Search results for "Ocean Acidification"

showing 10 items of 135 documents

The influence of high pCO2 on otolith shape, chemical and carbon isotope composition of six coastal fish species in a Mediterranean shallow CO2 vent

2017

Naturally acidified environments, such as CO2 vents, are important sites to evaluate the potential effects of increased ocean acidification on marine ecosystems and biota. Here we assessed the effect of high CO2/low pH on otolith shape and chemical composition of six coastal fish species (Chromis chromis, Coris julis, Diplodus vulgaris, Gobius bucchichi, Sarpa salpa, Symphodus ocellatus) in a Mediterranean shallow CO2 vent. Taking into consideration the major and trace elements found near the vent and the gradient of dissolved inorganic carbon, we compared the otolith chemical signatures of fish exposed long-term to elevated CO2 emissions and reduced pH (mean pH 7.8) against fish living in …

0106 biological sciencesSymphodus ocellatus010504 meteorology & atmospheric sciencesbiologyEcology010604 marine biology & hydrobiologyCoastal fishOcean acidificationAquatic Sciencebiology.organism_classificationChromis chromis01 natural sciencesEcology Evolution Behavior and SystematicOceanographymedicine.anatomical_structureDissolved organic carbonmedicineDiplodus vulgarisChemical compositionEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesOtolith
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Living in a high CO2 world: a global meta-analysis shows multiple trait-mediated fish responses to ocean acidification

2018

International audience; Understanding how marine organisms will be affected by global change is of primary importance to ensure ecosystem functioning and nature contributions to people. This study meets the call for addressing how life‐history traits mediate effects of ocean acidification on fish. We built a database of overall and trait‐mediated responses of teleost fish to future CO2 levels by searching the scientific literature. Using a meta‐analytical approach, we investigated the effects of projected CO2 levels by IPCC for 2050–2070 and 2100 on fish eco‐physiology and behavior from 320 contrasts on 42 species, stemming from polar to tropical regions. Moreover, since organisms may exper…

0106 biological sciencesgrowth[SDE.MCG]Environmental Sciences/Global Changesteleostssurvival010603 evolutionary biology01 natural sciencescalcification14. Life underwaterdevelopment[SDV.BDD]Life Sciences [q-bio]/Development Biologyfish traitsEcology Evolution Behavior and SystematicsteleostbehaviorEcology010604 marine biology & hydrobiologyOcean acidification15. Life on land13. Climate action[SDE]Environmental SciencesTraitEnvironmental scienceFish <Actinopterygii>heterogeneity[SDE.BE]Environmental Sciences/Biodiversity and Ecologyfish traitmetabolismEcological Monographs
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Simplification, not “tropicalization”, of temperate marine ecosystems under ocean warming and acidification

2021

Ocean warming is altering the biogeographical distribution of marine organisms. In the tropics, rising sea surface temperatures are restructuring coral reef communities with sensitive species being lost. At the biogeographical divide between temperate and tropical communities, warming is causing macroalgal forest loss and the spread of tropical corals, fishes and other species, termed “tropicalization”. A lack of field research into the combined effects of warming and ocean acidification means there is a gap in our ability to understand and plan for changes in coastal ecosystems. Here, we focus on the tropicalization trajectory of temperate marine ecosystems becoming coral-dominated systems…

Aquatic Organismsnatural analoguesEffects of global warming on oceanskelp forestswarm-temperateAnimalsEnvironmental ChemistrySeawaterMarine ecosystemEcosystembiogeographyEcosystemGeneral Environmental ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologyCoral ReefsEcologyfungitechnology industry and agricultureMarine habitatsOcean acidificationCoral reefHydrogen-Ion Concentrationbiochemical phenomena metabolism and nutritionrange shiftKelp forestclimate changeHabitat destructionEnvironmental sciencescleractinian coralsgeographic locationsGlobal Change Biology
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Shallow water marine sediment bacterial community shifts along a natural CO2 gradient in the Mediterranean Sea off Vulcano, Italy.

