Search results for "DIAGENESI"

showing 10 items of 130 documents

Bone diagenesis of archaeological human remains from Apulia (Italy) investigated by ATR-FTIR and XRF spectroscopy

2023

The analysis of the organic and mineral content of biological samples allows to define post-mortem alterations and the preservation status of ancient human remains. Here, we report a physical-chemical characterization of bone specimens from some skeletal remains found in Apulia (Italy) dating back to the prehistoric, classic-hellenistic, and medieval periods. Specific infrared band ratios from Attenuated Total Reflectance-Fourier Transform InfraRed and X-ray fluorescence spectroscopies were considered to evaluate the extent of the diagenetic process and the elemental composition of bone.Physical-chemical post-mortem transformations were related to the soil composition and specificity of tis…

Archaeological boneMechanics of MaterialsMechanical EngineeringXRFGeneral Materials ScienceSettore CHIM/06 - Chimica OrganicaCondensed Matter PhysicsHuman remainsDiagenesisATR-FTIRSettore CHIM/02 - Chimica Fisica
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Sulfur isotope's signal of nanopyrites enclosed in 2.7 Ga stromatolitic organic remains reveal microbial sulfate reduction.

2018

18 pages; International audience; Microbial sulfate reduction (MSR) is thought to have operated very early on Earth and is often invoked to explain the occurrence of sedimentary sulfides in the rock record. Sedimentary sulfides can also form from sulfides produced abiotically during late diagenesis or metamorphism. As both biotic and abiotic processes contribute to the bulk of sedimentary sulfides, tracing back the original microbial signature from the earliest Earth record is challenging. We present in situ sulfur isotope data from nanopyrites occurring in carbonaceous remains lining the domical shape of stromatolite knobs of the 2.7-Gyr-old Tumbiana Formation (Western Australia). The anal…

ArcheanBiogeochemical cycleGeologic Sediments010504 meteorology & atmospheric sciencesIronGeochemistrychemistry.chemical_elementSulfides010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundδ34S[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDV.MP ] Life Sciences [q-bio]/Microbiology and ParasitologySulfur IsotopesMicrobial matAnaerobiosisstromatoliteSulfateEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental SciencebiologyChemistrySulfatessulfur biogeochemical cycleWestern Australiabiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySulfurDiagenesisTumbiana FormationStromatolite13. Climate actionAnaerobic oxidation of methaneGeneral Earth and Planetary SciencesOxidation-Reductionmicrobial sulfate reduction
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A quantitative high-resolution summer temperature reconstruction based on sedimentary pigments from Laguna Aculeo, central Chile, back to AD 850

2009

We present a pigment-based quantitative high-resolution (five years) austral summer DJF (December to February) temperature reconstruction for Central Chile back to AD 850. We used non-destructive in situ multichannel reflection spectrometry data from a short sediment core of Laguna Aculeo (33°50′S/70°54′W, 355 m a.s.l., central Chile). Calibration-in-time (period AD 1901—2000, cross-validated with split periods) revealed robust correlations between local DJF temperatures and total sedimentary chlorin (relative absorption band depth (RABD) centred in 660—670 nm RABD660;670: r=0.79, P<0.01; five-years triangular filtered) and the degree of pigment diagenesis ( R660nm/670 nm: r=0.82, P<…

ArcheologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologyDischargePaleontologyClimate changeGlacier910 Geography & travelDiagenesisOceanography550 Earth sciences & geologyPhanerozoicPhysical geographyQuaternaryCenozoicHoloceneGeologyEarth-Surface ProcessesThe Holocene
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Biological mineral content in Iberian skeletal cremains for control of diagenetic factors employing multivariate statistics

2013

Abstract The aim of this study was to define a strategy for a correct selection of bone samples by employing inductively coupled plasma optical emission spectroscopy (ICP-OES) for reconstructing the biological mineral content in bones through the determination of major elements, trace elements and Rare Earth Elements (REE, lanthanides) in skeletal cremains of ancient Iberians (III–II B.C), discovered in the Necropolis of Corral de Saus (Moixent, Valencia) between 1972 and 1979. The biological mineral content was determined taking into account diagenetic factors. A control method for a better reading of results was applied. To explore large geochemical datasets and to reduce the number of va…

ArcheologyMultivariate statisticsSoil testInductively coupled plasma atomic emission spectroscopyPrincipal component analysisPartial least squares regressionDendrogramMineralogyLinear discriminant analysisGeologyDiagenesisJournal of Archaeological Science
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Inverted responses of the carbon cycle to orbital forcing in Mesozoic peri‐platform marginal basins: implications for astrochronology

2020

International audience; Astrochronology depends on the faithful record of insolation forcing in climatic proxies, including the carbon isotope composition measured on bulk carbonates (δ13Ccarb). In marginal basins close to carbonate platforms, the source of carbonate is varied, which can impact the record of the astronomical cycles in the δ13Ccarb signal. We compare here the δ13Ccarb values together with detrital and weathering proxies before and during a crisis in the platform carbonate production (Weissert event, Valanginian, ~135 Ma) to document how a change in the carbonate source can affect the record of the orbital forcing by the carbon isotope system. The level of burial diagenesis w…

Astrochronology010506 paleontologyAtmospheric ScienceOrbital forcingGeochemistryPaleontologyWeatheringStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesDiagenesisCarbon cyclechemistry.chemical_compoundchemistry13. Climate action[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarlCarbonateGeology0105 earth and related environmental sciences
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Biogeochemical Cycling of Nitrogen on the Early Earth

