Search results for "Ego"

showing 10 items of 10822 documents

Pharmaceuticals and other urban contaminants threaten Amazonian freshwater ecosystems

2021

Abstract Urban areas in the Brazilian Amazon have grown at an unprecedented rate during the last years. About 90% of the wastewater produced by these urban areas are discharged untreated into Amazonian freshwater ecosystems, constituting a potential environmental pathway for pharmaceuticals and other chemicals consumed by modern societies (e.g. psychostimulants, personal-care products, hormones). The distribution of these chemicals into the Amazon River and their potential risks for freshwater biodiversity have not been evaluated so far. Here, we show the results of the largest chemical monitoring campaign conducted in the Amazon region. We assessed exposure patterns for 43 pharmaceuticals …

010504 meteorology & atmospheric sciencesAmazonianBiodiversity010501 environmental sciences01 natural sciencesFreshwater ecosystemFreshwater ecosystemRiversEnvironmental protectionUrbanizationTributaryparasitic diseasesChemical risk assessmentGE1-350CitiesEcosystem0105 earth and related environmental sciencesGeneral Environmental Sciencegeographygeography.geographical_feature_categoryAmazon rainforestAmazon RiverFreshwater ecosystemsfood and beveragesQ Science (General)BiodiversityContaminationEnvironmental sciencesWastewaterPharmaceutical PreparationsPharmaceuticalEnvironmental sciencePharmaceuticalsWater Pollutants Chemicalgeographic locationsEnvironmental MonitoringEnvironment International
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Simulated European stalagmite record and its relation to a quasi-decadal climate mode

2013

Abstract. A synthetic stalagmite record for the Bunker cave is constructed using a combined climate-stalagmite modeling approach. The power spectrum of the simulated speleothem calcite δ18O record has a pronounced peak at quasi-decadal time scale. Interestingly, mixing processes in the soil and karst above the cave represent a natural low-pass filter of the speleothem climate archive. We identify a quasi-decadal mode characterized by a "tripole pattern" of sea surface temperature affecting stalagmite δ18O values. This pattern, which is well-known in literature as the quasi-decadal mode in the North Atlantic, propagates eastwards and affects western European temperature surrounding the cave.…

010504 meteorology & atmospheric sciencesAtmospheric circulationδ18OStratigraphylcsh:Environmental protectionSpeleothemStalagmite010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compound03 medical and health sciencesCavelcsh:Environmental pollutionlcsh:TD169-171.8lcsh:Environmental sciences030304 developmental biology0105 earth and related environmental sciencesCalcitelcsh:GE1-350Global and Planetary Changegeography0303 health sciencesgeography.geographical_feature_categoryPaleontologyKarstchemistry13. Climate actionClimatologylcsh:TD172-193.5GeologyTeleconnectionClimate of the Past
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Strombolian eruptions and dynamics of magma degassing at Yasur Volcano (Vanuatu)

2020

Abstract Open vent basaltic volcanoes account for a substantial portion of the global atmospheric outgassing flux, largely through passive degassing and mild explosive activity. We present volcanic gas flux and composition data from Yasur Volcano, Vanuatu collected in July 2018. The average volcanic plume chemistry is characterised by a mean molar CO2/SO2 ratio of 2.14, H2O/SO2 of 148 and SO2/HCl of 1.02. The measured mean SO2 flux in the period of 6th to 9th July is 4.9 kg s−1. Therefore, the mean fluxes of the other species are 7.5 kg∙s−1 CO2, 208 kg∙s−1 H2O and 4.8 kg∙s−1 HCl. The degassing regime at Yasur volcano ranges from ‘passive’ to ‘active’ styles, with the latter including Stromb…

010504 meteorology & atmospheric sciencesBasaltic open vent volcanoessub-05Gas fluxes010502 geochemistry & geophysics01 natural sciencesStrombolian activityFlux (metallurgy)Geochemistry and PetrologyCrystal content in magmaPetrology0105 earth and related environmental sciencesBasaltgeographygeography.geographical_feature_categoryBasaltic open vent volcanoes Crystal content in magma Gas fluxes Magma fluxes Strombolian activity YasurStrombolian eruptionMagma fluxesOutgassingGeophysicsVolcanoVolcanic plumeMagmaInclusion (mineral)YasurGeology
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A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop

2019

Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large-volume pyroclastic deposits and later-stage deformation related to post-caldera resurgence and volcanism. Unrest episodes are not always followed by an eruption; however, every eruption is preceded by unrest. The Campi Flegrei caldera (CFc), located along the eastern Tyrrhenian coastline in southern Italy, is close to the densely populated area of Naples. It is one of the most dangerous volcanoes on Earth and represents a key example of an acti…

010504 meteorology & atmospheric sciencesCalderasGeochemistryEnergy Engineering and Power TechnologyPyroclastic rockVolcanologyMagma chamberVolcanism010502 geochemistry & geophysics01 natural sciencesdrillingsouthern ItalycalderaCaldera14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMechanical Engineeringlcsh:QE1-996.5VolcanologyMagellanPlus workshopInternational Ocean Discovery Programlcsh:GeologyCampi Flegrei calderaVolcanoItaly13. Climate actionEruptionMagmacaldera Campi Flegrei monitopring system hydrothermal system IODPCampi FlegreiGeology
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Hydrothermal pressure-temperature control on CO2 emissions and seismicity at Campi Flegrei (Italy)

