Search results for "UI"

showing 10 items of 43725 documents

First in-situ measurements of plume chemistry at mount garet volcano, island of gaua (Vanuatu)

2020

Recent volcanic gas compilations have urged the need to expand in-situ plume measurements to poorly studied, remote volcanic regions. Despite being recognized as one of the main volcanic epicenters on the planet, the Vanuatu arc remains poorly characterized for its subaerial emissions and their chemical imprints. Here, we report on the first plume chemistry data for Mount Garet, on the island of Gaua, one of the few persistent volatile emitters along the Vanuatu arc. Data were collected with a multi-component gas analyzer system (multi-GAS) during a field campaign in December 2018. The average volcanic gas chemistry is characterized by mean molar CO2/SO2, H2O/SO2, H2S/SO2 and H2/SO2 ratios …

010504 meteorology & atmospheric sciencesvolcanic gas compositionsGeochemistryFlux010502 geochemistry & geophysicslcsh:Technology01 natural scienceslcsh:ChemistryVanuatu[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGeneral Materials ScienceGas composition[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentlcsh:QH301-705.5Instrumentation0105 earth and related environmental sciencesFluid Flow and Transfer Processesgeographygeography.geographical_feature_categorySubductionlcsh:TProcess Chemistry and TechnologyGeneral Engineeringlcsh:QC1-999Gas analyzerComputer Science ApplicationsPlumelcsh:Biology (General)lcsh:QD1-999Mount GaretVolcanolcsh:TA1-2040SubaerialPeriod (geology)volatile fluxeslcsh:Engineering (General). Civil engineering (General)GauaGaua Mount Garet Multi-GAS Vanuatu Volatile fluxes Volcanic gas compositionslcsh:PhysicsMulti-GAS
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Simulating speleothem growth in the laboratory: Determination of the stable isotope fractionation (δ13C and δ18O) between H2O, DIC and CaCO3

2019

Abstract Here we present novel cave-analogue experiments directly investigating stable carbon and oxygen isotope fractionation between the major involved species of the carbonate system (HCO3−, CO2, CaCO3 and H2O). In these experiments, which were performed under controlled conditions inside a climate box, a thin film of solution flew down an inclined marble or glass plate. After different distances of flow and, thus, residence times on the plate, pH, electrical conductivity, supersaturation with respect to calcite, precipitation rate as well as the δ18O and δ13C values of the dissolved inorganic carbon (DIC) and the precipitated CaCO3 were obtained. Progressive precipitation of CaCO3 along…

010504 meteorology & atmospheric sciencesδ18OStable isotope ratioAnalytical chemistryGeologyFractionation010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenEquilibrium fractionationIsotope fractionation13. Climate actionGeochemistry and PetrologyIsotopes of carbonRayleigh fractionationGeology0105 earth and related environmental sciencesChemical Geology
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Holocene vegetation and fire history of the mountains of Northern Sicily (Italy)

2016

Knowledge about vegetation and fire history of the mountains of Northern Sicily is scanty. We analysed five sites to fill this gap and used terrestrial plant macrofossils to establish robust radiocarbon chronologies. Palynological records from Gorgo Tondo, Gorgo Lungo, Marcato Cixé, Urgo Pietra Giordano and Gorgo Pollicino show that under natural or near natural conditions, deciduous forests (Quercus pubescens, Q. cerris, Fraxinus ornus, Ulmus), that included a substantial portion of evergreen broadleaved species (Q. suber, Q. ilex, Hedera helix), prevailed in the upper meso- mediterranean belt. Mesophilous deciduous and evergreen broadleaved trees (Fagus sylvatica, Ilex aquifolium) dominat…

010506 paleontologyArcheologyAbies nebrodensiSettore AGR/05 - Assestamento Forestale E Selvicoltura010504 meteorology & atmospheric sciencesFagus sylvaticaMacrofossilPlant ScienceMediterranean580 Plants (Botany)01 natural sciencesFagus sylvaticaClimate changeAbies nebrodensisIlex aquifoliumBeechHolocene0105 earth and related environmental sciencesArcheology (arts and humanities)biologyEcologyPaleontologyVegetationEvergreenbiology.organism_classificationDeciduousCharcoalPollen570 Life sciences; biology
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Chemical and mineralogical analyses on stones from Sagunto Castle (Spain)

