Lavik Gaute, Stührmann Torben, Brüchert Volker, Van der Plas Anja, Mohrholz Volker, Lam Phyllis, Mussmann Marc, Fuchs Bernhard M, Amann Rudolf, Lass Ulrich, Kuypers Marcel M M
Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, D-28359 Bremen, Germany.
Nature. 2009 Jan 29;457(7229):581-4. doi: 10.1038/nature07588. Epub 2008 Dec 10.
Coastal waters support approximately 90 per cent of global fisheries and are therefore an important food reserve for our planet. Eutrophication of these waters, due to human activity, leads to severe oxygen depletion and the episodic occurrence of hydrogen sulphide-toxic to multi-cellular life-with disastrous consequences for coastal ecosytems. Here we show that an area of approximately 7,000 km(2) of African shelf, covered by sulphidic water, was detoxified by blooming bacteria that oxidized the biologically harmful sulphide to environmentally harmless colloidal sulphur and sulphate. Combined chemical analyses, stoichiometric modelling, isotopic incubations, comparative 16S ribosomal RNA, functional gene sequence analyses and fluorescence in situ hybridization indicate that the detoxification proceeded by chemolithotrophic oxidation of sulphide with nitrate and was mainly catalysed by two discrete populations of gamma- and epsilon-proteobacteria. Chemolithotrophic bacteria, accounting for approximately 20 per cent of the bacterioplankton in sulphidic waters, created a buffer zone between the toxic sulphidic subsurface waters and the oxic surface waters, where fish and other nekton live. This is the first time that large-scale detoxification of sulphidic waters by chemolithotrophs has been observed in an open-ocean system. The data suggest that sulphide can be completely consumed by bacteria in the subsurface waters and, thus, can be overlooked by remote sensing or monitoring of shallow coastal waters. Consequently, sulphidic bottom waters on continental shelves may be more common than previously believed, and could therefore have an important but as yet neglected effect on benthic communities.
沿海水域支撑着全球约90%的渔业,因此是我们星球重要的食物储备地。由于人类活动导致这些水域富营养化,进而引发严重的氧气消耗,并间歇性出现对多细胞生物有毒的硫化氢,给沿海生态系统带来灾难性后果。在此我们表明,一片面积约7000平方公里、覆盖着含硫水的非洲大陆架区域,因细菌大量繁殖而实现了解毒,这些细菌将对生物有害的硫化氢氧化为对环境无害的胶体硫和硫酸盐。综合化学分析、化学计量模型、同位素培养、比较16S核糖体RNA、功能基因序列分析以及荧光原位杂交表明,解毒过程是通过硫化物与硝酸盐的化学无机营养氧化进行的,主要由γ-和ε-变形菌的两个不同种群催化。化学无机营养细菌约占含硫水域浮游细菌的20%,在有毒的含硫次表层水和鱼类及其他游泳生物生存的含氧表层水之间形成了一个缓冲区。这是首次在开放海洋系统中观察到化学无机营养菌对含硫水域的大规模解毒现象。数据表明,硫化物可被次表层水中的细菌完全消耗,因此在对浅海沿海水域的遥感或监测中可能被忽略。因此,大陆架上的含硫底层水可能比之前认为的更为常见,从而可能对底栖生物群落产生重要但尚未得到重视的影响。