Search results for "Early diagenesis"

showing 2 items of 2 documents

Carbon, iron and sulphur cycling in the sediments of a Mediterranean lagoon (Ghar El Melh, Tunisia)

2019

Coastal lagoon sediments are important for the biogeochemical carbon cycle at the land-ocean transition, as they form hotspots for organic carbon burial, as well as potential sites for authigenic carbonate formation. Here, we employ an early diagenetic model to quantify the coupled redox cycling of carbon, iron and sulphur in the sediments of the shallow Ghar El Melh (GEM) lagoon (Tunisia). The model simulated depth profiles show a good correspondence with available pore water data (dissolved inorganic carbon, NH 4 + , total alkalinity, Ca 2+ , Fe 2+ and SO 4 2− ) and solid phase data (organic matter, pyrite, calcium carbonate and iron (oxyhydr)oxides). This indicates that the model is abl…

0106 biological sciencesBiogeochemical cycle010504 meteorology & atmospheric scienceschemistry.chemical_elementAquatic ScienceOceanography01 natural sciencesCarbon cyclechemistry.chemical_compoundMarine sedimentsAuthigenic carbonate formationDissolved organic carbonOrganic matter14. Life underwaterBiologyEarly diagenesis0105 earth and related environmental scienceschemistry.chemical_classificationTotal organic carbon010604 marine biology & hydrobiologyAuthigenicPyrite formationchemistry13. Climate actionEnvironmental chemistry[SDE]Environmental SciencesEnvironmental scienceCarbonateCarbonSciences exactes et naturelles
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A genetic link between synsedimentary tectonics-expelled fluids, microbial sulfate reduction and cone-in-cone structures

2018

14 pages; International audience; The late Jurassic (Tithonian) marlstones of the Boulonnais area (English Channel, France) contains diagenetic carbonate beds and nodules. Some nodules exhibit cone-in-cone structures on their lower face. We studied such nodules using various techniques of imaging and chemical (major and trace-elements) and isotopic analyses (Ccarb, Corg, O and S stable isotopes). We interpret the cone-in-cone to be the end product of carbonate-nodule formation during early diagenesis. The diagenetic carbonate precipitation was induced by microbial activity (bacteria and(?) archeae) fueled by upward-migrating fluids. Fluid expulsion was itself triggered by synsedimentary fau…

Late jurassicgenetic structures010504 meteorology & atmospheric sciencesStratigraphyCone-in-cone structuresGeochemistryBoulonnais areaFault (geology)010502 geochemistry & geophysicsOceanography01 natural scienceschemistry.chemical_compound[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryHydrocarbon source-rocksSulfateEarly diagenesis0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryStable isotope ratioGeologyCarbonate nodulesDiagenesisTectonicsGeophysicschemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyAnaerobic oxidation of methaneCarbonateEconomic Geologysense organsAnaerobic oxidation of methaneGeologyMarine and Petroleum Geology
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