Search results for "ISOTOPE"

showing 10 items of 2232 documents

Parasite infection alters host stable-isotope composition under controlled feeding

2016

1) Stable isotopes are widely used for studying trophic relationships, but variation driven by environmental conditions or food availability complicates the interpretation of trophic dynamics. Parasites are ubiquitous and known to affect physiological functions of their hosts, but only few studies have assessed the effects of parasites on isotope composition of hosts. 2) We measured the changes in two of the most commonly used stable isotopes in food-web studies, nitrogen (i.e. 15N:14N ratio; denoted as δ15N) and carbon (13C:12C; δ13C) in Daphnia hosts exposed to infection by a parasitic micosporidian in the laboratory. Isotopic signatures of hosts fed a standardised controlled diet were co…

2. Zero hunger0106 biological sciences0301 basic medicinenitrogen isotopesδ13CHost (biology)EcologyStable isotope ratiohost–parasite interactionδ15NAquatic ScienceBiologybiology.organism_classification010603 evolutionary biology01 natural sciencesDaphniaIsotopes of nitrogen03 medical and health sciences030104 developmental biologyfood sourcecarbon isotopesParasite hostingta1181Trophic levelenergy limitationFreshwater Biology
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2020

Strontium isotopes in biogenic apatite, especially enamel, are widely employed to determine provenance and track migration in palaeontology and archaeology. Body tissues record the 87Sr/86Sr of bioavailable Sr of ingested food and water. To identify non-local individuals, knowledge of the 87Sr/86Sr of a non-migratory population is required. However, varying factors such as tissue turnover rates, feeding selectivity, Sr content, digestibility of food, and the ingestion of mineral dust can influence body tissue 87Sr/86Sr. To evaluate the Sr contribution of diet and water to mammalian hard tissues 87Sr/86Sr, controlled feeding studies are necessary. Here we present 87Sr/86Sr from controlled fe…

2. Zero hungereducation.field_of_studyEcologybiologyEnamel paintRodentChemistry010401 analytical chemistryPopulationCavia010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesIsotopes of strontium0104 chemical sciencesBioavailabilityGuinea pigAnimal sciencevisual_artbiology.animalvisual_art.visual_art_mediumIngestioneducationEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesFrontiers in Ecology and Evolution
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Decay of48-50Ar isotopes

2011

International audience; Information on β-decay properties of neutron-rich 84-05Ar was obtained at the ISOLDE mass-separator facility at CERN using isobaric selectivity. This was achieved by a combination of a plasma-ion source with a cooled transfer line and subsequent mass-separation. Normally, argon beams cannot be mass-separated from intense multi-charged symmetric fission krypton and xenon. Several techniques were used successfully in order to overcome this problem. Implication of the obtained information for a better understanding of the origin of the 48Ca/46Ca isotopic anomaly discovered in inclusions from the Allende meteorite is discussed.

23.40.-s 27.40.+zHistoryArgonIsotopeFissionKryptonchemistry.chemical_element[PHYS.NEXP]Physics [physics]/Nuclear Experiment [nucl-ex]Computer Science ApplicationsEducationNuclear physicsXenonAllende meteoritechemistryIsobaric processAnomaly (physics)Atomic physicsNuclear ExperimentJournal of Physics: Conference Series
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Spectroscopic studies of neutron-deficient light nuclei: decay properties of 21Mg, 25Si and 26P

2003

Neutron‐deficient nuclei with Tz equals to −3/2 and −2 have been produced at the GANIL/LISE3 facility in fragmentation reactions of a 95 MeV/u 36Ar primary beam in a 12C target. For the first time, β‐delayed proton and β‐γ emission has been simultaneously observed in the decay of 21Mg, 25Si and 26P. The decay scheme of the latter is proposed and the Gamow‐Teller strength distribution in its β decay is compared to shell‐model calculations based on the USD interaction. The B(GT) values derived from the absolute measurement of the β‐branching ratios are in agreement with the quenching factor of about 60% obtained for allowed Gamow‐Teller transitions in this mass region. A precise half‐life of …

23.50.+z 23.40.-s 23.20.Lv 27.30.+tPhysicsDecay schemeProtonIsotopes of germaniumBranching fractionNuclear Theory[PHYS.NEXP]Physics [physics]/Nuclear Experiment [nucl-ex]7. Clean energyNuclear physicsDouble beta decayNeutronProton emissionAtomic physicsNuclear ExperimentRadioactive decayAIP Conference Proceedings
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Population of lead isotopes in binary reactions using a Rb 94 radioactive beam

2020

8 pags., 9 figs.

