Collaborative Research: Multiple Sulfur Isotope Tracers of the Subsurface Biosphere in Oceanic Basement

合作研究：海洋基底地下生物圈的多种硫同位素示踪剂

• 批准号: 0753126
• 负责人: Shuhei Ono
• 金额: $ 12.83万
• 依托单位: Massachusetts Institute of Technology
• 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
• 起止时间: 2007-07-01 至 2009-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0753126&HistoricalAwards=false
• 关键词: Collaborative; Research; Multiple; Sulfur; Isotope

ABSTRACT 0622949/0622982/0623550 (Alt/Rouxel/Ono)Intellectual Merit: Fluids circulate at low temperatures (100C) through the upper oceanic crust on mid ocean ridge flanks and in ocean basins providing vast potential habitats for a subsurface biosphere. This work tests the hypothesis that microbial sulfate reduction occurs in crystalline oceanic basement rocks (basalts and gabbros), and that it is a widespread and important processes affecting the sulfur budget of the oceanic crust. The research plan entails determining the contents and stable isotope ratios of sulfur (S) and selenium (Se) in altered oceanic basement. Specific analyses include ion microprobe analyses of del 34S of individual sulfide grains, whole rock S and Se contents, Se isotopes and multiple-sulfur isotope ratio analyses (del 33S, del 34S and del 36S). The data enable testing for microbial signatures, provide evidence for fluid evolution, help constrain redox conditions and the sources of S in the rocks (remobilized basaltic sulfide or seawater), and aid in understanding the effects of microbial activity on the budget for S during alteration of oceanic basement. The research focuses on upper oceanic basement from well-studied IODP Site U1301, but also includes gabbros from ODP Hole 735B, and limited analyses of other basaltic basement. Results of the work help improve our understanding of microbial activity during alteration of ocean crust, and provide a basis for establishing links between geochemistry and microbiology. Broader Impacts:This research will support two early career scientists and one senior scientist in Washington DC, Massachusetts, and Michigan, respectively. The research is multi-institutional and will engage undergraduates in research. The work leverages NSF investments by using samples collected by the NSF-Ocean Drilling program.

摘要0622949/0622982/0623550（Alt/Rouxel/Ono）智力优势：流体在低温（100 ℃）下通过大洋中脊侧翼的上洋壳和海洋盆地循环，为地下生物圈提供了巨大的潜在栖息地。本工作验证了微生物硫酸盐还原发生在结晶大洋基底岩石（玄武岩和辉长岩）中的假设，并且它是影响大洋地壳硫收支的广泛而重要的过程。研究计划是测定蚀变洋基中硫（S）和硒（Se）的含量和稳定同位素比值。 具体分析包括单个硫化物颗粒的del 34 S离子探针分析、全岩S和Se含量、Se同位素和多种硫同位素比值分析（del 33 S、del 34 S和del 36 S）。这些数据使测试微生物的签名，提供证据的流体演化，有助于约束氧化还原条件和来源的S在岩石（再活化玄武岩硫化物或海水），并帮助了解微生物活动的影响，预算的S在海洋基底的蚀变。研究重点是来自IODP站点U1301的上大洋基底，但也包括ODP 735 B孔的辉长岩，以及对其他玄武岩基底的有限分析。 这项工作的结果有助于提高我们对海洋地壳蚀变过程中微生物活动的理解，并为建立地球化学和微生物学之间的联系提供了基础。更广泛的影响：这项研究将分别支持华盛顿特区、马萨诸塞州和密歇根州的两名早期职业科学家和一名高级科学家。 这项研究是多机构的，将从事本科生的研究。 这项工作通过使用NSF海洋钻探计划收集的样本来利用NSF的投资。