Search results for "Geochemistry"

showing 10 items of 2967 documents

Early Paleocene Paleoceanography and Export Productivity in the Chicxulub Crater

2021

The Chicxulub impact caused a crash in productivity in the world''s oceans which contributed to the extinction of ~75% of marine species. In the immediate aftermath of the extinction, export productivity was locally highly variable, with some sites, including the Chicxulub crater, recording elevated export production. The long-term transition back to more stable export productivity regimes has been poorly documented. Here, we present elemental abundances, foraminifer and calcareous nannoplankton assemblage counts, total organic carbon, and bulk carbonate carbon isotope data from the Chicxulub crater to reconstruct changes in export productivity during the first 3 Myr of the Paleocene. We sh…

bepress|Physical Sciences and Mathematics|Earth Sciences|Paleontologybepress|Physical Sciences and Mathematicsbepress|Physical Sciences and Mathematics|Earth Sciences|Sedimentology010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciencesbepress|Physical Sciences and Mathematics|Earth SciencesEarthArXiv|Physical Sciences and Mathematics|Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnImpact craterPaleoceanographyPhytoplanktonPhotic zone14. Life underwaterSDG 14 - Life Below WaterEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Sedimentology0105 earth and related environmental sciencesbiologyTerrigenous sedimentPaleontologyEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Geochemistry15. Life on landEarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Paleontologybiology.organism_classificationhumanitiesEarthArXiv|Physical Sciences and MathematicsOceanographyProductivity (ecology)13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyEnvironmental sciencebepress|Physical Sciences and Mathematics|Earth Sciences|Geochemistry
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The coralline red alga Lithophyllum kotschyanum f. affine as proxy of climate variability in the Yemen coast, Gulf of Aden (NW Indian Ocean)

2014

Abstract Recent investigations have shown the potential of red coralline algae as paleoclimatic archive. A previously unexplored subfamily of coralline algae, the Lithophylloideae, was investigated from the Gulf of Aden (Balhaf, Yemen). Seasonal changes in Mg/Ca, Li/Ca and Ba/Ca composition of Lithophyllum kotschyanum f. affine were investigated by Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS). For the first time in coralline algae, the Li/Ca composition was analyzed and showed a highly significant and positive correlation with Mg/Ca and SST. Monthly algal Mg/Ca and Li/Ca variations indicate a positive correlation with sea surface temperature (SST), and sea surface…

biologyChemistrygeochemical proxies crustose coralline algae climate record Indian OceanCoralline algaeGEO/01 - PALEONTOLOGIA E PALEOECOLOGIAbiology.organism_classificationLithophyllum kotschyanumThallusIndian oceanSea surface temperatureOceanographyGeochemistry and PetrologyUpwellingLithophyllumSea surface salinityGeochimica et Cosmochimica Acta
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Sclerochronology and geochemical variation in limpet shells (Patella vulgata): A new archive to reconstruct coastal sea surface temperature

2007

[1] Climate archives contained in shells of the European limpet, Patella vulgata, accumulated in archaeological deposits can potentially provide much needed information about Holocene environmental change in midlatitude coastal areas. Before reconstructing climate information preserved in these zooarchaeological records, we studied the controls on oxygen and carbon isotope ratios (δ18O and δ13C, respectively) in modern specimens. We tested the hypothesis that P. vulgata precipitates its shell in isotopic equilibrium with the ambient water by comparing δ18OSHELL with predicted values. Predicted δ18OSHELL was constructed using observed sea surface temperature (SST) records and the equilibrium…

biologyEnvironmental changeδ18OLimpetbiology.organism_classificationEquilibrium fractionationSea surface temperatureGeophysicsOceanographyGeochemistry and PetrologyIsotopes of carbonSclerochronologyPatella vulgataGeologyGeochemistry, Geophysics, Geosystems
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Accumulation of Pb and Zn in Bidens triplinervia and Senecio sp. spontaneous species from mine spoils in Peru and their potential use in phytoremedia…

2012

Abstract Heavy metal toxicity has become a global concern due to the ever-increasing contamination of soil, water and crops. Until recent decades little has been known about the remediation of mining sites using spontaneous plants in Latin America. Soil and plant samples were taken in Peru, at a polymetallic mine (mainly silver, lead and copper) in Cajamarca Province, Hualgayoc district. Top soils (0–20 cm) were analyzed for physical and chemical properties by standard methods. Total Pb and Zn concentrations in top soils were determined by ICP-OES. Similar metals in plants were analyzed separately (aerial and root system). Ti content was used as an indicator for contamination of plant sampl…

biologyEnvironmental remediationBidens triplinerviaMetal toxicitySeneciobiology.organism_classificationPhytoremediationGeochemistry and PetrologyLoamEnvironmental chemistryBotanySoil waterEnvironmental scienceEconomic GeologyHyperaccumulatorJournal of Geochemical Exploration
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Pseudo-boudins in Pegmatite, Arunta, Australia

