Marine Biotechnology Research Center, State Key Laboratory of Microbial Technology, Shandong University, Qingdao, China; Joint Research Center for Marine Microbial Science and Technology, Shandong University and Ocean University of China, China.
MOE Key Laboratory of Evolution and Marine Biodiversity, Frontiers Science Center for Deep Ocean Multispheres and Earth System & College of Marine Life Sciences, Ocean University of China, Qingdao, China; School of Life Sciences, University of Warwick, Coventry, UK; Joint Research Center for Marine Microbial Science and Technology, Shandong University and Ocean University of China, China.
Sci Total Environ. 2024 Oct 20;948:174723. doi: 10.1016/j.scitotenv.2024.174723. Epub 2024 Jul 11.
The deep marine sediments represent a major repository of organic matter whilst hosting a great number of uncultivated microbes. Microbial metabolism plays a key role in the recycling of organic matter in the deep marine sediments. D-amino acids (DAAs) and DAA-containing muropeptides, an important group of organic matter in the deep marine sediments, are primarily derived from bacterial peptidoglycan decomposition. Archaea are abundant in the deep ocean microbiome, yet their role in DAA metabolism remains poorly studied. Here, we report bioinformatic investigation and enzymatic characterization of deep marine sedimentary archaea involved in DAA metabolism. Our analyses suggest that a variety of archaea, particularly the Candidatus Bathyarchaeota and the Candidatus Lokiarchaeaota, can metabolize DAAs. DAAs are converted into L-amino acids via amino acid racemases (Ala racemase, Asp racemase and broad substrate specificity amino acid racemase), and converted into α-keto acid via d-serine ammonia-lyase, whereas DAA-containing di-/tri-muropeptides can be hydrolyzed by peptidases (dipeptidase and D-aminopeptidase). Overall, this study reveals the identity and activity of deep marine sedimentary archaea involved in DAA metabolism, shedding light on the mineralization and biogeochemical cycling of DAAs in the deep marine sediments.
深海沉积物是有机质的主要储存库,同时还栖息着大量未培养的微生物。微生物代谢在深海沉积物中有机质的循环中起着关键作用。D-氨基酸(DAA)和含 DAA 的肽聚糖,是深海沉积物中一类重要的有机质,主要来源于细菌肽聚糖的分解。古菌在深海微生物组中丰度很高,但它们在 DAA 代谢中的作用仍研究甚少。在这里,我们报告了参与 DAA 代谢的深海沉积物古菌的生物信息学研究和酶学特征。我们的分析表明,多种古菌,特别是候选古菌门和候选 Lokiarchaeota 门,能够代谢 DAA。DAA 通过氨基酸消旋酶(Ala 消旋酶、Asp 消旋酶和广泛底物特异性氨基酸消旋酶)转化为 L-氨基酸,并通过 D-丝氨酸氨裂解酶转化为α-酮酸,而含 DAA 的二肽/三肽聚糖可以被肽酶(二肽酶和 D-氨基肽酶)水解。总的来说,这项研究揭示了参与 DAA 代谢的深海沉积物古菌的身份和活性,为深海沉积物中 DAA 的矿化和生物地球化学循环提供了新的认识。