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盐度作为普氏鲁杰氏菌DSS-3中DMSP降解的调节剂。

Salinity as a regulator of DMSP degradation in Ruegeria pomeroyi DSS-3.

作者信息

Salgado Paula, Kiene Ronald, Wiebe William, Magalhães Catarina

机构信息

EcoBioTec Laboratory, Interdisciplinary Centre of Marine and Environmental Research (CIIMAR/CIMAR), University of Porto, Rua dos Bragas 289, P 4050-123, Porto, Portugal,

出版信息

J Microbiol. 2014 Nov;52(11):948-54. doi: 10.1007/s12275-014-4409-1. Epub 2014 Oct 3.

Abstract

Dimethylsulfoniopropionate (DMSP) is an important carbon and sulfur source to marine bacterial communities and the main precursor of dimethylsulfide (DMS), a gas that influences atmospheric chemistry and potentially the global climate. In nature, bacterial DMSP catabolism can yield different proportions of DMS and methanethiol (MeSH), but relatively little is known about the factors controlling the pathways of bacterial degradation that select between their formation (cleavage vs. demethiolation). In this study, we carried out experiments to evaluate the influence of salinity on the routes of DMSP catabolism in Ruegeria pomeroyi DSS-3. We monitored DMS and MeSH accumulation in cell suspensions grown in a range of salinities (10, 20, 30 ppt) and with different DMSP amendments (0, 50, 500 µM). Significantly higher concentrations of DMS accumulated in low salinity treatments (10 ppt; P < 0.001), in both Marine Basal Medium (MBM) and half-strength Yeast Tryptone Sea Salts (1/2 YTSS) media. Results showed a 47.1% and 87.5% decrease of DMS accumulation, from salinity 10 to 20 ppt, in MBM and 1/2 YTSS media, respectively. On the other hand, MeSH showed enhanced accumulations at higher salinities (20, 30 ppt), with a 90.6% increase of MeSH accumulation from the 20 ppt to the 30 ppt salinity treatments. Our results with R. pomeroyi DSS-3 in culture are in agreement with previous results from estuarine sediments and demonstrate that salinity can modulate selection of the DMSP enzymatic degradation routes, with a consequent potential impact on DMS and MeSH liberation into the atmosphere.

摘要

二甲基巯基丙酸内盐(DMSP)是海洋细菌群落重要的碳和硫来源,也是二甲基硫醚(DMS)的主要前体,DMS这种气体影响着大气化学,甚至可能影响全球气候。在自然界中,细菌对DMSP的分解代谢能够产生不同比例的DMS和甲硫醇(MeSH),但对于控制细菌降解途径(在二者形成之间进行选择,即裂解与脱甲基化)的因素,人们了解得相对较少。在本研究中,我们开展实验以评估盐度对海氏鲁杰氏菌DSS-3中DMSP分解代谢途径的影响。我们监测了在一系列盐度(10、20、30 ppt)下生长且添加不同浓度DMSP(0、50、500 µM)的细胞悬液中DMS和MeSH的积累情况。在低盐度处理(10 ppt)中,无论是在海洋基础培养基(MBM)还是半强度酵母胰蛋白胨海盐培养基(1/2 YTSS)中,DMS的积累浓度都显著更高(P < 0.001)。结果显示,在MBM和1/2 YTSS培养基中,盐度从10 ppt升至20 ppt时,DMS积累量分别下降了47.1%和87.5%。另一方面,MeSH在较高盐度(20、30 ppt)下积累量增加,盐度从20 ppt升至30 ppt时,MeSH积累量增加了90.6%。我们对海氏鲁杰氏菌DSS-3进行培养得到的结果与之前河口沉积物的结果一致,表明盐度能够调节DMSP酶促降解途径的选择,进而可能影响DMS和MeSH向大气中的释放。

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