2008

biologyGeochemistryGeologybiology.organism_classificationPegmatiteAruntaGeologyJournal of Structural Geology
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The geochemistry of Tl and its isotopes during magmatic and hydrothermal processes: The peralkaline Ilimaussaq complex, southwest Greenland

2014

Abstract We use thallium (Tl) concentrations, K/Rb, K/Tl and Rb/Tl ratios and Tl isotopes in minerals from the alkaline to peralkaline Ilimaussaq complex (South Greenland) to trace magmatic differentiation, crustal assimilation, magmatic degassing, ore precipitation and hydrothermal metasomatism. Closed-system magmatic differentiation is marked by a coherent decrease of K/Tl- and K/Rb-ratios, whereas crustal assimilation results in a strong Tl-enrichment, causing low K/Tl-ratios compared to K/Rb-ratios. Thallium isotopes show only slight changes during orthomagmatic differentiation and the assimilation of crustal material cannot be traced, since the isotopic composition of the average crust…

biologyGeochemistryMineralogyGeologyengineering.materialbiology.organism_classificationPeralkaline rockHydrothermal circulationMagmatic waterAstrophylliteGeochemistry and PetrologySilicate mineralsengineeringIgneous differentiationMetasomatismLileGeologyChemical Geology
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Radial cracks around α-quartz inclusions in almandine: Constraints on the metamorphic history of the Oman mountains

1993

Radiating tensional cracks around α-quartz inclusions in almandine have been observed in metapelite samples from the southeastern Saih Hatat tectonic window, northeastern Oman Mountains. These almandines show an inclusion-rich (glaucophane + epidote) and strongly deformed core with inclusions of different mineral phases. The rim of the same almandines is inclusion-poor and shows only quartz, apatite, zircon, rutile and BaAl phosphates as inclusions. Quartz and apatite inclusions in the rim are single crystals often surrounded by radial cracks. These radial cracks developed during uplift by the dilation of α-quartz (4–5 vol%) without a phase transformation. Subsequently, these cracks were fi…

biologyGlaucophaneMetamorphic rockMineralogyEpidoteengineering.materialbiology.organism_classificationPhengiteAlmandineAlbiteGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)engineeringQuartzGeologyZirconEarth and Planetary Science Letters
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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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Record of 1.82 Ga Andean-type continental arc magmatism in NE Rajasthan, India: Insights from zircon and Sm–Nd ages, combined with Nd–Sr isotope geoc…

2009

Abstract We document a Palaeoproterozoic Andean-type continental arc granitoid emplacement event in the northwestern segment of the Aravalli mountain range, NW India. Our study is focused on the Jasrapur pluton which is dominated by monzogranites with a subordinate amount of granodiorite and quartz monzodiorite. These rocks carry typical continental arc geochemical signatures, such as high-K calc-alkaline, mildly peraluminous, I-type and magnesian features, as well as high Rb and low Nb, Y and Rb/Zr ratios, decoupling between LILE and HFSE, and negative Nb–Ta and Ti anomalies. Conventional geothermobarometric estimates suggest high temperature (~ 800 °C) and pressure (≥ 600 MPa) conditions …

biologyPlutonIsotope geochemistryContinental crustMagmatismPartial meltingGeochemistryGeologybiology.organism_classificationGeologyLileZirconContinental arcGondwana Research
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Tellurite-dependent blackening of bacteria emerges from the dark ages

2019

Environmental contextAlthough tellurium is a relatively rare element in the earth’s crust, its concentration in some niches can be naturally high owing to unique geology. Tellurium, as the oxyanion, is toxic to prokaryotes, and although prokaryotes have evolved resistance to tellurium, no universal mechanism exists. We review the interaction of tellurite with prokaryotes with a focus on those unique strains that thrive in environments naturally rich in tellurium. AbstractThe timeline of tellurite prokaryotic biology and biochemistry is now over 50 years long. Its start was in the clinical microbiology arena up to the 1970s. The 1980s saw the cloning of tellurite resistance determinants whil…

biologytellurite transporttellurium nanoparticlesThe RenaissanceContext (language use)010501 environmental sciencesbiology.organism_classification01 natural sciencesTellurite transporttellurite resistanceClinical microbiologytellurite bioprocessingtellurite toxicityGeochemistry and PetrologyChemistry (miscellaneous)Evolutionary biologyEnvironmental ChemistryBacteria0105 earth and related environmental sciencesEnvironmental Chemistry
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