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缺氧早期地球海洋的湖泊类似物中的病毒活性。

Viral activity in lake analogs of anoxic early Earth oceans.

作者信息

Varona Natascha S, Wallace Bailey A, Bosco-Santos Alice, Mullinax Julianna, Stiffler Alexandra K, O'Beirne Molly D, Ford Josh, Fulton James M, Werne Josef P, Gilhooly William P, Silveira Cynthia B

机构信息

Department of Biology, University of Miami, Coral Gables, FL, 33146, USA.

Institute of Earth Surface Dynamics, University of Lausanne, Vaud, Switzerland.

出版信息

Microbiome. 2025 Apr 26;13(1):104. doi: 10.1186/s40168-025-02085-y.

Abstract

BACKGROUND

Meromictic lakes, with their stratified water columns, are modern analogs for ancient euxinic (anoxic and sulfidic) oceans, where anaerobic sulfur-oxidizing purple and green sulfur bacteria (PSB and GSB) dominated as primary producers. Recent studies suggest a potential role of viruses in the metabolisms and biosignatures of these bacteria, but conclusive evidence of viral replication and activity in such lakes is still lacking.

RESULTS

Here, we investigate viral activity in the upper mixed layer (mixolimnion), the anoxic bottom (monimolimnion), and the microbial plate (a dense layer of phototrophic sulfur bacteria forming at the boundary between the oxygenated mixolimnion and the anoxic monimolimnion) of three meromictic lakes: Poison and Lime Blue Lakes (WA, USA) and Mahoney Lake (BC, CA). Geochemical profiles of two lakes, Mahoney and Poison, which are dominated by PSB, show a sharp chemocline, whereas Lime Blue displays a less steep chemical gradient and hosts a mixture of PSB and GSB. Viral gene transcription and epifluorescence microscopy revealed depth-dependent patterns in viral activity. The two strongly stratified, PSB-dominated lakes showed a significant decrease in the virus-to-microbe ratio (VMR) in their microbial plates, suggesting reduced viral particle production via lysis. Metatranscriptome data corroborated this trend by showing lower levels of viral gene expression in these microbial plates, higher expression of CRISPR defense and lysogeny-related genes, and relatively high expression of photosynthesis-related viral genes. Conversely, the third lake, which harbors a mix of PSB and GSB, exhibited low microbial density, high VMR, and high viral transcriptional activity. Viral transcription levels significantly correlated with VMR in the microbial plates and bottom layers, but this relationship was absent in low-density, oxic surface samples.

CONCLUSIONS

Here, two independent lines of evidence, abundances and gene expression, show reduced viral lytic production in microbial plates dominated by PSB in stratified lakes. This suggests that viral lysis may contribute less to bacterial community structuring in these high-density microbial plates. Rather, other viral-mediated mechanisms, such as lysogeny and the expression of auxiliary metabolic genes, may represent a more significant viral influence on bacterial physiology and geochemistry. These patterns in virus-bacteria interactions may be consequential for the interpretations of biosignatures left by these bacterial groups in the geologic record. Video Abstract.

摘要

背景

具有分层水柱的半混合湖是古代缺氧(无氧且含硫化物)海洋的现代类似物,在这些海洋中,厌氧硫氧化紫色和绿色硫细菌(PSB和GSB)作为主要生产者占据主导地位。最近的研究表明病毒在这些细菌的代谢和生物特征中可能发挥作用,但在这类湖泊中病毒复制和活性的确凿证据仍然缺乏。

结果

在这里,我们研究了美国华盛顿州的毒湖和石灰蓝湖以及加拿大不列颠哥伦比亚省的马奥尼湖这三个半混合湖的上混合层(混水层)、缺氧底部(死水层)和微生物板(在含氧混水层与缺氧死水层之间的边界形成的一层密集的光合硫细菌)中的病毒活性。以PSB为主的马奥尼湖和毒湖的地球化学剖面显示出明显的化学跃变层,而石灰蓝湖的化学梯度较缓,并且含有PSB和GSB的混合物。病毒基因转录和落射荧光显微镜揭示了病毒活性随深度变化的模式。两个强烈分层、以PSB为主的湖泊在其微生物板中的病毒与微生物比率(VMR)显著降低,这表明通过裂解产生的病毒颗粒减少。宏转录组数据证实了这一趋势,显示这些微生物板中病毒基因表达水平较低,CRISPR防御和溶原性相关基因表达较高,以及光合作用相关病毒基因表达相对较高。相反,第三个湖泊含有PSB和GSB的混合物,其微生物密度低、VMR高且病毒转录活性高。病毒转录水平与微生物板和底层中的VMR显著相关,但在低密度、有氧的表层样本中不存在这种关系。

结论

在这里,丰度和基因表达这两条独立的证据表明,在分层湖泊中以PSB为主的微生物板中病毒裂解产生减少。这表明病毒裂解对这些高密度微生物板中细菌群落结构的贡献可能较小。相反,其他病毒介导的机制,如溶原性和辅助代谢基因的表达,可能对细菌生理学和地球化学代表更显著的病毒影响。病毒与细菌相互作用的这些模式可能对解释这些细菌群体在地质记录中留下的生物特征具有重要意义。视频摘要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/67a1/12032784/8a6ccb39f4bb/40168_2025_2085_Fig1_HTML.jpg

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