Physiology and Molecular Ecology of Microbial Filamentous Sulfur Formation

近年来，我们发现了一种不同寻常的海洋细菌，它将硫化氢氧化成一种新的丝状元素硫，同时将二氧化碳固定在细胞材料中。系统发育研究已将这种微生物归入变形杆菌的epsilon亚科中的Arcobacter属。微生物丝状硫的产生发生在高流体流量的海洋硫化物环境中，包括沿海盐沼小溪、硫化物沉积物和世界各地的海洋热液喷口。在之前的研究中，我们从海岸沉积物(沿海菌株推定命名为硫磺假丝假丝酵母)和深海热液环境中培养出了这种产生丝状物的微生物，并对这一有趣的类群的生理、形态和系统发育进行了研究。本项目的总体目标将是扩大对丝状硫磺形成的微生物生态的研究。到目前为止，对“硫化念珠菌”样生物的丰度、分布、多样性和功能知之甚少。通过与现有的和新开发的针对16S rRNA的不同特异性的荧光标记寡核苷酸进行荧光原位杂交(FISH)，将评估环境样本中的丰度和分布。将从硫化海洋和热液环境中提取基因组DNA和RNA，用于利用变性梯度凝胶电泳(DGGE)、小亚基rRNA基因克隆和测序进行多样性分析。这些数据将为设计更精细的针对组、物种和菌株的16S rRNA探针奠定基础。微电极测量将与FISH一起使用，以测量实验室和环境样品中的相关物理化学参数。“Candidatus Arcobacter Sulfidicus”可能通过另一种途径固定二氧化碳，而不是Calvin-Bassham-Benson循环，其基础是1)缺乏Rubisco，这是许多细菌和绿色植物用于将二氧化碳合并到细胞物质中的代谢途径的关键酶，以及2)细胞的小d13C分馏。因此，这种微生物似乎是第一种无色硫氧化化学自养细菌，它不使用广泛存在的Calvin-Bassham-Benson途径进行固碳。这是一个具有进化意义的发现，我们建议在我们的模式沿海株中阐明这一途径。证据还表明，这种生物能够固定氮，这一点将在更多的研究中得到证实。这项研究的总体意义在于描述了这一独特的自养硫化物氧化过程发生的参数和机制，以及在许多不同环境中负责微生物的丰度、分布和基因多样性。最后，这些结果将增强我们对一种新型的、迄今为止未被考虑的硫磺循环组成部分的生理学和生态学的了解。丝状硫的形成可能是热液喷口的一个重要过程，它延伸到浅层地下生物圈，仅受无机营养物质(如硫化氢和二氧化碳、氮气)的驱动。

In recent years, we have discovered an unusual marine bacterium that oxidizes hydrogen sulfide into a novel filamentous form of elemental sulfur, while fixing CO2 into cell material. Phylogenetic studies have placed this organism into the genus Arcobacter of the epsilon subdivision of the Proteobacteria. Microbial filamentous sulfur production occurs in high fluid flow marine sulfidic environments, including coastal salt marsh creeks, sulfidic sediments, and marine hydrothermal vents worldwide. During the previous research period, we were able to cultivate this filament-producing organism from coastal sediments (coastal strain putatively named "Candidatus Arcobacter sulfidicus") and deep-sea hydrothermal environments, and have investigated the physiology, morphology and phylogeny of this interesting group. The overall goal of the present project will be to expand studies on the microbial ecology of filamentous sulfur formation. So far, little is known of the abundance, distribution, diversity, and function of "Candidatus Arcobacter sulfidicus"-like organisms in situ. Abundance and distribution will be assessed in environmental samples by employing fluorescent in situ hybridization (FISH) with existing and newly developed fluorescently labeled oligonucleotides of different specificity targeting the 16S rRNA. Genomic DNA and RNA will be extracted from sulfidic marine and hydrothermal environments for diversity analyses using denaturing gradient gel electrophoresis (DGGE), small-subunit rRNA gene cloning and sequencing. These data will form the basis for the design of more refined group-, species-, and strain-specific 16S rRNA probes. Microelectrode measurements will be used in concert with FISH to measure relevant physicochemical parameters in laboratory and environmental samples. "Candidatus Arcobacter sulfidicus" is likely to fix CO2 by an alternative pathway other than the Calvin-Bassham-Benson cycle based on 1) the absence of Rubisco, a key enzyme of a metabolic pathway used by many bacteria and green plants for incorporating CO2 into cell material, and 2) the small d13C fractionation by the cells. Thus, this organism seems to be the first colorless sulfur-oxidizing chemolithoautotrophic bacterium that does not use the widespread Calvin-Bassham-Benson pathway for carbon fixation. This is a finding of evolutionary significance and we propose to elucidate the pathway in our model coastal strain. Evidence also suggests that this organism is capable of fixing nitrogen and this will be confirmed in additional studies. The overall significance of this research lies in the characterization of the parameters and mechanisms by which this unique process of autotrophic sulfide oxidation occurs, as well as the abundance, distribution and genotypic diversity of the responsible microbes in a number of different environments. Finally, the results will enhance our knowledge of the physiology and ecology of a novel, and heretofore-unconsidered component of the sulfur cycle. Filamentous sulfur formation may be an important process at hydrothermal vents, extending into the shallow subsurface biosphere and driven by inorganic nutrients alone (i.e. H2S and CO2, N2).