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多瑙河岸边浅层地下水中的病毒产生。

Virus production in shallow groundwater at the bank of the Danube River.

机构信息

Department of Functional and Evolutionary Ecology, University of Vienna, Vienna, Austria.

出版信息

PLoS One. 2024 Aug 29;19(8):e0306346. doi: 10.1371/journal.pone.0306346. eCollection 2024.

Abstract

Viruses play a crucial role in regulating prokaryotic populations, yet their impact on subsurface environments, specifically groundwater habitats, remains poorly understood. In this study, we employed the virus-dilution approach to measure lytic virus production rates in shallow groundwater located near the city of Vienna (Austria) during the period from July-November 2020. Physico-chemical parameters (pH, electrical conductivity, water temperature, concentration of dissolved oxygen), prokaryotic, and viral abundance, and viral decay rates were monitored as well. Our findings revealed low virus-to-prokaryote ratios varying between 0.9-3.9 throughout the study period and a lack of correlation between prokaryotic and viral abundance in groundwater. Virus production rates varied between 9-12% of viral abundance h-1 in July-August and between 34-36% of viral abundance h-1 in October-November. Seasonal variations in virus production rates were found to be correlated with electrical conductivity, revealing ~3.5 times higher virus production rates during periods with high electrical conductivity and low groundwater recharge in October-November compared to July-August with higher groundwater recharge and lower electrical conductivity. Our data indicate that groundwater recharge disrupts the balance between virus and prokaryotic host communities, resulting in a deficiency of suitable prokaryotic host cells for viral proliferation.

摘要

病毒在调节原核生物种群方面起着至关重要的作用,但它们对地下环境,特别是地下水生境的影响仍知之甚少。在这项研究中,我们采用病毒稀释法来测量 2020 年 7 月至 11 月期间在维也纳市附近的浅层地下水中的裂解病毒产生率。同时监测了物理化学参数(pH 值、电导率、水温和溶解氧浓度)、原核生物和病毒丰度以及病毒衰减率。我们的研究结果表明,在整个研究期间,病毒与原核生物的比例很低,变化范围为 0.9-3.9,并且地下水中的原核生物丰度与病毒丰度之间没有相关性。病毒产生率在 7 月至 8 月间变化范围为病毒丰度的 9-12%h-1,在 10 月至 11 月间变化范围为病毒丰度的 34-36%h-1。病毒产生率的季节性变化与电导率相关,表明在 10 月至 11 月期间,电导率高且地下水补给低的时期,病毒产生率比 7 月至 8 月期间高 3.5 倍,此时地下水补给高而电导率低。我们的数据表明,地下水补给破坏了病毒和原核生物宿主群落之间的平衡,导致适合病毒增殖的原核生物宿主细胞不足。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a3dc/11361564/fdc68d8a7151/pone.0306346.g001.jpg

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