Search results for "LCA"

showing 10 items of 1995 documents

New Insights into the Provenance of the Obsidian Fragments of the Island of Ustica (Palermo, Sicily)

2016

In this study we applied a multidisciplinary approach, coupling geophysical and geochemical measurements, to unveil the provenance of 170 obsidian flakes, collected on the volcanic island of Ustica (Sicily). On this island there are some prehistoric settlements dated from the Neolithic to the Middle Bronze Age. Despite not having geological outcrops of obsidian rocks, the countryside of Ustica is rich in fragments of this volcanic glass, imported from other source areas. The study of obsidian findings was carried out first through visual observations and density measurements. At least two different obsidian families have been distinguished, probably imported from Lipari and Pantelleria isla…

010506 paleontologyArcheologyHistoryProvenance060102 archaeologyVolcanic islandOutcrop06 humanities and the arts01 natural sciencesArchaeologyVolcanic glassPrehistorychemistry.chemical_compoundchemistryBronze Age0601 history and archaeologyGeology0105 earth and related environmental sciencesEMPAArchaeometry
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Copper supply during the Final Neolithic at the Saint-Blaise/Bains des Dames site (Neuchâtel, Switzerland)

2009

The Saint-Blaise/Bains des Dames stratified site in Neuchâtel, Switzerland, contains several occupations that span the Late through Final Neolithic, including the Horgen, Lüscherz, and Auvernier-Cordé periods. As part of a study on prehistoric metallurgy in western Switzerland, we compare the lead isotope ratios (multicollector inductively coupled plasma mass spectrometer) and elemental compositions (instrumental neutron activation analysis) of the site's numerous copper finds to a database of corresponding measurements for copper ores throughout Europe. The results show a considerable variation in copper compositions present at the site, suggesting complex economic relationships and multip…

010506 paleontologyArcheologyProvenance[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryLead isotope analysischemistry.chemical_element01 natural sciencesPrehistoryFinal Neolithic- Archeometry- Pb isotope analysis - Archeometallurgy - CopperGEO/08 - GEOCHIMICA E VULCANOLOGIA550 Earth sciences & geology0601 history and archaeologyMC-ICP-MSComputingMilieux_MISCELLANEOUSddc:599.90105 earth and related environmental sciences[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory060102 archaeologyMc icp msMetal analysisFinal Neolithic06 humanities and the artsMetal analysisArchaeologyCopperGeographychemistryAnthropologyCopper
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Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption

2021

Climatic warming from the last glacial maximum to the current interglacial period was punctuated by a similar to 1300 years long cold period, commonly referred to as the Younger Dryas (YD). Several hypotheses have been proposed for the mechanism triggering the abrupt inception of the YD, including freshwater forcing, an extra-terrestrial impact, and aerosols from volcanic eruptions. Here, we use synchronised sulphate and sulphur records from both Greenland and Antarctic ice cores to reconstruct volcanic forcing between 13,200-12,800 a BPGICC05 (years before 1950 CE on the Greenland Ice Core Chronology 2005; GICC05). This continuous reconstruction of stratospheric sulphur injections highligh…

010506 paleontologyArcheologyYounger Dryas010504 meteorology & atmospheric sciences530 PhysicsCIRCULATIONIce cores; Laacher See eruption; Sulphate; Volcanic radiative forcing; Younger DryasSULFURForcing (mathematics)01 natural sciencesVolcanic radiative forcingANTARCTIC ICE-CORESOCEANIce coreCHRONOLOGYYounger Dryas550 Earth sciences & geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeologyLast Glacial MaximumRECORDWAIS DIVIDESulphateRadiative forcingGREENLANDLaacher See eruptionVolcano13. Climate actionIce coresClimatologySYNCHRONIZATIONInterglacialClimate modelSULFATEGeologyQuaternary Science Reviews
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The first archaeometric characterization of obsidian artifacts from the archaeological site of Samshvilde (South Georgia, Caucasus)

