Search results for "δ13C"

showing 10 items of 109 documents

Low-frequency noise inδ13C andδ18O tree ring data: A case study ofPinus uncinatain the Spanish Pyrenees

2010

[1] Isotopic discrimination measurements in tree rings are becoming increasingly important estimators of past environmental change. Potential biases inherent to these parameters, including age trend and level offset are, however, not well understood. We here perform measurements on a new millennium-long data set of decadally resolved δ18O and δ13C discrimination from 25 high-elevation pine trees in the Spanish Pyrenees to investigate whether such low-frequency biases exist and how they alter the long-term behavior of derived time series. Alignment of the tree ring data by biological age reveals age trends over the first one to four centuries after germination. On average, isotope values cha…

Atmospheric ScienceGlobal and Planetary ChangeSeries (stratigraphy)Environmental changeδ13Cδ18OStable isotope ratioEcologyEstimatorDendrochronologyEnvironmental ChemistryPhysical geographyTree (set theory)General Environmental ScienceMathematicsGlobal Biogeochemical Cycles
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Sources, degassing, and contamination of CO2, H2O, He, Ne, and Ar in basaltic glasses from Kolbeinsey Ridge, North Atlantic

2005

Abstract New volatile data (CO2, H2O, He, Ne, and Ar) are presented for 24 submarine basaltic glasses from the Kolbeinsey Ridge, Tjornes Fracture Zone and Mohns Ridge, North Atlantic. Low CO2 and He contents indicate that magmas were strongly outgassed with the extent of degassing increasing toward the south, as expected from shallower ridge depths. Ne and Ar are significantly more abundant in the southernmost glasses than predicted for degassed melt. The strong atmospheric isotopic signal associated with this excess Ne and Ar suggests syn- or posteruptive contamination by air. Degassing, by itself, cannot generate the large variations in δ13C values of dissolved CO2 or coupled CO2-Ar varia…

Basaltδ13CGeochemistry and PetrologyHomogeneousGeochemistryFracture zoneContaminationGeologyMantle (geology)Geochimica et Cosmochimica Acta
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Sexes in gynodioeciousGeranium sylvaticumdo not differ in their isotopic signature or photosynthetic capacity

2017

• In gynodioecious plants, females are expected to produce more or better seeds than hermaphrodites in order to be maintained within the same population. Even though rarely measured, higher seed production can be achieved through differences in physiology. • In this work, we measured sexual dimorphism in several physiological traits in the gynodioecious plant Geranium sylvaticum. Photosynthetic rate, stomatal conductivity, transpiration rate, water use efficiency and isotopic signatures were measured in plants growing in two habitats differing in light availability. • Females have been reported to produce more seeds than hermaphrodites. However, we did not observe any significant difference…

C240 Plant Cell Science0106 biological sciencesLightGeraniumPopulationFlowersmetsäkurjenpolviPlant ScienceGynodioecy010603 evolutionary biology01 natural sciencesGeranium sylvaticumBotanyC750 Plant Biochemistrygynodioecyisotopic signaturesWater-use efficiencyeducationEcology Evolution Behavior and SystematicsTranspirationSex Characteristicseducation.field_of_studyphotosynthesisbiologyδ13CReproductionfood and beveragesPlant TranspirationGeneral Medicinebiology.organism_classificationPhotosynthetic capacitySexual dimorphismsexual dimorphismSeedsGeranium sylvaticumshadeta1181010606 plant biology & botanyPlant Biology
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Holocene climate variability in Sicily from a discontinuous stalagmite record and the Mesolithic to Neolithic transition

2006

AbstractFabric and stable isotopic composition of a Holocene stalagmite (CR1) from a cave in northern Sicily record changes in paleorainfall in the early Holocene. High δ13C stable isotope values in the calcite deposited from ca. 8500 to ca. 7500 yr ago are interpreted as reflecting periods of high rainfall. The wet phase was interrupted by two periods of multi-century duration characterized by relatively cool and dry winters centered at ca. 8200 and ca. 7500 yr ago, highlighted by low δ13C and δ18O values. A high variability of δ13C values is recorded from ca. 7500 to ca. 6500 yr ago and indicates that the transition from a pluvial early Holocene to the present-day climate conditions was p…

Calcite010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ13Cδ18OStable isotope ratioStalagmite01 natural scienceschemistry.chemical_compoundArts and Humanities (miscellaneous)chemistryPluvialClimatologyGeneral Earth and Planetary SciencesPhysical geographyGeologyMesolithicHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesStalagmite Sicily Early Holocene paleorainfall
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The effects of drip rate and geometry on the isotopic composition of speleothems: Evaluation with an advection-diffusion-reaction model

2022

Abstract The curvature and slope of speleothem surfaces have been shown to affect the reaction rates in the aqueous carbonate system by altering the thickness of the CaCO3-precipitating solution. However, the effects of speleothem geometry and drip rate on the speleothem’s carbon and oxygen isotopic composition have yet to be investigated. Over more strongly sloping surfaces, solutions are thinner and flow faster. The effects of thinner and faster-flowing solutions on the isotopic composition of carbonate minerals precipitated from these solutions are of opposite sense. Thinner solutions enhance rates of CO2 degassing and mineral formation, increasing the degree of isotopic distillation of …

Calcitegeographygeography.geographical_feature_categoryStalactiteδ13Cδ18OCarbonate mineralsSpeleothemGeometryReaction ratechemistry.chemical_compoundchemistryGeochemistry and PetrologyCarbonateGeochimica et Cosmochimica Acta
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Modelling carbon isotopes of carbonates in cave drip water

