Search results for "3C"

showing 10 items of 396 documents

Carbon, nitrogen and oxygen isotope fractionation during food cooking: Implications for the interpretation of the fossil human record.

2017

13 pages; International audience; ObjectivesStable isotope data provide insight into the reconstruction of ancient human diet. However, cooking may alter the original stable isotope compositions of food due to losses and modifications of biochemical and water components.MethodsTo address this issue, carbon, nitrogen and oxygen isotope ratios were measured on meat aliquots sampled from various animals such as pork, beef, duck and chicken, and also from the flesh of fishes such as salmon, European seabass, European pilchard, sole, gilt-head bream, and tuna. For each specimen, three pieces were cooked according to the three most commonly-known cooking practices: boiling, frying and roasting on…

010506 paleontologyMeatSwine[SHS.ANTHRO-BIO]Humanities and Social Sciences/Biological anthropologyEUROPEAN PILCHARDBiology01 natural sciencesIsotopes of oxygenAnthropology PhysicalIsotopesSalmon[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrymedicinestable isotopeAnimals0601 history and archaeologyFood sciencehumans0105 earth and related environmental sciencesRoasting2. Zero hungerCooking Practices060101 anthropologycookingδ13CStable isotope ratioFossilsFleshfoodfood and beverages06 humanities and the arts[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrymedicine.drug_formulation_ingredient13. Climate actionAnthropology[ SHS.ANTHRO-BIO ] Humanities and Social Sciences/Biological anthropologyCattleAnatomyTunadietChickensFood Analysis
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Carbon and Oxygen Isotope Signals from the Callovian–Oxfordian in French Sedimentary Basins

2013

3 pages; International audience; High-resolution carbon and oxygen isotope data from the Paris Basin and the Subalpine Basin (France) are available in a precise biostratigraphic framework for the Callovian-Oxfordian stages. A biostratigraphically well-constrained δ13C curve, derived from bulk carbonates in the Paris Basin and the Subalpine Basin, is provided in order to document carbon-cycle evolution and to serve as a chemostratigraphic reference for the Callovian-Oxfordian in the Tethyan domain. Sea-temperature reconstructions, using diagenetically screened belemnite and oyster data, reveal major climate perturbations at the Middle-Late Jurassic transition.

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesCallovianBelemnitechemistry.chemical_elementStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenCarbon cycleOxfordianPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryδ13CBivalveCarbon cycleSedimentary basin[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryPalaeotemperatures[ SDE.MCG ] Environmental Sciences/Global Changeschemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMontane ecologyCarbonGeology
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The Valanginian isotope event: a complex suite of palaeoenvironmental perturbations.

2011

17 pages; International audience; The Valanginian records a severe crisis of carbonate systems, both on platforms and in the pelagic realm. This crisis is roughly concomitant with the Weissert Event, characterized by a positive δ13C excursion of about 2‰in marine carbonates. However, it is unclear if the response of these two carbonate systems to the global perturbations is contemporaneous, or if they react differently. For this purpose, accumulation rates of pelagic carbonates produced by nannofossils and of platform-derived carbonates have been quantified in a hemipelagic environment (the Vocontian Basin, SE France) that has the potential to record the reaction of both shallow-water and p…

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesGeochemistryClimate changeWeathering[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesCarbon cyclePaleontologychemistry.chemical_compound[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryClimate changeCarbonate production crisis14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesδ13CExcursionPaleontologyPelagic zoneAccumulation ratesCyclostratigraphy[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global Changeschemistry13. Climate actionValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeologyδ13C Weissert Event
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Calcareous nannofossil response to Late Cretaceous climate change in the eastern Tethys (Zagros Basin, Iran)

