Search results for "CEA"

showing 8 items of 6048 documents

Late Jurassic (Kimmeridgian–Tithonian) stable isotopes (δ18O, δ13C) and Mg/Ca ratios: New palaeoclimate data from Helmsdale, northeast Scotland

2010

Abstract The data presented here provide the first detailed stable isotope ( δ 18 O, δ 13 C) and geochemical (Mg/Ca) investigation of Kimmeridgian–Tithonian belemnites from the Helmsdale Coast, Scotland, UK. Oxygen and carbon stable isotope values from well preserved specimens range from − 2.8 to + 0.3‰ and from − 2.3 to + 2.8‰ respectively. The oxygen isotope data are consistent with palaeotemperatures of up to 24 °C in the Early Kimmeridgian cymodoce Zone and down to 11 °C in the Mid Tithonian rotunda–fittoni Zones. These estimates are strongly supported by the Mg/Ca data, which also indicate a cooling episode (and very similar palaeotemperatures, 11–22 °C) at this time. The cooling event…

δ13Cbiologyδ18OStable isotope ratioPaleontologyOceanographybiology.organism_classificationIsotopes of oxygenPaleontologyIsotopes of carbonChemostratigraphyPaleoclimatologyBelemnitesEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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A 2600-year record of past polycyclic aromatic hydrocarbons (PAHs) deposition at Holzmaar (Eifel, Germany)

2014

Polycyclic aromatic hydrocarbons (PAHs) are a proxy for climate- and human-related historical fire activity which has rarely been used beyond 1800 AD. We explored the concentration and composition patterns of PAHs together with other proxies (charcoal, C, N, S, δ13C, δ15N, and δ34S) in a sediment core of Holzmaar as indicators of variations in climate and anthropogenic activity over the past 2600 years. The concentrations of pyrogenic PAHs remained low (< 500 ng g− 1) from the pre-Roman Iron Age (600 BC) until the first significant increases to ca. 1000–1800 ng g− 1 between 1700 and 1750 AD related to regional iron production. The highest increases in pyrogenic PAH concentrations occurred w…

δ13Cbusiness.industryPaleontologyδ15NOceanographyδ34SIron AgeEnvironmental chemistryvisual_artvisual_art.visual_art_mediumSedimentary organic matterCoalPolycyclic HydrocarbonsbusinessCharcoalEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Unraveling environmental histories from skeletal diaries — Advances in sclerochronology

2013

High-resolution proxy archives from aquatic settings are essential to better understand processes and mechanisms of global change. During the last decade, it has become increasingly evident that calcified tissues of bivalve mollusks and cold-water corals, in particular, can significantly increase our knowledge of seasonal to multi-decadal paleoclimate and paleoenvironmental variability in the extratropical oceans and coastal marine settings. Daily, tidal, fortnightly and annual growth patterns of periodically formed skeletal hard parts provide a means to place the proxy record in a precise temporal context. Their extreme longevity coupled with the running similarity between growth increment…

δ13Cδ18OPaleontologyGlobal changeOceanographyProxy (climate)Waves and shallow waterOceanographySclerochronologyPaleoclimatologyResource useEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Carbon cycle and sea-water palaeotemperature evolution at the Middle-Late Jurassic transition, eastern Paris Basin (France).

2014

14 pages; International audience; A very high-resolution carbon and oxygen stable isotope analysis (bulk-carbonate) of a biostratigraphically well-constrained Callovian-Oxfordian series is provided here for the first time. The homogeneity of the clayey series and the weak diagenetic alteration allow the isotopic signal variations to be considered as primary in origin. A prominent and brief negative excursion in the δ13C curve (−2‰), occurring at the start of the Middle Callovian (Jason Zone - Obductum Subzone) and correlated regionally, suggests a possible methane release. The increasing δ13C values thereafter up to the Early Oxfordian, concomitant with a warming episode, highlight the buri…

δ18OStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCallovianOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyIsotopes of oxygenCarbon cycleOxfordianPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterIsotope analysisδ13CbiologyCarbon isotopesGeologybiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySea-water paleotemperatures[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsPaleoenvironmental changes13. Climate actionIsotopes of carbon[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOxygen isotopesEconomic GeologyGlobal coolingBelemnitesGeology
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Variation in Sr uptake in the shell of the freshwater gastropod Bithynia tentaculata from Lake Arreo (northern Spain) and culture experiments

