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冻原土壤病毒介导微生物群落对气候变暖的响应。

Tundra Soil Viruses Mediate Responses of Microbial Communities to Climate Warming.

机构信息

School of Biological Science and Technology, University of Jinan, Jinan, Shandong Province, China.

Institute of Marine Science and Technology, Shandong University, Qingdao, Shandong Province, China.

出版信息

mBio. 2023 Apr 25;14(2):e0300922. doi: 10.1128/mbio.03009-22. Epub 2023 Feb 14.

Abstract

The rise of global temperature causes the degradation of the substantial reserves of carbon (C) stored in tundra soils, in which microbial processes play critical roles. Viruses are known to influence the soil C cycle by encoding auxiliary metabolic genes and infecting key microorganisms, but their regulation of microbial communities under climate warming remains unexplored. In this study, we evaluated the responses of viral communities for about 5 years of experimental warming at two depths (15 to 25 cm and 45 to 55 cm) in the Alaskan permafrost region. Our results showed that the viral community and functional gene composition and abundances (including viral functional genes related to replication, structure, infection, and lysis) were significantly influenced by environmental conditions such as total nitrogen (N), total C, and soil thawing duration. Although long-term warming did not impact the viral community composition at the two depths, some glycoside hydrolases encoded by viruses were more abundant at both depths of the warmed plots. With the continuous reduction of total C, viruses may alleviate methane release by altering infection strategies on methanogens. Importantly, viruses can adopt lysogenic and lytic lifestyles to manipulate microbial communities at different soil depths, respectively, which could be one of the major factors causing the differences in microbial responses to warming. This study provides a new ecological perspective on how viruses regulate the responses of microbes to warming at community and functional scales. Permafrost thawing causes microbial release of greenhouse gases, exacerbating climate warming. Some previous studies examined the responses of the microbial communities and functions to warming in permafrost region, but the roles of viruses in mediating the responses of microbial communities to warming are poorly understood. This study revealed that warming induced changes in some viral functional classes and in the virus/microbe ratios for specific lineages, which might influence the entire microbial community. Furthermore, differences in viral communities and functions, along with soil depths, are important factors influencing microbial responses to warming. Collectively, our study revealed the regulation of microbial communities by viruses and demonstrated the importance of viruses in the microbial ecology research.

摘要

全球气温上升导致冻原土壤中大量碳 (C) 储量减少,而微生物过程在其中起着关键作用。病毒通过编码辅助代谢基因和感染关键微生物来影响土壤碳循环,但它们在气候变暖下对微生物群落的调节仍未得到探索。在这项研究中,我们评估了在阿拉斯加多年冻土区两个深度(15 到 25 厘米和 45 到 55 厘米)的实验增温约 5 年后病毒群落的响应。我们的结果表明,病毒群落及其功能基因组成和丰度(包括与复制、结构、感染和裂解相关的病毒功能基因)受到总氮 (N)、总 C 和土壤解冻持续时间等环境条件的显著影响。尽管长期增温没有影响两个深度的病毒群落组成,但在变暖样地的两个深度,病毒编码的一些糖苷水解酶更加丰富。随着总 C 的持续减少,病毒可能通过改变对产甲烷菌的感染策略来缓解甲烷的释放。重要的是,病毒可以采用溶原和裂解生活方式来分别操纵不同土壤深度的微生物群落,这可能是导致微生物对变暖响应差异的主要因素之一。本研究从群落和功能尺度上提供了一个关于病毒如何调节微生物对变暖响应的新生态视角。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2e76/10127799/6387feb03f04/mbio.03009-22-f001.jpg

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