2021

Fluids supplied by stored magma at depth are causal factors of volcanic unrest, as they can cause pressurization/heating of hydrothermal systems. However, evidence for links between hydrothermal pressurization, CO2 emission and volcano seismicity have remained elusive. Here, we use recent (2010−2020) observations at Campi Flegrei caldera (CFc) to show hydrothermal pressure, gas emission and seismicity at CFc share common source areas and well-matching temporal evolutions. We interpret the recent escalation in seismicity and surface gas emissions as caused by pressure-temperature increase at the top of a vertically elongated (0.3–2 km deep) gas front. Using mass (steam) balance consideration…

010504 meteorology & atmospheric sciencesCampi Flegrei mantle geochemistry CO2 emission Fumarole compositions Hydrothermal systems Volcanic unrest Volcano seismicityInduced seismicity010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationHydrothermal systemsCabin pressurizationGeochemistry and PetrologyCalderaPetrologyFumarole compositions0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryVolcanic unrest; Hydrothermal systems; Campi Flegrei; Fumarole compositions; CO2 emission; Volcano seismicityFront (oceanography)Volcano seismicityGeophysicsVolcanoVolume (thermodynamics)Volcanic unrestCO2 emissionMagmaCampi FlegreiGeology
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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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Kinematics, deformation partitioning and late Variscan magmatism in the Agly massif, Eastern Pyrenees, France

2020

International audience; In order to constrain the finite deformation pattern of the Variscan basement of the Agly massif, a detailed structural analysis over the whole Agly massif was performed. Our investigation combined geological mapping, reappraisal of published and unpublished data completed with our own structural work. Results are provided in the form of new tectonic maps and series of regional cross-sections through the Agly massif. At variance from previous studies, we identified three deformation fabrics named D1, D2 and D3. The D1 deformation is only relictual and characterized by a broadly northwest-southeast striking and eastward dipping foliation without any clear mineral and …

010504 meteorology & atmospheric sciencesCrustal thinningPlutonGneiss domeMetamorphism[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesTranspressionLineationPetrologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesVariscan orogengeographygeography.geographical_feature_categorylcsh:QE1-996.5GeologyMassifPlutonismAgly Massiflcsh:GeologySinistral and dextral[SDU]Sciences of the Universe [physics]eastern pyreneesShear zoneGeology
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A geological field trip to the Côte d'Ivoire-Ghana transform margin

1998

Abstract During the Equanaute survey (June 1992), fourteen submersible dives were performed between 4950 and 2250 m water depths across the southern slope of the Cote d'Ivoire-Ghana Marginal Ridge (CIGMR), in the eastern Equatorial Atlantic. The CIGMR, a high-standing topographic marginal ridge along the Cote d'Ivoire-Ghana transform margin, is believed to result from a complex structural evolution due to the specific wrench-related rifting between Western Equatorial Africa and Northeastern Brazil, in Early Cretaceous times. In this paper we report and discuss geological observations made during dives, and sample analyses to resolve the lithology, paleoenvironmental conditions, age and orig…

010504 meteorology & atmospheric sciencesCôte d’Ivoire-GhanaLithologyAtlantique EquatorialMid-Atlantic RidgeAquatic ScienceStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontology14. Life underwaterGéologieCôte d’lvoire-Ghana0105 earth and related environmental sciencesEquatorial AtlanticgeographyRiftgeography.geographical_feature_categoryMarge transformanteGeology15. Life on landTectonics13. Climate actionRidgeClastic rockSedimentary rockTransform marginGeologyOceanologica Acta
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Measuring, modelling and managing gully erosion at large scales: A state of the art

2018

Soil erosion is generally recognized as the dominant process of land degradation. The formation and expansion of gullies is often a highly significant process of soil erosion. However, our ability to assess and simulate gully erosion and its impacts remains very limited. This is especially so at regional to continental scales. As a result, gullying is often overlooked in policies and land and catchment management strategies. Nevertheless, significant progress has been made over the past decades. Based on a review of >590 scientific articles and policy documents, we provide a state-of-the-art on our ability to monitor, model and manage gully erosion at regional to continental scales. In this…

010504 meteorology & atmospheric sciencesData productsDrainage basinGully erosionSpatial data010502 geochemistry & geophysics01 natural sciencesModellingGully erosionGully expansionSpatial analysisSoil Erosion0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybusiness.industryEnvironmental resource managementSediment yieldSedimentContinental15. Life on landMeasuringRegionalEuropeCurrent (stream)PolicyContinental Europe Gully erosion Gully expansion Gully initiation Measuring Modelling Policy Prediction Regional Sediment yield Spatial dataSection (archaeology)Land degradationGeneral Earth and Planetary SciencesEnvironmental sciencePredictionbusinessGully initiationEarth-Science Reviews
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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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