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Collaborative Research: Loihi Seamount as an Observatory for the Study of Neutrophilic Iron-Oxidizing Bacteria and the Microbial Iron Cycle

Collaborative Research: Loihi Seamount as an Observatory for the Study of Neutrophilic Iron-Oxidizing Bacteria and the Microbial Iron Cycle
合作研究:洛伊希海山作为研究中性粒细胞铁氧化细菌和微生物铁循环的观测站
批准号:
0810973
负责人:
David Emerson
金额:
$11.47万
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2007
资助国家:
美国
项目状态:
已结题
起止时间:
2007-11-01 至 2010-08-31

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中文摘要
翻译
金属对生命的重要性早已为人们所认识。铁(Fe)是地壳中含量第四丰富的元素,也是第二丰富的氧化还原活性元素,使其成为最重要的环境金属。认识到这一点,最近对环境中微生物铁氧化还原转化的研究激增,导致了许多令人兴奋的发现,并增强了对这些过程重要性的认识(Lovley 2000)。然而,这些研究大多集中在还原性铁循环和生物,如地杆菌科。这在一定程度上是因为铁氧化生物,特别是那些生活在环中性pH环境中的生物,在实验室中培养和研究是出了名的困难。然而,最近在这方面的成功已经导致了许多新的化学岩石自养铁氧化细菌(FeOB)的分离。对这些细菌的研究揭示了它们在生理上和系统发育上的显著多样性。考虑到铁是地壳中最丰富的岩石自养能量来源,这也许不应该令人惊讶,但这与目前对他们的研究的关注不一致。这个项目正在夏威夷海底山启动一个微生物观测站,用于研究铁氧化细菌(. femo)。该项目的主要目的是阐明这群原核生物的生理、系统发育和生化多样性。之所以选择Loihi作为研究地点,是因为:(1)FeOB之前在Loihi得到了认可和研究;(2) Loihi具有广泛的FeOB生境,从热液流体到岩石,从低流量、低t (10C)渗漏到高流量、高t (60C)喷口;(3)前人的研究为今后的研究提供了良好的地球化学框架;(4)洛伊岛位于夏威夷大岛西南25英里处,交通十分便利。该研究小组代表了FeOB的专业知识的横截面。FeMO项目的主要组成部分包括:(1)FeOB的培养分析,(2)Fe氧化速率的动力学研究,(3)Fe氧化酶的生化研究,以及(4)FeOB在固体岩石中的定殖和利用的生物地球化学研究。众所周知,微生物铁氧化还原转化会影响环境和人类健康,例如在有机污染物降解和通过有毒放射性核苷酸的吸收方面,特别是在陆地和沿海海洋生境中。在研究较少的贫营养深海中,化学自养FeOB最近被认为在生产新的生物质碳方面具有潜在的重要作用。这项研究在FeOB研究和了解其环境活动和能力方面取得了重大进展,并将使人们能够更准确地预测许多难以进入的栖息地的FeOB。FeMO的pi大量参与了世卫组织的初中和高中教师教育和加强工作。这些措施包括参加现有的夏季讲习班,开发新的学年周末小型讲习班,以及一名教师直接参与FeMO的实地工作。FeMO的参与者还在多个方面积极参与高等教育,包括通过Praxis项目专门招聘新英格兰女子学院(史密斯)的女性和少数族裔本科生进行暑期实习。
英文摘要
AbstractThe importance of metals to life has long been appreciated. Iron (Fe) is the fourth most abundant element, and the second most abundant redox-active element in Earth's crust, rendering it the most important environmental metal. In recognition of this, a recent surge in research on microbial Fe redox transformations in the environment has resulted in many exciting discoveries and enhanced appreciation for the importance of these processes (Lovley 2000). Most of these studies, however, have focused on the reductive Fe cycle and organisms such as the Geobacteraceae. This is in part because Fe-oxidizing organisms, particularly those who inhabit circumneutral pH habitats, have been notoriously difficult to culture and study in the lab. However, recent successes on this front have resulted in the isolation of a number of novel chemolithoautotrophic Fe-oxidizing bacteria (FeOB). Studies of these bacteria have revealed a remarkable diversity, both physiologically and phylogenetically. This perhaps should not be surprising given that Fe is the most abundant lithoautotrophic energy source in Earth's crust, but is not in keeping with the present attention given to their study. This project is initiating a microbial observatory for the study of iron-oxidizing bacteria (.FeMO.) at the Hawaiian Seamount, Loihi. The major purpose of the project is to elucidate the full physiological, phylogenetic, and biochemical diversity of this group of prokaryotes. Loihi was selected as the study site because: (1) FeOB have been recognized and studied there previously; (2) Loihi displays a wide-range of FeOB habitats: from hydrothermal fluids to rocks, from low-flow, low-T (10C) seeps to high-flow, high-T (60C) vents; (3) previous studies provided an excellent geochemical framework on which to base these studies; and (4) Loihi is very accessible, located only 25 miles SW of the big island of Hawaii. The research group represents a cross-section of expertise on FeOB. Principal components of the FeMO project include (1) cultural analysis of FeOB, (2) kinetic studies on Fe-oxidation rates, (3) biochemical studies on the Fe oxidase, and (4) biogeochemical studies on colonization and solid rock utilization by FeOB. Microbial Fe redox transformations are well known to impact environmental and human health, for example in organic contaminant degradation and via sorption of toxic radionucleotides, particularly in terrestrial and coastal marine habitats. In the more poorly studied, oligotrophic deep-sea, chemoautotrophic FeOB have recently been recognized for their potentially important role in production of new biomass carbon. This research is leading to significant advances in the study of FeOB and understanding their environmental activities and capabilities, and would enable more accurate predictions about them in many poorly-accessible habitats. The FeMO PIs are involved heavily in middle and high-school teacher education and enhancement efforts at WHOI. These include participation in existing summer workshops, the development of a new school-year weekend mini-workshop, and the direct involvement of a teacher in the FeMO fieldwork. FeMO participants are also be strongly involved with higher education on multiple fronts, including the specific recruitment of female and minority undergraduates from a New England women's college (Smith) for summer internships via the Praxis program.
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会议论文
NNA: Collaborative Research: Interactions of the Microbial Iron and Methane Cycles in the Tundra Ecosystem
A holistic framework for hybrid modelling of solid-liquid flows
Collaborative Research: The Role of Iron-oxidizing Bacteria in the Sedimentary Iron Cycle: Ecological, Physiological and Biogeochemical Implications
HIGH PERFORMANCE COMPUTING SUPPORT FOR UNITED KINGDOM CONSORTIUM ON TURBULENT REACTING FLOWS (UKCTRF)
国内基金
海外基金
Research on Quantum Field Theory without a Lagrangian Description
  • 批准号:
    24ZR1403900
  • 项目类别:
    省市级项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    SATOSHI NAWATA
  • 依托单位:
Cell Research
Cell Research
Cell Research (细胞研究)