Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans

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’...

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Published in:Microbiome
Main Authors: Teng, Zhao-Jie, Qin, Qi-Long, Zhang, Weipeng, Li, Jian, Fu, Hui-Hui, Wang, Peng, Lan, Musheng, Lu, Guangfu, He, Jianfeng, McMinn, Andrew, Wang, Min, Chen, Xiu-Lan, Zhang, Yu-Zhong, Chen, Yin, Li, Chun-Yang
Format: Text
Language:English
Published: BioMed Central 2021
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Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8520302/
https://doi.org/10.1186/s40168-021-01153-3
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spelling ftpubmed:oai:pubmedcentral.nih.gov:8520302 2023-05-15T13:53:04+02:00 Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans Teng, Zhao-Jie Qin, Qi-Long Zhang, Weipeng Li, Jian Fu, Hui-Hui Wang, Peng Lan, Musheng Lu, Guangfu He, Jianfeng McMinn, Andrew Wang, Min Chen, Xiu-Lan Zhang, Yu-Zhong Chen, Yin Li, Chun-Yang 2021-10-16 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8520302/ https://doi.org/10.1186/s40168-021-01153-3 en eng BioMed Central http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8520302/ http://dx.doi.org/10.1186/s40168-021-01153-3 © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/ (https://creativecommons.org/publicdomain/zero/1.0/) ) applies to the data made available in this article, unless otherwise stated in a credit line to the data. CC0 PDM CC-BY Microbiome Research Text 2021 ftpubmed https://doi.org/10.1186/s40168-021-01153-3 2021-10-24T00:37:19Z 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 ... Text Antarc* Antarctic Arctic Phytoplankton PubMed Central (PMC) Antarctic Arctic Microbiome 9 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Research
spellingShingle Research
Teng, Zhao-Jie
Qin, Qi-Long
Zhang, Weipeng
Li, Jian
Fu, Hui-Hui
Wang, Peng
Lan, Musheng
Lu, Guangfu
He, Jianfeng
McMinn, Andrew
Wang, Min
Chen, Xiu-Lan
Zhang, Yu-Zhong
Chen, Yin
Li, Chun-Yang
Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
topic_facet Research
description 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 ...
format Text
author Teng, Zhao-Jie
Qin, Qi-Long
Zhang, Weipeng
Li, Jian
Fu, Hui-Hui
Wang, Peng
Lan, Musheng
Lu, Guangfu
He, Jianfeng
McMinn, Andrew
Wang, Min
Chen, Xiu-Lan
Zhang, Yu-Zhong
Chen, Yin
Li, Chun-Yang
author_facet Teng, Zhao-Jie
Qin, Qi-Long
Zhang, Weipeng
Li, Jian
Fu, Hui-Hui
Wang, Peng
Lan, Musheng
Lu, Guangfu
He, Jianfeng
McMinn, Andrew
Wang, Min
Chen, Xiu-Lan
Zhang, Yu-Zhong
Chen, Yin
Li, Chun-Yang
author_sort Teng, Zhao-Jie
title Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
title_short Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
title_full Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
title_fullStr Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
title_full_unstemmed Biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
title_sort biogeographic traits of dimethyl sulfide and dimethylsulfoniopropionate cycling in polar oceans
publisher BioMed Central
publishDate 2021
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8520302/
https://doi.org/10.1186/s40168-021-01153-3
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Phytoplankton
genre_facet Antarc*
Antarctic
Arctic
Phytoplankton
op_source Microbiome
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8520302/
http://dx.doi.org/10.1186/s40168-021-01153-3
op_rights © The Author(s) 2021
https://creativecommons.org/licenses/by/4.0/Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/ (https://creativecommons.org/publicdomain/zero/1.0/) ) applies to the data made available in this article, unless otherwise stated in a credit line to the data.
op_rightsnorm CC0
PDM
CC-BY
op_doi https://doi.org/10.1186/s40168-021-01153-3
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