2011

Abstract C isotopes in cave drip water are affected by both the C isotope composition of soil air and host rock carbonate. Furthermore, the C isotope composition of cave drip water strongly depends on the calcite dissolution system, i.e., open, closed and intermediate conditions. Here, we present a calcite dissolution model, which calculates the 14C activity and δ13C value of the dissolved inorganic carbon of the drip water. The model is based on the chemical equations describing calcite dissolution ( H 2 O + CaCO 3 + CO 2 ⇔ Ca 2 + + 2HCO 3 - ). The most important improvement, relative to previous models, is the combination of the open and closed system conditions in order to simulate the C…

Calcitegeographygeography.geographical_feature_categoryδ13CIsotopeMineralogychemistry.chemical_compoundCavechemistryGeochemistry and PetrologyIsotopes of carbonDissolved organic carbonCarbonateDissolutionGeologyGeochimica et Cosmochimica Acta
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Comparison of δ(13)C and δ(18)O from cellulose, whole wood, and resin-free whole wood from an old high elevation Pinus uncinata in the Spanish centra…

2016

δ(13)C and δ(18)O values from sapwood of a single Pinus uncinata tree, from a high elevation site in the Spanish Pyrenees, were determined to evaluate the differences between whole wood and resin-free whole wood. This issue is addressed for the first time with P. uncinata over a 38-year long period. Results are also compared with published isotope values of α-cellulose samples from the same tree. The differences in δ(13)C and δ(18)O between whole wood and resin-free whole wood vary within the analytical uncertainty of 0.3 and 0.5 ‰, respectively, indicating that resin extraction is not necessary for sapwood of P. uncinata. Mean differences between cellulose and whole wood are 0.9 ‰ (δ(13)C)…

Carbon Isotopes010504 meteorology & atmospheric sciencesδ13Cδ18O010401 analytical chemistryOxygen IsotopesPinus01 natural sciencesWood0104 chemical sciencesInorganic ChemistryPinus <genus>chemistry.chemical_compoundHorticulturechemistryResin extractionSpainHigh elevationLong periodEnvironmental ChemistryEnvironmental scienceCelluloseCellulose0105 earth and related environmental sciencesGeneral Environmental ScienceIsotopes in environmental and health studies
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Microstructure-specific carbon isotopic signatures of organic matter from ∼3.5 Ga cherts of the Pilbara Craton support a biologic origin.

2016

21 pages; International audience; The ∼3.5 Ga Dresser Formation from the North Pole Dome of the Pilbara Craton (Western Australia) contains some of the oldest evidence for life on Earth. Here, we present a detailed study of microstructure-specific carbon isotopic composition of organic matter (OM) preserved in Dresser Formation bedded cherts and hydrothermal chert vein using in situ Secondary-Ion Mass Spectrometry (SIMS). The OM in these rocks occurs mainly as clots that, together with minor fine OM layers and laminae, are considered primary textures formed prior to host rock lithification. Other than rare OM-rich stylolites, no evidence was found for later OM migration beyond the micromete…

Carbon isotope ratio010504 meteorology & atmospheric sciencesMetamorphic rockPilbara CratonMineralogy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesMicrofossilsPilbara cratonGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryDresser FormationOrganic matterLithificationAnkerite0105 earth and related environmental scienceschemistry.chemical_classificationδ13CGeology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrychemistry13. Climate actionStylolite[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrganic matterVein (geology)SIMSGeology
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Organic carbon and nitrogen stable isotopes in the intertidal sediments from the Yangtze Estuary, China

2005

The natural isotopic compositions and C/N elemental ratios of sedimentary organic matter were determined in the intertidal flat of the Yangtze Estuary. The results showed that the ratios of carbon and nitrogen stable isotopes were respectively -29.8 per thousand to -26.0 per thousand and 1.6 per thousand-5.5 per thousand in the flood season (July), while they were -27.3 per thousand to -25.6 per thousand and 1.7 per thousand-7.8 per thousand in the dry season (February), respectively. The delta(13)C signatures were remarkably higher in July than in February, and gradually increased from the freshwater areas to the brackish areas. In contrast, there were relatively complex seasonal and spati…

ChlorophyllChinaGeologic SedimentsTime FactorsAquatic ScienceOceanographyRiversSedimentary organic matterOrganic matterchemistry.chemical_classificationTotal organic carbonCarbon IsotopesNitrogen Isotopesδ13CStable isotope ratioChlorophyll Aδ15NPollutionIsotopes of nitrogenOceanographychemistryIsotopes of carbonEnvironmental chemistrySeasonsGeologyEnvironmental MonitoringMarine Pollution Bulletin
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Climate signals in δ13C of wood lignin methoxyl groups from high-elevation larch trees

2016

Abstract In this study, a barely used method to measure δ13C values from lignin methoxyl groups (δ13Cmethoxyl) of tree‐rings is applied to high alpine larch trees to test their potential as a climate proxy. Thirty-seven larch trees (Larix decidua Mill.) were sampled at a tree line site near Simplon Village in the Valais/Switzerland. Samples were used to measure tree-ring width, and from five individuals, δ13Cmethoxyl was determined at annual resolution from 1971 to 2009, and at pentadal resolution from 1747 to 2009. The physiological tree responses to increasing atmospheric CO2 concentration since 1850 and the corresponding decrease in δ13C (Suess effect) were corrected using a range of pub…

Correction method010504 meteorology & atmospheric sciencesOceanographyAtmospheric sciences01 natural sciencesSuess effectchemistry.chemical_compoundHigh elevationCo2 concentrationLigninEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesδ13Cbiology010401 analytical chemistryPaleontology15. Life on landbiology.organism_classification0104 chemical scienceschemistry13. Climate actionClimatologyLarchGeologyTree linePalaeogeography, Palaeoclimatology, Palaeoecology
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