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TitleEvaporite deposition in the mid-Neoproterozoic as a driver for changes in seawater chemistry and the biogeochemical cycle of sulfur
 
AuthorPrince, J K G; Rainbird, R HORCID logo; Wing, B A
SourceGeology 2019 p. 1-5, https://doi.org/10.1130/G45464.1
Image
Year2019
Alt SeriesNatural Resources Canada, Contribution Series 20180383
PublisherGeological Society of America
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf (Adobe® Reader®)
ProvinceNorthwest Territories
NTS78B/04; 78B/05; 87G/01; 87G/02; 87G/07; 87G/08; 87G/09; 87G/10; 87G/15; 87G/16; 87H; 88A/01; 88A/02; 88A/07; 88A/08
AreaVictoria Island; Minto Inlet; Wynniatt Bay
Lat/Long WENS-117.1667 -111.1667 72.5000 71.0000
Subjectssedimentology; geochemistry; bedrock geology; lithology; sedimentary rocks; evaporites; gypsum; anhydrite; calcite; dolomites; limestones; shales; mudstones; grainstones; siltstones; claystones; arenites; sulphates; depositional history; depositional environment; paleoenvironment; sea water geochemistry; sulphur geochemistry; isotopic studies; atmospheric geochemistry; oxygen geochemistry; biogeochemistry; modelling; basins; tectonic setting; paleoclimates; Neoproterozoic; Tonian; Minto Inlet Formation; Shaler Supergroup; Rodinia; Precambrian; Proterozoic
Illustrationstime series; bar graphs; location maps; geoscientific sketch maps; lithologic sections; geochemical profiles; graphs
ProgramGEM: Geo-mapping for Energy and Minerals PGE/Base Metals - Victoria Island (NWT and Nunavut)
Released2019 02 26
AbstractWe utilized a novel approach to modeling the oceanic sulfur cycle by combining delta-34S and delta-33S curves from sulfate evaporite minerals in order to investigate redox conditions during the mid-Neoproterozoic. This technique allowed us to estimate the oxidized and reduced proportions of the total oceanic sulfur sink. Isotopic data from the mid-Neoproterozoic Minto Inlet Formation (Victoria Island, Northwest Territories, Canada; ca. 850 Ma) show a limited range (16.8 per mille ± 1.4 per mille) in delta-34S of seawater sulfate and a sulfur cycle that is strongly shifted toward the sulfate sink (pyrite burial fraction, fp, = 0.2), suggesting oxidizing conditions in the ocean and atmosphere at the time of deposition. These evaporites and others, which were deposited contemporaneously within a huge intracontinental basin, acted as a chemical pump, removing sulfate from the oceans and oxygen from the atmosphere to be buried as sulfate evaporites.
Summary(Plain Language Summary, not published)
We analyzed sulphur isotopes from sulfate evaporite minerals from the Minto Inlet Formation (Shaler Supergroup)in order to investigate redox conditions in the ocean approximately 850 million years ago. The isotopic data show a limited range in d34S of seawater sulfate and a sulfur cycle that is strongly shifted toward the sulfate sink, suggesting oxidizing conditions in the ocean and atmosphere at the time of deposition. These evaporites and others, which were deposited contemporaneously within a huge intracontinental basin, acted as a chemical pump, removing sulfate from the oceans and oxygen from the atmosphere to be buried as sulfate evaporites.
GEOSCAN ID313580

 
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