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谨慎地变暖改变了过去土地利用历史所引起的多维土壤遗留效应。

Warming deferentially altered multidimensional soil legacy induced by past land use history.

机构信息

Key Laboratory of Biometallurgy of Ministry of Education, School of Minerals Processing and Bioengineering, Central South University, Changsha, 410083, China.

Key Laboratory of Plant Nutrition and Fertilizer, Ministry of Agriculture, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.

出版信息

Sci Rep. 2018 Jan 24;8(1):1546. doi: 10.1038/s41598-018-19912-y.

Abstract

The legacy effects of previous land use and climate history may affect current soil function. However, the manner in which these legacy effects of land use are modulated by the subsequent climate remains unclear. For this reason, we investigated how the legacies of soil multiple functions left by conversion of grassland to agricultural management were mediated by climate warming with a reciprocal transplant approach. The overall legacy was further separated into the contributions by changes in the abiotic properties of the soil (abiotic process) and microbial community (biotic process). We here hypothesized that warming may mediate the legacy effects of previous land use, mainly by changing biotic processes. Results indicated that warming significantly influenced the total legacies of soil respiration and three exoenzyme activities representing recalcitrant carbon, nitrogen, and phosphorus cycling, but did not affect the total legacy of β-1,4-glucosidase activity, which is involved in labile carbon cycling. The relative contributions of abiotic and biotic processes to the warming effects on the total legacy depended on the type of soil function. The effects of warming on land use change legacies were derived from altered bacterial community structure. The results of the present study suggest that climate conditions could interact with land use legacy to determine the ecosystem functions in a process-specific way.

摘要

先前土地利用和气候历史的遗留效应对当前土壤功能可能会产生影响。然而,土地利用的这些遗留效应对后续气候的调节方式尚不清楚。出于这个原因,我们采用往复移植的方法,研究了草原转化为农业管理后土壤多种功能的遗留效应对气候变暖的响应机制。整体遗留效应进一步分为土壤非生物特性(非生物过程)和微生物群落(生物过程)变化所带来的影响。我们假设,变暖可能主要通过改变生物过程来调节先前土地利用的遗留效应。结果表明,变暖显著影响土壤呼吸和代表难降解碳、氮和磷循环的三种外切酶活性的总遗留效应,但不影响参与易降解碳循环的β-1,4-葡萄糖苷酶活性的总遗留效应。非生物和生物过程对变暖影响总遗留效应的相对贡献取决于土壤功能的类型。变暖对土地利用变化遗留效应的影响源自于细菌群落结构的改变。本研究的结果表明,气候条件可能会与土地利用遗留效应相互作用,以特定的方式决定生态系统功能。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/edd1/5784121/d7a7ce64db8c/41598_2018_19912_Fig1_HTML.jpg

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