2013

Variations in the nitrogen isotope composition of ancient organic matter and associated sediments provide clues for the early evolution of Earth's atmosphere–ocean–biosphere system. In particular, large isotopic variations have been linked to the protracted oxygenation of Earth's atmosphere during the Precambrian. Important problems being investigated include the nature of the variations observed at specific times in Earth's history and the degree of preservation of ancient nitrogen biogeochemical signatures during diagenesis and metamorphism. Interpreting these records in Archean sedimentary environments and their possible implications for the evolution of Earth's early atmosphere, ocean, …

AtmospherePrecambrianBiogeochemical cycleGeochemistry and PetrologyEarth scienceArcheanEarth and Planetary Sciences (miscellaneous)BiogeochemistryEarly EarthNitrogen cycleGeologyDiagenesisElements
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Amygdaloidal basalts: Isotopic and petrographic evidence for non-diagenetic crustal source of carbonate inclusions

1980

Even though carbonate amygdules in volcanics are generally assumed to be diagenetic in origin, the authors are of the opinion that almost all carbonate inclusions in the investigated amygdaloidal volcanic rocks from Sicily (Italy), Pindos (Greece) and Bohemia (Czechoslovakia), have a different origin. On the basis of a mineralogical, petrological and geochemical study these “amygdules” are interpreted as being remains ofmagmatic incorporation of carbonate. Therefore, the identification of carbonate globules in volcanics purely on field observations, is inadequate to distinguish true amygdules from carbonate assimilation remnants. A nomenclature of the various types of inclusions is proposed…

Basaltgeographygeography.geographical_feature_categoryAmygduleAlkali basaltGeochemistryDiagenesisPetrographyVolcanic rockchemistry.chemical_compoundGeophysicschemistryGeochemistry and PetrologyMagmaCarbonatePetrologyGeologyTMPM Tschermaks Mineralogische und Petrographische Mitteilungen
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Fracture stratigraphy and oil first migration in Triassic shales, Favignana Island, western Sicily, Italy

2021

This study aims at evaluating the control exerted by fracture stratigraphy and diagenetic processes on oil first migration through an outcropping, mixed carbonate-siliciclastic succession. The present work included results of sedimentological, paleontological, mineralogical, petrographic, structural, and microstructural analyses carried out on organic-rich shales exposed at the Favignana Island of Sicily, Italy. The analyses focus on Upper Triassic yellowish siltstones and greyish laminated dolomitic limestones, which form a 10's of m-thick succession exposed along the westernmost portion of the Sicilian fold-and-thrust belt. The studied succession deposited in a coastal lagoon associated t…

BeddingCarbonate platformOutcropStratigraphyFracture (mineralogy)GeochemistryGeologyBrittle deformationOceanographyDiagenesisPetrographyGeophysicsStratigraphySource rockUpper TriassicAnoxic coastal lagoonEconomic GeologyDiagenetic evolutionSicilyMixed carbonate-siliciclasticGeologyMarine and Petroleum Geology
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Mineralogical variability of Callovo-Oxfordian clays from the Paris Basin and the Subalpine Basin.

2006

High-resolution clay mineralogical data at the Middle/Upper Jurassic boundary from the French Subalpine Basin, the Jura Mountains and the Paris Basin (ANDRA boreholes) from Callovo-Oxfordian clayey deposits allow spatial and temporal terrigenous flux evolution to be considered over a period of 6 to 7 Myr. Recorded diachronisms of major mineralogical changes and complex clays distribution at the Paris Basin scale result to combined palaeogeographic/eustatic variations and climate input. In the French Subalpine Basin, mineralogical homogeneity confirms the burial diagenesis influence, but other terrigenous supplies must be involved in contrast to the Paris Basin domains. Volcanogenic clays (b…

Bentonites010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesCallovian[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/VolcanologyBiostratigraphyStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesOxfordianPaleontologyPalaeovolcanismParis Basin[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgPhanerozoic[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesGlobal and Planetary ChangeTerrigenous sedimentDiagenesisClay minerals[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate actionClastic rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesSedimentary rockFrancePalaeogeographyGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Iron isotope signature of magnetofossils and oceanic biogeochemical changes through the Middle Eocene Climatic Optimum.

2021

21 pages; International audience; Magnetotactic bacteria (MTB) intracellularly precipitate magnetite (Fe3O4) crystals that can be preserved in the geological record. When MTB die, the so-called magnetofossils constitute valuable proxies for paleoenvironmental reconstructions and are suspected to represent some of the oldest traces of biomineralization on Earth. Yet, the biogenicity of putative magnetofossils found in ancient terrestrial and extra-terrestrial samples is still largely debated and their significance for past climate still holds uncertainties. Here we studied a sedimentary sequence from the Indian Ocean (ODP Hole 711A) recording the Middle Eocene Climatic Optimum (MECO) through…

Biogeochemical cycle010504 meteorology & atmospheric sciencesGeochemistryTrace elementIron isotopesFe sequential extraction010502 geochemistry & geophysicsMass-independent fractionationHyperthermal01 natural sciencesDiagenesischemistry.chemical_compoundMagnetotactic bacteriaIsotope fractionationMagnetofossilschemistry13. Climate actionGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryBiosignatureMECOMagnetofossilGeology0105 earth and related environmental sciencesMagnetite
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