Search results for "Authigenic"

showing 10 items of 35 documents

The behaviour of REEs in Thailand's Mae Klong estuary: Suggestions from the Y/Ho ratios and lanthanide tetrad effects

2007

Abstract The concentrations of Rare Earth Elements and yttrium (REY) were measured in dissolved phase, in suspended particulate matter (SPM) and in sediments in seven sampling stations in the Mae Klong estuarine system (Inner Thailand Gulf) in order to study their behaviour and distribution pattern. The analysed samples generally show high Rare Earth Element (REE) content in the dissolved phase, with high Medium Rare Earth Elements (MREEs) and Y enrichments in the shale-normalized pattern (versus PAAS). These chemical features are interpreted in terms of direct influences of weathering processes of REE-rich minerals (e.g., phosphates), which abundantly out-crop in the Mae Klong watershed. T…

Rare-earth elementSettore AGR/13 - Chimica Agrariachemistry.chemical_elementMineralogyWeatheringFractionationYttriumAuthigenicAquatic ScienceParticulatesOceanographyAdsorptionchemistryAluminosilicateEnvironmental chemistryGeologyrare earth elementstetrad effectY/Ho ratioMae Klong RiverGulf of ThailandEstuarine, Coastal and Shelf Science
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Onset of the Messinian Salinity Crisis: Sedimentological, petrographic and geochemical characterization of the pre-salt sediments from a new core (Ca…

2022

The present study aims to reconstruct the environmental changes leading to the Messinian Salinity Crisis during the transition from the Tortonian-Messinian marine conditions to the Messinian evaporitic environments. The core 3AGN2S04, recently drilled in the Caltanissetta Basin (Sicily), was analyzed to reveal the petrographic, mineralogical and geochemical characteristics of the late Tortonian – early Messinian pre-salt sediments. In particular, the facies characterization of the carbonates and organic-rich shales of the Calcare di Base (CdB) member allowed to understand its significance in the paleoenvironmental evolution towards salt deposition and to the reconstruct the brecciation proc…

GeophysicsStratigraphyMessinian Salinity Crisis Calcare di base Evaporites Authigenic carbonates Oxygen and carbon isotopes Organic-rich sedimentsEconomic GeologyGeologyOceanography
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Zirconium–hafnium and rare earth element signatures discriminating the effect of atmospheric fallout from hydrothermal input in volcanic lake water

2016

The geochemical behaviour of Rare Earth Elements, Zr and Hf was investigated in the thermal waters of Nevado del Ruiz volcano system. A wide range of pH, between 1.0 and 8.8, characterizes these fluids. The acidicwaters are sulphate dominatedwith different Cl/SO4 ratios. The important role of the pH and the ionic complexes for the distribution of REE, Zr a nd Hf in the aqueous phase was evidenced. The pH rules the precipitation of authigenic Fe and Al oxyhydroxides producing changes in REE, Zr, Hf amounts and strong anomalies of Cerium. The precipitation of alunite and jarosite removes LREE from the solution, changing the REE distribution in acidic waters. Y-Ho and Zr-Hf (twin pairs) have a…

Rare Earth Elements010504 meteorology & atmospheric sciencesGeochemistrychemistry.chemical_element010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationLakeRare earth elements Zirconium Hafnium CO2-rich waters Lake Aeolian inputGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryPrecipitation0105 earth and related environmental sciencesgeographyZirconiumgeography.geographical_feature_categoryCO 2 -rich watersRare-earth elementGeologyAuthigenicHafniumAeolian inputVolcanochemistryZirconiumOil shaleGeologyHafnium
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Methane-derived carbonate conduits from the late Aptian of Salinac (Marne Bleues, Vocontian Basin, France): Petrology and biosignatures

2015

Abstract Peculiar carbonate bodies occur in distinct marl layers of the Marnes Bleues Formation (Aptian–Albian, Vocontian Basin, Southern France). The carbonate conduits exhibit pipe- or sausage-like forms and a central channel. Their sizes range between 30 and 60 cm in length and 5–10 cm in diameter. The conduit carbonates consist of automicrite authigenically formed within the sediment. Millimeter-sized aggregates of framboidal pyrite are abundant within the conduit automicrites, probably representing former colonies of sulfate reducing bacteria. The central channel reflects former pathways of reduced fluids in the carbonate conduit. Ni-enrichments at the margins of the central cavity are…

StratigraphyMineralogyGeologyAuthigenicengineering.materialOceanographychemistry.chemical_compoundGeophysicschemistry13. Climate actionIsotopes of carbonAnaerobic oxidation of methaneMarlengineeringCarbonateEconomic GeologyPyriteSulfateSulfate-reducing bacteriaGeologyMarine and Petroleum Geology
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Geochemistry and mineralogy of sediments and authigenic carbonates from the Malta Plateau, Strait of Sicily (Central Mediterranean): Relationships wi…

