Department of Microbiology, College of Science, Oregon State University, Corvallis, OR, United States of America.
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, United States of America.
PeerJ. 2023 Mar 28;11:e15119. doi: 10.7717/peerj.15119. eCollection 2023.
Methane seeps are highly abundant marine habitats that contribute sources of chemosynthetic primary production to marine ecosystems. Seeps also factor into the global budget of methane, a potent greenhouse gas. Because of these factors, methane seeps influence not only local ocean ecology, but also biogeochemical cycles on a greater scale. Methane seeps host specialized microbial communities that vary significantly based on geography, seep gross morphology, biogeochemistry, and a diversity of other ecological factors including cross-domain species interactions. In this study, we collected sediment cores from six seep and non-seep locations from Grays and Quinault Canyons (46-47°N) off Washington State, USA, as well as one non-seep site off the coast of Oregon, USA (45°N) to quantify the scale of seep influence on biodiversity within marine habitats. These samples were profiled using 16S rRNA gene sequencing. Predicted gene functions were generated using the program PICRUSt2, and the community composition and predicted functions were compared among samples. The microbial communities at seeps varied by seep morphology and habitat, whereas the microbial communities at non-seep sites varied by water depth. Microbial community composition and predicted gene function clearly transitioned from on-seep to off-seep in samples collected from transects moving away from seeps, with a clear ecotone and high diversity where methane-fueled habitats transition into the non-seep deep sea. Our work demonstrates the microbial and metabolic sphere of influence that extends outwards from methane seep habitats.
甲烷渗漏是高度丰富的海洋生境,为海洋生态系统提供了化学合成初级生产力的来源。渗漏物也构成了甲烷全球预算的一部分,而甲烷是一种强效温室气体。由于这些因素,甲烷渗漏不仅影响当地海洋生态,而且还影响更大规模的生物地球化学循环。甲烷渗漏物中存在着特殊的微生物群落,这些微生物群落因地理位置、渗漏总形态、生物地球化学以及包括跨域物种相互作用在内的许多其他生态因素而有很大差异。在这项研究中,我们从美国华盛顿州的 Grays 和 Quinault 峡谷(北纬 46-47°)的六个渗漏和非渗漏地点以及美国俄勒冈州海岸的一个非渗漏地点采集了沉积物岩芯,以量化渗漏对海洋生境中生物多样性的影响规模。这些样品使用 16S rRNA 基因测序进行了分析。使用程序 PICRUSt2 生成了预测的基因功能,并比较了样品之间的群落组成和预测功能。渗漏处的微生物群落因渗漏形态和生境而异,而非渗漏处的微生物群落则因水深而异。从远离渗漏处的横截线上采集的样品中,微生物群落组成和预测的基因功能明显从渗漏处向非渗漏处过渡,在甲烷燃料生境向非渗漏深海过渡的生态过渡带中,多样性很高。我们的工作展示了从甲烷渗漏生境向外扩展的微生物和代谢影响范围。