2019

Abstract For the first time, an archaeometric study was carried out on the carbonate rock ashlars of the Sagunto Castle. The studied site is one of the most important and best preserved Spanish archaeological and architectural monuments, characterized by different construction phases from the Roman period to Modern Ages. Forty samples collected from thirteen different structures of Sagunto Castle and two quarries, located in the Sagunto's hill were used for comparative purposes. The samples were analyzed by X-ray diffraction, X-ray fluorescence and inductively coupled plasma mass spectrometry to determine their mineralogical and elemental composition. The obtained data show similar chemical…

010506 paleontologyArcheologyElemental composition060102 archaeologyOutcropRemainsBuilding stone06 humanities and the artsMineralogyMiddle ages01 natural sciencesArchaeologyRoman periodBuilding stone; Chemistry; Fortress; Middle ages; Mineralogy; Remains; Roman periodFortressChemistryPeriod (geology)Carbonate rock0601 history and archaeologyarchaeometrics; carbonate rock ashlars; X-ray fluorescence and inductively coupled plasma mass spectrometry0105 earth and related environmental sciencesJournal of Archaeological Science: Reports
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Oppida, Agglomerations, and Suburbia: the Bibracte Environs and New Perspectives on Late Iron Age Urbanism in Central-eastern France

2013

This paper explores the nature and chronology of La Tène and early Roman unenclosed agglomerations in central-eastern France. It has been prompted by the discovery of a c. 115 ha La Tène D2b/Augustan (c. 50 BC to AD 15) site close to Bibracte in the Morvan, located around the source of the River Yonne. This complex provides a new perspective on the chronology and role of Late La Tène and early Roman unenclosed settlements, adding further complexity to the story of the development of Late La Tène oppida. It indicates that these ‘agglomerations’ followed remarkably varied chronological trajectories, raising important issues concerning the nature of landscape and social change at the end of th…

010506 paleontologyArcheologyOppidum060102 archaeologyUrban agglomeration[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryAgglomerationSocial change06 humanities and the arts01 natural sciencesArchaeologyLate iron ageGeographyLa TèneIron Age[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryHuman settlementLandscape archaeology.Agglomération Antiquité Source de l'Yonne0601 history and archaeologyFranceUrbanismComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesChronology
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Rhinocerotid tooth enamel 18O/16O variability between 23 and 12 Ma in southwestern France.

2006

Abstract The relationship between the oxygen isotope ratio of mammal tooth enamel and that of drinking water was used to reconstruct changes in the Miocene oxygen isotope ratio of rainfall (meteoric water δ 18 O MW ). These, in turn, are related to climatic parameters (temperature, precipitation and evaporation rate). δ 18 O values of rhinocerotid teeth from the Aquitaine Basin (southwestern France) suggest a significant climatic change between 17 and 12 Ma, characterized by cooling together with precipitation increase, in agreement with other terrestrial and oceanic records. To cite this article: I. Bentaleb et al., C. R. Geoscience 338 (2006).

010506 paleontologyGeochemistry010502 geochemistry & geophysicsPalaeoclimate01 natural sciencesIsotopes of oxygenMammal/dk/atira/pure/sustainabledevelopmentgoals/clean_water_and_sanitationPaleontologystomatognathic system[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryPaleoclimatologymedicinePrecipitation0105 earth and related environmental sciencesGlobal and Planetary ChangeEnamel paintStable isotope ratioAquitaineMioceneOxygen isotope ratio cycleTooth enamelstomatognathic diseasesmedicine.anatomical_structure13. Climate actionEnamelvisual_artOxygen isotopesMeteoric watervisual_art.visual_art_mediumGeneral Earth and Planetary Sciencessense organs[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologySDG 6 - Clean Water and SanitationGeology
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Coarsely crystalline cryogenic cave carbonate – a new archive to estimate the Last Glacial minimum permafrost depth in Central Europe

