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The Rise of Biogenic Silicon Cycling and Microbial Silicification Promoted Mesoproterozoic Chert Deposition

https://doi.org/10.2139/ssrn.4679510
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Germanium/silicon of the Ediacaran-Cambrian Laobao cherts: Implications for the bedded chert formation and paleoenvironment interpretations
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Silicon isotopes and trace elements in chert record early Archean basin evolution
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Silicon isotopes reveal a decline in oceanic dissolved silicon driven by biosilicification: A prerequisite for the Cambrian Explosion?
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Formation of the massive bedded chert and coupled Silicon and Iron cycles during the Ediacaran-Cambrian transition
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Ge/Si in Hamersley BIF as tracer of hydrothermal Si and Ge inputs to the Paleoproterozoic ocean
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Recent advances in the study of the Mesoproterozoic geochronology in the North China Craton
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A large and complete Jurassic geothermal field at Claudia, Deseado Massif, Santa Cruz, Argentina
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Silicon content of individual cells of Synechococcus from the North Atlantic Ocean
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The chemical form of silicon in marine Synechococcus
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Primary silica precipitate at the Precambrian/Cambrian boundary in the South Oman Salt Basin, Sultanate of Oman
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Mixed seawater and hydrothermal sources of nodular chert in Middle Permian limestone on the eastern Paleo-Tethys margin (South China)
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Significant contribution of picoplankton size fraction to biogenic silica standing stocks in the Western Pacific Ocean
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Sunspot cycles recorded in Mesoproterozoic carbonate biolaminites
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Sulfur isotope composition of carbonate-associated sulfate from the Mesoproterozoic Jixian Group, North China: Implications for the marine sulfur cycle
inferredcites →https://doi.org/10.1016/j.precamres.2016.12.005openalex-extracted
Greenalite precipitation linked to the deposition of banded iron formations downslope from a late Archean carbonate platform
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Tracing the evolution of dissolved organic carbon (DOC) pool in the Ediacaran ocean by Germanium/silica (Ge/Si) ratios of diagenetic chert nodules from the Doushantuo Formation, South China
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Silicate deposition during decomposition of cyanobacteria may promote export of picophytoplankton to the deep ocean
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Significant silicon accumulation by marine picocyanobacteria
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Parallel phylogeography of Prochlorococcus and Synechococcus
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Late Neoproterozoic seawater oxygenation by siliceous sponges
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Silicifying Biofilm Exopolymers on a Hot-Spring Microstromatolite: Templating Nanometer-Thick Laminae
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inferredcites →https://doi.org/10.1111/gbi.12434openalex-extracted
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inferredcites →https://doi.org/10.1111/gbi.12476openalex-extracted
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inferredcites →https://doi.org/10.1111/jpy.12545openalex-extracted
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inferredcites →https://doi.org/10.1111/sed.12419openalex-extracted
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inferredcites →https://doi.org/10.1130/2006.2405(07)openalex-extracted
The 3.466 Ga “Kitty's Gap Chert,” an early Archean microbial ecosystem
inferredcites →https://doi.org/10.1130/b25555.1openalex-extracted
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inferredcites →https://doi.org/10.1130/b31181.1openalex-extracted
Sedimentology and geochemistry of Archean silica granules
inferredcites →https://doi.org/10.1130/b31339.1openalex-extracted
An authigenic origin for Precambrian greenalite: Implications for iron formation and the chemistry of ancient seawater
inferredcites →https://doi.org/10.1130/g35187.1openalex-extracted
Primary silica granules—A new mode of Paleoarchean sedimentation
inferredcites →https://doi.org/10.1130/g47394.1openalex-extracted
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inferredcites →https://doi.org/10.1146/annurev-earth-040809-152356openalex-extracted
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inferredcites →https://doi.org/10.1146/annurev-marine-121211-172346openalex-extracted
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inferredcites →https://doi.org/10.1306/011704740561openalex-extracted
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inferredcites →https://doi.org/10.2110/jsr.2020.7openalex-extracted
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MICROFABRICS IN MESOPROTEROZOIC MICRODIGITATE STROMATOLITES: EVIDENCE OF BIOGENICITY AND ORGANOMINERALIZATION AT MICRON AND NANOMETER SCALES
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Iron Formation: The Sedimentary Product of a Complex Interplay among Mantle, Tectonic, Oceanic, and Biospheric Processes
inferredcites →https://doi.org/10.2307/3514743openalex-extracted
Secular change in chert distribution; a reflection of evolving biological participation in the silica cycle
inferredcites →https://doi.org/10.3389/fmars.2017.00397openalex-extracted
Biosilicification Drives a Decline of Dissolved Si in the Oceans through Geologic Time
inferredcites →https://doi.org/10.5194/bg-13-6003-2016openalex-extracted
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inferredcites →https://doi.org/10.5194/bg-18-1269-2021openalex-extracted
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