Search results for "Aragonite"

showing 10 items of 90 documents

Ca-rich carbonates associated with ultrabasic-ultramafic melts. Carbonatite or limestone xenoliths? A case study from the late Miocene Morron de Vill…

2016

The volcanic products of the late Miocene Morron de Villamayor volcano (Calatrava Volcanic Field, central Spain) are known for being one of the few outcrops of leucitites in the entire circum-Mediterranean area. These rocks are important because aragonite of mantle origin has been reported as inclusion in olivine macrocrysts. We use petrographic observations, mineral compositions, as well as oxygen and carbon isotope ratios coupled with experimental petrology to understand the origin of carbonate phase in these olivine-phyric rocks. Groundmass and macrocryst olivines range from δ18OVSMOW of +4.8‰, typical of mantle olivine values, to +7.4‰, indicating contamination by sedimentary carbonate.…

alkali basalts010504 meteorology & atmospheric sciencesGeochemistrySkarnMediterraneanengineering.material010502 geochemistry & geophysics01 natural sciencespetrologygeochemistry; petrology; carbonate; carbonatite; olivine; mantle; alkaline; Spain; Cenozoic; MagmatismPetrographychemistry.chemical_compoundcarbonateGeochemistry and PetrologyUltramafic rockolivineNeogene volcanism0105 earth and related environmental sciencesgeochemistryPeridotiteOlivineCenozoicAragoniteMagmatismcarbonatitechemistry13. Climate actionSpainCarbonatiteengineeringCarbonatealkalineGeologymantle
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Tarbellastraea (Scleractinia): A new stable isotope archive for Late Miocene paleoenvironments in the Mediterranean

2008

Abstract Geochemical proxy records of sea surface temperature (SST) or sea surface salinity (SSS) variability on intra- and interannual time-scales in corals from geological periods older than Pleistocene are extremely rare due to pervasive diagenetic alteration of coralline aragonite. Very recently, however, stable isotope data (δ18O, δ13C) from specimens of Porites of Late Miocene age (10 Ma) have been shown to preserve original environmental signatures. In this paper we describe new finds of the zooxanthellate corals Porites and Tarbellastraea in exceptional aragonite preservation from the island of Crete in sediments of Tortonian (∼ 9 Ma) and Early Messinian (∼ 7 Ma) age. Systematic, co…

biologyδ18OAragonitePoritesPaleontologyScleractiniaengineering.materialLate MioceneOceanographybiology.organism_classificationSea surface temperaturePaleontologyOceanographySclerochronologyPaleoclimatologyengineeringEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Designed peptides for biomineral polymorph recognition: a case study for calcium carbonate

2020

With their unique ability for substrate recognition and their sequence-specific self-assembly properties, peptides play an important role in controlling the mineralization of inorganic materials in natural systems and in controlling the assembly of soft materials into complex structures required for biological functions. Here we report the use of an engineered heptapeptide that can differentiate between the crystalline anhydrous polymorphs of calcium carbonate. This peptide contains the positively charged amino acid arginine as well as proline rather than the prototypical negatively charged aspartate or glutamate units. Its affinity to vaterite compared to aragonite was demonstrated by fluo…

chemistry.chemical_classificationCalciteArginineStereochemistryAragoniteBiomedical EngineeringPeptideGeneral ChemistryGeneral Medicineengineering.materialAmino acidchemistry.chemical_compoundCrystallographyCalcium carbonatechemistryVateriteengineeringGeneral Materials ScienceProlineJ. Mater. Chem. B
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Observaciones sobre algunos caracteres de valor taxonómico en el grupo de los carófitos

1990

The variability of the microstructurals characters and mineralogical composition of the oogonia of some charophytes extant and fossils is described. Two types of microstructures (W & V) are find. These are conservative into populations and are not able to change by the environmental factors. Moreover, these structures are quite constant in some of the phylogenetics groups studied. Consequently it is proposed its utilization in taxonomy. The apparition of original compounds in the Charophyta (vaterite. whewelite, aragonite, etc.) is important because it supports an old idea that considerates the Charophyta as an autonomous class between the Clorophyta and the Traqueophyta.<br><b…

evoluciónQH301-705.5Plant ScienceBiologyengineering.materialtaxonomíaMineralogical compositionmineralogical compositiontaxonomyExtant taxonPhylogeneticsVateritelcsh:BotanyBotanyevolutionBiology (General)Charophytalcsh:QH301-705.5microestructuraAragonitecomposición mineralógicaBotanybiology.organism_classificationCharophyteslcsh:QK1-989lcsh:Biology (General)QK1-989microstructurescarófitosengineeringTaxonomy (biology)Collectanea Botanica
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Electron Spin Resonance and Thermoluminescence dating of shells and sediments from Sambaqui (shell mound) Santa Marta II, Brazil

2020

In Tupi, the word Sambaqui means “mound of shells”. These archaeological sites are cultural vestiges left by the prehistoric occupation of the Brazilian coast from five to six thousand years ago. Mollusks, fishes, and other marine edible foods were important for the survival of this population. The remains of foods, mainly shells, were heaped up, giving a mound of different proportions, which became part of the landscape of the Brazilian coastal plain. Due to the large number of Sambaquis in Brazil and considering that Sambaqui Santa Marta II, Laguna, SC, has not yet been dated, Electron Spin Resonance (ESR) measurements were performed in aragonite shells collected from different layers of …

geographyeducation.field_of_studygeography.geographical_feature_categoryThermoluminescence datingCoastal plainTLSettore ING-IND/20 - Misure E Strumentazione NucleariAragonitePopulationGeneral Medicineengineering.materialArchaeologySettore FIS/07 - Fisica Applicata(Beni Culturali Ambientali Biol.e Medicin)law.inventionPrehistorylawengineeringShellSedimentRadiocarbon datingDatingeducationGeologyAccelerator mass spectrometryESR
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Moroccan speleothem and tree ring records suggest a variable positive state of the North Atlantic Oscillation during the Medieval Warm Period

