Search results for "Trace element"

showing 10 items of 321 documents

Zinc isotopes in Late Pleistocene fossil teeth from a Southeast Asian cave setting preserve paleodietary information

2020

Significance Dietary habits, especially meat consumption, represent a key aspect in the behavior and evolution of fossil hominin species. Here, we explore zinc (Zn) isotope ratios in tooth enamel of fossil mammals. We show discrimination between different trophic levels and demonstrate that Zn isotopes could prove useful in paleodietary studies of fossil hominin, or other mammalian species, to assess their consumption of animal versus plant resources. We also demonstrate the high preservation potential of pristine diet-related Zn isotope ratios, even under tropical conditions with poor collagen preservation, such as the studied depositional context in Southeast Asia. However, assessing the …

[SHS.ANTHRO-BIO]Humanities and Social Sciences/Biological anthropologyDIAGENESIS010502 geochemistry & geophysics01 natural sciencesBiochemistry[SHS]Humanities and Social SciencesMAMMALIAN ASSEMBLAGESAsia SoutheasternTrophic leveltrophic ecologyMultidisciplinarygeography.geographical_feature_categoryEnamel paintStable isotope ratioEcologyFossilsFRACTIONATIONzincBONE-COLLAGENHominidaeBiological SciencesIsotopes of nitrogenCavesvisual_artDiet Paleolithicvisual_art.visual_art_mediumZinc IsotopesCollagen[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologydiagenesisGeology010506 paleontologyPleistoceneOXYGEN ISOTOPESSTRONTIUM ISOTOPESstable isotopesSoutheast asianTOOTHDIETCavestomatognathic systemAnimals0105 earth and related environmental sciencesgeographyArchéozoologieTrace elementNITROGENstomatognathic diseasesELEMENTdietTooth
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Geochemistry, Sr–Nd–Pb isotopes and geochronology of amphibole- and mica-bearing lamprophyres in northwestern Iran: Implications for mantle wedge het…

2015

Highlights • Northwestern Iranian lamprophyres have alkaline and calc-alkaline nature. • Studied lamprophyres are emplaced during Late Cretaceous to Late Miocene time. • Lamprophyres originated from different metasomatised lithospheric mantle. Abstract Lamprophyres of different age showing distinctive mineralogy, geochemistry and isotopic ratios are exposed in northwestern Iran. They can be divided into Late Cretaceous sannaite, Late Oligocene-Early Miocene camptonite (amphibole-bearing) and Late Miocene minette (mica-bearing) and spessartite (amphibole-bearing) lamprophyres. Sannaites have high-Ti amphibole along with high-Ti and Al clinopyroxene, and they are characterised by homogeneous …

alkaline and calc-alkaline lamprophyres; geochemistry Sr-Nd-Pb isotopes; geochronology; mantle heterogeneity; IranContinental collisionMantle wedgeGeochronologyPartial meltingGeochemistryTrace elementGeologySr-Nd-Pb isotopesIranLate Mioceneengineering.materialMantle (geology)GeochemistryGeochemistry and PetrologyengineeringAlkaline and calc-alkaline lamprophyresMantle heterogeneityGeologyAmphiboleHornblendeLithos
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Major ions and trace elements composition of rainwater around the two industrial areas of Milazzo and Priolo Gargallo (Sicily - Italy)

2023

This database shows the concentration of major ions and trace elements in rainwater from two polluted industrial areas of Sicily, Milazzo and Priolo Gargallo, collected from June 2018 to July 2019, through a network of 11 bulk collectors to sample bulk atmospheric deposition, for a total of 131 samples collected. Different sources, both natural and anthropogenic, for both major ions and trace elements have been recognised. This study also highlighted some critical issues with common methods of sampling and analysing atmospheric deposition. The analysis and comparison of two different aliquots, filtered and unfiltered rainwater, has shown that the filtration method removes from the sample a …

atmospheric deposition acidity neutralization major ions marine source anthropogenic source bulk atmospheric deposition rainwater industrial pollution trace elementsSettore GEO/08 - Geochimica E Vulcanologia
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Mount Etna volcanic emissions signature on the chemical composition of bulk atmospheric deposition in Sicily, Italy.

2022

Mt. Etna, on the eastern coast of Sicily (Italy), is one of the most active and most intensely monitored volcanoes on the Earth, widely recognized as a big source of volcanic gases, such as CO2, SO2, halogens, and many trace elements, including technological critical elements (TCEs), to the atmosphere on a regional and global scale. Mt. Etna emissions account for a significant percentage of the worldwide average volcanic budget and especially during eruptive periods, its products can be dispersed over great distances and they influence the chemical composition of the atmosphere of other continents too. The current knowledge about the geochemical cycle of TCEs is still scarce, nevertheless, …

atmospheric deposition major ions trace elements volcanic emissions Mt. EtnaSettore GEO/08 - Geochimica E Vulcanologia
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Isotope Fractionation of Selenium During Fungal Biomethylation by Alternaria alternata

