物量和活动

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摘要

Understanding the responses of terrestrial ecosystems to global change remains a major challenge of ecological research. We exploited a natural elevation gradient in a northern hardwood forest to determine how reductions in snow accumulation, expected with climate change, directly affect dynamics of soil winter frost, and indirectly soil microbial biomass and activity during the growing season. Soils from lower elevation plots, which accumulated less snow and experienced more soil temperature variability during the winter (and likely more freeze/thaw events), had less extractable inorganic nitrogen (N), lower rates of microbial N production via potential net N mineralization and nitrification, and higher potential microbial respiration during the growing season. Potential nitrate production rates during the growing season were particularly sensitive to changes in winter snow pack accumulation and winter soil temperature variability, especially in spring. Effects of elevation and winter conditions on N transformation rates differed from those on potential microbial respiration, suggesting that N-related processes might respond differently to winter climate change in northern hardwood forests than C-related processes.
机译:了解陆地生态系统对全球变化的反应仍然是生态研究的主要挑战。我们利用北部硬木森林中的自然海拔梯度来确定随着气候变化而预期的积雪减少如何直接影响土壤冬季霜冻的动态,并间接影响生长季节土壤微生物的生物量和活性。海拔较低的地块的土壤积雪较少,冬季的土壤温度变化较大(并且可能发生更多的冻融事件),可提取的无机氮(N)较少,通过潜在的净氮矿化产生的微生物氮的产生速率较低,硝化作用和生长季节更高的潜在微生物呼吸作用。生长季节潜在的硝酸盐生产率对冬季积雪和冬季土壤温度的变化特别敏感,特别是在春季。海拔和冬季条件对氮转化率的影响与对潜在微生物呼吸的影响不同,这表明北硬木森林中与氮相关的过程对冬季气候变化的响应可能与与碳相关的过程不同。

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