2020

Abstract Coniacian to Maastrichtian changes in calcareous nannofossil assemblages have been investigated in the eastern Tethyan Shahneshin section (central Zagros Basin, Iran). The nannofossil assemblages are mainly composed of Watznaueria spp. (avg. 54%), Retecapsa spp (avg. 7.9%), Cribrosphaerella ehrenbergii (avg. 7.7%) and Micula spp. (avg. 5.7%). Throughout the late Campanian, there is a trend to lower abundances in Watznaueria spp. together with increasing abundances of C. ehrenbergii and Arkhangelskiella cymbiformis, which are considered in this basin as the main cool-water taxa. Our results reveal that, despite a diagenetic impact on calcareous nannoflora, a number of primary paleoe…

010506 paleontologybiologyδ13CPaleontologyStructural basin010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesCretaceousDiagenesisForaminiferaPaleontologyBorealBenthic zoneCalcareousEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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ISOTOPIC TEMPERATURES FROM THE EARLY AND MID-PLIOCENE OF THE US MIDDLE ATLANTIC COASTAL PLAIN, AND THEIR IMPLICATIONS FOR THE CAUSE OF REGIONAL MARIN…

2017

Mean seasonal extreme temperatures on the seafloor calculated from the shell d 18 Oofthescallop Placopecten clintonius from the basal part of the early Pliocene Sunken Meadow Member (Yorktown Formation) in Virginia are very similar to those from the same horizon at the latitude of Cape Hatteras in North Carolina ( ~ 210 km to the south). The lowest and highest temperatures calculated from each shell (using d 18 O seawater ¼þ 0.7 % )givemean values for winter and summer of 8.4 6 1.1 8 C( 6 1 r ) and 18.2 6 0.6 8 CinVirginia,and8.6 6 0.4 8 Cand16.5 6 1.1 8 C in North Carolina (respective median temperatures: 13.3 8 C and 12.6 8 C). Patterns of ontogenetic variation in d 18 O, d 13 C and micro…

010506 paleontologygeographygeography.geographical_feature_categoryδ13CYorktown Formationδ18OCoastal plainPaleontologyOceanic climate010502 geochemistry & geophysics01 natural sciencesGulf StreamOceanographySclerochronologyPaleoclimatologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences
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A 4000-year long Late Holocene climate record from Hermes Cave (Peloponnese, Greece)

2020

The societal and cultural development during the Bronze Age and the subsequent Iron Age was enormous in Greece, however interrupted by two significant transformations around 4200 years b2k (Early Helladic II/III; b2k refers to years before 2000 CE) and 3200 years b2k (end of Late Helladic III). Artefacts and building remains provide some insights into the cultural evolution, but only little is known about environmental and climatic changes on a detailed temporal and spatial scale. Here we present a 4000-year long stalagmite record (GH17-05) from Hermes Cave, Greece, located on Mount Ziria in the close vicinity of the Late Bronze Age citadel of Mycenae and the Classical-Hellenistic polis of …

010506 paleontologygeographygeography.geographical_feature_categoryδ13Cδ18OSpeleothemStalagmite01 natural sciencesCaveBronze AgePaleoclimatologyPhysical geographyHoloceneGeology0105 earth and related environmental sciences
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Venerid bivalve Venus verrucosa as a high-resolution archive of seawater temperature in the Mediterranean Sea

2021

Abstract High-resolution stable isotope data (δ18O, δ13C) were used to study growth strategies of the bivalve Venus verrucosa collected from three sites of the eastern coast of the Adriatic Sea. The principal objectives of this study were to identify the main growing season and to evaluate the potential applicability of δ18Oshell values to reconstruct the seasonal temperature variability. Calcium carbonate for oxygen and carbon isotope analyses was obtained by drilling the outer shell layer. Temporal and spatial variations in temperature and salinity values at the study sites were simulated using the 3D numerical ocean model ROMS. Annual periodicity of growth patterns was confirmed by δ18Os…

010506 paleontologyδ13Cδ18OStable isotope ratioTemperature salinity diagramsPaleontologyGrowing season010502 geochemistry & geophysicsOceanography01 natural sciencesOceanographyMediterranean seaSeawater14. Life underwaterBayStable isotopes ; Paleotemperature ; Adriatic Sea ; Growth rateEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Experimental δ13C evidence for a contribution of methane to pelagic food webs in lakes

