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元分析表明,地上和地下生产力对干旱的响应不一致。

Meta-analysis shows non-uniform responses of above- and belowground productivity to drought.

机构信息

Department of Ecology, Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing, China.

Department of Ecology, Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing, China; Jiangsu Key Laboratory for Bioresources of Saline Soils, Jiangsu Synthetic Innovation Center for Coastal Bio-agriculture, Jiangsu Provincial Key Laboratory of Coastal Wetland Bioresources and Environmental Protection, Yancheng Teachers University, Yancheng City, China.

出版信息

Sci Total Environ. 2021 Aug 15;782:146901. doi: 10.1016/j.scitotenv.2021.146901. Epub 2021 Apr 5.

Abstract

Terrestrial productivity underpins ecosystem carbon (C) cycling and multi-trophic diversity. Despite the negative impacts of drought on terrestrial C cycling, our understanding of the responses of above- and belowground productivity to drought remains incomplete. Here, we synthesized the responses of terrestrial productivity and soil factors (e.g., soil moisture, soil pH, soil C, soil nitrogen (N), soil C:N, fungi:bacteria ratio, and microbial biomass C) to drought via a global meta-analysis of 734 observations from 107 studies. Our results revealed that the productivity variables above- and belowground (i.e., net primary productivity, aboveground net primary productivity, belowground net primary productivity, total biomass, aboveground biomass, root biomass, gross ecosystem productivity, and net ecosystem productivity) were decreased across all ecosystems. However, drought did not significantly affect litter mass across all ecosystems, and the responses of above- and belowground productivity to drought were non-uniform. Furthermore, the responses of these productivity variables to drought were more pronounced with drought intensity and duration, and consistent across ecosystem types and background climates. Drought significantly decreased soil moisture, soil C concentrations, soil C:N ratios, and microbial biomass C, whereas it enhanced soil pH values and fungi:bacteria ratios. Moreover, the negative effects of drought on above- and belowground productivity variables were correlated mostly with the response of soil pH to drought among all soil factors. Our study indicated that litter biomass, which mostly represents productivity levels via traditional ecosystem models, was not able to predict the responses of terrestrial ecosystem productivity to drought. The strong relationship between the responses of soil pH and terrestrial productivity to drought suggests that the incorporation of soil pH into Earth system models might facilitate the prediction of terrestrial C cycling and its feedbacks to drought.

摘要

陆地生产力是支撑生态系统碳(C)循环和多营养级多样性的基础。尽管干旱对陆地 C 循环有负面影响,但我们对地上和地下生产力对干旱的响应仍不完全了解。在这里,我们通过对来自 107 项研究的 734 个观测值进行全球荟萃分析,综合了陆地生产力和土壤因子(如土壤水分、土壤 pH 值、土壤 C、土壤氮(N)、土壤 C:N 比、真菌与细菌比以及微生物生物量 C)对干旱的响应。我们的研究结果表明,所有生态系统的地上和地下生产力变量(即净初级生产力、地上净初级生产力、地下净初级生产力、总生物量、地上生物量、根生物量、总生态系统生产力和净生态系统生产力)都有所下降。然而,干旱并没有显著影响所有生态系统的凋落物质量,而且地上和地下生产力对干旱的响应并不均匀。此外,这些生产力变量对干旱的响应随着干旱强度和持续时间的增加而更加显著,并且在生态系统类型和背景气候中具有一致性。干旱显著降低了土壤水分、土壤 C 浓度、土壤 C:N 比和微生物生物量 C,而增加了土壤 pH 值和真菌与细菌比。此外,干旱对地上和地下生产力变量的负面影响主要与所有土壤因子中土壤 pH 值对干旱的响应有关。我们的研究表明,凋落物生物量(主要通过传统生态系统模型来代表生产力水平)无法预测陆地生态系统生产力对干旱的响应。土壤 pH 值和陆地生产力对干旱的响应之间的强关系表明,将土壤 pH 值纳入地球系统模型可能有助于预测陆地 C 循环及其对干旱的反馈。

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