中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater

文献类型:期刊论文

作者Swanner, Elizabeth D.1,2; Maisch, Markus2; Wu, Wenfang2,3; Kappler, Andreas2
刊名SCIENTIFIC REPORTS
出版日期2018-03-09
卷号8
ISSN号2045-2322
DOI10.1038/s41598-018-22694-y
文献子类Article
英文摘要Many marine Precambrian iron formations (IF) record deep anoxic seawater enriched in Fe(II) (i.e. ferruginous) overlain by mildly oxygenated surface water. This is reflected by iron-rich sediments forming in deep basins, and relatively iron-poor sediments forming in shallow, sunlit waters. Such an iron gradient is often interpreted as a redox interface where dissolved Fe(II) was oxidized and precipitated as Fe(III)-bearing minerals. As such, sedimentary iron enrichments are proxy to the progressive oxidation of the oceans through geological time. However, this interpretation is founded on the assumption that Fe(II) could not persist within an oxygenated water column. Here, we cultivated cyanobacteria in an illuminated column supplied with Fe(II)-rich seawater medium in a laboratory-scale analog of a continental margin supporting IF deposition. We first observed Fe(II) oxidation with oxygen, then biologically-mediated reduction of Fe(III) (oxyhydr) oxides, which maintained a pool of Fe(II) in the presence of oxygen. Such steady-state iron redox cycling may have maintained dissolved, and hence mobile Fe(II) in oxygenated seawater above ferruginous deep basins such as those inferred for many Precambrian IF.
WOS关键词IRON ACQUISITION ; SOUTH-AFRICA ; CARBONATE PRECIPITATION ; HETEROTROPHIC BACTERIA ; SIDEROPHORE PRODUCTION ; TRANSVAAL SUPERGROUP ; SPATIAL VARIABILITY ; KAAPVAAL CRATON ; ARCHEAN OCEAN ; REDOX STATE
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000427017800001
出版者NATURE PUBLISHING GROUP
资助机构Carl Zeiss postdoctoral fellowship ; Carl Zeiss postdoctoral fellowship ; NSFC(41502320) ; NSFC(41502320) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; European Research Council (ERC)(307320-MICROFOX) ; European Research Council (ERC)(307320-MICROFOX) ; Deutsche Forschungsgemeinschaft (DFG) ; Deutsche Forschungsgemeinschaft (DFG) ; Open Access Publishing Fund of University of Tubingen ; Open Access Publishing Fund of University of Tubingen ; Carl Zeiss postdoctoral fellowship ; Carl Zeiss postdoctoral fellowship ; NSFC(41502320) ; NSFC(41502320) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; European Research Council (ERC)(307320-MICROFOX) ; European Research Council (ERC)(307320-MICROFOX) ; Deutsche Forschungsgemeinschaft (DFG) ; Deutsche Forschungsgemeinschaft (DFG) ; Open Access Publishing Fund of University of Tubingen ; Open Access Publishing Fund of University of Tubingen ; Carl Zeiss postdoctoral fellowship ; Carl Zeiss postdoctoral fellowship ; NSFC(41502320) ; NSFC(41502320) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; European Research Council (ERC)(307320-MICROFOX) ; European Research Council (ERC)(307320-MICROFOX) ; Deutsche Forschungsgemeinschaft (DFG) ; Deutsche Forschungsgemeinschaft (DFG) ; Open Access Publishing Fund of University of Tubingen ; Open Access Publishing Fund of University of Tubingen ; Carl Zeiss postdoctoral fellowship ; Carl Zeiss postdoctoral fellowship ; NSFC(41502320) ; NSFC(41502320) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; Sino-German (CSC-DAAD) postdoc scholarship, China Postdoc Science Foundation(2014M560115) ; European Research Council (ERC)(307320-MICROFOX) ; European Research Council (ERC)(307320-MICROFOX) ; Deutsche Forschungsgemeinschaft (DFG) ; Deutsche Forschungsgemeinschaft (DFG) ; Open Access Publishing Fund of University of Tubingen ; Open Access Publishing Fund of University of Tubingen
源URL[http://ir.iggcas.ac.cn/handle/132A11/83092]  
专题中国科学院地质与地球物理研究所
通讯作者Swanner, Elizabeth D.
作者单位1.Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA USA
2.Univ Tubingen, Dept Geosci, Tubingen, Germany
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Swanner, Elizabeth D.,Maisch, Markus,Wu, Wenfang,et al. Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater[J]. SCIENTIFIC REPORTS,2018,8.
APA Swanner, Elizabeth D.,Maisch, Markus,Wu, Wenfang,&Kappler, Andreas.(2018).Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater.SCIENTIFIC REPORTS,8.
MLA Swanner, Elizabeth D.,et al."Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater".SCIENTIFIC REPORTS 8(2018).

入库方式: OAI收割

来源:地质与地球物理研究所

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