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Liu J, Xue CX, Wang J, Crombie AT, Carrión O, Johnston AWB, Murrell JC, Liu J, Zheng Y, Zhang XH, Todd JD. Oceanospirillales containing the DMSP lyase DddD are key utilisers of carbon from DMSP in coastal seawater. MICROBIOME 2022; 10:110. [PMID: 35883169 PMCID: PMC9327192 DOI: 10.1186/s40168-022-01304-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/08/2022] [Accepted: 05/27/2022] [Indexed: 06/15/2023]
Abstract
BACKGROUND Ubiquitous and diverse marine microorganisms utilise the abundant organosulfur molecule dimethylsulfoniopropionate (DMSP), the main precursor of the climate-active gas dimethylsulfide (DMS), as a source of carbon, sulfur and/or signalling molecules. However, it is currently difficult to discern which microbes actively catabolise DMSP in the environment, why they do so and the pathways used. RESULTS Here, a novel DNA-stable isotope probing (SIP) approach, where only the propionate and not the DMS moiety of DMSP was 13C-labelled, was strategically applied to identify key microorganisms actively using DMSP and also likely DMS as a carbon source, and their catabolic enzymes, in North Sea water. Metagenomic analysis of natural seawater suggested that Rhodobacterales (Roseobacter group) and SAR11 bacteria were the major microorganisms degrading DMSP via demethylation and, to a lesser extent, DddP-driven DMSP lysis pathways. However, neither Rhodobacterales and SAR11 bacteria nor their DMSP catabolic genes were prominently labelled in DNA-SIP experiments, suggesting they use DMSP as a sulfur source and/or in signalling pathways, and not primarily for carbon requirements. Instead, DNA-SIP identified gammaproteobacterial Oceanospirillales, e.g. Amphritea, and their DMSP lyase DddD as the dominant microorganisms/enzymes using DMSP as a carbon source. Supporting this, most gammaproteobacterial (with DddD) but few alphaproteobacterial seawater isolates grew on DMSP as sole carbon source and produced DMS. Furthermore, our DNA-SIP strategy also identified Methylophaga and other Piscirickettsiaceae as key bacteria likely using the DMS, generated from DMSP lysis, as a carbon source. CONCLUSIONS This is the first study to use DNA-SIP with 13C-labelled DMSP and, in a novel way, it identifies the dominant microbes utilising DMSP and DMS as carbon sources. It highlights that whilst metagenomic analyses of marine environments can predict microorganisms/genes that degrade DMSP and DMS based on their abundance, it cannot disentangle those using these important organosulfur compounds for their carbon requirements. Note, the most abundant DMSP degraders, e.g. Rhodobacterales with DmdA, are not always the key microorganisms using DMSP for carbon and releasing DMS, which in this coastal system were Oceanospirillales containing DddD. Video abstract.
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Affiliation(s)
- Jingli Liu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences , Ocean University of China, Qingdao, China
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Chun-Xu Xue
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences , Ocean University of China, Qingdao, China
| | - Jinyan Wang
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences , Ocean University of China, Qingdao, China
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Andrew T Crombie
- School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Ornella Carrión
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Andrew W B Johnston
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - J Colin Murrell
- School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Ji Liu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences , Ocean University of China, Qingdao, China
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Yanfen Zheng
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences , Ocean University of China, Qingdao, China
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK
| | - Xiao-Hua Zhang
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences , Ocean University of China, Qingdao, China.
- Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China.
| | - Jonathan D Todd
- School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, UK.
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Park KT, Lee K, Shin K, Yang EJ, Hyun B, Kim JM, Noh JH, Kim M, Kong B, Choi DH, Choi SJ, Jang PG, Jeong HJ. Direct linkage between dimethyl sulfide production and microzooplankton grazing, resulting from prey composition change under high partial pressure of carbon dioxide conditions. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2014; 48:4750-4756. [PMID: 24724561 DOI: 10.1021/es403351h] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/03/2023]
Abstract
Oceanic dimethyl sulfide (DMS) is the enzymatic cleavage product of the algal metabolite dimethylsulfoniopropionate (DMSP) and is the most abundant form of sulfur released into the atmosphere. To investigate the effects of two emerging environmental threats (ocean acidification and warming) on marine DMS production, we performed a large-scale perturbation experiment in a coastal environment. At both ambient temperature and ∼ 2 °C warmer, an increase in partial pressure of carbon dioxide (pCO2) in seawater (160-830 ppmv pCO2) favored the growth of large diatoms, which outcompeted other phytoplankton species in a natural phytoplankton assemblage and reduced the growth rate of smaller, DMSP-rich phototrophic dinoflagellates. This decreased the grazing rate of heterotrophic dinoflagellates (ubiquitous micrograzers), resulting in reduced DMS production via grazing activity. Both the magnitude and sign of the effect of pCO2 on possible future oceanic DMS production were strongly linked to pCO2-induced alterations to the phytoplankton community and the cellular DMSP content of the dominant species and its association with micrograzers.
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Affiliation(s)
- Ki-Tae Park
- School of Environmental Science and Engineering, Pohang University of Science and Technology , Pohang 790-784, Korea
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