Search results for "GC"

showing 10 items of 606 documents

Chemical Composition and Biological Activities of Prangos ferulacea Essential Oils

2022

Prangos ferulacea (L.) Lindl, which belongs to the Apiaceae family, is a species that mainly grows in the eastern Mediterranean region and in western Asia. It has been largely used in traditional medicine in several countries and it has been shown to possess several interesting biological properties. With the aim to provide new insights into the phytochemistry and pharmacology of this species, the essential oils of flowers and leaves from a local accession that grows in Sicily (Italy) and has not yet been previously studied were investigated. The chemical composition of both oils, obtained by hydrodistillation from the leaves and flowers, was evaluated by GC-MS. This analysis allowed us to …

(Z)-β-ocimenePrangos ferulaceaantimicrobial activityApiaceae; <i>Prangos ferulacea</i>; (<i>Z</i>)-<i>β</i>-ocimene; GC-MS; antioxidant activity; antimicrobial activityOrganic ChemistryPharmaceutical Scienceantioxidant activityAntioxidantsAnalytical ChemistryAnti-Bacterial AgentsPlant LeavesAnti-Infective AgentsChemistry (miscellaneous)Drug DiscoveryOils VolatileMolecular MedicinePhysical and Theoretical ChemistryGC-MSSicilyApiaceae
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Influence of Wind on Suspended Matter in the Water of the Albufera of Valencia (Spain)

2021

Wind is one of the factors that has a great influence on suspended matter in lakes, especially in shallow lagoons. In order to know how wind affects the water in Albufera of Valencia, a shallow coastal lagoon, the measured variables of turbidity and transparency have been correlated with the estimates by processing Sentinel-2 satellite images with the Sen2Cor processor. Data from four years of study show that most of them are light to gentle easterly breezes and moderate to fresh westerly breezes. The results obtained show significant correlations between the measured variables and those obtained from the satellite images for total suspended matter and water transparency and with the averag…

010504 meteorology & atmospheric sciences0208 environmental biotechnologyOcean Engineering02 engineering and technologyAtmospheric sciences01 natural sciencesWind speedlcsh:Oceanographylcsh:VM1-989Wind effectlcsh:GC1-1581TurbidityEcologia de les albuferesShallow lakeValencia0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringtransparencyHydrologySuspended solidsbiologySedimentlcsh:Naval architecture. Shipbuilding. Marine engineeringbiology.organism_classificationTransparency (behavior)atmospheric_science020801 environmental engineeringTotal suspended matterwind effectshallow lakeEnvironmental scienceSatellitesuspended solidsSentinel-2Suspended matter
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Partitioning of nitrogen during melting and recycling in subduction zones and the evolution of atmospheric nitrogen

2019

Abstract The subduction of sediment connects the surface nitrogen cycle to that of the deep Earth. To understand the evolution of nitrogen in the atmosphere, the behavior of nitrogen during the subduction and melting of subducted sediments has to be estimated. This study presents high-pressure experimental measurements of the partitioning of nitrogen during the melting of sediments at sub-arc depths. For quantitative analysis of nitrogen in minerals and glasses, we calibrated the electron probe micro-analyzer on synthetic ammonium feldspar to measure nitrogen concentrations as low as 500 μg g−1. Nitrogen abundances in melt and mica are used together with mass balance calculations to determi…

010504 meteorology & atmospheric sciencesAnalytical chemistrychemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsFeldspar01 natural sciencesMantle (geology)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySubduction zonesNitrogen cycle0105 earth and related environmental sciencesMantle metasomatismSubductionGeologyNitrogenPartition coefficientchemistry13. Climate action[SDU]Sciences of the Universe [physics]visual_art[SDE]Environmental Sciencesvisual_art.visual_art_mediumSlabAtmosphere evolutionMicaGeologyNitrogen cycling
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Changements environnementaux survenant à la limite Oligocène/Miocène du bassin des Limagnes (Massif central, France).

