ISSN 1000-3665 CN 11-2202/P

    地下水中微生物对气候变化的响应研究进展

    Responses of groundwater microorganisms to climate change: a review

    • 摘要: 气候变化正加剧水循环失衡与水资源危机,对地下水系统构成严重威胁。微生物在地下水物质循环和能量流动过程中起到关键作用,了解地下生态系统中生物和非生物驱动因素的相互作用是预测未来气候变化对地下水资源和栖息地的影响所必需的。系统梳理了微生物群落在增温、降水变化、海水入侵和有机物输入等因素驱动下的响应规律。研究表明温度升高通过改变微生物酶活性、代谢速率及气体溶解度等,影响其群落结构与功能,并扰动食物网相互作用。持续干旱导致土壤干裂,削弱地下水补给并形成强渗流脉冲,进而改变群落结构,部分细菌以休眠保活,而真菌则表现出更强的耐旱能力。极端降水可显著增加补给量并抬升地下水水位,同时通过改变物理特性、溶解性有机碳和硝酸盐浓度等,驱动功能微生物群演化。海水入侵则促使海洋微生物进入含水层,影响微生物介导的碳、氮、硫等循环过程。此外,有机物输入变化可引起微生物群落的定向演替,并与污染物迁移转化存在耦合效应进而影响污染物降解效率。目前的研究多基于测序、稳定同位素探针等方法探究气候变化下微生物响应特征,未来亟需通过深化机理研究并发展包含微生物过程的高精度预测模型,为地下水资源保护与生态修复提供科学支撑。

       

      Abstract: Climate change is exacerbating the imbalance of the water circulation and the water resource crisis, posing a severe threat to groundwater systems. Microorganisms play a central role in regulating material recycling and energy fluxes in groundwater system. Understanding the interplay of biotic and abiotic drivers in subterranean ecosystems is required to anticipate effects of climate change on the sustainability of groundwater resources. Here, this review systematically synthesizes the responses of microbial communities to individual and multiple global change factors, including warming, altered precipitation, seawater intrusion, and organic matter input. It is well documented that a change in temperature affects microbial community composition and food web by altering microbial metabolic rates, enzyme activities, and gas solubility. Prolonged drought results in the decreased water retention capacity of soils and groundwater recharge. The associated formation of cracks could lead to stronger seepage water pulses, which were shown to be an important driver in microbial communities in groundwater. Sometimes bacteria can survive in a dormant state, while fungi show stronger drought tolerance. In case of heavy precipitation, it significantly increased groundwater recharge and raised groundwater level. At the same time, precipitation drives the evolution of groundwater microbiome by altering physical properties, dissolved organic carbon concentrations, and nitrate concentrations. Seawater intrusion promotes marine microorganisms to enter the aquifers, which impacts microbial-mediated processes involved in the cycling of carbon, nitrogen, sulfur, and other substances. Furthermore, inputs and variations in organic matter can induce the directional succession of microbial communities, which presents a coupling effect with the migration and transformation of pollutants to further regulate the efficiency of pollutant degradation. Based on high throughput sequencing, stable isotope probing, and numerical modeling, current studies have explored the response characteristics of microorganisms to climate change. However, significant gaps still exist in understanding microbial response mechanisms and predictions of model. Thus, prospective works are urgently needed to deepen mechanistic understanding and develop high-precision predictive models, further providing scientific support for groundwater resources protection and ecological restoration.

       

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