2010

The Sr uptake features in Bithynia tentaculata aragonite shells from monthly collections in Lake Arreo (northern Spain) over a two-year period are compared with those from the same species grown in culture experiments with similar waters under controlled temperature. The shell aragonite of B. tentaculata from Lake Arreo formed in isotopic equilibrium with the lake water. A comparison of the stable oxygen isotope values (δ18O) from the shells and waters allowed the selection of suitable shells for Sr uptake studies. The Sr/Ca molar ratio in B. tentaculata shells (Sr/Cashell) from the lake and from the culture experiments positively correlate with some chemical parameters like conductivity an…

δ18Ochemistry.chemical_elementMineralogyengineering.materialOceanographyIsotopes of oxygenBithynia tentaculataMollusk shellEcology Evolution Behavior and SystematicsEarth-Surface ProcessesStrontiumbiologyStable isotope ratioAragoniteTrace elementPaleontologyTentaculatabiology.organism_classificationOxygen isotopeAragonitechemistryStrontiumEnvironmental chemistryengineeringTrace elementGeology
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The Use of Stable Isotope Ratio Analysis to Trace European Sea Bass (D. labrax) Originating from Different Farming Systems

2020

This study aimed to determine whether isotopic ratio mass spectrometry (IRMS) can discriminate farmed European sea bass according to different farming systems and geographic origins. Dicentrarchus labrax of commercial size from three different rearing systems (concrete tank inland, sea cages, and extensive methods in valleys or salt works) were collected at the trading period (autumn&ndash

δ18Ostable isotopesgeographic origin01 natural sciencesArticle0404 agricultural biotechnologyAquacultureSettore AGR/20 - Zoocolturelcsh:ZoologyDicentrarchus labrax<i>Dicentrarchus labrax</i>lcsh:QL1-991Settore BIO/06 - Anatomia Comparata E CitologiaSea bassIsotope-ratio mass spectrometryaquaculture; Dicentrarchus labrax; stable isotopes; traceability; farming system; geographic origin; IRMS; sea bass; fish; authenticationfishaquaculture Dicentrarchus labrax stable isotopes traceability farming system geographic origin IRMS sea bass fish authenticationlcsh:Veterinary medicineGeneral Veterinaryδ13CbiologyStable isotope ratiobusiness.industry010401 analytical chemistry04 agricultural and veterinary sciencesδ15NIRMSbiology.organism_classification040401 food science0104 chemical sciencesFisherytraceabilityaquaculturelcsh:SF600-1100authenticationEnvironmental sciencefarming systemAnimal Science and ZoologyDicentrarchusbusinesssea bassAnimals
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Underground investigation of extensive air showers spectra at high energy range of cosmic rays and other research in the Pyhäsalmi mine

2020

Abstract High energy particles reaching the Earth’s atmosphere are known as cosmic rays. As a result of interactions with nuclei of air molecules, cosmic rays induce showers of secondary particles, which can be divided into 3 components: electromagnetic, hadronic and muonic components. The Experiment with Multi Muon Array (EMMA), located at the depth of 75 m in the Pyhäsalmi mine in Finland, investigates the muonic component of the Extensive Air Showers (EAS) to deduce the direction, energy, and the mass of the primary cosmic ray particles. In this paper we give a concise description and methodology used by EMMA followed by a brief review of the C14 experiment. Finally, we review the feasib…

ғарыш сәулелеріPhysics::Instrumentation and DetectorsastrofysiikkaAstrophysics::High Energy Astrophysical PhenomenaBoreholekneeOcean EngineeringCosmic rayhiukkasfysiikkaSpectral lineAtmosphereNuclear physicsnuclear and elementary particle physicscosmic rayshigh-energy muonжоғары энергиялы мюонPhysicsтізе аймағыtheoretical physicsRange (particle radiation)Muonastrophysicsкең ауқымды нөсер (КАН)Neutrino detectorilmaisimetExtensive Air Shower (EAS)EMMANeutrinokosminen säteily
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Flagship species of the Pieniny NP. protected ex situ at PAS BGCBDC seed bank at WARSAW-POWSIN

2014

Pieniny Mts. are important biodiversity hotspot in Central Europe. According to Pieniny National Park Long Term Conservation Plan 2000-2020 small, isolated populations of some of Pieniny NP flagship species can become extinct till 2020. That is why their ex situ preservation at seed bank is justified and reasonable as supplement of active and passive in situ conservation measures carried out by National Park staff. PAS Botanical Garden – Center for Biological Diversity Conservation at Warsaw-Powsin has a long tradition of cooperation with Pieniny National Park (S Poland). This article focuses on the actions undertaken during EU funded conservation project: “Ex situ conservation of native, t…

“FlorNaturOB” projectPieniny NP special interest plant speciesMinuartia setaceaseed dormancyDendranthema zawadzkiicryopreservationErysimum pieninicumFragmenta Naturae
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