2018

16 pages; International audience; Continental environments are very sensitive to climatic variations. A unique opportunity to study the climate changes around the Oligocene/Miocene boundary is offered by the Limagne graben Basin (France) where this stage boundary is well constrained by fossils. Indeed, some localities of the Limagne Graben Basin are so rich in mammal remains that they have become a European reference for mammal biostratigraphy. The dominant sedimentary facies of the lacustrine deposits in the northern part of the Limagne Graben Basin are composed of poorly cemented marls and calcarenites containing various plants and animals remains (e.g. algae, fish bones and teeth, gastro…

010504 meteorology & atmospheric sciencesContext (language use)Biostratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrycarbonates lacustresMarl14. Life underwaterstromatolitebassin des Limagnes0105 earth and related environmental sciencesPalynologygeographygeography.geographical_feature_categoryLimagne Basinisotopes de l’oxygènebiologylimite oligo-miocèneoxygen isotopeslcsh:QE1-996.5GeologyMassif15. Life on landbiology.organism_classificationlacustrine carbonateGrabenlcsh:GeologyStromatolite13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyapatitePeriod (geology)Oligocene/Miocene boundarybiozoneGeologyBSGF - Earth Sciences Bulletin
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Dukono, the predominant source of volcanic degassing in Indonesia, sustained by a depleted Indian-MORB

2017

Co-auteur étranger; International audience; Located on Halmahera island, Dukono is among the least known volcanoes in Indonesia. A compilation of the rare available reports indicates that this remote and hardly accessible volcano has been regularly in eruption since 1933, and has undergone nearly continuous eruptive manifestation over the last decade. The first study of its gas emissions, presented in this work, highlights a huge magmatic volatile contribution into the atmosphere, with an estimated annual output of about 290 kt of SO2, 5000 kt of H2O, 88 kt of CO2, 5 kt of H2S and 7 kt of H2. Assuming these figures are representative of the long-term continuous eruptive activity, then Dukon…

010504 meteorology & atmospheric sciencesDepleted mantle sourceLavaEarth sciencedegassing budget[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/Volcanology010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryevolution[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyDukono VolcanoSedimentologyComputingMilieux_MISCELLANEOUSMagma source0105 earth and related environmental sciencesDukono volcanogeographygeography.geographical_feature_categorySubductionGas emissionsmagma source evolution[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryVolcanodepleted mantle sourceDegassing budget13. Climate actionGeology
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Environmental change during the Early Cretaceous in the Purbeck-type Durlston Bay section (Dorset, Southern England): a biomarker approach.

2007

20 pages; International audience; The Purbeck-type section (Durlston Bay, Dorset, UK) exhibits littoral lagoonal to lacustrine facies. It shows a gradual climatic/environmental change from semi-arid conditions associated with evaporites at the Jurassic–Cretaceous transition, to a more humid climate at the end of the Berriasian. Though generally organic-poor (total organic carbon, TOC, <1.3%), the Durlston Bay section shows an organic-rich episode (TOC up to 8.5%) located at the transition from evaporitic to more humid facies. A biomarker study was performed in order to determine the origin of the organic matter (OM) in the section and see if changes in organic sources accompanied the genera…

010504 meteorology & atmospheric sciencesEnvironmental change[SDE.MCG]Environmental Sciences/Global ChangesBotryococcus010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeBottom waterSteranechemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry0105 earth and related environmental sciencesTotal organic carbonbiologyEcology15. Life on landbiology.organism_classification[SDE.MCG.CPE]Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry6. Clean waterCretaceousPalynofacies[ SDE.MCG ] Environmental Sciences/Global Changeschemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBayGeology
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Some sedimentological and geochemical characters of the late Triassic Noto formation, source rock in the Ragusa basin (Sicily)

1990

URA 724 du CNRS a intégré UMR 6113 - ISTO CNRS Université d'Orléans; In the Ragusa basin (southeastern Sicily), the late Triassic Noto formation is considered as the main oil source rock. We provide a detailed description of the sedimentary facies determined from core samples, and discuss geochemical results, obtained for both kerogens and chloroform extractable hydrocarbons from samples where sedimentary organic matter is immature. Two main sedimentary sequences were encountered: (i) layers of limestones and of marls (or shales) alternating at a metric scale, and (ii) laminites having various types and carbonate contents. The high petroleum potentials (S2 up to 100 kg HC/t rock) are relate…

