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高寒土壤在气候变化下的微生物活性。

Microbial activity in alpine soils under climate change.

机构信息

Department of Ecological and Biological Sciences, University of Tuscia, Largo dell'Università, 01100 Viterbo, Italy.

Laboratory of Environmental Microbiology, Institute of Microbiology of the Czech Academy of Sciences, Vídeňská 1083, 14220 Praha 4, Czech Republic.

出版信息

Sci Total Environ. 2021 Aug 20;783:147012. doi: 10.1016/j.scitotenv.2021.147012. Epub 2021 Apr 10.

Abstract

Soil enzymatic activity was assessed in the Stelvio Pass area (Italian Central Alps) aiming to define the possible effects of climate change on microbial functioning. Two sites at two different elevations were chosen, a subalpine (2239 m) and an alpine belt (2604-2624 m), with mean annual air temperature differing by almost 3 °C, coherent with the worst future warming scenario (RCP 8.5) by 2100. The lower altitude site may represent a proxy of the potential future situation at higher altitude after the upward shift of subalpine vegetation due to climate change. Additionally, hexagonal open top chambers (OTCs) were installed at the upper site, to passively increase by about 2 °C the summer inner temperature to simulate short term effects of warming before the vegetation shift takes place. Soil physicochemical properties and the bacterial and fungal abundances of the above samples were also considered. The subalpine soils showed a higher microbial activity, especially for hydrolytic enzymes, higher carbon, ammonium and hydrogen (p < 0.001) contents, and a slightly higher PO content (p < 0.05) than alpine soils. Bacterial abundance was higher than fungal abundance, both for alpine and subalpine soils. On the other hand, the short term effect, which increased the mean soil temperature during the peak of the growing season in the OTC, showed to induce scarcely significant differences for edaphic parameters and microbial biomass content among the warmed and control plots. Using the manipulative warming experiments, we demonstrated that warming is able to change the enzyme activity starting from colder and higher altitude sites, known to be more vulnerable to the rising temperatures associated with climate change. Although five-years of experimental warming does not allow us to make bold conclusions, it appeared that warming-induced upwards vegetation shift might induce more substantial changes in enzymatic activities than the short-term effects, in the present vegetation context.

摘要

本研究旨在评估气候变化对土壤微生物功能的可能影响,因此选择了意大利中阿尔卑斯山的斯特尔维奥山口地区(Stelvio Pass area)进行土壤酶活性评估。该地区选择了两个不同海拔的地点,一个是亚高山带(2239 米),一个是高山带(2604-2624 米),两地的年平均气温相差近 3°C,与 2100 年最坏的未来变暖情景(RCP 8.5)一致。海拔较低的地点可能代表了由于气候变化,亚高山带植被向上迁移后,高海拔地区潜在未来情况的代表。此外,在较高的地点安装了六边形开顶箱(hexagonal open top chambers,OTCs),以被动地将夏季内部温度升高约 2°C,模拟植被迁移前的短期变暖效应。还考虑了上述样本的土壤物理化学性质以及细菌和真菌丰度。亚高山带土壤表现出更高的微生物活性,尤其是水解酶活性,其碳、铵和氢含量更高(p < 0.001),PO 含量略高(p < 0.05),而高山带土壤则相反。细菌丰度高于真菌丰度,高山带和亚高山带土壤均如此。另一方面,短期增温(在 OTC 中生长季高峰期增加土壤平均温度)的短期效应表明,在变暖和对照样地之间,土壤参数和微生物生物量含量几乎没有显著差异。通过操纵性增温实验,我们证明了增温能够改变较冷和较高海拔地区的酶活性,这些地区已知更容易受到与气候变化相关的升温影响。尽管五年的实验增温还不能让我们得出大胆的结论,但在当前的植被环境下,增温引起的植被向上迁移可能会引起比短期效应更显著的酶活性变化。

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