2012

Abstract. Cryogenic cave carbonate (CCC) represents a specific type of speleothem whose precipitation is triggered by freezing of mineralized karst water. Coarsely crystalline CCC, which formed during slow freezing of water in cave pools, has been reported from 20 Central European caves located in Germany, the Czech Republic, Slovakia and Poland. All these caves are situated in an area which was glacier-free during the Weichselian. Whereas the formation of usual types of speleothems in caves of this region usually ceased during the glacials, coarsely crystalline CCC precipitation was restricted to glacial periods. Since this carbonate type represents a novel, useful paleoclimate proxy, data…

010506 paleontologyGroundwater flowStratigraphylcsh:Environmental protectionGeochemistryAquifer010502 geochemistry & geophysicsPermafrost01 natural scienceslcsh:Environmental pollutionLatent heatlcsh:TD169-171.8Glacial periodGeomorphologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary ChangegeographyHydrogeologygeography.geographical_feature_categoryPaleontology13. Climate actionlcsh:TD172-193.5QuaternaryGroundwaterGeologyClimate of the Past
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Fossiliferous Holocene tufa of Mende (Lozère, southern France): implication for the Atlantic vegetation of the Causses Basin

2016

International audience; Tufas bearing plant macroremains are uncommon in the Causses Basin (southern France). Here, we report anew fossiliferous tufa deposits at Mende, in Lozère. This palaeontological site is the first Quaternary tufa from thenorthern part of the Causses Basin that yields such an abundance of plant macroremains. The radiocarbon dating showsthat these Holocene deposits are related to the Atlantic period. Geomorphology and mineralogy show that theplant-bearing deposit is a calcareous tufa only composed by calcite, deposited near to an outlet of cool water, linked tothe karstic hydrological system of the Causse de Mende. The flora exposed in this article is dominated by angio…

010506 paleontologyLeavesAngiosperms010504 meteorology & atmospheric sciencesTilia cordataStructural basin01 natural sciencesTufslaw.inventionFeuillesPaleontologyLozèrelawRadiocarbon datingCausses BasinHolocene0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryBassin des CaussesHolocenebiologylcsh:QE1-996.5GeologyVegetationTufasbiology.organism_classificationKarstlcsh:GeologyTufaAngiospermesQuaternary[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyHolocène
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Le système palatial franc: genèse et fonctionnement dans le nord-ouest du regnum

1990

Barbier Josiane. Le système palatial franc : genèse et fonctionnement dans le nord-ouest du regnum.. In: Bibliothèque de l'école des chartes. 1990, tome 148, livraison 2. pp. 245-299.

010506 paleontologyLinguistics and LanguageHistory060102 archaeologyCapitales et chefs-lieux06 humanities and the artsStructures administratives01 natural sciencesLanguage and LinguisticsRituels politiques[SHS.HIST] Humanities and Social Sciences/History0601 history and archaeology[SHS.HIST]Humanities and Social Sciences/History0105 earth and related environmental sciences
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High-resolution geochemical and biotic records of the Tethyan 'Bonarelli Level' (OAE2, latest Cenomanian) from the Calabianca-Guidaloca composite sec…

2004

Abstract High-resolution micropalaeontological and chemostratigraphic records for the upper Cenomanian portion of the Calabianca–Guidaloca composite section (NW Sicily) provide new insight into the palaeoclimatic and palaeoceanographic evolution of the Tethys Ocean. The Bonarelli Level equivalent was identified on the basis of lithology and well constrained by calcareous plankton biostratigraphy and radiolarian assemblages, as well as by the δ 13 C curve showing a marked positive excursion (up to 4.7‰). The Bonarelli Level equivalent deposition is characterized by highly eutrophic conditions as testified by radiolarian proliferation. Black shale samples from the Calabianca–Guidaloca composi…

010506 paleontologyLithologyBiostratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesMicrofossilsCretaceousForaminiferaPaleontologyPalaeoceanography14. Life underwaterSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyPaleontologyCretaceous Sicily Corg-rich deposits Bonarelli level equivalent Microfossils Geochemical proxies Palaeoceanography15. Life on landbiology.organism_classificationTethys OceanAnoxic watersCretaceous13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBonarelli level equivalentCenomanianGeology
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