Search results for "temperature proxy"

showing 2 items of 2 documents

Morphological variations of crossed-lamellar ultrastructures of Glycymeris bimaculata (Bivalvia) serve as a marine temperature proxy

2020

Abstract Bivalve shells are among the most promising archives for high-resolution seawater temperature reconstructions. However, despite major research advances in bivalve sclerochronology over the past decades, estimating water temperature from shells remains a challenging task. This is largely because the most frequently used and widely accepted temperature proxy in bivalves, i.e., the shell oxygen isotope (δ18Oshell) value, also requires knowledge of changes in δ18O of the water (δ18Owater) in which the bivalve lived, which is rarely available for ancient environments. According to a few recent studies, the size and shape of individual biomineral units (BMUs) of the shell ultrastructure …

0106 biological sciencesGlycymeris010504 meteorology & atmospheric sciencesbiologyBrackish waterδ18O010604 marine biology & hydrobiologyGlycymeris bimaculataAquatic ScienceOceanographybiology.organism_classificationBivalvia01 natural sciencesIsotopes of oxygenOceanography13. Climate actionSclerochronologyPaleoclimatology14. Life underwaterGeology0105 earth and related environmental sciencestemperature proxy ; bivalve sclerochronology ; paleoclimatology ; ultrastructure ; nearshore environment ; Adriatic Sea
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High-resolution records of growth temperature and life history of two Nacella limpet species, Tierra del Fuego, Argentina

2020

Stable isotope ratios in patelloid limpets of the genus Patella have been established as proxies for coastal environmental change at sub-monthly resolution along the eastern North Atlantic and Mediterranean Sea. Nacella deaurata (Gmelin, 1791) and N. magellanica (Gmelin, 1791) are common intertidal species of patelloid limpets inhabiting the coast of Tierra del Fuego, Argentina/Chile and are commonly found in Holocene archaeological deposits. Here, we examine oxygen and carbon isotope ratios (δ18Oshell and δ13Cshell, respectively) of modern specimens of N. deaurata and N. magellanica to test the hypotheses that: 1) they form their shells in isotopic equilibrium with ambient water; and 2) pr…

NacellaHistoria y ArqueologíaIntertidal zoneSCLEROCHRONOLOGYOceanographyArqueologíaCiencias de la Tierra y relacionadas con el Medio AmbienteInvestigación ClimatológicaHUMANIDADESMediterranean seaSclerochronologymedicineSOUTH AMERICAEcology Evolution Behavior and SystematicsHoloceneEarth-Surface ProcessesIsotope analysisbiologyTEMPERATURE PROXYLimpetPaleontologySeasonalitybiology.organism_classificationmedicine.diseaseCLIMATEOceanographyOXYGEN AND STABLE CARBON ISOTOPESSHELL MIDDENSGeologyCIENCIAS NATURALES Y EXACTAS
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