Search results for "13C"

showing 10 items of 194 documents

Water-extractable organic matter linked to soil physico-chemistry and microbiology at the regional scale

2015

10 pages; International audience; A better understanding of the links between dissolved organic matter and biogeochemical processes in soil could help in evaluating global soil dynamics. To assess the effects of land cover and parental material on soil biogeochemistry, we studied 120 soil samples collected from various ecosystems in Burgundy, France. The potential solubility and aromaticity of dissolved organic matter was characterised by pressurised hot-water extraction of organic carbon (PH-WEOC). Soil physico-chemical characteristics (pH, texture, soil carbon and nitrogen) were measured, as was the δ13C signature both in soils and in PH-WEOC. We also determined bacterial and fungal abund…

2. Zero hungerchemistry.chemical_classificationSoil biodiversityChemistrySoil biogeochemistrySoil organic matterSoil biology[ SDV.SA.SDS ] Life Sciences [q-bio]/Agricultural sciences/Soil studySoil ScienceSoil chemistryMicrobial community structureSoil scienceSoil carbonBurgundy region[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study15. Life on landcomplex mixturesMicrobiologyHumusPedogenesisEnvironmental chemistryδ13COrganic matterPressurised hot-water-extractable organic carbonSoil Biology and Biochemistry
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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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Stable isotopes covering 96-7 ka BP from stalagmite CM (Santo Tomas Cave, Cuba)

2020

We present a new speleothem trace element and stable isotope record, which extends previous paleoclimate evidence from Cuban speleothems to the last 96 ka. Stable isotope samples were micromilled at a resolution of 0.10-0.33mm, and measured using an IRMS equipped with a Gasbench. Line scans of Element/Calcium ratios of the speleothem were measured by laser ablation ICPMS and were reduced to the resolution of the stable isotope records.

AGESpeleothem sampleδ13C stackedδ13CEarth System Researchpaleoclimatologyδ18O stackedstackedCentral Americaδ18OMass spectrometer DeltaPlusXL coupled to a Gasbench IIspeleothemStable isotopes
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Petrography and carbonate isotope stratigraphy from MIS AND-1B core, Antarctica: Evidence of the early Pliocene warming event

2011

Abstract A large portion of ANDRILL (ANtarctic geological DRILLing) core AND-1B recovered in the Western Ross Sea and spanning the early Pliocene has been investigated in order to obtain a detailed carbonate isotope record from Antarctic margin sediments through the early Pliocene warming event. Petrographic observations and mineralogical analyses reveal the authigenic nature of the carbonate and small proportions of Fe and Mg incorporated within the calcite lattice. High productivity conditions testified by ~ 80 m-thick diatomite interval (383 to 460 mbsf) well fit with the composite nature of the authigenic carbonate generally characterizing organic matter-rich sediments. As is known, sed…

ANDRILLCalciteGlobal and Planetary Changegeographygeography.geographical_feature_categoryδ13CStable isotope ratioδ18OGlacierAuthigenicearly PlioceneOceanographypalaeoclimatePetrographychemistry.chemical_compoundPaleontologychemistrystable isotopeAntarcticaCarbonateGeologyGlobal and Planetary Change
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Reconstructing Bronze Age diets and farming strategies at the early Bronze Age sites of La Bastida and Gatas (southeast Iberia) using stable isotope …

2020

The El Argar society of the Bronze Age in the southeast of the Iberian Peninsula (2200–1550 cal BCE) was among the first complex societies in Europe. Its economy was based on cereal cultivation and metallurgy, it was organized hierarchically, and successively expanded its territory. Most of the monumentally fortified settlements lay on steeply sloped mountains, separated by fertile plains, and allowed optimal control of the area. Here, we explore El Argar human diets, animal husbandry strategies, and food webs using stable carbon and nitrogen isotope analysis of charred cereal grains as well as human and animal bone collagen. The sample comprised 75 human individuals from the sites of La Ba…

Agricultural cropsMaleComposite ParticlesBiochemistry01 natural sciencesAncient historyIsotopesBone and bonesMedicine and Health Sciences0601 history and archaeologyAnimal HusbandryChildHistory AncientTrophic levelIsotope analysisCarbon IsotopesMultidisciplinary060102 archaeologyδ13CEcologyPhysicsQRCarbon isotopesEukaryotafood and beveragesAgriculture06 humanities and the artsPlantsAnimal husbandryArchaeologyAnimals DomesticChild PreschoolPhysical SciencesWheatMedicineFemaleResearch ArticleCrops AgriculturalAdultAtoms010506 paleontologyAdolescentAnimal TypesScienceCropsAnimals WildForageBiologyResearch and Analysis MethodsWild animalsBone and BonesYoung AdultBronze AgeBarleyAnimalsHumansDomestic AnimalsGrassesParticle PhysicsDomesticationChemical CharacterizationEdible grainIsotope AnalysisNutrition0105 earth and related environmental sciencesNitrogen Isotopesbusiness.industryNitrogen isotopesOrganismsBiology and Life SciencesProteinsInfantDietYoung adultPreschool childAgricultureSpainEdible GrainbusinessCollagensZoologyCrop ScienceCereal Crops
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Carbon stable isotope composition of charophyte organic matter in a small and shallow Spanish water body as a baseline for future trophic studies