2019

This paper presents the first results about the provenance of obsidian fragments recovered in the archaeological site of Samshvilde (South Georgia, Caucasus) with the aim to obtain knowledge related to the network distribution and procurement of obsidian in Georgia. The geochemical characterization of thirty archaeological finds was obtained by the LA-ICP-MS method, an almost non-destructive technique capable of chemically characterizing the volcanic glass. A comparison of geochemical results obtained on both archaeological artefacts and geological samples collected from Chikiani outcrop in Georgia, together with literature data of southern Caucasus and eastern Turkey, allowed us to define …

010506 paleontologyArcheologygeographyProvenancegeography.geographical_feature_category060102 archaeologyOutcrop06 humanities and the arts01 natural sciencesArchaeologyVolcanic glassObsidian Trace elements LA-ICP-MS Samshvilde GeorgiaVolcanoAnthropology0601 history and archaeologySettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.Geology0105 earth and related environmental sciencesArchaeological and Anthropological Sciences
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The ELSA tephra stack: Volcanic activity in the Eifel during the last 500,000 years

2016

Abstract Tephra layers of individual volcanic eruptions are traced in several cores from Eifel maar lakes, drilled between 1998 and 2014 by the Eifel Laminated Sediment Archive (ELSA). All sediment cores are dated by 14C and tuned to the Greenland interstadial succession. Tephra layers were characterized by the petrographic composition of basement rock fragments, glass shards and characteristic volcanic minerals. 10 marker tephra, including the well-established Laacher See Tephra and Dumpelmaar Tephra can be identified in the cores spanning the last glacial cycle. Older cores down to the beginning of the Elsterian, show numerous tephra sourced from Strombolian and phreatomagmatic eruptions,…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEarth scienceGeochemistry010502 geochemistry & geophysicsOceanography01 natural sciencesLapilliStrombolian eruptionMaarVolcanoMagmaPhreatomagmatic eruptionTephraTephrochronologyGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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Influence of dissolved organic matter on rare earth elements and yttrium distributions in coastal waters

2010

International audience; Data collected during this study indicate that dissolved Y and REE (rare earth element) behaviour can be monitored through shale-normalised ratios. Relationships occurring between these ratios suggest that leaching from lithogenic materials is the main source of REE in the studied area. This process involves riverine detrital matter in the inner area of the Gulf of Palermo. Features of shale-normalised patterns and the relationship recognised between dissolved Fe and Y/Ho suggest that REE are released from Fe-rich coatings of atmospheric dust. Observed similarities between dissolved Fe and chlorophyll- content suggest that leaching of Fe-rich atmospheric particulates…

010506 paleontologyMineralogyrare earth elementsMediterranean010502 geochemistry & geophysics01 natural sciencesMediterranean seaDissolved organic carbonMediterranean Sea[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyOrganic matter14. Life underwaterScavengingEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental Sciencechemistry.chemical_classificationEcologyRare-earth elementAuthigenicParticulatesREE; Mediterranean; Ce anomalyREESettore GEO/08 - Geochimica E VulcanologiachemistryCe anomaly13. Climate actionEnvironmental chemistryGeneral Earth and Planetary SciencesSeawaterchlorophyll-YREE Ce anomaly Central Mediterranean late Quaternary Palaeoenvironmental reconstructionGeologyChemistry and Ecology
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The end of the Messinian salinity crisis: Evidences from the Chelif Basin (Algeria).

2007

How did the Messinian Salinity Crisis end is a matter of intense debate between two opposite concepts i.e., the generalised dilution event, the so-called Lago–Mare, followed by the sudden restoration of the marine conditions at the base of the Zanclean, or the early partial or complete marine refill that would have happened earlier during the upper Messinian. The Chelif Basin of Northwestern Algeria, one of the greatest Messinian marginal basins of the Mediterranean, provides an exceptional opportunity to study in detail how this major paleoenvironmental change occurred through continuous sedimentary records of the Miocene–Pliocene boundary. Five sections representative of both the central …

010506 paleontologyOstracodSettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OForaminiferaStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaPaleontologyMessinianOstracodZanclean14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyStable IsotopesMediterranean basinPaleontologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneAlgeriaClastic rockLago–MareSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyChelif basinGeologyMarine transgression
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Palynofacies and calcareous nannofossils in the Upper Kimmeridgian, southeastern Paris basin (France)

