Search results for "Conti"

showing 10 items of 3486 documents

A geotraverse across two paleo-subduction zones in Tien Shan, Tajikistan

2017

Abstract We present first LA-ICP-MS U–Pb zircon ages as well as geochemical and Sr–Nd–Pb isotope data for 14 magmatic rocks collected along ca. 400 km profile across the Chatkal-Kurama terrane in the Mogol-Tau and Kurama ranges and the Gissar Segment of the Tien Shan orogen in Tajikistan. These new data from supra-subduction and post-collisional magmatic rocks of two Late Paleozoic active margins constrain a tectonic model for terrane motions across two paleo-subduction zones: (1) The 425 Ma old Muzbulak granite of the Mogol-Tau range formed in a supra-subduction setting at the northern margin of the Turkestan Ocean. The north-dipping plate was subducted from the Early Silurian to the earli…

010504 meteorology & atmospheric sciencesSubductionContinental crustGeochemistryGeology010502 geochemistry & geophysicsOphiolite01 natural sciencesBatholithPassive marginCarboniferousGeology0105 earth and related environmental sciencesTerraneZircon
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Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the co…

2013

11 pages; International audience; The Neodymium(Nd) isotope composition of fish remains has beenwidely used to track past changes in oceanic circulation. Although the number of published Nd isotope data for the Cretaceous has markedly increased in the last years, no consensus has been reached on the structure of the oceanic circulation and its evolution during the Late Cretaceous. Yet this period is characterised bymajor geodynamical and climatic changes andmarked by the disappearance of global oceanic anoxic events inwhich changes in oceanic circulation modesmay have played a significant role. In this study we present the first record of Nd isotopic composition of fish remains from contine…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousIsotopic signaturePaleontologyContinental marginJapanGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryoceanic circulation14. Life underwater[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesRadiogenic nuclide[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySeafloor spreadingCretaceous[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPeriod (geology)Seawaterneodymium isotopesGeology
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13C composition of dissolved organic carbon in upland forested catchments of the Morvan Mountains (France): Influence of coniferous and deciduous veg…

2007

10 pages; International audience; One of the main environmental changes caused by human activities is that of land use. These changes influence the quantity and quality of the dissolved organic matter (DOM) fluxes through the vegetation–soil–stream system. The aim of this work is to evaluate the influence of the substitution of native deciduous forests by well managed coniferous forests on dissolved organic carbon (DOC) fluxes and their associated carbon isotopic composition (d13CDOC). DOC fluxes and d13CDOC were monitored for 2 years in the streams of four similar upland forested catchments in the Morvan Mountains (France). Mean annual DOC concentrations and fluxes were 2–4 times lower in …

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesDrainage basinSTREAMS01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeStream water[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryDissolved organic carbon[ SDE.MCG.SIC ] Environmental Sciences/Global Changes/domain_sde.mcg.sic[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environment[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentChemical composition0105 earth and related environmental sciencesWater Science and TechnologyStable isotopesHydrologygeographySoil organic mattergeography.geographical_feature_category[SDE.MCG.SIC]Environmental Sciences/Global Changes/domain_sde.mcg.sicSoil organic matter04 agricultural and veterinary sciencesVegetation15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDE.MCG.CPE]Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDE.MCG ] Environmental Sciences/Global ChangesDeciduous13. Climate actionSoil solutionSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceDissolved organic carbon
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Simulation of nitrous oxide emissions from wheat-cropped soils using CERES

2005

Estimation of nitrous oxide (N2O) emissions from arable soils, in relation to crop fertilization, is essential to devise strategies to mitigate the impact of agriculture on global warming. This paper presents the development and test of a N2O model resulting from the linkage of a dynamic soil-crop simulation model (CERES) with two sub-models of N2O production and reduction in soils. These sub-models (NOE and NGAS) account for both the nitrification and denitrification pathways. The resulting models (CERES–NOE and CERES–NGAS) were tested against experimental data collected on three contrasting wheat-cropped soils representative of the Beauce agricultural region in France. Although the input …

010504 meteorology & atmospheric sciences[SDV]Life Sciences [q-bio]Soil ScienceSoil scienceengineering.materialCERES01 natural sciencesModellingchemistry.chemical_compound[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentAGRONOMIE[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences2. Zero hungerNitrous oxideGlobal warming04 agricultural and veterinary sciencesNitrous oxideCalcisol15. Life on landSoil type[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentGreenhouse gaseschemistry13. Climate actionGreenhouse gasFertilizationSoil water[SDE]Environmental Sciences040103 agronomy & agricultureengineering0401 agriculture forestry and fisheriesEnvironmental scienceFertilizerArable landAgronomy and Crop Science
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Comparing methods for computation of run-up heights of landslide-generated tsunami in the Northern Sicily continental margin

2018

The North Sicily continental margin is a very active region located in the Central Mediterranean. Strong seismicity, active tectonics and volcanism, fluid escape, high sediment supply, and widespread mass movements historically have exposed this region to marine geohazards, with a potential for tsunami generation. Morpho-bathymetric analysis revealed that one of the most common mechanisms associated with marine geohazards is due to submarine mass failure processes, genetically linked to the other processes active in this margin. With the aim to assess the risks associated with landslide-generated anomalous waves, we selected two sectors of this margin, Gulf of Palermo to the west and Patti …

