Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China.
Department of Ocean Science, Hong Kong University of Science and Technology, Hong Kong, China.
mSystems. 2023 Apr 27;8(2):e0117922. doi: 10.1128/msystems.01179-22. Epub 2023 Mar 16.
Marine sediments are important methane reservoirs. Methane efflux from the seabed is significantly restricted by anaerobic methanotrophic (ANME) archaea through a process known as anaerobic oxidation of methane (AOM). Different clades of ANME archaea occupy distinct niches in methane seeps, but their underlying molecular mechanisms still need to be fully understood. To provide genetic explanations for the niche partitioning of ANME archaea, we applied comparative genomic analysis to ANME archaeal genomes retrieved from global methane seeps. Our results showed that ANME-2 archaea are more prevalent than ANME-1 archaea in shallow sediments because they carry genes that encode a significantly higher number of outer membrane multiheme -type cytochromes and flagellar proteins. These features make ANME-2 archaea perform direct interspecies electron transfer better and benefit more from electron acceptors in AOM. Besides, ANME-2 archaea carry genes that encode extra peroxidase compared to ANME-1 archaea, which may lead to ANME-2 archaea better tolerating oxygen toxicity. In contrast, ANME-1 archaea are more competitive in deep layers than ANME-2 archaea because they carry extra genes ( and ) for methylotrophic methanogenesis and a significantly higher number of and genes for hydrogenotrophic methanogenesis. Additionally, ANME-1 archaea carry exclusive genes (, , and ) involved in sulfide detoxification compared to ANME-2 archaea, leading to stronger sulfide tolerance. Overall, this study reveals the genomic mechanisms shaping the niche partitioning among ANME archaea in global methane seeps. Anaerobic methanotrophic (ANME) archaea are important methanotrophs in marine sediment, controlling the flux of biologically generated methane, which plays an essential role in the marine carbon cycle and climate change. So far, no strain of this lineage has been isolated in pure culture, which makes metagenomics one of the fundamental approaches to reveal their metabolic potential. Although the niche partitioning of ANME archaea was frequently reported in different studies, whether this pattern was consistent in global methane seeps had yet to be verified, and little was known about the genetic mechanisms underlying it. Here, we reviewed and analyzed the community structure of ANME archaea in global methane seeps and indicated that the niche partitioning of ANME archaea was statistically supported. Our comparative genomic analysis indicated that the capabilities of interspecies electron transfer, methanogenesis, and the resistance of oxygen and hydrogen sulfide could be critical in defining the distribution of ANME archaea in methane seep sediment.
海洋沉积物是重要的甲烷储层。通过一种称为厌氧甲烷氧化 (AOM) 的过程,海洋底栖的厌氧甲烷营养菌(ANME)显著限制了甲烷的排放。不同分支的 ANME 古菌在甲烷渗漏中占据不同的小生境,但它们的潜在分子机制仍需要充分理解。为了从遗传上解释 ANME 古菌的小生境分异,我们对从全球甲烷渗漏中获得的 ANME 古菌基因组进行了比较基因组分析。我们的结果表明,ANME-2 古菌在浅沉积物中比 ANME-1 古菌更为普遍,因为它们携带编码大量外膜多血红素型细胞色素和鞭毛蛋白的基因。这些特征使 ANME-2 古菌能够更好地进行种间电子转移,并从 AOM 中的电子受体中获益更多。此外,与 ANME-1 古菌相比,ANME-2 古菌携带编码额外过氧化物酶的基因,这可能使 ANME-2 古菌更好地耐受氧气毒性。相比之下,ANME-1 古菌在深层比 ANME-2 古菌更具竞争力,因为它们携带用于甲基营养型产甲烷和用于氢营养型产甲烷的额外基因(和)。此外,与 ANME-2 古菌相比,ANME-1 古菌携带参与硫化物解毒的特有基因(、和),从而具有更强的硫化物耐受性。总体而言,这项研究揭示了塑造全球甲烷渗漏中 ANME 古菌小生境分异的基因组机制。