Search results for "Seawater"

showing 10 items of 386 documents

The key role played by the Augusta basin (southern Italy) in the mercury contamination of the Mediterranean Sea.

2011

The Augusta basin, located in SE Sicily (southern Italy), is a semi-enclosed marine area, labelled as a highly contaminated site. The release of mercury into the harbour seawater and its dispersion to the blue water, make the Augusta basin a potential source of anthropogenic pollution for the Mediterranean Sea. A mass balance was implemented to calculate the HgT budget in the Augusta basin. Results suggest that an average of ∼0.073 kmol of HgT is released, by diffusion, on a yearly basis, from sediments to the seawater, with a consequent output of 0.162 kmol y(-1) to coastal and offshore waters; this makes the Augusta area an important contributor of mercury to the Mediterranean Sea. Owing …

010504 meteorology & atmospheric scienceschemistry.chemical_element010501 environmental sciencesManagement Monitoring Policy and LawStructural basin01 natural sciencesMediterranean seaOcean gyreMediterranean SeaWater Pollution ChemicalSeawater14. Life underwater0105 earth and related environmental sciencescomputer.programming_languagegeographygeography.geographical_feature_categoryPublic Health Environmental and Occupational HealthSedimentGeneral MedicineMercury6. Clean waterMercury (element)Settore GEO/08 - Geochimica E VulcanologiaOceanographychemistryHg sediment Augusta basinItaly13. Climate actionHarbourSeawaterSubmarine pipelinecomputerGeologyWater Pollutants ChemicalEnvironmental MonitoringJournal of environmental monitoring : JEM
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Influence of dissolved organic matter on rare earth elements and yttrium distributions in coastal waters

2010

International audience; Data collected during this study indicate that dissolved Y and REE (rare earth element) behaviour can be monitored through shale-normalised ratios. Relationships occurring between these ratios suggest that leaching from lithogenic materials is the main source of REE in the studied area. This process involves riverine detrital matter in the inner area of the Gulf of Palermo. Features of shale-normalised patterns and the relationship recognised between dissolved Fe and Y/Ho suggest that REE are released from Fe-rich coatings of atmospheric dust. Observed similarities between dissolved Fe and chlorophyll- content suggest that leaching of Fe-rich atmospheric particulates…

010506 paleontologyMineralogyrare earth elementsMediterranean010502 geochemistry & geophysics01 natural sciencesMediterranean seaDissolved organic carbonMediterranean Sea[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyOrganic matter14. Life underwaterScavengingEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental Sciencechemistry.chemical_classificationEcologyRare-earth elementAuthigenicParticulatesREE; Mediterranean; Ce anomalyREESettore GEO/08 - Geochimica E VulcanologiachemistryCe anomaly13. Climate actionEnvironmental chemistryGeneral Earth and Planetary SciencesSeawaterchlorophyll-YREE Ce anomaly Central Mediterranean late Quaternary Palaeoenvironmental reconstructionGeologyChemistry and Ecology
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Water mass exchange and variations in seawater temperature in the NW Tethys during the Early Jurassic: evidence from neodymium and oxygen isotopes of…

2009

10 pages; International audience; Oxygen and neodymium isotope analyses performed on biostratigraphically well-dated fish remains recovered from the Hettangian to Toarcian of the Paris Basin were used to reconstruct variations of Early Jurassic seawater temperature and to track oceanographic changes in the NW Tethys. Our results indicate a strong correlation between δ18O trends recorded by fish remains and belemnites, confirming the paleoenvironmental origin of oxygen isotope variations. Interestingly, temperatures recorded by pelagic fishes and nektobenthic belemnites and bottom dwelling fishes are comparable during the Late Pliensbachian sea-level lowstand but gradually differ during the …

010506 paleontologyWater mass[SDE.MCG]Environmental Sciences/Global ChangesToarcian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologyWater columnGeochemistry and PetrologyPaleoceanography[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrypaleoclimateEarth and Planetary Sciences (miscellaneous)14. Life underwater0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRadiogenic nuclidebiologyoxygen isotopesPelagic zonebiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphypaleoceanographyfish toothSeawaterneodymium isotopes[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyBelemnitesGeology
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Ion fractionation in young sea ice from Kongsfjorden, Svalbard

