Search results for "carbonates"

showing 10 items of 100 documents

A Cretaceous carbonate escarpment from Western Sicily (Italy): biostratigraphy and tectono-sedimentary evolution

2020

Abstract The presence of a huge carbonate slope of Cretaceous age is recorded in some imbricated thrust sheets from the Maghrebian fold-and-thrust belt cropping out in northwesternmost Sicily (southern Italy). The sedimentological features of this escarpment, named as the Western Sicily Cretaceous Escarpment (WSCE), have been recently described. The present paper aims to provide a detailed bio-chronostratigraphic characterization of the different facies types that occur in the four lithostratigraphic units spanning the whole slope depositional system. The detailed biostratigraphic analysis and correlation of a number of well-exposed sections allowed to differentiate eight informal biozones …

010506 paleontologygeographygeography.geographical_feature_categoryAptianbiologyCarbonate platformPaleontologyEscarpment010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousSedimentary depositional environmentchemistry.chemical_compoundPaleontologychemistryRudistsCretaceous Slope Biostratigraphy Rudists Tectonics CarbonatesCarbonateCenomanianGeology0105 earth and related environmental sciences
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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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Impact of high pCO2 on shell structure of the bivalve Cerastoderma edule

2016

Raised atmospheric emissions of carbon dioxide (CO2) result in an increased ocean pCO2 level and decreased carbonate saturation state. Ocean acidification potentially represents a major threat to calcifying organisms, specifically mollusks. The present study focuses on the impact of elevated pCO2 on shell microstructural and mechanical properties of the bivalve Cerastoderma edule. The mollusks were collected from the Baltic Sea and kept in flow-through systems at six different pCO2 levels from 900 μatm (control) to 24,400 μatm. Extreme pCO2 levels were used to determine the effects of potential leaks from the carbon capture and sequestration sites where CO2 is stored in sub-seabed geologica…

0106 biological sciencesCerastoderma edule010504 meteorology & atmospheric sciencesCarbonatesShell (structure)MineralogyAquatic ScienceOceanography01 natural scienceschemistry.chemical_compoundAnimal ShellsMollusc shellAnimalsSeawaterCardiidae0105 earth and related environmental sciencesbiology010604 marine biology & hydrobiologyOcean acidificationGeneral MedicineCarbon DioxideHydrogen-Ion Concentrationbiology.organism_classificationPollutionchemistryCarbon dioxideCarbonateSeawaterNorth SeaSaturation (chemistry)Environmental MonitoringMarine Environmental Research
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Ocean Acidification and the Loss of Phenolic Substances in Marine Plants

2012

Rising atmospheric CO(2) often triggers the production of plant phenolics, including many that serve as herbivore deterrents, digestion reducers, antimicrobials, or ultraviolet sunscreens. Such responses are predicted by popular models of plant defense, especially resource availability models which link carbon availability to phenolic biosynthesis. CO(2) availability is also increasing in the oceans, where anthropogenic emissions cause ocean acidification, decreasing seawater pH and shifting the carbonate system towards further CO(2) enrichment. Such conditions tend to increase seagrass productivity but may also increase rates of grazing on these marine plants. Here we show that high CO(2) …

0106 biological sciencesCymodocea nodosaved/biology.organism_classification_rank.speciesCarbonatesSecondary MetabolismMarine and Aquatic Scienceslcsh:MedicinePlant Science01 natural scienceschemistry.chemical_compoundGlobal Change Ecologylcsh:SciencePhysiological EcologyMultidisciplinaryAlismatalesbiologyEcologyEcologyPlant BiochemistryMarine EcologyOcean acidificationPotamogetonaceaeHydrogen-Ion ConcentrationSeagrassProductivity (ecology)ItalyCarbon dioxideCoastal EcologyResearch ArticleOceans and SeasMarine Biology010603 evolutionary biologyStatistics NonparametricHydrothermal VentsPhenolsPlant-Environment InteractionsTerrestrial plantSeawater14. Life underwaterocean acidification climate change mediterranean sea seagrassBiologyAnalysis of VarianceChemical EcologyMarylandved/biology010604 marine biology & hydrobiologyPlant Ecologyfungilcsh:R15. Life on landCarbon Dioxidebiology.organism_classificationSalinitychemistry13. Climate actionEarth Scienceslcsh:QRuppia maritima
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Geochemical survey of Levante Bay, Vulcano Island (Italy), a natural laboratory for the study of ocean acidification