2014

The effects of increasing atmospheric CO2 on ocean ecosystems are a major environmental concern, as rapid shoaling of the carbonate saturation horizon is exposing vast areas of marine sediments to corrosive waters worldwide. Natural CO2 gradients off Vulcano, Italy, have revealed profound ecosystem changes along rocky shore habitats as carbonate saturation levels decrease, but no investigations have yet been made of the sedimentary habitat. Here, we sampled the upper 2 cm of volcanic sand in three zones, ambient (median pCO(2) 419 mu atm, minimum Omega(arag) 3.77), moderately CO2-enriched (median pCO(2) 592 mu atm, minimum Omega(arag) 2.96), and highly CO2-enriched (median pCO(2) 1611 mu at…

Biogeochemical cycleGeologic SedimentsFORAMINIFERAMolecular Sequence DataSoil SciencePolymerase Chain ReactionPH GRADIENTForaminiferaCARBONMediterranean seaRNA Ribosomal 16SMediterranean SeaEcosystemSeawater14. Life underwaterMICROBIAL COMMUNITIESRelative species abundanceEcology Evolution Behavior and SystematicsEcologybiologyBacteriaEcologyOCEAN ACIDIFICATIONSedimentOcean acidificationBiodiversitySequence Analysis DNACORALCarbon DioxideHydrogen-Ion Concentrationbiology.organism_classificationSP NOV.Italy13. Climate actionGenes BacterialECOSYSTEMSeawaterGEN. NOV.TIDAL FLAT SEDIMENTMicrobial ecology
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Evolution and biomineralization of pteropod shells

2021

12 pages; International audience; Shelled pteropods, known as sea butterflies, are a group of small gastropods that spend their entire lives swimming and drifting in the open ocean. They build thin shells of aragonite, a metastable polymorph of calcium carbonate. Pteropod shells have been shown to experience dissolution and reduced thickness with a decrease in pH and therefore represent valuable bioindicators to monitor the impacts of ocean acidification. Over the past decades, several studies have highlighted the striking diversity of shell microstructures in pteropods, with exceptional mechanical properties, but their evolution and future in acidified waters remains uncertain. Here, we re…

Biomineralization0106 biological sciencesGastropodaShell (structure)Structural diversityContext (language use)engineering.material010603 evolutionary biology01 natural sciencesShellsCalcium Carbonate03 medical and health sciencesPaleontologychemistry.chemical_compoundSpecies SpecificityAnimal ShellsStructural BiologyThin shellsAnimalsBiominerals; Pteropods; Mollusc; Shells; Helical microstructure; Aragonite curved fibresSeawater14. Life underwater[SDV.IB.BIO]Life Sciences [q-bio]/Bioengineering/Biomaterials030304 developmental biology0303 health sciencesFossils[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]AragoniteOcean acidificationBiodiversityHydrogen-Ion ConcentrationBiological EvolutionAragonite curved fibresPteropodsCalcium carbonatechemistry13. Climate actionMicroscopy Electron ScanningBiomineralsengineeringHelical microstructureMolluscGeologyBiomineralizationJournal of Structural Biology
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Structural and functional organization of fish assemblages in a Mediterranean shallow CO2 vent.

2017

Gli effetti dell’acidificazione degli oceani a livello globale hanno richiamato l’attenzione degli scienziati su dei sistemi marini naturali quali i vent superficiali di CO₂. Si tratta di mesocosmi naturali, in quanto su piccole scale spaziali (anche di pochi metri) si osservano marcati gradienti di pH, dove poter testare ipotesi ecologiche dell’acidificazione delle acque marine. Obiettivo della tesi è studiare le risposte della popolazione ittica alla riduzione del pH in vent superficiali mediterranei utilizzando numerosi descrittori, quali la struttura di comunità, l’organizzazione trofica, le caratteristiche e la composizione chimica delle strutture carbonatiche. Inoltre poiché i vent so…

CO2 vent Mediterranean fish assemblages species composition trophic structure trophic transfer mercury bioaccumulation otolith chemistry and shape analysis ocean acidification Cymodocea nodosa meadow.
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Biogenic habitat shifts under long-term ocean acidification show nonlinear community responses and unbalanced functions of associated invertebrates

2019

Este artículo contiene 8 páginas, 4 figuras.

CO2 ventsEnvironmental Engineering010504 meteorology & atmospheric sciencesOceans and SeasOceans and SeaSnailsIntertidal zone010501 environmental sciencesEnvironmentsTransplant01 natural sciencesModels BiologicalNonlinear DynamicRocky shoreMediterranean SeaAnimalsEnvironmental ChemistryMarine ecosystemEcosystemSeawaterInvertebratePhase shiftWaste Management and DisposalEcosystem0105 earth and related environmental sciencesSeabiologyEcologyAnimalOcean acidificationCoralline algaeOcean acidificationBiodiversityCarbon Dioxidebiology.organism_classificationInvertebratesPollutionNonlinear DynamicsCarbon dioxideItalySnailBenthic zoneImpactsReefsEnvironmental scienceSpecies richnessCoralCo2 ventsVermetid reef
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Experimental conditions for respiration and growth studies of F0 and F1 larval and juvenile European seabass Dicentrarchus labrax