2010

Abstract A mud volcano field was recently discovered within the Malta Plateau in the Strait of Sicily (Central Mediterranean Sea). Box-core sediments and associated authigenic carbonates have been collected in water depths of 140–170 m from two distinctive sectors of the area, and analyzed for major, trace and rare earth elements, stable isotopes, and mineralogy. Relative homogeneity in the mineralogy and geochemistry of bulk sediments, and 210Pb activity distributions, argue against an active mud ejection activity. In the Malta Plateau western sector, the sediments show high concentrations of Fe, As, Sb, and Mo, exceeding the background values estimated for the Strait of Sicily. Active flu…

Methane oxidationGeochemistryMineralogyengineering.materialchemistry.chemical_compoundMediterranean seaSeep carbonateGeochemistry and PetrologygeographyPlateaugeography.geographical_feature_categoryδ13CAragoniteSediment geochemistrySettore GEO/07 - Petrologia E PetrografiaGeologyAuthigenicStable isotopeSettore GEO/08 - Geochimica E VulcanologiaStrait of SicilychemistryAnaerobic oxidation of methaneengineeringCarbonateGeologyMud volcano
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A diagenetic control on the Early Triassic Smithian-Spathian carbon isotopic excursions recorded in the marine settings of the Thaynes Group (Utah, U…

2016

17 pages; International audience; n the aftermath of the end-Permian mass extinction, Early Triassic sediments record some of the largest Phanerozoic carbon isotopic excursions. Among them, a global Smithian-negative carbonate carbon isotope excursion has been identified, followed by an abrupt increase across the Smithian–Spathian boundary (SSB; ~250.8 Myr ago). This chemostratigraphic evolution is associated with palaeontological evidence that indicate a major collapse of terrestrial and marine ecosystems during the Late Smithian. It is commonly assumed that Smithian and Spathian isotopic variations are intimately linked to major perturbations in the exogenic carbon reservoir. We present p…

Geologic Sediments010504 meteorology & atmospheric sciencesEarly TriassicCarbonates[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesCarbon CycleCarbon cycle[ SDE ] Environmental Scienceschemistry.chemical_compoundPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryUtahSulfur IsotopesPhanerozoicSeawater14. Life underwaterEcosystemEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental ScienceExtinction eventCarbon IsotopesPaleontologyAuthigenic[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryDiagenesischemistry13. Climate actionIsotopes of carbon[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDE]Environmental SciencesGeneral Earth and Planetary SciencesCarbonateGeologyGeobiology
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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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Taphonomy of insects in carbonates and amber

2004

Abstract The major taphonomic processes that control insect preservation in carbonate rocks (limestones, travertines and nodules) are biological: insect size and wingspan, degree of decomposition, presence of microbial mats, predation and scavenging; environmental: water surface tension, water temperature, density and salinity, current activity; and diagenetic: authigenic mineralisation, flattening, deformation, carbonisation. The major taphonomic processes that control the preservation of insects in fossil resins (amber and copal) are different, but can be considered under the same headings – biological: presence of resin producers, size and behaviour of insects; environmental: latitude, c…

Extinction eventTaphonomyExtinctionEcologyfungiPaleontologyAuthigenicOceanographyDiagenesisCarbonate rockSedimentary rockMicrobial matEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Integrative analysis of the mineralogical and chemical composition of modern microbialites from ten Mexican lakes: What do we learn about their forma…

2021

International audience; Interpreting the environmental conditions under which ancient microbialites formed relies upon comparisons with modern analogues. This is why we need a detailed reference framework relating the chemical and mineralogical compositions of modern microbialites to the physical and chemical parameters prevailing in the environments where they form. Here, we measured the chemical, including major and trace elements, and mineralogical composition of microbialites from ten Mexican lakes as well as the chemical composition of the surrounding waters. Saturation states of lakes with different mineral phases were systematically determined and correlations between solution and so…

(Mg-)calcite010504 meteorology & atmospheric sciencesREE+YDolomiteGeochemistryalkalinityengineering.material010502 geochemistry & geophysics01 natural sciencesaragonitechemistry.chemical_compoundmonohydrocalciteGeochemistry and Petrologyhydromagnesite0105 earth and related environmental sciencesCalciteAragoniteTrace elementmicrobialitesAuthigenic6. Clean waterDiagenesisMonohydrocalcitecrater lakechemistry13. Climate actionkerolite[SDE]Environmental SciencesengineeringCarbonate
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Submarine canyon morphologies in the Gulf of Palermo (Southern Tyrrhenian Sea) and possible implications for geo-hazard

2011

12 pages, 12 figures, 1 table.

CanyonMass failure processegeographyMass failure processesgeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaContinental shelfSouthern MediterraneanAnticlineSubmarine canyonAuthigenicGeo-hazardStructural basinOceanographySwath mappingSubmarine canyonPaleontologyGeophysicsEcho soundingGeochemistry and PetrologySubmarine canyonsSubmarine pipelineGeologySeismologyMarine Geophysical Research
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