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  1. Lloyd, Karen G. (Ed.)
    ABSTRACT The ecological drivers that concurrently act upon both a virus and its host and that drive community assembly are poorly understood despite known interactions between viral populations and their microbial hosts. Hydraulically fractured shale environments provide access to a closed ecosystem in the deep subsurface where constrained microbial and viral community assembly processes can be examined. Here, we used metagenomic analyses of time-resolved-produced fluid samples from two wells in the Appalachian Basin to track viral and host dynamics and to investigate community assembly processes. Hypersaline conditions within these ecosystems should drive microbial community structure to a similar configuration through time in response to common osmotic stress. However, viral predation appears to counterbalance this potentially strong homogeneous selection and pushes the microbial community toward undominated assembly. In comparison, while the viral community was also influenced by substantial undominated processes, it assembled, in part, due to homogeneous selection. When the overall assembly processes acting upon both these communities were directly compared with each other, a significant relationship was revealed, suggesting an association between microbial and viral community development despite differing selective pressures. These results reveal a potentially important balance of ecological dynamics that must be in maintained within this deep subsurface ecosystem in order for the microbial community to persist over extended time periods. More broadly, this relationship begins to provide knowledge underlying metacommunity development across trophic levels. IMPORTANCE Interactions between viral communities and their microbial hosts have been the subject of many recent studies in a wide range of ecosystems. The degree of coordination between ecological assembly processes influencing viral and microbial communities, however, has been explored to a much lesser degree. By using a combined null modeling approach, this study investigated the ecological assembly processes influencing both viral and microbial community structure within hydraulically fractured shale environments. Among other results, significant relationships between the structuring processes affecting both the viral and microbial community were observed, indicating that ecological assembly might be coordinated between these communities despite differing selective pressures. Within this deep subsurface ecosystem, these results reveal a potentially important balance of ecological dynamics that must be maintained to enable long-term microbial community persistence. More broadly, this relationship begins to provide insight into the development of communities across trophic levels. 
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  2. Abstract

    Sediment cores were collected under ice‐cover in late winter from three wetlands located along a subsurface hydrologic gradient within the Prairie Pothole Region of North America. Within each core, sediment porewaters were analyzed byin situvoltammetry for a suite of redox active species as a function of depth and revealed shifts in complex oxidation‐reduction dynamics related to ice cover in these wetlands. We observed a reduced sulfur boundary that is close to or above the sediment‐water interface (SWI) under ice cover. In contrast, the reduced sulfur boundary retreats several centimeters deeper in the sediments under ice‐free conditions. These findings are analogous to previous observations in shallow lakes that show anoxia at the SWI during ice cover but not under ice‐free conditions. Further, biogeochemical processes varied depending upon wetland type. During winter, sulfide levels in sediment porewaters in groundwater fed “flow‐through” wetlands were significantly lower than under ice‐free conditions. The converse applied to groundwater discharge wetlands where reduced sulfur concentrations in porewaters increased under ice cover. Decreases in ice cover extent and duration due to climate change coupled with profound landscape changes due to agriculture will affect the biogeochemical cycles of these wetlands and could lead to increased carbon emissions in the future.

     
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