首页> 美国卫生研究院文献>Frontiers in Microbiology >Out of the dark: transitional subsurface-to-surface microbial diversity in a terrestrial serpentinizing seep (Manleluag, Pangasinan, the Philippines)
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Out of the dark: transitional subsurface-to-surface microbial diversity in a terrestrial serpentinizing seep (Manleluag, Pangasinan, the Philippines)

机译:走出黑暗:地面蛇形渗漏中地下到地下的微生物多样性(Manleluag,Pangasinan,菲律宾)

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摘要

In the Zambales ophiolite range, terrestrial serpentinizing fluid seeps host diverse microbial assemblages. The fluids fall within the profile of Ca2+-OH-type waters, indicative of active serpentinization, and are low in dissolved inorganic carbon (DIC) (<0.5 ppm). Influx of atmospheric carbon dioxide (CO2) affects the solubility of calcium carbonate as distance from the source increases, triggering the formation of meter-scale travertine terraces. Samples were collected at the source and along the outflow channel to determine subsurface microbial community response to surface exposure. DNA was extracted and submitted for high-throughput 16S rRNA gene sequencing on the Illumina MiSeq platform. Taxonomic assignment of the sequence data indicates that 8.1% of the total sequence reads at the source of the seep affiliate with the genus Methanobacterium. Other major classes detected at the source include anaerobic taxa such as Bacteroidetes (40.7% of total sequence reads) and Firmicutes (19.1% of total reads). Hydrogenophaga spp. increase in relative abundance as redox potential increases. At the carbonate terrace, 45% of sequence reads affiliate with Meiothermus spp. Taxonomic observations and geochemical data suggest that several putative metabolisms may be favorable, including hydrogen oxidation, H2-associated sulfur cycling, methanogenesis, methanotrophy, nitrogen fixation, ammonia oxidation, denitrification, nitrate respiration, methylotrophy, carbon monoxide respiration, and ferrous iron oxidation, based on capabilities of nearest known neighbors. Scanning electron microscopy and energy dispersive X-ray spectroscopy suggest that microbial activity produces chemical and physical traces in the precipitated carbonates forming downstream of the seep's source. These data provide context for future serpentinizing seep ecosystem studies, particularly with regards to tropical biomes.
机译:在Zambales蛇绿岩范围内,陆生蛇毒化液渗漏会容纳各种微生物。流体属于Ca 2 + -OH -型水的轮廓,表明发生了主动蛇纹石化,并且溶解的无机碳(DIC)含量低(<0.5 ppm )。随着距源的距离增加,大气二氧化碳(CO2)的流入会影响碳酸钙的溶解度,从而引发米级石灰华阶地的形成。在源处和沿流出通道收集样品,以确定地下微生物群落对表面暴露的响应。提取DNA并提交给Illumina MiSeq平台进行高通量16S rRNA基因测序。序列数据的分类分配表明,总序列的8.1%在与甲基杆菌属的渗入关联的来源处读取。在来源处检测到的其他主要类别包括厌氧类群,例如拟杆菌(占总序列读数的40.7%)和Firmicutes(占总读数的19.1%)。氢加氢菌属相对丰度随着氧化还原电位的增加而增加。在碳酸盐阶地,45%的序列读数与Meiothermus spp相关。分类学观察和地球化学数据表明,几种可能的新陈代谢可能是有利的,包括氢氧化,H2相关的硫循环,甲烷生成,甲烷氧化,固氮,氨氧化,反硝化,硝酸盐呼吸,甲基营养,一氧化碳呼吸和亚铁氧化,基于最近的已知邻居的能力。扫描电子显微镜和能量色散X射线光谱学表明,微生物活动会在渗流源下游形成的沉淀碳酸盐中产生化学和物理痕迹。这些数据为将来的蛇形渗流生态系统研究提供了背景,特别是在热带生物群落方面。

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