010504 meteorology & atmospheric sciencestsunami run-up submarine landslideLandslideVolcanismEnvironmental Science (miscellaneous)Induced seismicity010502 geochemistry & geophysicsGeotechnical Engineering and Engineering GeologyOceanography01 natural sciencesTectonicsContinental marginMargin (machine learning)Earth and Planetary Sciences (miscellaneous)Submarine pipelineSeismologyGeology0105 earth and related environmental sciencesSubmarine landslide
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First in-situ measurements of plume chemistry at mount garet volcano, island of gaua (Vanuatu)

2020

Recent volcanic gas compilations have urged the need to expand in-situ plume measurements to poorly studied, remote volcanic regions. Despite being recognized as one of the main volcanic epicenters on the planet, the Vanuatu arc remains poorly characterized for its subaerial emissions and their chemical imprints. Here, we report on the first plume chemistry data for Mount Garet, on the island of Gaua, one of the few persistent volatile emitters along the Vanuatu arc. Data were collected with a multi-component gas analyzer system (multi-GAS) during a field campaign in December 2018. The average volcanic gas chemistry is characterized by mean molar CO2/SO2, H2O/SO2, H2S/SO2 and H2/SO2 ratios …

010504 meteorology & atmospheric sciencesvolcanic gas compositionsGeochemistryFlux010502 geochemistry & geophysicslcsh:Technology01 natural scienceslcsh:ChemistryVanuatu[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGeneral Materials ScienceGas composition[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentlcsh:QH301-705.5Instrumentation0105 earth and related environmental sciencesFluid Flow and Transfer Processesgeographygeography.geographical_feature_categorySubductionlcsh:TProcess Chemistry and TechnologyGeneral Engineeringlcsh:QC1-999Gas analyzerComputer Science ApplicationsPlumelcsh:Biology (General)lcsh:QD1-999Mount GaretVolcanolcsh:TA1-2040SubaerialPeriod (geology)volatile fluxeslcsh:Engineering (General). Civil engineering (General)GauaGaua Mount Garet Multi-GAS Vanuatu Volatile fluxes Volcanic gas compositionslcsh:PhysicsMulti-GAS
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Evidence of aerial volcanic activity during the Valanginian along the northern Tethys margin.

2009

7 pages; International audience; Stratigraphic measurement and sampling on three sections (Vergol, La Charce, and Montclus) through Valanginian deposits from the Vocontian Basin (southeastern France) reveals the occurrence of centimetre thick ochre-coloured layers, which can be correlated from one section to another. At least twelve of these are identified in sediments dated from the Pertransiens to Furcillata ammonite Zones. These horizons appear similar to previously described Oxfordian and Aptian bentonites, also from the Vocontian Basin. Clay-mineralogical and geochemical data are similar in the Valanginian ochre horizons and their enclosing marls except in one of these that shows a cla…

010506 paleontologyAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesBentonite.PaleontologyVolcanismPassive margin[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesAmmoniteHorizon (geology)geographygeography.geographical_feature_categoryPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageCretaceousVocontian BasinVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyValanginianlanguageBentoniteGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Environmental and climatic controls of the clay mineralogy of Albian deposits in the Paris and Vocontian basins (France)

2020

18 pages; International audience; High-resolution clay mineral analyses were performed on lower and middle Albian deposits from the Paris and Vocontian basins in order to specify the weathering conditions that prevailed at that time. The clay mineral assemblages are composed of small proportions of chlorite and vermiculitic clays associated with abundant illite, R0 type illite-smectite mixed-layers (smectite) and kaolinite. Clay minerals originated from the physical alteration and chemical weathering of rocks and soils outcropping on the Variscan massifs bordering the studied areas. In the Paris Basin, the covariation of illite and kaolinite suggests the reworking of these latter minerals f…

010506 paleontologyAptianOutcropGeochemistryWeatheringengineering.materialPalaeoclimate010502 geochemistry & geophysics01 natural sciencesParis BasinKaoliniteMortoniceras0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyPaleontologyAlbianMassifbiology.organism_classificationClay mineralsVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringClay mineralsGeologyCretaceous Research
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A 2500 year record of natural and anthropogenic soil erosion in South Greenland

2012

International audience; The environmental impact of the Norse landnám in Greenland has been studied extensively. But to date, no study has quantified the soil erosion that Norse agricultural practices are believed to have caused. To resolve this problem, a high resolution sedimentary record from Lake Igaliku in South Greenland is used to quantitatively reconstruct 2500 years of soil erosion driven by climate and historical land use. An accurate chronology allows for the estimation of detritic fluxes and their uncertainties. Land clearance and the introduction of grazing livestock by the Norse around 1010 AD caused an acceleration of soil erosion up to 8 mm/century in 1180 AD which is two-fo…

010506 paleontologyArcheology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesGreenland01 natural sciencesNatural (archaeology)Grazing[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentOvergrazing[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangeLand useEastern settlementLandnámAgricultureGeologyVegetation15. Life on land[ SDE.MCG ] Environmental Sciences/Global ChangesOceanographyDisturbance (ecology)13. Climate actionSoil erosionNorseLand degradationErosionPhysical geographyGeologyQuaternary Science Reviews
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Vegetation and climate record from Abric Romaní (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)

2019

This study addresses the pollen record of Abric Romani archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of A…

010506 paleontologyArcheologyGlobal and Planetary ChangegeographyHumid continental climategeography.geographical_feature_category010504 meteorology & atmospheric sciencesPleistoceneSteppeGeologyVegetation01 natural sciencesInterglacialPaleoclimatologyPhysical geographyGlacial periodStadialEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesQuaternary Science Reviews
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