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生态系统依赖型土壤碳储存对磷富集的响应。

Ecosystem-dependent responses of soil carbon storage to phosphorus enrichment.

机构信息

Institute of Ecology, College of Urban and Environmental Sciences, and Key Laboratory for Earth Surface Processes of the Ministry of Education, Peking University, Beijing, 100871, China.

University of Bordeaux, INRAE, BIOGECO, Pessac, 33615, France.

出版信息

New Phytol. 2023 Jun;238(6):2363-2374. doi: 10.1111/nph.18907. Epub 2023 Apr 10.

Abstract

Phosphorus deposition can stimulate both plant carbon inputs and microbial carbon outputs. However, how P enrichment affects soil organic carbon (SOC) storage and the underlying mechanisms remain unclear. We conducted a meta-analysis of 642 SOC observations from 213 field P addition experiments world-wide and explored the regulations of plant inputs, microbial outputs, plant characteristics, and environmental and experimental factors on SOC responses. We found that, globally, P addition stimulated SOC by 4.0% (95% CI: 2.0-6.0%), but the stimulation only occurred in forest and cropland rather than in grassland. Across sites, the response of SOC correlated with that of plant aboveground rather than belowground biomass, suggesting that the change in plant inputs from aboveground was more important than that from belowground in regulating SOC changes due to P addition. Among multiple factors, plant N fixation status and mean annual temperature were the best predictors for SOC responses to P addition, with SOC stimulation being higher in ecosystems dominated by symbiotic nitrogen fixers and ecosystems in high-temperature regions like tropical forests. Our findings highlight the differential and ecosystem-dependent responses of SOC to P enrichment and can contribute to accurate predictions of soil carbon dynamics in a P-enriched world.

摘要

磷沉积可以刺激植物碳输入和微生物碳输出。然而,磷富集如何影响土壤有机碳(SOC)储存及其潜在机制仍不清楚。我们对全球范围内 213 个野外磷添加实验的 642 个 SOC 观测值进行了荟萃分析,探讨了植物输入、微生物输出、植物特性以及环境和实验因素对 SOC 响应的调控。结果表明,全球范围内,磷添加刺激 SOC 增加了 4.0%(95%置信区间:2.0-6.0%),但这种刺激仅发生在森林和农田,而不是草地。在不同地点,SOC 的响应与地上生物量而不是地下生物量相关,这表明由于磷添加,植物地上部分输入的变化比地下部分输入的变化更重要,从而调节 SOC 的变化。在多种因素中,植物固氮状态和年平均温度是 SOC 对磷添加响应的最佳预测因子,在以共生固氮生物为主导的生态系统和热带雨林等高温地区的生态系统中,SOC 的刺激作用更高。我们的研究结果强调了 SOC 对磷富集的差异化和生态系统依赖性响应,并有助于准确预测富含磷的世界中土壤碳动态。

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