2013

Abstract Shallow submarine gas vents in Levante Bay, Vulcano Island (Italy), emit around 3.6t CO2 per day providing a natural laboratory for the study of biogeochemical processes related to seabed CO2 leaks and ocean acidification. The main physico-chemical parameters (T, pH and Eh) were measured at more than 70 stations with 40 seawater samples were collected for chemical analyses. The main gas vent area had high concentrations of dissolved hydrothermal gases, low pH and negative redox values all of which returned to normal seawater values at distances of about 400 m from the main vents. Much of the bay around the vents is corrosive to calcium carbonate; the north shore has a gradient in s…

0106 biological sciencesSettore BIO/07 - EcologiaBiogeochemical cycle010504 meteorology & atmospheric sciencesCarbonatesAquatic ScienceOceanography01 natural sciencesCalcium CarbonateMarine geochemistrychemistry.chemical_compoundCarbon capture and storageSeawater14. Life underwaterSeabed0105 earth and related environmental sciences010604 marine biology & hydrobiologyCarbonate saturation stateOcean acidificationOcean acidificationCarbon DioxidePollutionSettore GEO/08 - Geochimica E VulcanologiaVolcanic ventsOceanographyCalcium carbonatechemistryBaysItaly13. Climate actionCarbon dioxideCarbonateSeawaterBayGeologyWater Pollutants ChemicalEnvironmental MonitoringMarine Pollution Bulletin
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Specifications for carbonate content quantification in recent marine sediments using Rock-Eval pyrolysis

2019

11 pages; International audience; The amount of CaCO3 in sediments and/or sedimentary rocks is usually measured by calcimetry while the nature of the carbonates is determined by X-ray diffraction. Recently, a carbonate recognition method based on the results of Rock-Eval pyrolysis was proposed in 2014 by Pillot et al. [1]. Rock-Eval pyrolysis is also widely used for the characterization of recent sediments. However, later in 2015 Baudin et al. [2] noticed that some of the characteristics of recent sediments tended to produce different results from those of more classical Rock-Eval analyses, causing bias in interpretations.In this study, the thermal stability of fossil and recent marine carb…

020209 energyGeochemistrySalt (chemistry)Mineralogy[SDU.STU]Sciences of the Universe [physics]/Earth Sciences02 engineering and technologyAnalytical Chemistrychemistry.chemical_compound020401 chemical engineering[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry0202 electrical engineering electronic engineering information engineeringRecent sedimentsAcid attack0204 chemical engineeringChemical decompositionComputingMilieux_MISCELLANEOUSTotal organic carbonchemistry.chemical_classificationCalciteRock-EvalSedimentCarbonates decompositionFuel Technologychemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateSedimentary rockRock evalClay mineralsPyrolysisGeologyPyrolysis
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A New Niche for Anoxygenic Phototrophs as Endoliths

2018

ABSTRACT Anoxygenic phototrophic bacteria (APBs) occur in a wide range of aquatic habitats, from hot springs to freshwater lakes and intertidal microbial mats. Here, we report the discovery of a novel niche for APBs: endoliths within marine littoral carbonates. In a study of 40 locations around Isla de Mona, Puerto Rico, and Menorca, Spain, 16S rRNA high-throughput sequencing of endolithic community DNA revealed the presence of abundant phylotypes potentially belonging to well-known APB clades. An ad hoc phylogenetic classification of these sequences enabled us to refine the assignments more stringently. Even then, all locations contained such putative APBs, often reaching a significant pro…

0301 basic medicineChloroflexi (phylum)030106 microbiologyCarbonatesFresh WaterCyanobacteriaApplied Microbiology and BiotechnologyMicrobial Ecology03 medical and health sciencescarbonateBacteria AnaerobicAlgaemicrobiomesBacterial ProteinsPhylogenetics[ SDV.MP ] Life Sciences [q-bio]/Microbiology and ParasitologyChlorophytaRNA Ribosomal 16SMicrobial matAnaerobiosisintertidalPhotosynthesisBacteriochlorophyllsPhylogenygeographygeography.geographical_feature_categoryEcologybiologyPhototrophEcologybioerosionCoral ReefsMicrobiotaBioerosionCoral reefChloroflexibiology.organism_classification[ SDV.IB.BIO ] Life Sciences [q-bio]/Bioengineering/BiomaterialsAnoxygenic photosynthesisPhototrophic ProcessesFood ScienceBiotechnology
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Thermomineral waters of Greece: geochemical characterization

