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Hydrogen production in photosynthetic microbial mats in the Elkhorn Slough estuary Monterey Bay

机译:蒙特里湾Elkhorn泥沼河口光合微生物垫中的氢气产生

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摘要

Hydrogen (H2) release from photosynthetic microbial mats has contributed to the chemical evolution of Earth and could potentially be a source of renewable H2 in the future. However, the taxonomy of H2-producing microorganisms (hydrogenogens) in these mats has not been previously determined. With combined biogeochemical and molecular studies of microbial mats collected from Elkhorn Slough, Monterey Bay, California, we characterized the mechanisms of H2 production and identified a dominant hydrogenogen. Net production of H2 was observed within the upper photosynthetic layer (0–2 mm) of the mats under dark and anoxic conditions. Pyrosequencing of rRNA gene libraries generated from this layer demonstrated the presence of 64 phyla, with Bacteriodetes, Cyanobacteria and Proteobacteria dominating the sequences. Sequencing of rRNA transcripts obtained from this layer demonstrated that Cyanobacteria dominated rRNA transcript pyrotag libraries. An OTU affiliated to Microcoleus spp. was the most abundant OTU in both rRNA gene and transcript libraries. Depriving mats of sunlight resulted in an order of magnitude decrease in subsequent nighttime H2 production, suggesting that newly fixed carbon is critical to H2 production. Suppression of nitrogen (N2)-fixation in the mats did not suppress H2 production, which indicates that co-metabolic production of H2 during N2-fixation is not an important contributor to H2 production. Concomitant production of organic acids is consistent with fermentation of recently produced photosynthate as the dominant mode of H2 production. Analysis of rRNA % transcript:% gene ratios and H2-evolving bidirectional [NiFe] hydrogenase % transcript:% gene ratios indicated that Microcoelus spp. are dominant hydrogenogens in the Elkhorn Slough mats.
机译:从光合微生物垫中释放的氢气(H2)促进了地球的化学演化,并且将来可能成为可再生氢气的来源。但是,尚未确定这些垫子中产生H2的微生物(氢原)的分类。通过对从加利福尼亚州蒙特雷湾的Elkhorn Slough收集的微生物垫进行生物地球化学和分子研究相结合,我们表征了H2产生的机理并确定了主要的氢源。在黑暗和缺氧条件下,在垫子的上部光合作用层(0–2 mm)内观察到H2的净产生。从这一层产生的rRNA基因文库的焦磷酸测序证明存在64个门,其中细菌杆菌,蓝细菌和变形杆菌占主导。从这一层获得的rRNA转录物的测序表明,蓝藻占主导地位的rRNA转录物pyrotag文库。隶属于Microcoleus spp的OTU。是rRNA基因和转录文库中最丰富的OTU。剥夺阳光垫会导致随后的夜间H2产生量减少一个数量级,这表明新固定的碳对H2产生至关重要。抑制垫子中固氮(N2)并不能抑制H2的产生,这表明在固氮过程中H2的代谢代谢不是对H2产生的重要贡献。伴随产生的有机酸与最近产生的光合产物的发酵是H2产生的主要方式一致。对rRNA%转录物:%基因比率和H2进化的双向[NiFe]氢化酶%转录物:%基因比率的分析表明,Microcoelus spp。是Elkhorn泥沼垫中的主要氢。

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