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根据未来降水模式重新评估森林干旱实验、生态系统碳和分解率的响应:一项荟萃分析。

Revaluating forest drought experiments according to future precipitation patterns, ecosystem carbon and decomposition rate responses: A meta-analysis.

机构信息

Earthwatch Institute, Mayfield House, 256 Banbury Road, Oxford, OX2 7DE, UK.

Scion, Titokorangi Drive, Private Bag 3020, Rotorua, 3046, New Zealand.

出版信息

Ambio. 2022 May;51(5):1227-1238. doi: 10.1007/s13280-021-01645-4. Epub 2021 Oct 25.

DOI:10.1007/s13280-021-01645-4
PMID:34697767
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8931167/
Abstract

Moisture availability is a strong determinant of decomposition rates in forests worldwide. Climate models suggest that many terrestrial ecosystems are at risk from future droughts, suggesting moisture limiting conditions will develop across a range of forests worldwide. The impacts of increasing drought conditions on forest carbon (C) fluxes due to shifts in organic matter decay rates may be poorly characterised due to limited experimental research. To appraise this question, we conducted a meta-analysis of forest drought experiment studies worldwide, examining spatial limits, knowledge gaps and potential biases. To identify limits to experimental knowledge, we projected the global distribution of forest drought experiments against spatially modelled estimates of (i) future precipitation change, (ii) ecosystem total above-ground C and (iii) soil C storage. Our assessment, involving 115 individual experimental study locations, found a mismatch between the distribution of forest drought experiments and regions with higher levels of future drought risk and C storage, such as Central America, Amazonia, the Atlantic Forest of Brazil, equatorial Africa and Indonesia. Decomposition rate responses in litter and soil were also relatively under-studied, with only 30 experiments specifically examining the potential experimental impacts of drought on C fluxes from soil or litter. We propose new approaches for engaging experimentally with forest drought research, utilising standardised protocols to appraise the impacts of drought on the C cycle, while targeting the most vulnerable and relevant forests.

摘要

水分可用性是全球森林分解速率的一个重要决定因素。气候模型表明,许多陆地生态系统面临未来干旱的风险,这表明全球范围内的一系列森林将面临水分限制条件。由于有机物质分解率的变化,增加干旱条件对森林碳(C)通量的影响可能由于实验研究的限制而特征描述不足。为了评估这个问题,我们对全球范围内的森林干旱实验研究进行了荟萃分析,考察了空间限制、知识空白和潜在偏差。为了确定实验知识的限制,我们根据(i)未来降水变化、(ii)生态系统总地上 C 和(iii)土壤 C 储量的空间模型估计,将全球森林干旱实验的分布与实验进行了对比。我们的评估涉及 115 个独立的实验研究地点,发现森林干旱实验的分布与未来干旱风险和 C 储量较高的地区(如中美洲、亚马逊地区、巴西大西洋森林、赤道非洲和印度尼西亚)不匹配。凋落物和土壤分解率的响应也相对研究不足,只有 30 个实验专门研究了干旱对土壤或凋落物中 C 通量的潜在实验影响。我们提出了新的方法来参与森林干旱研究的实验,利用标准化的协议来评估干旱对 C 循环的影响,同时针对最脆弱和相关的森林。

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Revaluating forest drought experiments according to future precipitation patterns, ecosystem carbon and decomposition rate responses: A meta-analysis.根据未来降水模式重新评估森林干旱实验、生态系统碳和分解率的响应:一项荟萃分析。
Ambio. 2022 May;51(5):1227-1238. doi: 10.1007/s13280-021-01645-4. Epub 2021 Oct 25.
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本文引用的文献

1
Inexpensive throughfall exclusion experiment for single large trees.针对单株大树的低成本林冠穿透排除实验。
Appl Plant Sci. 2020 Feb 14;8(2):e11325. doi: 10.1002/aps3.11325. eCollection 2020 Feb.
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Temperature and rainfall interact to control carbon cycling in tropical forests.温度和降雨相互作用,共同控制热带森林中的碳循环。
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The impacts of increasing drought on forest dynamics, structure, and biodiversity in the United States.日益加剧的干旱对美国森林动态、结构和生物多样性的影响。
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Soil animal responses to moisture availability are largely scale, not ecosystem dependent: insight from a cross-site study.土壤动物对水分可利用性的响应在很大程度上与尺度有关,而不是依赖于生态系统:来自跨站点研究的见解。
Glob Chang Biol. 2014 Aug;20(8):2631-43. doi: 10.1111/gcb.12522. Epub 2014 Apr 30.
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Tree Physiol. 2013 Oct;33(10):1003-5. doi: 10.1093/treephys/tpt092.
9
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New Phytol. 2012 Aug;195(3):518-522. doi: 10.1111/j.1469-8137.2012.04224.x. Epub 2012 Jun 27.
10
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