4.8 Article

Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans

Journal

MICROBIOME
Volume 9, Issue 1, Pages -

Publisher

BMC
DOI: 10.1186/s40168-021-01153-3

Keywords

Polar oceans; DMS; DMSP cycling; Geographic distribution; Phylogenetic diversity

Categories

Funding

  1. National Key Research and Development Program of China [2016YFA0601303, 2018YFC1406700]
  2. National Science Foundation of China [91851205, 31630012, U1706207, 42076229, 31870052, 31800107, 91751101, 41706152, 41676180]
  3. Fundamental Research Funds for the Central Universities [202172002]
  4. Major Scientific and Technological Innovation Project (MSTIP) of Shandong Province [2019JZZY010817]
  5. Program of Shandong for Taishan Scholars [tspd20181203]
  6. Qingdao National Laboratory for Marine Science and Technology [2017ASTCP-OS14, QNLM2016ORP0310]

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This study provides a global overview of the biogeographic traits of known bacterial genes involved in DMS/DMSP cycling in the Arctic and Antarctic oceans. It reveals that intense DMS/DMSP cycling occurs in polar oceans, with specific microbial enzymes playing key roles. The microbial assemblages in polar oceans are shaped more by water depth than geographic distance, suggesting habitat differences are crucial factors in shaping microbial communities involved in DMS/DMSP cycling.
Background: Dimethyl sulfide (DMS) is the dominant volatile organic sulfur in global oceans. The predominant source of oceanic DMS is the cleavage of dimethylsulfoniopropionate (DMSP), which can be produced by marine bacteria and phytoplankton. Polar oceans, which represent about one fifth of Earth's surface, contribute significantly to the global oceanic DMS sea-air flux. However, a global overview of DMS and DMSP cycling in polar oceans is still lacking and the key genes and the microbial assemblages involved in DMSP/DMS transformation remain to be fully unveiled. Results: Here, we systematically investigated the biogeographic traits of 16 key microbial enzymes involved in DMS/DMSP cycling in 60 metagenomic samples from polar waters, together with 174 metagenome and 151 metatranscriptomes from non-polar Tara Ocean dataset. Our analyses suggest that intense DMS/DMSP cycling occurs in the polar oceans. DMSP demethylase (DmdA), DMSP lyases (DddD, DddP, and DddK), and trimethylamine monooxygenase (Tmm, which oxidizes DMS to dimethylsulfoxide) were the most prevalent bacterial genes involved in global DMS/DMSP cycling. Alphaproteobacteria (Pelagibacterales) and Gammaproteobacteria appear to play prominent roles in DMS/DMSP cycling in polar oceans. The phenomenon that multiple DMS/DMSP cycling genes co-occurred in the same bacterial genome was also observed in metagenome assembled genomes (MAGs) from polar oceans. The microbial assemblages from the polar oceans were significantly correlated with water depth rather than geographic distance, suggesting the differences of habitats between surface and deep waters rather than dispersal limitation are the key factors shaping microbial assemblages involved in DMS/DMSP cycling in polar oceans. Conclusions: Overall, this study provides a global overview of the biogeographic traits of known bacterial genes involved in DMS/DMSP cycling from the Arctic and Antarctic oceans, laying a solid foundation for further studies of DMS/DMSP cycling in polar ocean microbiome at the enzymatic, metabolic, and processual levels.

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