2011

AbstractThe fractionation of major sea-water ions, or deviation in their relative concentrations from Standard Mean Ocean Water ratios, has been frequently observed in sea ice. It is generally thought to be associated with precipitation of solid salts at certain eutectic temperatures. the variability found in bulk sea-ice samples indicates that the fractionation of ions depends on the often unknown thermal history of sea ice, which affects the structure of pore networks and fate of solid salts within them. Here we investigate the distribution of ions in Arctic sea ice that is a few weeks old with a reconstructible thermal history. We separate the centrifugable (interconnected) and entrapped…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesBiogeochemistryMineralogyFractionation01 natural sciencesArctic ice packOceanographySea ice growth processes13. Climate actionSea iceSeawaterPrecipitationGeology0105 earth and related environmental sciencesEarth-Surface ProcessesEutectic systemAnnals of Glaciology
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Venerid bivalve Venus verrucosa as a high-resolution archive of seawater temperature in the Mediterranean Sea

2021

Abstract High-resolution stable isotope data (δ18O, δ13C) were used to study growth strategies of the bivalve Venus verrucosa collected from three sites of the eastern coast of the Adriatic Sea. The principal objectives of this study were to identify the main growing season and to evaluate the potential applicability of δ18Oshell values to reconstruct the seasonal temperature variability. Calcium carbonate for oxygen and carbon isotope analyses was obtained by drilling the outer shell layer. Temporal and spatial variations in temperature and salinity values at the study sites were simulated using the 3D numerical ocean model ROMS. Annual periodicity of growth patterns was confirmed by δ18Os…

010506 paleontologyδ13Cδ18OStable isotope ratioTemperature salinity diagramsPaleontologyGrowing season010502 geochemistry & geophysicsOceanography01 natural sciencesOceanographyMediterranean seaSeawater14. Life underwaterBayStable isotopes ; Paleotemperature ; Adriatic Sea ; Growth rateEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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How ocean acidification can benefit calcifiers.

2017

Reduction in seawater pH due to rising levels of anthropogenic carbon dioxide (CO2) in the world's oceans is a major force set to shape the future of marine ecosystems and the ecological services they provide [1,2]. In particular, ocean acidification is predicted to have a detrimental effect on the physiology of calcifying organisms [3]. Yet, the indirect effects of ocean acidification on calcifying organisms, which may counter or exacerbate direct effects, is uncertain. Using volcanic CO2 vents, we tested the indirect effects of ocean acidification on a calcifying herbivore (gastropod) within the natural complexity of an ecological system. Contrary to predictions, the abundance of this cal…

0106 biological sciences010504 meteorology & atmospheric sciencesEnvironmental changeOceans and SeasGastropodaVolcanic EruptionsBiology01 natural sciencesGeneral Biochemistry Genetics and Molecular Biologychemistry.chemical_compoundAbundance (ecology)AnimalsMarine ecosystemEcosystemSeawater14. Life underwaterEcosystem0105 earth and related environmental sciencesBiomass (ecology)Biochemistry Genetics and Molecular Biology (all)Primary producersEcology010604 marine biology & hydrobiologyfungiOcean acidificationCarbon DioxideHydrogen-Ion ConcentrationAgricultural and Biological Sciences (all)chemistry13. Climate actionCarbon dioxideCalciumGeneral Agricultural and Biological SciencesAcidsgeographic locationsCurrent biology : CB
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Deciphering carbon sources of mussel shell carbonate under experimental ocean acidification and warming.

2018

Abstract Ocean acidification and warming is widely reported to affect the ability of marine bivalves to calcify, but little is known about the underlying mechanisms. In particular, the response of their calcifying fluid carbonate chemistry to changing seawater carbonate chemistry remains poorly understood. The present study deciphers sources of the dissolved inorganic carbon (DIC) in the calcifying fluid of the blue mussel (Mytilus edulis) reared at two pH (8.1 and 7.7) and temperature (16 and 22 °C) levels for five weeks. Stable carbon isotopic ratios of seawater DIC, mussel soft tissues and shells were measured to determine the relative contribution of seawater DIC and metabolically gener…

0106 biological sciences010504 meteorology & atmospheric sciencesMytilus edulisOceans and SeasCarbonateschemistry.chemical_elementAquatic ScienceOceanography01 natural scienceschemistry.chemical_compoundCalcification Physiologichemic and lymphatic diseasesDissolved organic carbonAnimalsSeawater0105 earth and related environmental sciencesCarbon IsotopesChemistry010604 marine biology & hydrobiologyOcean acidificationGeneral MedicineMusselHydrogen-Ion ConcentrationPollutionIsotopes of carbonEnvironmental chemistryCarbonateSeawaterCarbonBlue musselcirculatory and respiratory physiologyMarine environmental research
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Higher sensitivity towards light stress and ocean acidification in an Arctic sea-ice-associated diatom compared to a pelagic diatom.