2013

We present a magnesium (Mg) and strontium (Sr) record from an aragonitic speleothem (Grotte de Piste, Morocco, 34‬°N; 04°W) providing a reconstruction of effective rainfall from 619 to 1962 AD. The corresponding drip site was monitored over 2 yr for drip water Mg/Ca and Sr/Ca ratios. Results show evidence for prior aragonite precipitation, which can explain negative correlations between speleothem Mg and Sr concentrations. The data shown here have important climate implications concerning the evolution of the North Atlantic Oscillation (NAO). A comparison of the stalagmite data from Grotte de Piste with an updated tree ring based drought reconstruction from Morocco and other NAO related pro…

geographygeography.geographical_feature_categoryAragonitePisteSpeleothemStalagmiteengineering.materialGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyPeninsulaNorth Atlantic oscillationClimatologyEarth and Planetary Sciences (miscellaneous)DendrochronologyengineeringPrecipitationGeologyEarth and Planetary Science Letters
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LA-ICP-MS analyses on coral growth increments reveal heavy winter rain in the Eastern Mediterranean at 9 Ma

2009

Abstract Sediment particles incorporated into coral skeletons reflect variation in composition and amount of suspended material in ambient water during coral growth. They can be used to identify periods of enhanced storm frequency and associated freshwater discharge. Tortonian (Late Miocene) Porites corals from Crete (Aegean Sea, Eastern Mediterranean) show pronounced annual density bands in X-ray photographs. δ18O compositional variability reflects the annual banding equivalent with a ~ 7 °C annual sea surface temperature (SST) cycle over a seven-year period. Fine sediment particles are concentrated in layers with skeletal porosity parallel to growth increments. Variations in the chemical …

geographygeography.geographical_feature_categoryCoralAragoniteTrace elementPaleontologySedimentLate MioceneMineral dustengineering.materialOceanographyOceanographyErosionengineeringReefEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Nutrients attenuate the negative effect of ocean acidification on reef coral calcification in the Arabian Sea upwelling zone (Masirah Island, Oman)

2021

Tropical shallow-water reefs are the most diverse ecosystem in the ocean. Its persistence rests upon adequate calcification rates of the reef building biota, such as reef corals. Optimum calcification rates of reef corals occur in oligotrophic environments with high seawater saturation states of aragonite (Ωsw), which leads to increased vulnerability to anthropogenic ocean acidification and eutrophication. The calcification response of reef corals to this changing environment is largely unknown, however. Here, we present annually and sub-annually resolved records of calcification rates (n = 3) of the coral Porites from the nutrient rich and low Ωsw Arabian Sea upwe…

geographygeography.geographical_feature_categorybiologyCoralAragonitePoritesfungitechnology industry and agricultureOcean acidificationengineering.materialbiochemical phenomena metabolism and nutritionbiology.organism_classificationOceanographyengineeringpopulation characteristicsEnvironmental scienceUpwellingEcosystemEutrophicationReefgeographic locations
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Stable carbon and oxygen isotope fractionation in bivalve (Placopecten magellanicus) larval aragonite

2008

Abstract The relationship between stable isotope composition (δ13C and δ18O) in seawater and in larval shell aragonite of the sea scallop, Placopecten magellanicus, was investigated in a controlled experiment to determine whether isotopes in larval shell aragonite can be used as a reliable proxy for environmental conditions. The linear relationship between δ13CDIC and δ13Caragonite (r2 = 0.97, p  δ 13 C DIC = 1.15 ( ± 0.05 ) ∗ δ 13 C aragonite - 0.85 ( ± 0.04 ) The relationship between δ13CDIC and δ13Caragonite described for P. magellanicus resulted in larval shell aragonite that was depleted on average by 1.82‰ (SD = 0.22‰, range = 1.1–2.1‰) from predicted equilibrium values based on the r…

δ13CIsotopebiologyChemistryStable isotope ratioAragonitefungiOxygen isotope ratio cycleengineering.materialbiology.organism_classificationIsotopes of oxygenPlacopecten magellanicusOceanographyGeochemistry and PetrologyEnvironmental chemistryengineeringSeawaterGeochimica et Cosmochimica Acta
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Variation in Sr uptake in the shell of the freshwater gastropod Bithynia tentaculata from Lake Arreo (northern Spain) and culture experiments

2010

The Sr uptake features in Bithynia tentaculata aragonite shells from monthly collections in Lake Arreo (northern Spain) over a two-year period are compared with those from the same species grown in culture experiments with similar waters under controlled temperature. The shell aragonite of B. tentaculata from Lake Arreo formed in isotopic equilibrium with the lake water. A comparison of the stable oxygen isotope values (δ18O) from the shells and waters allowed the selection of suitable shells for Sr uptake studies. The Sr/Ca molar ratio in B. tentaculata shells (Sr/Cashell) from the lake and from the culture experiments positively correlate with some chemical parameters like conductivity an…

δ18Ochemistry.chemical_elementMineralogyengineering.materialOceanographyIsotopes of oxygenBithynia tentaculataMollusk shellEcology Evolution Behavior and SystematicsEarth-Surface ProcessesStrontiumbiologyStable isotope ratioAragoniteTrace elementPaleontologyTentaculatabiology.organism_classificationOxygen isotopeAragonitechemistryStrontiumEnvironmental chemistryengineeringTrace elementGeology
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