3106PopulationNuclear TheoryBinary number[PHYS.NEXP]Physics [physics]/Nuclear Experiment [nucl-ex]01 natural sciences7. Clean energyParticle detectorNuclear physicsnuclear reaction ; transfer reaction ; radioactive beam0103 physical sciencesNuclear ReactionsNeutronNuclear Physics - Experiment010306 general physicseducationNuclear Experimentnuclear reactionsPhysicseducation.field_of_studyisotoopitScience & TechnologyIsotope010308 nuclear & particles physicsPhysicsPhysics NuclearPhysical Sciencestransfer reactionsPhysics::Accelerator Physicslow and intermediate energy heavy-ion reactionslyijymodels nad methods for nuclear reactionsNucleonydinfysiikkaBeam (structure)Radioactive beamPhysical Review C
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Identification of the crossing point at N=21 between normal and intruder configurations

2017

R. Lica et al. -- 6 pags., 3 figs. -- Open Access funded by Creative Commons Atribution Licence 4.0

3106[PHYS.NEXP]Physics [physics]/Nuclear Experiment [nucl-ex]magnesium114 Physical sciences01 natural sciencesREGIONNuclear physics0103 physical sciencesNuclear Physics - Experiment010306 general physicsSpectroscopyPhysicsLarge Hadron ColliderNUCLEISTABILITYIsotopeta114010308 nuclear & particles physicsIsland of inversionaluminiumSHELL CLOSUREisland of inversionMODELISOTOPESbeta decayAtomic physicsGround stateRelative energyPhysical Review C
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Long-term summer temperature variations in the Pyrenees from detrended stable carbon isotopes

2015

Abstract Substantial effort has recently been put into the development of climate reconstructions from tree-ring stable carbon isotopes, though the interpretation of long-term trends retained in such timeseries remains challenging. Here we use detrended δ13C measurements in Pinus uncinata tree-rings, from the Spanish Pyrenees, to reconstruct decadal variations in summer temperature back to the 13th century. The June-August temperature signal of this reconstruction is attributed using decadally as well as annually resolved, 20th century δ13C data. Results indicate that late 20th century warming has not been unique within the context of the past 750 years. Our reconstruction contains greater …

530 PhysicsIsotopes of carbonStable isotope ratioClimatologyGlobal warmingPaleoclimatologyEarth and Planetary Sciences (miscellaneous)DendrochronologyClimate changeContext (language use)Dendroclimatology550 Earth sciences & geologyGeologyGeochronometria
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Combining inorganic and organic carbon stable isotope signatures in the Schwalbenberg Loess-Palaeosol-Sequence near Remagen (Middle Rhine valley, Ger…

2020

Western Central European Loess-Palaeosol-Sequences (LPS) provide valuable terrestrial records of palaeoenvironmental conditions, which formed in response to variability in the North Atlantic climate systems. Over the last full glacial cycle (∼130 ka), climate oscillations within these systems are best documented in deep sea- and ice cores; the responses of terrestrial systems are not yet fully understood. A better understanding of metabolism governing input and output variables of organic- and inorganic C pools is, however, crucial for investigating landscape-atmospheric feedback processes and in particularly, for understanding the formation of calcareous LPS as environmental archives. Here…

550 Earth sciencesSchwalbenberg LPSGeneral Earth and Planetary Sciencesstable isotopeslcsh:Qenvironmental changeOIS 3Loess-Palaeosol-Sequenceslcsh:Science550 Geowissenschaften
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Persistent link between Caribbean precipitation and Atlantic Ocean circulation during the Last Glacial revealed by a speleothem record from Puerto Ri…

2020

The sensitivity of tropical Atlantic precipitation patterns to the mean position of the Intertropical Convergence Zone (ITCZ) at different time scales is well‐known. However, recent research suggests a more complex behavior of the northern hemispheric tropical rain belt related to the ITCZ in the western tropical Atlantic. Here we present a precisely dated speleothem multi‐proxy record from a well‐monitored cave in Puerto Rico, covering the period between 46.2 and 15.3 ka. The stable isotope and trace element records document a pronounced response of regional rainfall to abrupt climatic excursions in the North Atlantic across the Last Glacial such as Heinrich stadials and Dansgaard/Oeschger…

551.7Atmospheric Sciencegeographygeography.geographical_feature_categoryStable isotope ratio550.28Last GlacialspeleothemsOcean currentPaleontologySpeleothemstable isotopesprecipitation reconstructionOceanographyOceanographyHeinrich stadialsPrecipitationGlacial periodGeologyDansgaard/Oeschger cycles
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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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