Search results for "oxygen isotope"

showing 10 items of 58 documents

Data for: High-resolution records of growth temperature and life history of two Nacella limpet species, Tierra del Fuego, Argentina

2019

Excel files containing oxygen and stable carbon isotope data from shell carbonate. The patelloid limpet species, Nacella deaurata and N. magellanica, were collected alive from locations in the Beagle Channel of Tierra del Fuego, Argentina. THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE. TO VIEW A LIST OF FILES AND ACCESS THE FILES IN THIS DATASET CLICK ON THE DOI-LINK ABOVE

Paleoclimate ProxyStable IsotopeOxygen IsotopeInterdisciplinary sciencesOtherCarbon Isotope
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Uniform climate sensitivity in tree-ring stable isotopes across species and sites in a mid-latitude temperate forest.

2014

Tree-ring stable isotopes, providing insight into drought-induced eco-physiological mechanisms, are frequently used to reconstruct past changes in growing season temperature and precipitation. Their climatic response is, however, still not fully understood, particularly for data originating from non-extreme, mid-latitude environments with differing ecological conditions. Here, we assess the response of δ(13)C, δ(18)O and tree-ring width (TRW) from a temperate mountain forest in the Austrian pre-Alps to climate and specific drought events. Variations in stem growth and isotopic composition of Norway spruce, common beech and European larch from dry, medium and moist sites are compared with re…

PhysiologyCloud coverClimateGrowing seasonLarixPlant ScienceForestsOxygen IsotopesAtmospheric sciencesSoilTemperate climateFagusPhotosynthesisPiceaBeechTranspirationCarbon IsotopesbiologyPlant StemsEcologyTemperatureTemperate forestbiology.organism_classificationddc:DroughtsSunlightEnvironmental scienceLarchTemperate rainforestTree physiology
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General Statistical Framework for Quantitative Proteomics by Stable Isotope Labeling

2014

Pedro J. Navarro et al.

ProteomicsSaccharomyces cerevisiae ProteinsProteomeQuantitative proteomicsGene Expressionstable isotope labelingSaccharomyces cerevisiaeyeastOxygen Isotopescomputer.software_genreBiochemistryStatistical powerInterpretation (model theory)statistical analysisStable isotope labeling by amino acids in cell cultureQuantitative proteomicsData MiningModels StatisticalChromatographyChemistryMolecular Sequence AnnotationHydrogen PeroxideGeneral ChemistryVariance (accounting)Isotope LabelingStable Isotope LabelingBiological systemNull hypothesiscomputerData integrationJournal of Proteome Research
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The hyperfine structure in the rotational spectra of D2(17)O and HD(17)O: Confirmation of the absolute nuclear magnetic shielding scale for oxygen

2015

Guided by theoretical predictions, the hyperfine structures of the rotational spectra of mono- and bideuterated-water containing (17)O have been experimentally investigated. To reach sub-Doppler resolution, required to resolve the hyperfine structure due to deuterium quadrupole coupling as well as to spin-rotation (SR) and dipolar spin-spin couplings, the Lamb-dip technique has been employed. The experimental investigation and in particular, the spectral analysis have been supported by high-level quantum-chemical computations employing coupled-cluster techniques and, for the first time, a complete experimental determination of the hyperfine parameters involved was possible. The experimental…

RotationGeneral Physics and AstronomyOxygen Isotopesquantum-chemical calculationParamagnetismrotational spectroscopyPhysics::Atomic PhysicsDeuterium OxidePhysical and Theoretical ChemistryHyperfine structureOxygen-17ChemistrySpectrum AnalysisWaterDeuterium17O NMR shieldinghyperfine parameterModels ChemicalDeuteriumElectromagnetic shieldingQuadrupoleQuantum TheoryDiamagnetismRotational spectroscopyAtomic physicsElectromagnetic PhenomenaLamb-dip technique
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Eclogites and garnet pyroxenites: Similarities and differences

2010

Eclogites and garnet pyroxenites are genetically linked to basaltic precursors. Traditionally garnet pyroxenites are linked to fractionation of basaltic Magmas Over a range of mantle pressures and more recently they have been implicated in the genesis of ocean islands. in contrast eclogites are linked to the subduction of slab basalt and gabbro precursors which may be hydrothermally altered. Recently this subduction paradigm has been questioned. We present mineralogical, trace element and O isotopic data for eclogites and garnet pyroxenites that reveal some similarities but also important chemical and isotopic differences that support a distinct provenance (i.e., age and process). Continent…

SALT-LAKE-CRATERSM-NDGeochemistryResearch Groups and Centres\Earth Sciences\Ancient and Modern Earth SystemsXENOLITHIC ECLOGITESMantle (geology)ONTONG JAVA PLATEAUxenolithsResearch Groups and Centres\Earth Sciences\GeochemistryGeochemistry and PetrologyTRACE-ELEMENTSFaculty of Science\Earth SciencesXenolithHIGH-PRECISIONgarnet pyroxenitesLU-HFWEST-AFRICAPeridotiteBasaltgeographygeography.geographical_feature_categorySOLOMON-ISLANDSGabbrooxygen isotopesmantle eclogitesmineral chemistryCratonIgneous rockGeophysicsEclogiteGeologyKAAPVAAL CRATONJournal of Volcanology and Geothermal Research
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Oxygen isotope and salinity measurements of coastal surface waters in the Gulf of Maine

2020

These data include salinity and oxygen isotope measurements of water samples collected from coastal sites along the Gulf of Maine between 2003 and 2015. In particular, a suite of samples were collected along the coast of Maine, east of Penobscot Bay, on a monthly basis between April 2014 and March 2015. These data also include several freshwater samples collected from the Kennebec and Penobscot Rivers on a semi-monthly basis in 2014 and 2015. For the water samples with sample IDs starting with DSW, JSW, NSW, or OSW: The water samples were collected by hand from shore or boat using French square glass bottles with phenolic polycone lined caps. Salinity was measured using a Oakton SALT 6+ han…

