Search results for "Geochemistry"

showing 10 items of 2967 documents

Terrestrial Inputs Drive Seasonality in Organic Matter and Nutrient Biogeochemistry in a High Arctic Fjord System (Isfjorden, Svalbard)

2020

Climate-change driven increases in temperature and precipitation are leading to increased discharge of freshwater and terrestrial material to Arctic coastal ecosystems. These inputs bring sediments, nutrients and organic matter (OM) across the land-ocean interface with a range of implications for coastal ecosystems and biogeochemical cycling. To investigate responses to terrestrial inputs, physicochemical conditions were characterized in a river- and glacier-influenced Arctic fjord system (Isfjorden, Svalbard) from May to August in 2018 and 2019. Our observations revealed a pervasive freshwater footprint in the inner fjord arms, the geochemical properties of which varied spatially and seaso…

light climate0106 biological sciencesBiogeochemical cyclelcsh:QH1-199.5010504 meteorology & atmospheric sciencesFreshetOcean EngineeringFjordlcsh:General. Including nature conservation geographical distributionAquatic ScienceOceanographyPermafrost01 natural sciencesOrganic matterlcsh:Sciencecoastal biogeochemistryVDP::Landbruks- og Fiskerifag: 900::Fiskerifag: 920VDP::Mathematics and natural science: 4000105 earth and related environmental sciencesWater Science and Technologychemistry.chemical_classificationGlobal and Planetary Changegeographygeography.geographical_feature_category010604 marine biology & hydrobiologyAquatic ecosystemfreshwater inputsBiogeochemistryVDP::Matematikk og Naturvitenskap: 400dissolved organic matterglacier runoffclimate changeOceanographychemistryArcticEnvironmental sciencelcsh:Q
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Halogens and trace metal emissions from the ongoing 2008 summit eruption of Kīlauea volcano, Hawai`i

2012

Volcanic plume samples taken in 2008 and 2009 from the Halemàumàu eruption at Kīlauea provide new insights into Kīlauea's degassing behaviour. The Cl, F and S gas systematics are consistent with syn-eruptive East Rift Zone measurements suggesting that the new Halemàumàu activity is fed by a convecting magma reservoir shallower than the main summit storage area. Comparison with degassing models suggests that plume halogen and S composition is controlled by very shallow (<3m depth) decompression degassing and progressive loss of volatiles at the surface. Compared to most other global volcanoes, Kīlauea's gases are depleted in Cl with respect to S. Similarly, our Br/S and I/S ratio measurem…

magma chamberaerosolHalideMineralogyMagma chambervolcanic eruptionchemistry.chemical_compoundGeochemistry and PetrologyemissionTrace metalaciditymercury (element)geographygeography.geographical_feature_categoryplumesolubilitydegassingparticle sizehalogenlavatrace metalSilicateAerosolPlumevolcanoVolcanochemistryEnvironmental chemistryMagmaisotopic ratioGeologyGeochimica et Cosmochimica Acta
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Elemental and isotope covariation of noble gases in mineral phases from Etnean volcanics erupted during 2001–2005, and genetic relation with peripher…

2008

Abstract During 2001–2005, Mount Etna was characterized by intense eruptive activity involving the emission of petrologically different products from several vents, which involved at least two types of magma with different degrees of evolution. We investigated the ratios and abundances for noble-gas isotopes in fluid inclusions trapped in olivines and pyroxenes in the erupted products. We confirm that olivine has the most efficient crystalline structure for preserving the pristine composition of entrapped gases, while pyroxene can suffer diffusive He loss. Both the minerals also experience noble gas air contamination after eruption. Helium isotopes of the products genetically linked to the …

magma degassing.geographygeography.geographical_feature_categoryOlivinefluid inclusionhelium isotopeTrace elementGeochemistryPyroxeneengineering.materialnoble gaseMantle (geology)Settore GEO/08 - Geochimica E VulcanologiaVolcanic rockGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)engineeringFluid inclusionsMetasomatismGeologymagma degassing
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Sedimentation and tropical vegetation changes in Southern Benin (West Africa), carbon-13 tracing of organic matter dynamics and fluctuations of the s…

2007

12 pages; International audience

mangrovepaleoenvironment[SDE.MCG]Environmental Sciences/Global Changes[ SDV.SA.SDS ] Life Sciences [q-bio]/Agricultural sciences/Soil study13C/12C isotope ratio[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDE.MCG] Environmental Sciences/Global Changes[ SDE.MCG ] Environmental Sciences/Global ChangesOuémé-Sô[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyBeninsea level fluctuation[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil studydelta faciesComputingMilieux_MISCELLANEOUS
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Geochemical and eco-toxicological evaluations in box-core sediments from the Sicilian coast, central Mediterranean

2007

marine sediment geochemistry trace metal IPASettore GEO/08 - Geochimica E Vulcanologia
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Motivation and Preferences of Visitors in the Bohemian Paradise UNESCO Global Geopark