2020

75 °C). In terms of pH most results vary from 5.5 to 823 °C) ii) warm (23 40 °C) iii) thermal (40 75 °C) and iv) hyperthermal (&gtfew springs show either very low pH (&lt10) proposing serpentinization processes. Regarding TDS concentrations collected waters can be subdivided into low salinity (up to 1.5 g/L) brackish (up to 20 g/L) and saline (up to 43 g/L). The medium high salinities can be justified by mixing with sea water and/or strong waterrock interaction processes. Isotope composition of O and H ranges from 12.7 to +2.7 ‰ SMOW and from 91 to +12 ‰ SMOW respectively and is generally comprised between the Global Meteoric Water Line and the East Mediterranean Meteoric Water Line. Only few water samples show a positive shift for δ18O possibly related to high temperature waterrock interaction processes. Carbon dioxide (18 997000 μmol/mol) or N2 (1100 989000 μmol/mol) or CH4 (&ltMany geothermal areas of Greece are located in regions affected by Miocene or Quaternary volcanism and in continental basins characterised by elevated heat flow. Moreover the majority of them is found along the coast as well as in islands of the Aegean Sea and thus thermal water is often brackish to saline due to marine intrusion into costal aquifer. In the present study almost 300 thermal and cold mineral water samples were collected along the Hellenic territory with their physicochemical parameters (temperature pH electrical conductivity and Eh) and the amount of bicarbonates (titration with 0.1N HCl) being determined in situ. Additionally gases found either in free or dissolved phase were sampled. Both water and gas samples were analysed at the INGVPa laboratories for major ions (Ion Chromatography) silica (Inductively Coupled Plasma Optical Emission Spectrometry) chemical composition of free and dissolved gases (Gas Chromatography) water isotopes (O and H) and carbon and helium isotopes of free and dissolved gases (Mass Spectrometry). The temperature of the investigated waters ranges from 6.5 to 98°C pH from 1.96 to 11.98 whilst Total Dissolved Solids (TDS) from 0.06 to 43 g/L. Based on the temperature parameter waters can be divided into four groups: i) cold (&lt0.5 913000 μmol/mol) are the prevailing gas species found in the studied sites. The δ13CCO2 values ranged from 20.1 to +8.5 ‰ whilst the isotope ratio of He from 0.21 to 6.71 R/RA.4) suggesting interaction with H2Srich gases or very high pH values (&gtSettore GEO/08 - Geochimica E Vulcanologia
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Dependence of plasma pH on oxygen saturation

1969

Abstract The influence of haemoglobin oxygenation on the pH value of the blood plasma of healthy adolescents was investigated at 38°C by varying the parameters CO2 pressure, Hb concentration and buffer bases. A total of 5000 measurements gave the following results: 1. 1. The pHs difference between oxygenated and deoxygenated blood increases with diminishing CO2 pressure and with increasing Hb concentration. There is a linear relation between the pHs changes and the O2 saturation of the haemoglobin. 2. 2. Quantitatively these relationships can be expressed by the following equation: δpHs = (8 − pH ox − log 0.03 Pco 2 ) · [Hb] 225 · (100 − So 2 100 where ΔpHs is the pHs difference between par…

Acid-Base EquilibriumPulmonary and Respiratory MedicineAdolescentPhysiologyChemistryPartial PressureAnalytical chemistryOxygenationVenous bloodPlasmaBuffersCarbon DioxideHydrogen-Ion ConcentrationOxygenBicarbonatesHemoglobinsBloodBiochemistryBlood plasmaLinear relationHumansBase excessOxygen saturationBlood phRespiration Physiology
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Unstimulated salivary flow rate, pH and buffer capacity of saliva in healthy volunteers

2004

Objectives: To assess the salivary flow rate, pH, and buffer capacity of healthy volunteers, and their relationships with age, gender, obesity, smoking, and alcohol consumption, and to establish the lower-end value of normal salivary flow (oligosialia). Methods: A prospective study was conducted in 159 healthy volunteers (age > 18 years, absence of medical conditions that could decrease salivary flow). Unstimulated whole saliva was collected during ten minutes, and salivary flow rate (ml/min), pH, and bicarbonate concentration (mmol/l) were measured using a Radiometer ABL 520. The 5 percentile of salivary flow rate and bicarbonate concentration was considered the lower limit of normality. R…

AdultMaleSalivamedicine.medical_specialtyAdolescentBicarbonateSecretory RateSalivary buffer capacityBufferschemistry.chemical_compoundSex FactorsOligosialiaInternal medicineSalivary flow rateHealthy volunteersmedicineHumansProspective StudiesWhole salivaSalivaProspective cohort studyAgedbusiness.industryAge FactorsGastroenterologyGeneral MedicineHydrogen-Ion ConcentrationMiddle AgedSalivary flow rateBicarbonatesEndocrinologychemistryFemaleSalivationSecretory RatebusinessAlcohol consumptionRevista Española de Enfermedades Digestivas
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