Department of Integrative Biology, University of Colorado Denver, Denver, CO, USA.
Department of Microbiology, The Ohio State University, Columbus, OH, USA.
Environ Microbiol. 2017 Jun;19(6):2192-2209. doi: 10.1111/1462-2920.13703. Epub 2017 Mar 28.
Despite being key contributors to biogeochemical processes, archaea are frequently outnumbered by bacteria, and consequently are underrepresented in combined molecular surveys. Here, we demonstrate an approach to concurrently survey the archaea alongside the bacteria with high-resolution 16S rRNA gene sequencing, linking these community data to geochemical parameters. We applied this integrated analysis to hydric soils sampled across a model methane-emitting freshwater wetland. Geochemical profiles, archaeal communities, and bacterial communities were independently correlated with soil depth and water cover. Centimeters of soil depth and corresponding geochemical shifts consistently affected microbial community structure more than hundreds of meters of lateral distance. Methanogens with diverse metabolisms were detected across the wetland, but displayed surprising OTU-level partitioning by depth. Candidatus Methanoperedens spp. archaea thought to perform anaerobic oxidation of methane linked to iron reduction were abundant. Domain-specific sequencing also revealed unexpectedly diverse non-methane-cycling archaeal members. OTUs within the underexplored Woesearchaeota and Bathyarchaeota were prevalent across the wetland, with subgroups and individual OTUs exhibiting distinct occupancy and abundance distributions aligned with environmental gradients. This study adds to our understanding of ecological range for key archaeal taxa in a model freshwater wetland, and links these taxa and individual OTUs to hypotheses about processes governing biogeochemical cycling.
尽管古菌是生物地球化学过程的主要贡献者,但它们的数量通常比细菌少,因此在综合分子调查中代表性不足。在这里,我们展示了一种同时使用高分辨率 16S rRNA 基因测序对古菌和细菌进行调查的方法,将这些群落数据与地球化学参数联系起来。我们将这种综合分析应用于在一个模型甲烷排放淡水湿地中采集的水湿土壤。地球化学剖面、古菌群落和细菌群落都与土壤深度和水覆盖层独立相关。数厘米的土壤深度和相应的地球化学变化比数百米的水平距离更能持续地影响微生物群落结构。在整个湿地中检测到了具有不同代谢途径的产甲烷菌,但在深度上却呈现出惊人的 OTU 级别的分区。被认为与铁还原有关的进行厌氧甲烷氧化的疑似 Methanoperedens 古菌很丰富。基于特定领域的测序还揭示了出乎意料的多样化的非甲烷循环古菌成员。在整个湿地中普遍存在未充分研究的 Woesearchaeota 和 Bathyarchaeota 的 OTUs,亚群和个别 OTUs 与环境梯度相一致,具有独特的占据和丰度分布。本研究增加了我们对模型淡水湿地中关键古菌类群生态范围的理解,并将这些类群和个别 OTU 与关于控制生物地球化学循环的过程的假设联系起来。