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微生物对磷的竞争限制了成熟森林对 CO 的响应。

Microbial competition for phosphorus limits the CO response of a mature forest.

机构信息

College of Life Sciences, Zhejiang University, Hangzhou, China.

Hawkesbury Institute for the Environment, Western Sydney University, Penrith, New South Wales, Australia.

出版信息

Nature. 2024 Jun;630(8017):660-665. doi: 10.1038/s41586-024-07491-0. Epub 2024 Jun 5.

DOI:10.1038/s41586-024-07491-0
PMID:38839955
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11186757/
Abstract

The capacity for terrestrial ecosystems to sequester additional carbon (C) with rising CO concentrations depends on soil nutrient availability. Previous evidence suggested that mature forests growing on phosphorus (P)-deprived soils had limited capacity to sequester extra biomass under elevated CO (refs. ), but uncertainty about ecosystem P cycling and its CO response represents a crucial bottleneck for mechanistic prediction of the land C sink under climate change. Here, by compiling the first comprehensive P budget for a P-limited mature forest exposed to elevated CO, we show a high likelihood that P captured by soil microorganisms constrains ecosystem P recycling and availability for plant uptake. Trees used P efficiently, but microbial pre-emption of mineralized soil P seemed to limit the capacity of trees for increased P uptake and assimilation under elevated CO and, therefore, their capacity to sequester extra C. Plant strategies to stimulate microbial P cycling and plant P uptake, such as increasing rhizosphere C release to soil, will probably be necessary for P-limited forests to increase C capture into new biomass. Our results identify the key mechanisms by which P availability limits CO fertilization of tree growth and will guide the development of Earth system models to predict future long-term C storage.

摘要

陆地生态系统在 CO 浓度升高的情况下固碳(C)的能力取决于土壤养分的供应情况。先前的证据表明,在磷(P)匮乏的土壤上生长的成熟森林在高浓度 CO 下固碳的能力有限(参考文献),但对生态系统 P 循环及其对 CO 的响应的不确定性是对气候变化下陆地 C 汇进行机制预测的一个关键瓶颈。在这里,通过为暴露在高浓度 CO 下的有限 P 成熟森林编制第一个全面的 P 预算,我们表明,土壤微生物捕获的 P 极有可能限制生态系统 P 循环和植物吸收的 P 可用性。树木有效地利用了 P,但微生物对矿化土壤 P 的先占似乎限制了树木在高浓度 CO 下增加 P 吸收和同化的能力,因此也限制了它们固碳的能力。刺激微生物 P 循环和植物 P 吸收的植物策略,例如增加根际 C 向土壤的释放,可能对于 P 限制的森林增加新生物量中的 C 捕获是必要的。我们的结果确定了 P 供应限制树木生长 CO 施肥的关键机制,并将指导地球系统模型的开发,以预测未来的长期 C 储存。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/b727fe790e06/41586_2024_7491_Fig12_ESM.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/930a7075b6c9/41586_2024_7491_Fig1_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/8b92faae0e16/41586_2024_7491_Fig6_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/176aa8b9363d/41586_2024_7491_Fig7_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/1b22f2d9ae4a/41586_2024_7491_Fig8_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/0f430bae12d0/41586_2024_7491_Fig9_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/0f10c763f4ee/41586_2024_7491_Fig10_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/33df1648b9eb/41586_2024_7491_Fig11_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c9a7/11186757/b727fe790e06/41586_2024_7491_Fig12_ESM.jpg

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Direct evidence for phosphorus limitation on Amazon forest productivity.直接证据表明磷限制了亚马逊森林的生产力。
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