2006

We tested the hypothesis that low stable carbon isotope (δ13C) values commonly observed for zooplankton in humic lakes are due to their feeding on isotopically light methane-oxidizing microbes, and thus that methane-derived carbon is important in the food webs of these lakes. In replicate laboratory cultures, Daphnia longispina, a common crustacean zooplankter in humic lakes, were fed microbial suspensions with or without enrichment by biogenic methane. The δ13C values of Daphnia indicated consumption of 13C-depleted methanotrophic bacteria, while growth rates, survival, and reproduction of Daphnia in cultures enriched with methane were equal to or greater than those in nonenriched cultures…

0106 biological sciences010504 meteorology & atmospheric sciencesbiologyδ13CEcology010604 marine biology & hydrobiologyfungichemistry.chemical_elementPelagic zoneAquatic ScienceOceanographybiology.organism_classification01 natural sciencesDaphniaCrustaceanZooplanktonMethanechemistry.chemical_compoundchemistryIsotopes of carbonCarbon0105 earth and related environmental sciences
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Within trophic level shifts in collagen-carbonate stable carbon isotope spacing are propagated by diet and digestive physiology in large mammal herbi…

2018

Stable carbon isotope analyses of vertebrate hard tissues such as bones, teeth, and tusks provide information about animal diets in ecological, archeological, and paleontological contexts. There is debate about how carbon isotope compositions of collagen and apatite carbonate differ in terms of their relationship to diet, and to each other. We evaluated relationships between δ13Ccollagen and δ13Ccarbonate among free-ranging southern African mammals to test predictions about the influences of dietary and physiological differences between species. Whereas the slopes of δ13Ccollagen–δ13Ccarbonate relationships among carnivores are ≤1, herbivore δ13Ccollag…

0106 biological sciences0301 basic medicine10253 Department of Small Animalsgrassmedicine.medical_treatmentZoologyBiology010603 evolutionary biology01 natural sciences2309 Nature and Landscape ConservationC3 C403 medical and health scienceschemistry.chemical_compoundLow-protein dietmedicineC3Ecology Evolution Behavior and SystematicsOriginal ResearchC4browseNature and Landscape ConservationTrophic levelHerbivore630 AgricultureEcologyδ13CStable isotope ratiomethane1105 Ecology Evolution Behavior and Systematics030104 developmental biologychemistry13. Climate actionIsotopes of carbon570 Life sciences; biologyCarbonateMammalprotein2303 EcologyEcology and Evolution
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Variability in δ13C values between individual Daphnia ephippia: Implications for palaeo-studies

2018

The stable carbon isotope ratio (δ13 C value) of Daphnia spp. resting egg shells (ephippia) provides information on past changes in Daphnia diet. Measurements are typically performed on samples of _20 ephippia, which obscures the range of values associated with individual ephippia. Using a recently developed laser ablation-based technique, we perform multiple δ13 C analyses on individual ephippia, which show a high degree of reproducibility (standard deviations 0.1e0.5‰). We further measured δ13 C values of 13 ephippia from surface sediments of three Swiss lakes. In the well-oxygenated lake with low methane concentrations, δ13 C values are close to values typical for algae (_31.4‰) and the …

0106 biological sciencesArcheology010504 meteorology & atmospheric sciencesEvolutionhiilita1171Daphnia [water flea]01 natural sciencesDaphniaCarbon cycleStable carbon isotopesAlgaeBehavior and SystematicsPalaeolimnologyTavernemedicineEphippiaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesStable isotopesPresentisotoopitGlobal and Planetary Changebiologyδ13CEcologyStable isotope ratio010604 marine biology & hydrobiologykausivaihtelutGeologySeasonalitySeasonalitybiology.organism_classificationmedicine.diseasepaleolimnologiaLaser ablationEuropeLakesArchaeology13. Climate actionIsotopes of carbonvesikirputta1181Daphnia ephippiaPhysical geographyQuaternary Science Reviews
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