Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, 1797AB Den Burg, P.O. Box 59, Texel, The Netherlands.
Department of Microbiology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Nijmegen, The Netherlands.
Microbiome. 2024 May 27;12(1):98. doi: 10.1186/s40168-024-01816-x.
Recent studies have reported the identity and functions of key anaerobes involved in the degradation of organic matter (OM) in deep (> 1000 m) sulfidic marine habitats. However, due to the lack of available isolates, detailed investigation of their physiology has been precluded. In this study, we cultivated and characterized the ecophysiology of a wide range of novel anaerobes potentially involved in OM degradation in deep (2000 m depth) sulfidic waters of the Black Sea.
We have successfully cultivated a diverse group of novel anaerobes belonging to various phyla, including Fusobacteriota (strain S5), Bacillota (strains A1 and A2), Spirochaetota (strains M1, M2, and S2), Bacteroidota (strains B1, B2, S6, L6, SYP, and M2P), Cloacimonadota (Cloa-SY6), Planctomycetota (Plnct-SY6), Mycoplasmatota (Izemo-BS), Chloroflexota (Chflx-SY6), and Desulfobacterota (strains S3 and S3-i). These microorganisms were able to grow at an elevated hydrostatic pressure of up to 50 MPa. Moreover, this study revealed that different anaerobes were specialized in degrading specific types of OM. Strains affiliated with the phyla Fusobacteriota, Bacillota, Planctomycetota, and Mycoplasmatota were found to be specialized in the degradation of cellulose, cellobiose, chitin, and DNA, respectively, while strains affiliated with Spirochaetota, Bacteroidota, Cloacimonadota, and Chloroflexota preferred to ferment less complex forms of OM. We also identified members of the phylum Desulfobacterota as terminal oxidizers, potentially involved in the consumption of hydrogen produced during fermentation. These results were supported by the identification of genes in the (meta)genomes of the cultivated microbial taxa which encode proteins of specific metabolic pathways. Additionally, we analyzed the composition of membrane lipids of selected taxa, which could be critical for their survival in the harsh environment of the deep sulfidic waters and could potentially be used as biosignatures for these strains in the sulfidic waters of the Black Sea.
This is the first report that demonstrates the cultivation and ecophysiology of such a diverse group of microorganisms from any sulfidic marine habitat. Collectively, this study provides a step forward in our understanding of the microbes thriving in the extreme conditions of the deep sulfidic waters of the Black Sea. Video Abstract.
最近的研究报告了参与有机物质(OM)降解的关键厌氧菌的身份和功能,这些厌氧菌存在于深海(>1000 米)硫化物海洋栖息地中。然而,由于缺乏可用的分离株,其生理学的详细研究受到了阻碍。在这项研究中,我们培养并表征了一系列新型厌氧菌的生态生理学,这些厌氧菌可能参与了黑海深(2000 米深度)硫化水中的 OM 降解。
我们成功地培养了一群属于各种门的新型厌氧菌,包括厚壁菌门(菌株 S5)、芽孢杆菌门(菌株 A1 和 A2)、螺旋体门(菌株 M1、M2 和 S2)、拟杆菌门(菌株 B1、B2、S6、L6、SYP 和 M2P)、Cloacimonadota(Cloa-SY6)、浮霉菌门(Plnct-SY6)、支原体门(Izemo-BS)、绿弯菌门(Chflx-SY6)和脱硫杆菌门(菌株 S3 和 S3-i)。这些微生物能够在高达 50 MPa 的静水压力下生长。此外,本研究表明,不同的厌氧菌专门降解特定类型的 OM。与厚壁菌门、芽孢杆菌门、浮霉菌门和支原体门相关的菌株分别被发现专门降解纤维素、纤维二糖、几丁质和 DNA,而与螺旋体门、拟杆菌门、Cloacimonadota 和绿弯菌门相关的菌株则偏好发酵更简单形式的 OM。我们还鉴定出脱硫杆菌门的成员为末端氧化剂,可能参与发酵过程中产生的氢气的消耗。这些结果得到了培养微生物分类群的(宏)基因组中编码特定代谢途径蛋白的基因的鉴定支持。此外,我们分析了选定分类群的膜脂组成,这对于它们在深海硫化物环境中的生存可能至关重要,并可能作为黑海硫化物水中这些菌株的生物标志物。
这是第一项报告,证明了从任何硫化物海洋栖息地培养和研究如此多样化的微生物群的能力。总的来说,这项研究为我们了解黑海深海硫化物水中微生物在极端条件下的生存提供了一个新的进展。