Howard Erinn C, Henriksen James R, Buchan Alison, Reisch Chris R, Bürgmann Helmut, Welsh Rory, Ye Wenying, González José M, Mace Kimberly, Joye Samantha B, Kiene Ronald P, Whitman William B, Moran Mary Ann
Department of Microbiology, University of Georgia, Athens, GA 30602, USA.
Science. 2006 Oct 27;314(5799):649-52. doi: 10.1126/science.1130657.
Flux of dimethylsulfide (DMS) from ocean surface waters is the predominant natural source of sulfur to the atmosphere and influences climate by aerosol formation. Marine bacterioplankton regulate sulfur flux by converting the precursor dimethylsulfoniopropionate (DMSP) either to DMS or to sulfur compounds that are not climatically active. Through the discovery of a glycine cleavage T-family protein with DMSP methyltransferase activity, marine bacterioplankton in the Roseobacter and SAR11 taxa were identified as primary mediators of DMSP demethylation to methylmercaptopropionate. One-third of surface ocean bacteria harbor a DMSP demethylase homolog and thereby route a substantial fraction of global marine primary production away from DMS formation and into the marine microbial food web.
海洋表层水体中二甲基硫(DMS)的通量是大气中硫的主要自然来源,并通过气溶胶形成影响气候。海洋浮游细菌通过将前体二甲基磺基丙酸(DMSP)转化为DMS或转化为对气候无活性的硫化合物来调节硫通量。通过发现一种具有DMSP甲基转移酶活性的甘氨酸裂解T家族蛋白,玫瑰杆菌属和SAR11类群中的海洋浮游细菌被确定为DMSP去甲基化生成甲基巯基丙酸的主要介质。三分之一的海洋表层细菌含有DMSP去甲基酶同源物,从而使全球海洋初级生产的很大一部分从DMS形成转向海洋微生物食物网。