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Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent

机译:全球分解实验表明,土壤动物对分解的影响取决于气候

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摘要

Climate and litter quality are primary drivers of terrestrial decomposition and, based on evidence from multisite experiments at regional and global scales, are universally factored into global decomposition models. In contrast, soil animals are considered key regulators of decomposition at local scales but their role at larger scales is unresolved. Soil animals are consequently excluded from global models of organic mineralization processes. Incomplete assessment of the roles of soil animals stems from the difficulties of manipulating invertebrate animals experimentally across large geographic gradients. This is compounded by deficient or inconsistent taxonomy. We report a global decomposition experiment to assess the importance of soil animals in C mineralization, in which a common grass litter substrate was exposed to natural decomposition in either control or reduced animal treatments across 30 sites distributed from 43 degree S to 68 degree N on six continents. Animals in the mesofaunal size range were recovered from the litter by Tullgren extraction and identified to common specifications, mostly at the ordinal level. The design of the trials enabled faunal contribution to be evaluated against abiotic parameters between sites. Soil animals increase decomposition rates in temperate and wet tropical climates, but have neutral effects where temperature or moisture constrain biological activity. Our findings highlight that faunal influences on decomposition are dependent on prevailing climatic conditions. We conclude that (1) inclusion of soil animals will improve the predictive capabilities of region- or biome-scale decomposition models, (2) soil animal influences on decomposition are important at the regional scale when attempting to predict global change scenarios, and (3) the statistical relationship between decomposition rates and climate, at the global scale, is robust against changes in soil faunal abundance and diversity.
机译:气候和垃圾质量是陆地分解的主要驱动力,根据区域和全球规模的多站点实验的证据,普遍将其纳入全球分解模型。相比之下,土壤动物在地方尺度上被认为是分解的关键调节剂,但在更大尺度上它们的作用尚待解决。因此,将土壤动物排除在有机矿化过程的整体模型之外。对土壤动物作用的不完整评估是由于在较大的地理梯度上实验性地处理无脊椎动物而造成的。分类不足或不一致会使情况更加复杂。我们报告了一项全球分解实验,以评估土壤动物在C矿化中的重要性,其中常见的草屑底物在从60°N到60°N的30个站点的对照或减少动物处理中暴露于自然分解大洲。通过Tullgren提取从同窝中恢复了中足大小范围的动物,并按照共同的标准对其进行了鉴定,主要是按序数水平。试验的设计使动物的贡献可以根据站点之间的非生物参数进行评估。在温带和潮湿的热带气候中,土壤动物会增加分解速率,但在温度或湿度限制其生物活性的情况下,土壤动物具有中性作用。我们的发现表明,动物对分解的影响取决于主要的气候条件。我们得出的结论是:(1)包含土壤动物将提高区域或生物群落尺度分解模型的预测能力;(2)在尝试预测全球变化情况时,土壤动物对分解的影响在区域尺度上很重要;(3) )在全球范围内,分解速率与气候之间的统计关系对于抵御土壤动物丰度和多样性的变化是有力的。

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