What are the sources and mechanisms of iron enrichments during oceanic anoxic event 2? - Evidence from iron stable isotopes
海洋缺氧事件2期间铁富集的来源和机制是什么?
基本信息
- 批准号:0929383
- 负责人:
- 金额:$ 14.97万
- 依托单位:
- 依托单位国家:美国
- 项目类别:Standard Grant
- 财政年份:2009
- 资助国家:美国
- 起止时间:2009-09-01 至 2011-08-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5). This project will investigate the paleo-geological history of Ocean Anoxic Event II (OAEII, ~94 Ma) by iron isotopic analyses (d56Fe) of total iron in archived sediment cores from the proto North Atlantic and bordering Western Interior Seaway, including several from DSDP and ODP. OAEII sediments are characterized by concentrations of high organic carbon (OC) which might have resulted either from 1) increased preservation of OC resulting from more anoxic conditions globally, or 2) increased surface ocean productivity. The effects of iron on ocean productivity and the overall carbon cycle during OAEII is a major aim of this research. To this end, the research will investigate the relative inputs of Fe to euxinic sediments from hydrothermal inputs versus that remobilized from shelf sediments that should carry a distinctly lower d56Fe value than the hydrothermal source. The d56Fe values and FeT/Al ratios of sedimentary iron in euxinic sediments of OAEII will reflect the relative contribution from hydrothermal sources. This research will try to constrain the overall mass balance of iron in the ocean during OAEII and thus expand the use of Fe isotopic analyses for paleo-environmental assessment.Broader impacts: The research supports an undergraduate student, a postdoc, and an early career female scientist. As part of the Center for Ocean Science Education Excellence at Rutgers University, the PI will work with the Center?s Director to incorporate the research results into online educational materials directed at K-12 teachers, K -16 students, and coastal managers.
项目成果
期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
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Silke Severmann其他文献
Silke Severmann的其他文献
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{{ truncateString('Silke Severmann', 18)}}的其他基金
Collaborative Research: US GEOTRACES GP17-ANT: Iron redox cycling in the Amundsen Sea in the water column and shelf sediments
合作研究:US GEOTRACES GP17-ANT:阿蒙森海水柱和陆架沉积物中的铁氧化还原循环
- 批准号:
2124172 - 财政年份:2022
- 资助金额:
$ 14.97万 - 项目类别:
Standard Grant
Collaborative Research: Investigation of paired uranium and chromium isotope behavior during authigenic metal uptake into continental margin sediments
合作研究:研究大陆边缘沉积物吸收自生金属过程中的成对铀和铬同位素行为
- 批准号:
1657690 - 财政年份:2017
- 资助金额:
$ 14.97万 - 项目类别:
Standard Grant
Collaborative Research (OSU, USC, RU): Continental Shelf Diagenesis II: The Importance of Increasing Oceanic Hypoxia to Coastal Iron Supply and the Ocean's Iron Isotope Composition
合作研究(俄勒冈州立大学、南加州大学、俄罗斯大学):大陆架成岩作用 II:海洋缺氧加剧对沿海铁供应和海洋铁同位素组成的重要性
- 批准号:
1029739 - 财政年份:2011
- 资助金额:
$ 14.97万 - 项目类别:
Continuing Grant
Collaborative Research (OSU, USC, UCR): Continental Shelf Diagenesis: The Importance of Fresh Continental Material Degradation and Seasonal Diagenesis to Coastal Iron Supply
合作研究(OSU、USC、UCR):大陆架成岩作用:新鲜大陆物质降解和季节性成岩作用对沿海铁供应的重要性
- 批准号:
0624704 - 财政年份:2006
- 资助金额:
$ 14.97万 - 项目类别:
Standard Grant
Collaborative Research (UCR, OSU and ASU): Combined Fe-S Stable Isotopes in Modern Anoxic Environments and the Effect of Fe versus S Limitation
合作研究(UCR、OSU 和 ASU):现代缺氧环境中的组合 Fe-S 稳定同位素以及 Fe 与 S 限制的影响
- 批准号:
0551716 - 财政年份:2006
- 资助金额:
$ 14.97万 - 项目类别:
Continuing Grant
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