010504 meteorology & atmospheric sciencesGeochemistryMineralogy010502 geochemistry & geophysics01 natural sciencesSedimentary depositional environmentchemistry.chemical_compoundNotoGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryKerogenSedimentary organic matterParent rockSicily0105 earth and related environmental sciencesMaturity (geology)kerogen typeclay/carbonate sequencesRagusa basinTriassicSource rockchemistryFaciesSedimentary rocksource rock sedimentologymodeling of oil formationGeology
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Shallow system rejuvenation and magma discharge trends at Piton de la Fournaise volcano (La Réunion Island)

2017

International audience; Basaltic magma chambers are often characterized by emptying and refilling cycles that influence their evolution in space and time, and the associated eruptive activity. During April 2007, the largest historical eruption of Piton de la Fournaise (Île de La Réunion, France) drained the shallow plumbing system (>240×106 m3>240×106 m3) and resulted in collapse of the 1-km-wide summit crater. Following these major events, Piton de la Fournaise entered a seven-year long period of near-continuous deflation interrupted, in June 2014, by a new phase of significant inflation. By integrating multiple datasets (lava discharge rates, deformation, seismicity, gas flux, gas composi…

010504 meteorology & atmospheric sciencesLavaeffusive paroxysmMagma chamber010502 geochemistry & geophysicseffusive trend01 natural sciencesEffusive eruptionImpact crater[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryeffusive paroxysm; effusive trends; Piton de la Fournaise; shallow plumbing system; unloading; Geophysics; Geochemistry and Petrology; Earth and Planetary Sciences (miscellaneous); Space and Planetary ScienceGeochemistry and Petrologyunloading[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyEarth and Planetary Sciences (miscellaneous)Petrology0105 earth and related environmental sciencesBasaltgeographygeography.geographical_feature_categoryeffusive trendsFumarolePiton de la FournaiseGeophysicsVolcanoshallow plumbing systemSpace and Planetary ScienceMagmaGeologySeismology
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The imprint of subduction fluids on subducted MORB-derived melts (Sierra del Convento Mélange, Cuba)

2011

International audience; Major and trace element signatures and Sr-Nd-Pb isotope data for muscovite (Ms)-bearing amphibolite blocks and associated muscovite-bearing trondhjemite and quartz-muscovite rocks from the Sierra del Convento melange (eastern Cuba) indicate that Proto-Caribbean oceanic crust underwent wet partial melting processes during Mesozoic subduction and after accretion to the upper plate. Trace element normalized patterns of Ms-bearing amphibolites are enriched in light rare earth elements (LREE) and large-ion lithophile elements (LILE) and evidence variable trace element transfer from the Proto-Caribbean subducting slab to the mantle wedge. Ms-bearing trondhjemites show LREE…

010504 meteorology & atmospheric sciencesMantle wedge[SDE.MCG]Environmental Sciences/Global ChangesFluid compositionTrondhjemiteGeochemistrySedimentary imprint010502 geochemistry & geophysics01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochemistry and PetrologyOceanic crust0105 earth and related environmental sciencesBasaltTrace elementsSubductionbiologyPartial meltingTrace elementGeologySr-Nd-Pb isotopesbiology.organism_classification13. Climate actionAdakiteLileGeologySlab meltsLithos
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Geodynamic control on carbonate diagenesis: Petrographic and isotopic investigation of the Upper Jurassic formations of the Paris Basin (France).

2007

23 pages; International audience; The Oxfordian and Kimmeridgian carbonates of the eastern edge of the Paris Basin display poor reservoir properties (Φb15% and Kb0.1 md). The petrographic investigation and the resultant paragenetic sequence show that this is due to extensive precipitation of 2 types of almost synchronous blocky LMC (Low Magnesian Calcite) cements during mesogenesis (burial). Stable isotope investigation of these non-recrystallized cements, through both microdrilling sampling and in-situ SIMS (Secondary IonMass Spectrometry) analysis, shows that they originated from slightly buffered meteoric fluids (−3‰SMOW to −8‰SMOW) flowing through the Malm carbonate aquifers of the east…

010504 meteorology & atmospheric sciencesStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCarbonates010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyBasin evolution01 natural sciencesUnconformityDiagenesisPetrographyPaleontologychemistry.chemical_compoundUnconformities[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryLower Cretaceous0105 earth and related environmental sciencesStable isotopesgeographygeography.geographical_feature_categoryGeologyMassif[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesDenudationchemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMeteoric waterCarbonateGeology
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