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随着群落适应,热带土壤变暖时微生物多样性下降,呼吸作用增强幅度超过预测。

Microbial diversity declines in warmed tropical soil and respiration rise exceed predictions as communities adapt.

作者信息

Nottingham Andrew T, Scott Jarrod J, Saltonstall Kristin, Broders Kirk, Montero-Sanchez Maria, Püspök Johann, Bååth Erland, Meir Patrick

机构信息

School of Geography, University of Leeds, Leeds, UK.

School of Geosciences, University of Edinburgh, Edinburgh, UK.

出版信息

Nat Microbiol. 2022 Oct;7(10):1650-1660. doi: 10.1038/s41564-022-01200-1. Epub 2022 Sep 5.

DOI:10.1038/s41564-022-01200-1
PMID:36065063
Abstract

Perturbation of soil microbial communities by rising temperatures could have important consequences for biodiversity and future climate, particularly in tropical forests where high biological diversity coincides with a vast store of soil carbon. We carried out a 2-year in situ soil warming experiment in a tropical forest in Panama and found large changes in the soil microbial community and its growth sensitivity, which did not fully explain observed large increases in CO emission. Microbial diversity, especially of bacteria, declined markedly with 3 to 8 °C warming, demonstrating a breakdown in the positive temperature-diversity relationship observed elsewhere. The microbial community composition shifted with warming, with many taxa no longer detected and others enriched, including thermophilic taxa. This community shift resulted in community adaptation of growth to warmer temperatures, which we used to predict changes in soil CO emissions. However, the in situ CO emissions exceeded our model predictions threefold, potentially driven by abiotic acceleration of enzymatic activity. Our results suggest that warming of tropical forests will have rapid, detrimental consequences both for soil microbial biodiversity and future climate.

摘要

气温上升对土壤微生物群落的扰动可能会对生物多样性和未来气候产生重要影响,特别是在热带森林中,那里丰富的生物多样性与大量的土壤碳储量并存。我们在巴拿马的一片热带森林中进行了为期两年的原位土壤升温实验,发现土壤微生物群落及其生长敏感性发生了巨大变化,但这并不能完全解释观测到的二氧化碳排放量的大幅增加。微生物多样性,尤其是细菌多样性,在升温3至8摄氏度时显著下降,这表明在其他地方观察到的正温度-多样性关系出现了破裂。微生物群落组成随升温而变化,许多分类群不再被检测到,而其他分类群则有所富集,包括嗜热分类群。这种群落变化导致群落生长适应更温暖的温度,我们利用这一点来预测土壤二氧化碳排放量的变化。然而,原位二氧化碳排放量超出我们模型预测的三倍,这可能是由酶活性的非生物加速驱动的。我们的结果表明,热带森林变暖将对土壤微生物生物多样性和未来气候产生迅速而有害的影响。

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