2022

Water parameters in the 2 years before spawning of F0 (08.02.2016-06.03.2018) and during larval and juvenile phase of F1: Larval period until 17.05.2018 (48 dph, 900 dd) and 01.06.2018 (63 dph, ~900 dd) for warm and cold life condition respectively, for the juveniles until 28.09.2018 (180 dph, ~4000 dd) and 12.02.2019 (319 dph, ~5100 dd) for warm and cold conditioned fish respectively. Means ± s.e. over all replicate tanks per condition. Temperature (Temp.), pH (free scale), salinity, oxygen and total alkalinity (TA) were measured weekly in F1 and monthly in F0; sea water (SW) measurements were conducted in 2017 and 2018. Water parameters during larval and early juvenile phase of F0: Larval…

Calculated by CO2sys_xls_program Lewis and WallaceSalinityAlkalinityLife stageType of studyTemperature waterGermanyCalculatedAlkalinity totalSalinity standard errortotallarval growthteleostexperiment2006pH2007 with purified m cresol purpleOcean acidificationMeasured spectrophotometrically Dickson et alTemperatureWeilheimPartial pressure of carbon dioxide (water) at sea surface temperature (wet air) standard errorSilicatedissolvedLaboratory experimentSEAL AA3 segmented flow autoanalyzerSilicate standard errorstandard errorMultiprobeEarth System ResearchWTW 340imetabolic rateswaterGenerationOxygen dissolvedMultiprobe WTW 340iPhosphateocean warmingAlkalinity total standard errorjuvenile growthCarbon dioxide (water) partial pressurepH meter (WTW 3110) with electrode (WTW Sentix 41)DATE TIMEWTW Oxi 340i probeTemperature water standard errorCarbon dioxide water partial pressurepH standard errorXylem Analytics GermanySalinometer (WTW LF325 Xylem Analytics Germany Weilheim Germany)Calculated by CO2sys_xls_program (Lewis and Wallace 2006)OxygenTreatmentDATE/TIMEPartial pressure of carbon dioxide water at sea surface temperature wet airSalinometer WTW LF325Oxygen dissolved standard errorMeasured spectrophotometrically (Dickson et al. 2007) with purified m-cresol purplepH meter WTW 3110 with electrode WTW Sentix 41Phosphate standard error
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Sicilian CO2 vents show effects of ocean acidification on rocky shores

2011

Carbon dioxide ocean acidification climate change Mediterranean
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Calcification is not the Achilles' heel of cold-water corals in an acidifying ocean

2015

Ocean acidification is thought to be a major threat to coral reefs: laboratory evidence and CO2 seep research has shown adverse effects on many coral species, although a few are resilient. There are concerns that cold-water corals are even more vulnerable as they live in areas where aragonite saturation (?ara) is lower than in the tropics and is falling rapidly due to CO2 emissions. Here, we provide laboratory evidence that net (gross calcification minus dissolution) and gross calcification rates of three common cold-water corals, Caryophyllia smithii, Dendrophyllia cornigera, and Desmophyllum dianthus, are not affected by pCO2 levels expected for 2100 (pCO2 1058 ?atm, ?ara 1.29), and nor a…

CnidariaSettore BIO/07 - EcologiaCaryophyllia smithiiCoralcold-water coralsocean acidificationengineering.materialCaryophyllia smithiiDendrophyllia cornigeraCold-water coralcalcification and dissolutionCalcification PhysiologicAnthozoaTheoryofComputation_ANALYSISOFALGORITHMSANDPROBLEMCOMPLEXITYComputingMethodologies_SYMBOLICANDALGEBRAICMANIPULATIONMediterranean SeaAnimalsEnvironmental ChemistrySeawaterGlobal ChangeReefDesmophyllum dianthuGeneral Environmental ScienceGlobal and Planetary ChangegeographyDesmophyllum dianthusgeography.geographical_feature_categorybiologyEcology2300EcologyAragoniteOcean acidificationfungiCalcification and dissolutionOcean acidificationCoral reefbiochemical phenomena metabolism and nutritionCarbon DioxideHydrogen-Ion Concentrationbiology.organism_classificationAnthozoaOceanographyengineeringCold-water coralsgeographic locationsMathematicsofComputing_DISCRETEMATHEMATICS
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