Adam-Beyer Nicole, Laufer-Meiser Katja, Fuchs Sebastian, Schippers Axel, Indenbirken Daniela, Garbe-Schönberg Dieter, Petersen Sven, Perner Mirjam
Marine Geosystems, GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany.
Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany.
Front Microbiol. 2023 Oct 11;14:1173613. doi: 10.3389/fmicb.2023.1173613. eCollection 2023.
In order to expand the knowledge of microbial ecosystems from deep-sea hydrothermal vent systems located on the Central and South-East Indian Ridge, we sampled hydrothermal fluids, massive sulfides, ambient water and sediments of six distinct vent fields. Most of these vent sites were only recently discovered in the course of the German exploration program for massive sulfide deposits and no previous studies of the respective microbial communities exist. Apart from typically vent-associated chemosynthetic members of the orders , , and , high numbers of uncultured and unspecified Bacteria were identified via 16S rRNA gene analyses in hydrothermal fluid and massive sulfide samples. The sampled sediments however, were characterized by an overall lack of chemosynthetic Bacteria and the presence of high proportions of low abundant bacterial groups. The archaeal communities were generally less diverse and mostly dominated by members of and , partly exhibiting high proportions of unassigned Archaea. Correlations with environmental parameters were primarily observed for sediment communities and for microbial species (associated with the nitrogen cycle) in samples from a recently identified vent field, which was geochemically distinct from all other sampled sites. Enrichment cultures of diffuse fluids demonstrated a great potential for hydrogen oxidation coupled to the reduction of various electron-acceptors with high abundances of and species. Overall, given the large number of currently uncultured and unspecified microorganisms identified in the vent communities, their respective metabolic traits, ecosystem functions and mediated biogeochemical processes have still to be resolved for estimating consequences of potential environmental disturbances by future mining activities.
为了拓展对位于中印度洋海岭和东南印度洋海岭深海热液喷口系统微生物生态系统的认识,我们对六个不同喷口区的热液流体、块状硫化物、周围海水和沉积物进行了采样。这些喷口地点大多是在德国大规模硫化物矿床勘探计划过程中最近才发现的,此前没有对相应微生物群落进行过研究。除了典型的与喷口相关的、、和目化学合成成员外,通过16S rRNA基因分析在热液流体和块状硫化物样本中还鉴定出大量未培养和未明确的细菌。然而,所采集的沉积物的特点是总体上缺乏化学合成细菌,且存在高比例的低丰度细菌类群。古菌群落通常多样性较低,主要由和的成员主导,部分未分类古菌比例较高。主要在沉积物群落以及来自一个最近发现的、地球化学特征与所有其他采样地点不同的喷口区样本中的微生物物种(与氮循环相关)中观察到与环境参数的相关性。扩散流体的富集培养显示出在氢气氧化与各种电子受体还原耦合方面具有巨大潜力,其中和物种丰度较高。总体而言,鉴于在喷口群落中鉴定出大量目前未培养和未明确的微生物,它们各自的代谢特征、生态系统功能和介导的生物地球化学过程仍有待解决,以便评估未来采矿活动可能造成的环境干扰的后果。