2005

AbstractThe Upper Kimmeridgian Members “Calcaires blancs supérieurs” and the “Marnes à exogyres supérieures” of the southeastern Paris basin were investigated for their palynofacies and calcareous nannofossils. These members display alternating limestone-marl lithotypes and represent shallow marine palaeoenvironments. The lower carbonate member is interpreted as a proximal palaeoenvironment (palaeobathymetry = 5 to 10 m), where storm and swell deposits were prevalent and the salinity was occasionally weak. The relative richness of brown phytoclasts in this part is favoured by good preservation related to restricted conditions. These conditions would explain the dominance of the nannofoss…

010506 paleontologyPalaeoenvironments010502 geochemistry & geophysics01 natural sciencesPalynofaciesSedimentary depositional environmentCoccolithPaleontologychemistry.chemical_compoundMarlCalcareous nannofossilsDominance (ecology)14. Life underwaterCoquina0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalynologyUpper KimmeridgianMarine shallow-water dépositsGeologyParis basinPalynofacieschemistryCarbonate[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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The metamorphic rocks of the Nunatak Viedma in the Southern Patagonian Andes: Provenance sources and implications for the early Mesozoic Patagonia-An…

2019

The Nunatak Viedma within the Southern Patagonian Icefield has been considered as a volcanic center based on its geomorphologic features, despite the fact that field explorations by Eric Shipton determined its metamorphic nature 70 years ago. We carried out fieldwork to characterize this isolated outcrop and performed the first U-Pb dating in detrital zircons from the basement rocks located inside the Southern Patagonian Icefield. We recognized very-low grade metamorphic rocks, corresponding principally to metapelites and metapsammites, and scarce metabasites. Detrital zircons in three metapsammitic samples (composite group of 240 grains) yielded prominent age population peaks at ∼1090, ∼96…

010506 paleontologyProvenanceNunatakVery-low grade metamorphic rocksOutcropMetamorphic rockPopulationDetrital zircons agesDETRITAL ZIRCONS AGES[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesSouthwestern GondwanaCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]Southern Patagonian Andes//purl.org/becyt/ford/1.5 [https]PaleontologyAntarctic PeninsulaCarboniferousGeologíaVERY-LOW GRADE METAMORPHIC ROCKSeducationCiencias Exactas y NaturalesSOUTHWESTERN GONDWANA0105 earth and related environmental sciencesEarth-Surface Processesgeographyeducation.field_of_studygeography.geographical_feature_categoryVolcanic arcGeologySOUTHERN PATAGONIAN ANDESGondwanaANTARCTIC PENINSULANUNATAK VIEDMANunatak ViedmaCIENCIAS NATURALES Y EXACTASGeology
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Integrated bio- and carbon-isotope stratigraphy of the Upper Cretaceous Gurpi Formation (Iran): A new reference for the eastern Tethys and its implic…

2018

29 pages; International audience; A high-resolution stratigraphic analysis of the Upper Cretaceous Gurpi Formation has been undertaken in the Shahneshin section (Zagros Basin, Iran). New results on calcareous nannofossils, planktic foraminifers, dinoflagellate cysts and high-resolution carbon and oxygen stable isotopes form the basis of a reference section for the eastern Tethys that spans the upper Coniacian to the late Danian. Carbon-isotope correlation to Gubbio, Italy and the NW German chalk allows for the identification of many isotopic events as well as for the definition of new events in the Campanian and Maastrichtian. Our results allow for a review of the accurate position of the C…

010506 paleontologyStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryStage (stratigraphy)Calcareous nannofossils14. Life underwater0105 earth and related environmental sciencesbiologyStable isotope ratioDinoflagellate cystsCarbon isotopesDinoflagellatePaleontologyPlanktic foraminiferaPlanktonbiology.organism_classificationZagrosCretaceousStratigraphy13. Climate actionIsotopes of carbonTethyan realm[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyConiacian–MaastrichtianGeologyCretaceous Research
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