2011

The natural abundance of stable Se isotopes may reflect sources and formation conditions of methylated Se. We aimed at (1) quantifying the degree of methylation of selenate [Se(VI)] and (hydro)selenite [Se(IV)] by the fungus Alternaria alternata at pH 4 and 7 and (2) determining the effects of these different Se sources and pH values on 82Se/76Se ratios (δ82/76Se) in methylselenides. Alternaria alternata was incubated with Se(VI) and Se(IV) in closed microcosms for 11-15 days and additionally with Se(IV) for 3-5 days at 30 °C. We determined Se concentrations and δ82/76Se values in source Se(VI) and Se(IV), media, fungi, and trapped methylselenides. In Se(VI) incubations, methylselenide vola…

biologyIsotopeAlternariachemistry.chemical_elementGeneral ChemistryMethylationFungi imperfectiFractionationChemical Fractionationbiology.organism_classificationMethylationAlternaria alternataSelenateTrace ElementsSeleniumchemistry.chemical_compoundIsotope fractionationIsotopeschemistryEnvironmental chemistryEnvironmental ChemistryBiotransformationSeleniumEnvironmental Science & Technology
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Effect of organic matrices on the determination of the trace element chemistry (Mg, Sr, Mg/Ca, Sr/Ca) of aragonitic bivalve shells (<i>Arctica …

2010

The element chemistry of biogenic carbonates can provide important data on past environments. However, the Sr/Ca and Mg/Ca ratios as well as the Mg and Sr concentrations of biological carbonates, especially aragonitic bivalves often depart from apparent thermodynamic equilibrium. When measured in situ by means of LA-ICP-MS, the Mg concentration is often substantially enriched (two- to threefold) near the organic-rich, annual growth lines. To test the hypothesis that some organic components exert a major influence on the skeletal metal content, the element chemistry of different shell components (insoluble organic matrix, IOM; dissolved CaCO3 and soluble organics, SOM) of Arctica islandica w…

biologyMagnesiumTrace elementchemistry.chemical_elementCalciumbiology.organism_classificationMetalGeophysicschemistryGeochemistry and PetrologyInductively coupled plasma atomic emission spectroscopyEnvironmental chemistryvisual_artvisual_art.visual_art_mediumBivalve shellArctica islandicaChemical compositionGEOCHEMICAL JOURNAL
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Unraveling the origin of the Late Triassic multitaxic bone accumulation at Krasiejów (S Poland) by diagenetic analysis

2012

Abstract A study of aquatic and terrestrial vertebrate remains from a bonebed in the Late Triassic continental succession near Krasiejow (S Poland) shows it was deposited by a single catastrophic event, perhaps a flood. Hardparts of Metoposaurus, Paleorhinus, and Stagonolepis show sedimentary infill and geochemical evidence for early diagenesis at different times and in different microenvironments. The infills in the aquatic animal bones (sediment, pyrite and calcite) show deposition in a freshwater environment, while those in the terrestrial Stagonolepis remains (mainly barite) point to an arid terrestial environment. The trace element content of the remains, together with the absence of a…

biologyTrace elementPaleontologySedimentMetoposaurusOceanographyPaleorhinusbiology.organism_classificationDeposition (geology)DiagenesisPaleontologySedimentary rockStagonolepisEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Trophic Transfer of Trace Elements in an Isotopically Constructed Food Chain From a Semi-enclosed Marine Coastal Area (Stagnone di Marsala, Sicily, M…

2012

Trace element accumulation is particularly important in coastal and transitional environments, which act as contaminant buffers between the continental and marine systems. We compared trace element transfer to the biota in two locations with different open-sea exposures in a semi-enclosed marine coastal area (Stagnone di Marsala, Sicily, Italy) using isotopically reconstructed food chains. Samples of sediment, macroalgae, seagrasses, invertebrates, fish, and bird feathers were sampled in July 2006 and analysed for stable carbon and nitrogen isotopes (δ(13)C, δ(15)N) and trace elements (arsenic [As], cadmium [Cd], total mercury [THg], and lead [Pb]). Trophic magnification factors were calcul…

biomagnification transitional systems Stagnone di MarsalaSettore BIO/07 - EcologiaGeologic SedimentsFood ChainHealth Toxicology and MutagenesisBiomagnificationToxicologyPoaceaeFood chainAnimalsSicilyTrophic levelBiodilutionCarbon IsotopesNitrogen IsotopesTrace elementFishesSedimentBiotaGeneral MedicineFeathersSeaweedPollutionInvertebratesIsotopes of nitrogenTrace ElementsEnvironmental chemistryEnvironmental scienceWater Pollutants ChemicalEnvironmental Monitoring
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Application of the moss bag biomonitoring technique in an active volcanic environment (Mt. Etna, Italy).

2011

This paper presents the preliminary results of a biomonitoring study based on the use of moss bags exposed at 24 sites on Etna volcano. Sphagnum mosses were used to study bioaccumulation originating from atmospheric deposition, by measuring the tissue contents of major and a large suite of trace elements. Elements, such as Tl, Bi, As, Se, Cu and Cd, display high concentrations in the exposed samples close to the active vents. This study confirms the effectiveness of the moss bags technique also in active volcanic areas.

biomonitoring moss bags Mt. Etna volcanic emissions trace elementsSettore GEO/08 - Geochimica E Vulcanologia
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CHEMICAL AND MINERALOGICAL CHARACTERIZATION OF ETNEAN VOLCANIC EMISSIONS USING ACTIVE BIOMONITORING TEC HNIQUE (MOSS-BAGS)

2011

biomonitoring moss-bags trace elementsSettore GEO/08 - Geochimica E Vulcanologia
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