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土壤生物对全球变化响应的元分析。

A meta-analysis of responses of soil biota to global change.

机构信息

Department of Biological Sciences, Northern Arizona University, PO Box 5640, Flagstaff, AZ 86011, USA

出版信息

Oecologia. 2011 Mar;165(3):553-65. doi: 10.1007/s00442-011-1909-0. Epub 2011 Jan 28.

Abstract

Global environmental changes are expected to impact the abundance of plants and animals aboveground, but comparably little is known about the responses of belowground organisms. Using meta-analysis, we synthesized results from over 75 manipulative experiments in order to test for patterns in the effects of elevated CO(2), warming, and altered precipitation on the abundance of soil biota related to taxonomy, body size, feeding habits, ecosystem type, local climate, treatment magnitude and duration, and greenhouse CO(2) enrichment. We found that the positive effect size of elevated CO(2) on the abundance of soil biota diminished with time, whereas the negative effect size of warming and positive effect size of precipitation intensified with time. Trophic group, body size, and experimental approaches best explained the responses of soil biota to elevated CO(2), whereas local climate and ecosystem type best explained responses to warming and altered precipitation. The abundance of microflora and microfauna, and particularly detritivores, increased with elevated CO(2), indicative of microbial C limitation under ambient CO(2). However, the effects of CO(2) were smaller in field studies than in greenhouse studies and were not significant for higher trophic levels. Effects of warming did not depend on taxon or body size, but reduced abundances were more likely to occur at the colder and drier sites. Precipitation limited all taxa and trophic groups, particularly in forest ecosystems. Our meta-analysis suggests that the responses of soil biota to global change are predictable and unique for each global change factor.

摘要

全球环境变化预计会影响地上动植物的丰度,但对于地下生物的响应,我们知之甚少。我们通过荟萃分析,综合了 75 多项控制性实验的结果,以检验大气 CO2 浓度升高、气候变暖以及降水改变对与分类学、体型、食性、生态系统类型、当地气候、处理幅度和持续时间以及温室 CO2 富集有关的土壤生物丰度的影响模式。我们发现,CO2 浓度升高对土壤生物丰度的正向效应大小随时间而减小,而变暖的负向效应大小和降水的正向效应大小随时间而增大。营养类群、体型和实验方法最好地解释了土壤生物对 CO2 浓度升高的响应,而当地气候和生态系统类型最好地解释了对变暖以及降水改变的响应。微生物和微小动物,特别是分解者的丰度随着 CO2 浓度升高而增加,表明在大气 CO2 下微生物受到 C 限制。然而,CO2 的影响在田间研究中比在温室研究中要小,并且对于较高的营养水平并不显著。变暖的影响不依赖于分类群或体型,但在较冷和较干燥的地点,丰度减少的可能性更大。降水限制了所有分类群和营养类群,特别是在森林生态系统中。我们的荟萃分析表明,土壤生物对全球变化的响应是可预测的,并且对每个全球变化因素都是独特的。

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