2015

<p>Quantitative descriptions of foodweb structure based on isotope niche space require knowledge of producers’ isotopic signatures. In freshwater ecosystems charophytes are one of the main components of submerged vegetation and the feeding base for many herbivorous consumers, but knowledge about their organic carbon isotopic signatures is sparse. In this study, the δ<sup>13</sup>C organic values (and organic %C and %N) of the four species of submerged macrophytes (three charophytes - <em>Chara hispida</em>, <em>Nitella hyalina</em> and <em>Tolypella glomerata </em>- and one angiosperm, <em>Myriophyllum spicatum</em>) growing …

Albufera de Valencia Natural Park.NicheMyriophyllum spicatumChara hispidaAquatic Scienceδ13C signatureBotanyOrganic matterlcsh:Physical geographylcsh:Environmental sciencesWater Science and TechnologyTrophic levellcsh:GE1-350Total organic carbonchemistry.chemical_classificationNitella hyalinaEcologyMyriophyllumbiologyEcologyStable isotope ratiolcsh:Geography. Anthropology. RecreationTolypella glomeratabiology.organism_classificationMacrophytelcsh:GchemistryBenthic zonelcsh:GB3-5030Journal of Limnology
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Investigating the dietary life histories and mobility of children buried in St Gertrude Church cemetery, Riga, Latvia, 15th–17th centuries ad *

2020

Carbon and nitrogen isotope profiles were obtained from incremental dentine analysis of 19 non‐adults from a cemetery in Riga, Latvia. The research compared the life histories and diet between people buried in two mass graves and the general cemetery. The δ13C profiles of several children from the mass graves were similar but did not resemble the patterns seen in children from the general cemetery, suggesting that they probably represented a different population group. The rise in δ15N values towards the end of the life of four individuals from one mass grave suggests they were victims of an historically documented famine.

ArcheologyHistoryeducation.field_of_studyGeographyδ13CPopulationFamineeducationArchaeologyIsotopes of nitrogenArchaeometry
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Sources of geomaterials in the Sicani Mountains during the Early Middle Ages: A case study of Contrada Castro, central western Sicily

2022

From 2017, an unknown rural settlement in Contrada Castro at Corleone (Palermo Province, western Sicily) was investigated as part of the `Harvesting Memories Project¿. The stratigraphic sequence, supported by radiocarbon dating, has demonstrated a reoccupation of a pre-Roman site during the transition between the Byzantine and Islamic periods. In particular, the main occupation occurred in the late 8th¿9th century when pottery kilns and a probable warehouse were constructed. During the 10th¿11th century, a new structure with different orientations replaced the previous buildings that had already collapsed. Specifically focusing on a perspective of the household production and its relationsh…

ArcheologyPolarized lightMicroscopyPotteryhttp://aims.fao.org/aos/agrovoc/c_f12113cdGeomaterials sourcingArchaeometryhttps://csic-primo.hosted.exlibrisgroup.com/permalink/f/dhf3c4/34CSIC_ALMA_AU9817823577904201http://aims.fao.org/aos/agrovoc/c_4185ArchaeologySettore BIO/03 - Botanica Ambientale E ApplicataEarth and Planetary Sciences (miscellaneous)Landscapearchaeometry geomaterials sourcing landscape Medieval archaeology polarized light microscopy pottery SicilyMedieval archaeologySicily
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Climate signals in carbon and oxygen isotope ratios of Pinus cembra tree‐ring cellulose from the Călimani Mountains, Romania

2020

Abstract We analyze annually resolved tree-ring stable carbon (I´13C) and oxygen (I´18O) isotopic chronologies from Swiss stone pine (Pinus cembra L.) in Romania. The chronologies cover the period between 1876 and 2012 and integrate data from four individual trees from the Calimani Mts in the eastern Carpathians where climatic records are scarce and starts only from 1961. Calibration trials show that the I´13C values correlate with local April-May relative humidity and with regional to larger scale (European) summer precipitation. I´18O correlates significantly with local relative humidity, cloud cover, maximum temperature, as well as European scale drought conditions. In all cases, the cli…

Atmospheric Science010504 meteorology & atmospheric sciencesδ13Cδ18OPinus cembra15. Life on land010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenfood.foodMediterranean seafood13. Climate actionClimatologyDendrochronologyEnvironmental sciencePrecipitationPhysical geographyPressure system0105 earth and related environmental sciencesInternational Journal of Climatology
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δ13C variations in tree rings as an indication of severe changes in the urban air quality

2002

Abstract Annual growth rings sampled from three free-standing trees (Platanus hybrida sp.), grew in the metropolitan area of Palermo (Italy) and covering a 118 years time span (1880–1998), have been studied for their 13C/12C carbon isotope ratios. It has been found that the 13C/12C tree ring record, during the study time interval, decreased of −3.6‰, from −26.4‰ in 1880 to −30‰ in 1998. Such a progressive depletion has been attributed to the addition of anthropogenic 13C depleted carbon dioxide to the local atmosphere. The observed 13C/12C decrease has been used to infer some possible pathways of atmospheric CO2 change in the study urban area.

Atmospheric ScienceAir pollutionMineralogyUrban environmentAtmospheric sciencesmedicine.disease_causeAtmospherechemistry.chemical_compoundmedicineDendrochronologyEnvironmental geochemistryAir quality indexGeneral Environmental Scienceδ13Cbiologybiology.organism_classificationStable carbon isotopeSettore GEO/08 - Geochimica E VulcanologiaPlatanuschemistryCarbon dioxideIsotopes of carbonCarbon dioxideEnvironmental scienceDendrochemistryTree ring
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