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首页> 外文期刊>Geobiology >Assessing the influence of physical, geochemical and biological factors on anaerobic microbial primary productivity within hydrothermal vent chimneys.
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Assessing the influence of physical, geochemical and biological factors on anaerobic microbial primary productivity within hydrothermal vent chimneys.

机译:评估物理,地球化学和生物学因素对热液喷口烟囱中厌氧微生物初级生产力的影响。

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Chemosynthetic primary production supports hydrothermal vent ecosystems, but the extent of that productivity and its governing factors have not been well constrained. To better understand anaerobic primary production within massive vent deposits, we conducted a series of incubations at 4, 25, 50 and 90C using aggregates recovered from hydrothermal vent structures. We documented in situ geochemistry, measured autochthonous organic carbon stable isotope ratios and assessed microbial community composition and functional gene abundances in three hydrothermal vent chimney structures from Middle Valley on the Juan de Fuca Ridge. Carbon fixation rates were greatest at lower temperatures and were comparable among chimneys. Stable isotope ratios of autochthonous organic carbon were consistent with the Calvin-Benson-Bassham cycle being the predominant mode of carbon fixation for all three chimneys. Chimneys exhibited marked differences in vent fluid geochemistry and microbial community composition, with structures being differentially dominated by gamma () or epsilon () proteobacteria. Similarly, qPCR analyses of functional genes representing different carbon fixation pathways showed striking differences in gene abundance among chimney structures. Carbon fixation rates showed no obvious correlation with observed in situ vent fluid geochemistry, community composition or functional gene abundance. Together, these data reveal that (i) net anaerobic carbon fixation rates among these chimneys are elevated at lower temperatures, (ii) clear differences in community composition and gene abundance exist among chimney structures, and (iii) tremendous spatial heterogeneity within these environments likely confounds efforts to relate the observed rates to in situ microbial and geochemical factors. We also posit that microbes typically thought to be mesophiles are likely active and growing at cooler temperatures, and that their activity at these temperatures comprises the majority of endolithic anaerobic primary production in hydrothermal vent chimneys. 2013 Blackwell Publishing Ltd.Registry Number/Name of Substance 0 (Carbon Isotopes). 0 (Carbon Radioisotopes). 0 (RNA, Ribosomal, 16S).
机译:化学合成的初级生产支持热液喷口生态系统,但是生产力的程度及其控制因素尚未得到很好的限制。为了更好地了解大量通风口沉积物中的厌氧初级生产,我们使用了从热液通风口结构中回收的骨料在4、25、50和90°C进行了一系列孵育。我们记录了原位地球化学,测量了自生有机碳稳定同位素比率,并评估了胡安德富卡岭中谷三个热液喷口烟囱结构中的微生物群落组成和功能基因丰度。碳固定率在较低温度下最大,在烟囱中可比。本地有机碳的稳定同位素比与卡尔文-本森-巴瑟姆循环是所有三个烟囱的主要固碳模式一致。烟囱在排放流体的地球化学和微生物群落组成方面表现出显着差异,其结构以γ()或ε()变形杆菌为主导。同样,代表不同碳固定途径的功能基因的qPCR分析显示,烟囱结构之间的基因丰度存在显着差异。碳固定率与观察到的原位流体地球化学,群落组成或功能基因丰度没有明显的相关性。这些数据加在一起表明(i)这些烟囱中的净厌氧碳固定率在较低温度下会升高;(ii)烟囱结构之间的群落组成和基因丰度存在明显差异;(iii)这些环境中可能存在巨大的空间异质性混淆了将观测到的速率与原位微生物和地球化学因子相关联的努力。我们还假设,通常被认为是嗜温菌的微生物可能会在较低温度下活跃并生长,并且在这些温度下它们的活性构成了热液通风烟囱中大部分内质厌氧初级产物。 2013 Blackwell Publishing Ltd.注册编号/物质名称0(碳同位素)。 0(碳放射性同位素)。 0(RNA,核糖体,16S)。

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