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潮间带蓝藻席的氢气输出:来源、通量及群落组成的影响

Hydrogen export from intertidal cyanobacterial mats: sources, fluxes and the influence of community composition.

作者信息

Hoffmann Dörte, Maldonado Juan, Wojciechowski Martin F, Garcia-Pichel Ferran

机构信息

School of Life Sciences, Arizona State University, Tempe, AZ, 85287-4501, USA.

出版信息

Environ Microbiol. 2015 Oct;17(10):3738-53. doi: 10.1111/1462-2920.12769. Epub 2015 Mar 4.

DOI:10.1111/1462-2920.12769
PMID:25580666
Abstract

Microbial mats from marine intertidal settings have been reported to release significant quantities of H2 , in a unique trait among other mats and microbial communities. However, the H2 source and ecophysiological mechanisms that enable its export are not well understood. We examined H2 accumulation and export in three types of greenhouse-reared mats, from the intertidal region of Guerrero Negro, Mexico, and kept under natural light-dark conditions and wetting and drying cycles simulating low-, mid- and high-tidal height periodicity. All mats released H2 reproducibly and sustainably for 1.5 years. Net H2 export took place in a pulsed daily manner, starting after dusk, and waning in the morning, as photosynthesis resumed. Mid- and low-tidal mats developed high concentrations, capable of sustaining export fluxes that represented 2-4% of the water split through primary productivity. Neither N2 fixation nor direct photolytic hydrogenogenesis was significant to this H2 export, which was fermentative in origin, variable among mats, originating from cyanobacterial photosynthate. Analyses of community composition by pyrosequencing of 16S rRNA and hoxH genes indicate that filamentous non-heterocystous cyanobacteria (e.g. Lyngbya, Microcoleus) were important in the process of H2 export, as was the relatively low abundance and activity of methanogens and sulfate reducers.

摘要

据报道,来自海洋潮间带环境的微生物席会释放大量氢气,这是其他微生物席和微生物群落所没有的独特特征。然而,氢气的来源以及使其输出的生态生理机制尚不清楚。我们研究了三种在温室中培育的微生物席的氢气积累和输出情况,这些微生物席取自墨西哥格雷罗内格罗的潮间带区域,并置于自然光照-黑暗条件以及模拟低潮、中潮和高潮高度周期性的干湿循环环境中。所有微生物席在1.5年的时间里都能持续稳定地释放氢气。氢气的净输出以每日脉冲的方式进行,在黄昏后开始,随着光合作用的恢复在早晨减弱。中潮和低潮微生物席积累了高浓度的氢气,能够维持相当于通过初级生产力分解的水的2%-4%的输出通量。固氮作用和直接光解产氢对这种氢气输出都没有显著影响,其来源是发酵作用,不同微生物席之间存在差异,源自蓝藻光合产物。通过对16S rRNA和hoxH基因进行焦磷酸测序分析群落组成表明,丝状非异形蓝藻(如鞘丝藻、微鞘藻)在氢气输出过程中很重要,产甲烷菌和硫酸盐还原菌的相对低丰度和活性也是如此。

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