| Literature DB >> 27573103 |
Jing Sun1, Jonathan D Todd2, J Cameron Thrash3, Yanping Qian4, Michael C Qian4, Ben Temperton5, Jiazhen Guo6, Emily K Fowler2, Joshua T Aldrich7, Carrie D Nicora7, Mary S Lipton7, Richard D Smith7, Patrick De Leenheer8, Samuel H Payne7, Andrew W B Johnston2, Cleo L Davie-Martin1, Kimberly H Halsey1, Stephen J Giovannoni1.
Abstract
Marine phytoplankton produce ∼10(9) tonnes of dimethylsulfoniopropionate (DMSP) per year(1,2), an estimated 10% of which is catabolized by bacteria through the DMSP cleavage pathway to the climatically active gas dimethyl sulfide(3,4). SAR11 Alphaproteobacteria (order Pelagibacterales), the most abundant chemo-organotrophic bacteria in the oceans, have been shown to assimilate DMSP into biomass, thereby supplying this cell's unusual requirement for reduced sulfur(5,6). Here, we report that Pelagibacter HTCC1062 produces the gas methanethiol, and that a second DMSP catabolic pathway, mediated by a cupin-like DMSP lyase, DddK, simultaneously shunts as much as 59% of DMSP uptake to dimethyl sulfide production. We propose a model in which the allocation of DMSP between these pathways is kinetically controlled to release increasing amounts of dimethyl sulfide as the supply of DMSP exceeds cellular sulfur demands for biosynthesis.Entities:
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Year: 2016 PMID: 27573103 DOI: 10.1038/nmicrobiol.2016.65
Source DB: PubMed Journal: Nat Microbiol ISSN: 2058-5276 Impact factor: 17.745