185 research outputs found

    Environmental proteomics: A long march in the pedosphere

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    Environmental proteomics, the study of the expression profile of proteins extracted directly from living organisms and some stabilized extracellular proteins present in environmental samples, is a developing branch of soil science since the seminal papers appeared twenty years ago. Soil microbial communities hold the key to understanding terrestrial biodiversity; they are extremely complex and their physiological responses to dynamic environmental parameters are under-characterized. Therefore, the slow development of environment-related proteomic databases, and the high chemical reactivity of environmental matrices hamper the extraction, quantification, and characterization of proteins; and soil proteomics remains still in its infancy. We underscore the main achievements of environmental proteomics focusing on soil ecosystems, and we identify technical gaps that need to be bridged in the context of relevant ecological concepts that have received little attention in the development of proteomics methods. This analysis offers a new framework of research of soil proteomics toward improved understanding of the causal linkages between the structure and function of the soil microbiome, and a broader grasp of the sensitivity of terrestrial ecosystems to environmental change

    Tundra Soil Viruses Mediate Responses of Microbial Communities to Climate Warming

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    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. IMPORTANCE 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
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