SalinityGulf of MainewaterCommentWater sampleδ18O waterReference of dataDATE/TIMESample IDOxygen isotopesDATE TIMEEarth System ResearchLATITUDEYear of observationδ18OLONGITUDE
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The Postglacial Isotopic Record of Intermediate Water Connects Mediterranean Sapropels and Organic‐Rich Layers

2020

Carbon‐rich layers exist at both sides of the Mediterranean Sea sedimentary record and are called sapropels and organic rich layers (ORLs), respectively, in the eastern and western basins. They have different levels of organic carbon accumulation and seafloor oxygen deprivation. The most recent sapropel and ORL depositions have a different timing, approximately 10.8–6.1 and 14.5–9.0 ka, respectively. Here we investigate oxygen isotopic records of three foraminifera species that occupy different habitats within the Sicily Channel water column since ~12.0 ka, thus in the sill between the eastern and western Mediterranean basins. These data are ice volume corrected, to get information on water…

Sapropel Organic rich layerMediterranean climateAtmospheric Sciencecarbon isotope010504 meteorology & atmospheric sciencesGeochemistryPaleontology15. Life on land010502 geochemistry & geophysicsOceanography01 natural sciences13. Climate actionLIWoxygen isotope14. Life underwaterGeology0105 earth and related environmental sciencesPaleoceanography and Paleoclimatology
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Selective oxidative dehydrogenation of ethane over SnO2-promoted NiO catalysts

2012

[EN] Ni-Sn-O mixed oxides catalysts have been investigated for the oxidative dehydrogenation of ethane. The catalysts were prepared through the evaporation of aqueous solutions of nickel nitrate and tin oxalate and finally calcined in air at 500 degrees C for 2 h. These materials have been characterized by several techniques (N-2-adsorption, X-ray diffraction, High-Resolution Electron Microscopy, temperature programmed reduction, X-Ray Photoelectron Spectroscopy, Fourier Transformed Infrared Spectroscopy of adsorbed CO and O-18/O-16 isotope exchange). The addition of just a tiny amount of tin highly increases the selectivity to ethylene (from ca. 40% to 80-90%). Thus, high selectivity to et…

SnO2-promotedInorganic chemistrychemistry.chemical_elementInfrared spectroscopyTin oxideCatalysisOxalateCatalysisEthane ODHNiO catalystsEthane oxidationchemistry.chemical_compoundNickelEthyleneTin oxidechemistryDehydrogenationPhysical and Theoretical ChemistryTemperature-programmed reductionTinOxidative dehydrogenation of ethaneNickel oxideCatalyst characterization (XPS HREM oxygen isotope exchange FTIR CO adsorbed)
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Growth patterns of the topshell Phorcus lineatus (da Costa, 1778) in northern Iberia deduced from shell sclerochronology

2019

Combined shell growth pattern and oxygen isotope analysis has become a powerful approach in palaeoclimate and archaeological studies for reconstructing palaeoclimate conditions and littoral exploitation patterns, respectively. Recent investigations have shown that the gastropod Phorcus lineatus (da Costa, 1778) forms its shell in conditions of near equilibrium with the oxygen isotope signature of the seawater environment, demonstrating the utility of this species for reconstruction of sea surface temperature and determination of the season of harvest in archaeological studies. In contrast, the shell growth patterns of this species have received virtually no attention despite providing infor…

Subfossil010504 meteorology & atmospheric sciencesbiologyGrowth patternsGeology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesIsotopes of oxygenShellsSea surface temperatureOceanographySclerochronologyArchaeologyGeochemistry and PetrologySclerochronologyPhorcus lineatusLittoral zoneSeawaterGrowth rateStable oxygen isotopesPhorcus lineatusGeology0105 earth and related environmental sciencesPalaeoenvironmental reconstruction
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A 5500-year oxygen isotope record of high arctic environmental change from southern Spitsbergen

2017

The oxygen isotope composition of chironomid head capsules in a sediment core spanning the past 5500 years from Lake Svartvatnet in southern Spitsbergen was used to reconstruct the oxygen isotope composition of lake water (δ18Olw) and local precipitation. The δ18Olw values display shifts from the baseline variability consistent with the timing of recognized historical climatic episodes, such as the Roman Warm Period, the Dark Ages Cold Period and the ‘Little Ice Age’. The highest values of the record, ca. 3‰ above modern δ18Olw values, occur at ca. 1900–1800 cal. yr BP. Three negative excursions increasing in intensity toward the present, at 3400–3200, 1250–1100, and 350–50 cal. yr BP, are…

TEMPERATURE VARIABILITY1171 GeosciencesSpitsbergen010506 paleontologyArcheology010504 meteorology & atmospheric sciencesEnvironmental change"Little Ice Age'NORTH-ATLANTIC CLIMATE01 natural sciencesIsotopes of oxygenSVALBARD ICE CORESvalbardArcticSea iceEAST GREENLAND CURRENTPrecipitationRoman Warm Periodclimate0105 earth and related environmental sciencesEarth-Surface Processes‘Little Ice Age’Global and Planetary ChangegeographyHOLOCENE GLACIER FLUCTUATIONSgeography.geographical_feature_categoryEcologyLATE-PLEISTOCENEoxygen isotopesBaseline (sea)LAKE-WATER DELTA-O-18North AtlanticPaleontologytemperatureGlacierPALEOCLIMATE RECONSTRUCTIONOceanographyArctic13. Climate actionta1181SEA-ICEGeologyHIGH-RESOLUTIONHolocene
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