Department of Microbiology, University of Washington, Seattle, WA, USA.
Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, The Netherlands.
Sci Rep. 2018 Jun 11;8(1):8862. doi: 10.1038/s41598-018-27168-9.
The increase of extreme drought and precipitation events due to climate change will alter microbial processes. Perturbation experiments demonstrated that microbes are sensitive to environmental alterations. However, only little is known on the legacy effects in microbial systems. Here, we designed a laboratory microcosm experiment using aerobic methane-consuming communities as a model system to test basic principles of microbial resilience and the role of changes in biomass and the presence of non-methanotrophic microbes in this process. We focused on enrichments from soil, sediment, and water reflecting communities with different legacy with respect to exposure to drought. Recovery rates, a recently proposed early warning indicator of a critical transition, were utilized as a measure to detect resilience loss of methane consumption during a series of dry/wet cycle perturbations. We observed a slowed recovery of enrichments originating from water samples, which suggests that the community's legacy with a perturbation is a contributing factor for the resilience of microbial functioning.
由于气候变化,极端干旱和降水事件的增加将改变微生物过程。扰动实验表明,微生物对环境变化很敏感。然而,对于微生物系统中的遗留效应知之甚少。在这里,我们设计了一个实验室微宇宙实验,使用好氧甲烷消耗群落作为模型系统,以测试微生物弹性的基本原理以及生物量变化和非甲烷氧化微生物存在在此过程中的作用。我们专注于从土壤、沉积物和水的富集物中进行研究,这些富集物反映了在干旱暴露方面具有不同遗留特征的群落。恢复率,最近提出的用于检测临界转变的早期预警指标,被用作在一系列干湿循环扰动期间检测甲烷消耗弹性损失的一种手段。我们观察到来自水样的富集物恢复速度较慢,这表明群落的扰动遗留特征是微生物功能弹性的一个影响因素。