2020

Thalassiosira hyalina and Nitzschia frigida are important members of Arctic pelagic and sympagic (sea-ice-associated) diatom communities. We investigated the effects of light stress (shift from 20 to 380 µmol photons m-2  s-1 , resembling upwelling or ice break-up) under contemporary and future pCO2 (400 vs 1000 µatm). The responses in growth, elemental composition, pigmentation and photophysiology were followed over 120 h and are discussed together with underlying gene expression patterns. Stress response and subsequent re-acclimation were efficiently facilitated by T. hyalina, which showed only moderate changes in photophysiology and elemental composition, and thrived under high light aft…

0106 biological sciences010504 meteorology & atmospheric sciencesPhysiologyOceans and SeasPlant Science01 natural sciencesAcclimatizationSeawater14. Life underwater0105 earth and related environmental sciencesDiatomsgeographygeography.geographical_feature_categorybiologyEcologyArctic Regions010604 marine biology & hydrobiologyPelagic zoneOcean acidificationHydrogen-Ion Concentrationbiology.organism_classificationArctic ice packLight intensityDiatomArctic13. Climate actionUpwellingThe New phytologistReferences
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Drivers of shell growth of the bivalve, Callista chione (L. 1758) - Combined it environmental and biological factors

2018

WOS:000426027100014; Seasonal shell growth patterns were analyzed using the stable oxygen and carbon isotope values of live-collected specimens of the bivalve Callista chione from two sites in the Adriatic Sea (Pag and Cetina, Croatia). Micromilling was performed on the shell surface of three shells per site and shell oxygen isotopes of the powder samples were measured. The timing and rate of seasonal shell growth was determined by aligning the delta O-18(shell)-derived temperatures so that the best fit was achieved with the instrumental temperature curve. According to the data, shells grew only at very low rates or not at all during the winter months, i.e., between January and March. Shell…

0106 biological sciences010504 meteorology & atmospheric sciencesmussel mytilus-galloprovincialisCroatiaShell (structure)Oxygen IsotopesAquatic ScienceEnvironmentOceanography01 natural sciencesIsotopes of oxygenChionespisula-solidissimaBiological Factorswater temperatureSclerochronologySeasonal shell growth patternsSclerochronologycontinental-shelfBivalve molluskAnimals14. Life underwaterArctica islandicaparticulate organic-matter0105 earth and related environmental sciencesStable isotopesCarbon IsotopesBivalve mollusk ; Seasonal shell growth patterns ; Stable isotopes ; Sclerochronology ; Environment ; Biology ; Life history traitbiologyStable isotope ratiostable-isotope ratios010604 marine biology & hydrobiologyACLpopulation-dynamicsGeneral Medicineglycymeris-glycymerisLife history traitsbiology.organism_classificationPollutionBivalviaphacosoma-japonicumOceanographyIsotopes of carbonEnvironmental scienceSeawaterarctica-islandica[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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Ocean acidification at a coastal CO2 vent induces expression of stress-related transcripts and transposable elements in the sea anemone Anemonia viri…

2019

Published version, available at: https://doi.org/10.1371/journal.pone.0210358 Ocean acidification threatens to disrupt interactions between organisms throughout marine ecosystems. The diversity of reef-building organisms decreases as seawater CO2 increases along natural gradients, yet soft-bodied animals, such as sea anemones, are often resilient. We sequenced the polyA-enriched transcriptome of adult sea anemone Anemonia viridis and its dinoflagellate symbiont sampled along a natural CO2 gradient in Italy to assess stress levels in these organisms. We found that about 1.4% of the anemone transcripts, but only ~0.5% of the Symbiodinium sp. transcripts were differentially expressed. Processe…

0106 biological sciences0301 basic medicineAtmospheric ScienceMolecular biologyMarine and Aquatic SciencesGene ExpressionRetrotransposonSea anemone01 natural sciencesAnemoniaSequencing techniquesMobile Genetic ElementsMultidisciplinarybiologyQREukaryotaOcean acidificationAnemoneRNA sequencingGenomicsChemistryRetrotransposonsPhysical SciencesMedicineTranscriptome AnalysisResearch ArticleScienceZoology010603 evolutionary biology03 medical and health sciencesGreenhouse GasesCnidariaGenetic ElementsSea WaterGeneticsVDP::Matematikk og Naturvitenskap: 400::Basale biofag: 470Environmental ChemistryAnimalsMarine ecosystemBiology and life sciencesEcology and Environmental SciencesDinoflagellateChemical CompoundsOrganismsTransposable ElementsCorrectionAquatic EnvironmentsComputational BiologyCarbon Dioxidebiology.organism_classificationGenome AnalysisMarine EnvironmentsInvertebratesVDP::Mathematics and natural science: 400::Basic biosciences: 470Research and analysis methods:Genetikk og genomikk: 474 VDP::Marinbiologi:497 VDP::Økologi:488 [VDP]030104 developmental biologySea AnemonesMolecular biology techniquesAtmospheric ChemistryEarth SciencesSeawater
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