2021

There are some localities in the Bohemian Paradise Geopark that suffer from temporal overtourism in the high season. On the other hand, more than half of the geopark is not so often visited by tourists, although very attractive geosites can be found there too. In the most visited localities, nature is damaged due to overloading of the tourist infrastructure, while elsewhere there is pressure driven by municipalities to increase the number of tourists. For this reason, we organized a large questionnaire survey in summer 2020, which aimed to reveal the motivation of visitors of the geopark and their preferences regarding the places visited. The questionnaire combined several research methods:…

media_common.quotation_subject010502 geochemistry & geophysicsovertourism01 natural sciencesgeotourismgeopark managementovertourism; geoheritage; geopark management; geotourism; sustainable tourismPromotion (rank)geoheritage0502 economics and businessMental mappingMainstreamGeotourismsustainable tourismMarketingSustainable tourism0105 earth and related environmental sciencesmedia_common05 social scienceslcsh:QE1-996.5GeoparkQuestionnairelcsh:GeologyGeneral Earth and Planetary Sciences050212 sport leisure & tourismTourismGeosciences
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First combined flux chamber survey of mercury and CO2 emissions from soil diffuse degassing at Solfatara of Pozzuoli crater, Campi Flegrei (Italy): M…

2014

Abstract There have been limited studies to date targeting gaseous elemental mercury (GEM) flux from soil emission in enriched volcanic substrates and its relation with CO 2 release and tectonic structures. In order to evaluate and understand the processes of soil–air exchanges involved at Solfatara of Pozzuoli volcano, the most active zone of Campi Flegrei caldera (Italy), an intensive field measurement survey has been achieved in September 2013 by using high-time resolution techniques. Soil–air exchange fluxes of GEM and CO 2 have been measured simultaneously at 116 points, widely distributed within the crater. Quantification of gas flux has been assessed by using field accumulation chamb…

mercury flux carbon dioxide soil degassinggeographygeography.geographical_feature_categorygenetic structuresMineralogychemistry.chemical_elementHydrothermal circulationMercury (element)Settore GEO/08 - Geochimica E VulcanologiaVolcanic mercurychemistry.chemical_compoundTectonicsGeophysicsFlux (metallurgy)chemistryImpact craterVolcanoCarbon dioxideGeochemistry and PetrologyCarbon dioxideCalderaSoil degassingMercury fluxSolfataraGeology
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Cavezzo, the first Italian meteorite recovered by the PRISMA fireball network. Orbit, trajectory, and strewn-field

2020

ABSTRACT Two meteorite pieces have been recovered in Italy, near the town of Cavezzo (Modena), on 2020 January 4th. The associated fireball was observed on the evening of New Year’s Day 2020 by eight all-sky cameras of the PRISMA fireball network, a partner of FRIPON. The computed trajectory had an inclination angle of approximately 68° and a velocity at infinity of 12.8 km s−1. Together with the relatively low terminal height, estimated as 21.5 km, those values were indicating the significant possibility of a meteorite dropping event, as additionally confirmed by the non-zero residual total mass. The strewn-field was computed taking into account the presence of two bright light flashes, re…

meteoroids -methods: data analysis -techniques: image processing010502 geochemistry & geophysics01 natural sciencesStrewn fieldmeteorites0103 physical sciencesmeteorsmeteoroids010303 astronomy & astrophysicsmeteoroid0105 earth and related environmental sciencesPhysicsMeteoroidimage processing; meteorites; meteoroids; meteors; methods: data analysis; techniquesmeteorAstronomyAstronomy and Astrophysicsmethods: data analysismeteoriteimage processingMeteoriteSpace and Planetary Science[SDU]Sciences of the Universe [physics]data analysi [methods]TrajectoryOrbit (control theory)techniques
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The role of biotic and abiotic processes in the origin of Messinian evaporate-associated carbonates (Southern Italy)

2013

microbial carbonateevaporiteMessinian Salinity Crisigeochemistry
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Formation of microbial organic carbonates during the Late Jurassic from the Northern Tethys (Amu Darya Basin, Uzbekistan): implications for Jurassic …

2020

23 pages; International audience; The Late Jurassic was a period of major global carbon cycle perturbations with episodes of anoxia leading to regional accumulation of organic matter in sediments worldwide. The Tubiegatan section (SW Gissar Mountains, Uzbekistan) located in the Northern Tethys, shows atypical organic-rich limestone and marl deposits (up to 6% of total organic carbon) marked by pronounced negative excursions of δ13Ccarb (amplitude of ca. 12‰) and δ13Corg (amplitude of ca. 4‰) recorded during the Middle Oxfordian (Transversarium Zone). A transdisciplinary approach including sedimentology, palynofacies characterization, mineralogy, organic and inorganic geochemistry was carrie…

microbial/laminated sediments52 anoxia010504 meteorology & atmospheric sciencesGeochemistryLate Jurassic02 engineering and technologyOceanography01 natural scienceschemistry.chemical_compoundAnoxia[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl0202 electrical engineering electronic engineering information engineeringAmu Darya BasinOrganic matter14. Life underwaterMicrobial mat0105 earth and related environmental sciencesStable isotopesTotal organic carbonSabkhachemistry.chemical_classificationGlobal and Planetary Changegeographygeography.geographical_feature_category020206 networking & telecommunicationsorganic-rich carbonatesstable isotopes 5315. Life on landCretaceousPalynofacieschemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
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