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• W2119048543 startingPage "187" @default.
• W2119048543 abstract "Modern hydrothermal Fe-Si oxyhydroxide deposits are now known to be analogues to ancient siliceous iron formations. In this study, samples of Fe-Si oxyhydroxide deposits were collected from hydrothermal field on the Southwest Indian Ridge. An investigation of mineralization in these deposits was carried out based on a series of mineralogical and morphological methods. X-ray diffraction and selected area electron diffraction analysis show that amorphous opal and poorly crystalline ferrihydrite are the major minerals. Furthermore, some typical filament structures detected by scanning electronic microscopy examinations, probably indicating the presence of Fe-oxidizing bacteria (FeOB), are pervasive with the main constituents being Fe, Si, P, and C. We thus believe that chemolithoautotrophic FeOB play a significant role in the formation of Fe oxyhydroxide which can effectively oxidize reduced Fe(II) sourced from hydrothermal fluids. Precipitation of amorphous silica, in contrast, is only a passive process with the Fe oxyhydroxide acting as a template. The distinct microlaminae structure alternating between the Fe-rich and Si-rich bands was observed in our samples for the first time in modern seafloor hydrothermal systems. We propose that its formation was due to the episodic temperature variation of the hydrothermal fluid which controls the biogenic Fe oxyhydroxide formation and passive precipitation of silica in this system. Our results might provide a clue for the formation mechanism of ancient banded iron formations." @default.
• W2119048543 created "2016-06-24" @default.
• W2119048543 creator A5009425326 @default.
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• W2119048543 creator A5058751848 @default.
• W2119048543 creator A5080865186 @default.
• W2119048543 date "2015-01-01" @default.
• W2119048543 modified "2023-10-16" @default.
• W2119048543 title "Generation of hydrothermal Fe-Si oxyhydroxide deposit on the Southwest Indian Ridge and its implication for the origin of ancient banded iron formations" @default.
• W2119048543 cites W1499863402 @default.
• W2119048543 cites W1534791926 @default.
• W2119048543 cites W1554068896 @default.
• W2119048543 cites W1590863077 @default.
• W2119048543 cites W1595879896 @default.
• W2119048543 cites W1631013115 @default.
• W2119048543 cites W1935610446 @default.
• W2119048543 cites W1951468408 @default.
• W2119048543 cites W1963935934 @default.
• W2119048543 cites W1964107100 @default.
• W2119048543 cites W1975467093 @default.
• W2119048543 cites W1977533913 @default.
• W2119048543 cites W1977864076 @default.
• W2119048543 cites W1978000358 @default.
• W2119048543 cites W1978079527 @default.
• W2119048543 cites W1981544214 @default.
• W2119048543 cites W1989119772 @default.
• W2119048543 cites W1990176899 @default.
• W2119048543 cites W1992933657 @default.
• W2119048543 cites W1996895998 @default.
• W2119048543 cites W2002458511 @default.
• W2119048543 cites W2003214425 @default.
• W2119048543 cites W2003239079 @default.
• W2119048543 cites W2005611894 @default.
• W2119048543 cites W2018613188 @default.
• W2119048543 cites W2019153840 @default.
• W2119048543 cites W2027807325 @default.
• W2119048543 cites W2033651257 @default.
• W2119048543 cites W2034914622 @default.
• W2119048543 cites W2038587260 @default.
• W2119048543 cites W2039558285 @default.
• W2119048543 cites W2040326828 @default.
• W2119048543 cites W2040705298 @default.
• W2119048543 cites W2041885277 @default.
• W2119048543 cites W2041997393 @default.
• W2119048543 cites W2042380219 @default.
• W2119048543 cites W2043561742 @default.
• W2119048543 cites W2046227630 @default.
• W2119048543 cites W2046431125 @default.
• W2119048543 cites W2060258946 @default.
• W2119048543 cites W2063864272 @default.
• W2119048543 cites W2070567272 @default.
• W2119048543 cites W2071698372 @default.
• W2119048543 cites W2079782510 @default.
• W2119048543 cites W2081057026 @default.
• W2119048543 cites W2082627267 @default.
• W2119048543 cites W2085939977 @default.
• W2119048543 cites W2087756133 @default.
• W2119048543 cites W2088497697 @default.
• W2119048543 cites W2089239384 @default.
• W2119048543 cites W2090076848 @default.
• W2119048543 cites W2091602574 @default.
• W2119048543 cites W2093676326 @default.
• W2119048543 cites W2096644091 @default.
• W2119048543 cites W2098232539 @default.
• W2119048543 cites W2099341509 @default.
• W2119048543 cites W2101208644 @default.
• W2119048543 cites W2101516250 @default.
• W2119048543 cites W2108216860 @default.
• W2119048543 cites W2111436890 @default.
• W2119048543 cites W2118203054 @default.
• W2119048543 cites W2132277640 @default.
• W2119048543 cites W2132760947 @default.
• W2119048543 cites W2133388963 @default.
• W2119048543 cites W2137800485 @default.
• W2119048543 cites W2138101090 @default.
• W2119048543 cites W2141074377 @default.
• W2119048543 cites W2145114296 @default.
• W2119048543 cites W2147817273 @default.
• W2119048543 cites W2158140282 @default.
• W2119048543 cites W2161554960 @default.
• W2119048543 cites W2162082869 @default.
• W2119048543 cites W2163313531 @default.
• W2119048543 cites W2165952027 @default.
• W2119048543 cites W2166102005 @default.
• W2119048543 cites W2168644909 @default.
• W2119048543 cites W2171331577 @default.
• W2119048543 cites W2171500660 @default.
• W2119048543 cites W2180601736 @default.
• W2119048543 cites W2180824684 @default.
• W2119048543 cites W2318796451 @default.
• W2119048543 cites W2503268391 @default.
• W2119048543 cites W4255817930 @default.
• W2119048543 doi "https://doi.org/10.1002/2014jg002764" @default.
• W2119048543 hasPublicationYear "2015" @default.
• W2119048543 type Work @default.
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