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showing 10 items of 6821 documents

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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Variations morphologiques des Toxaster (Echinoida : Spatangoida) en regard des fluctuations spatiales (Arc de Castellane, SE France) et temporelles (…

2006

Resume L'impact du milieu sedimentaire sur l'installation, la croissance et la morphologie de spatangues primitifs du Cretace inferieur, est analyse chez le genre Toxaster dans le Valanginien et l'Hauterivien de l'Arc de Castellane au Nord de la plate-forme provencale. Les analyses concernent la dimension spatiale a partir de l'etude comparative de six populations isochrones de Toxaster granosus kiliani de la biozone a Verrucosum distribuees le long d'un gradient proximo-distal, puis la dimension temporelle a partir de l'etude d'une coupe de reference (Carajuan) couvrant l'intervalle stratigraphique Valanginien superieur–Hauterivien superieur et concernant principalement les especes T. gran…

010506 paleontologyMorphométrieMilieux sédimentairesSE FranceSpatanguesPaleontologyPaléoécologie010502 geochemistry & geophysics01 natural sciencesSpace and Planetary ScienceValanginien–Hauterivien[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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ESR/U-series chronology of early Neanderthal occupations at Cova Negra (Valencia, Spain)

2019

Abstract The spatiotemporal repartition of Neanderthal populations throughout the late Middle and early Upper Pleistocene is of great interest for our understanding of human evolution. Establishing a reliable chronology for human-bearing layers from prehistoric sites is thus essential for the study of Neanderthal population dynamics prior to modern human arrival in Europe. Cova Negra (Valencia, Spain) is one of the richest sites documenting Neanderthal fossil bones in the Iberian Peninsula (Arsuaga et al., 1989, 2007; Villaverde et al., 2014). The stratigraphic sequence includes 15 Middle Palaeolithic layers. Among them, four were dated by the ESR/U-series dating method on enamel from six h…

010506 paleontologyNeanderthalPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryStratigraphyPopulation010502 geochemistry & geophysics01 natural sciences[SHS]Humanities and Social SciencesPrehistoryCavebiology.animalEarth and Planetary Sciences (miscellaneous)RepartitioneducationComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesgeographyeducation.field_of_studygeography.geographical_feature_categorybiologyGeologyArchaeologyHuman evolutionGeologyChronology
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Climatic fluctuations and seasonality during the Late Jurassic (Oxfordian–Early Kimmeridgian) inferred from delta18O of Paris Basin oyster shells.

2008

10 pages; International audience; Oxygen isotope data from biostratigraphically well-dated oyster shells from the Late Jurassic of the eastern Paris Basin are used to reconstruct the thermal evolution of western Tethyan surface waters during the Early Oxfordian–Early Kimmeridgian interval. Seventy eight oyster shells were carefully screened for potential diagenetic alteration using cathodoluminescence microscopy. Isotope analyses were performed on nonluminescent parts of shells (n=264). Intra-shell δ18O variability was estimated by microsampling along a transect perpendicular to the growth lines of the largest oyster shell. The sinusoidal distribution of the δ18O values along this transect …

010506 paleontologyOysterδ18O[SDE.MCG]Environmental Sciences/Global ChangesJurassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologycarbonateGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.animalParis BasinEarth and Planetary Sciences (miscellaneous)medicinepaleotemperatureBathymetry14. Life underwaterTransect0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyoxygen isotopesSeasonalitymedicine.disease[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryDiagenesisWaves and shallow water[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphyoysters[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Continental-scale temperature variability during the past two millennia

2013

Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructi…

010506 paleontologyPALAEOCLIMATE AND PALAEOCENOGRAPHYPaleoclimate010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Climate change[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]910 Geography & travel01 natural sciencesCiencias de la Tierra y relacionadas con el Medio AmbienteInvestigación ClimatológicaCentennial550 Earth sciences & geology540 ChemistryPaleoclimatologyIce ageEarth temperaturePaleoclimatologySouthern Hemisphere0105 earth and related environmental sciencesCLIMATE SCIENCEAtmospherePaleoclimate; Temperature; Little Ice Age; Medieval Warm PeriodsTemperatureNorthern HemisphereClimatic changesScale (music)ClimatologyMedieval Warm PeriodsLittle Ice AgePeriod (geology)570 Life sciences; biologyGeneral Earth and Planetary SciencesCIENCIAS NATURALES Y EXACTASGeologyNature Geoscience
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Les ammonites du Pliensbachien du jebel Bou Rharraf (Haut Atlas oriental, Maroc).

2011

60 pages; International audience; L'originalité des dépôts sédimentaires et des faunes d'ammonites du jebel Bou Rharraf repose sur la présence de faciès « Ammonitico Rosso », les plus occidentaux connus pour le Pliensbachien, une forte diversité des Phylloceratida (Phylloceras, Calaiceras, Zetoceras, Partschiceras et Juraphyllites) et une disparité morphologique importante chez les Galaticeras, Miltoceras et les Tauromeniceras. Si quelques formes, telles que Miltoceras taguendoufi et Mauretaniaceras elmii nov. gen., nov. sp. ont un cachet endémique très affirmé, les faunes du Pliensbachien du Haut Atlas oriental sont classiques pour la marge sud de la Téthys occidentale. Trois genres (Callo…

010506 paleontologyPaleontologyJurassique inférieur010502 geochemistry & geophysicsPliensbachien01 natural sciencesMarocBiostratigraphieSpace and Planetary ScienceAmmonites[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyHaut AtlasPaléobiogéographie
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First report of Gogia (Eocrinoidea, Echinodermata) from the Early-Middle Cambrian of Sonora (Mexico), with biostratigraphical and palaeoecological co…

2009

10 pages; International audience; The blastozoan echinoderm genus Gogia is reported for the first time in the Early and the Middle Cambrian of Mexico. Reports in different members of the section of San José de Gracia (Sonora State, northwestern Mexico) extend the palaeogeographical range of the genus to the South Laurentia, and the stratigraphic range of Gogia granulosa to the whole first half of middle Middle Cambrian. Isolated plates occur in rocks deposited in detrital inner platform and complete specimens, in carbonate outer platform, confirming their ability to live in diverse environments. Their presence in these different environments through the Early-Middle Cambrian on Laurentia ag…

010506 paleontologyPaleozoicGogiaStratigraphyBiostratigraphyBlastozoa010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesGogiaBlastozoaPaleontology14. Life underwaterMiddle CambrianEocrinoideaMexico0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologybiologyPaleontologyPalaeoecologyCrinozoabiology.organism_classificationSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPaleoecologyLaurentia[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyEchinodermata
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The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years

2016

AbstractThe Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time and space. We highlight the prompt response of surface water ecosystems to both orbital- and suborbital-climatic variations.A markedly different spatial response was observed in calcareous plankton assemblages, possibly due to the influence of the North Atlantic climatic system in the western, central and northern areas and of the monsoon system in the easternmost and southern sites. Orbita…

010506 paleontologyQE1-996.5010504 meteorology & atmospheric sciencesGeologyForcing (mathematics)Environmental Science (miscellaneous)Plankton01 natural scienceslate quaternaryMediterranean seaOceanographyplanktonic foraminiferaClimatologyGeneral Earth and Planetary SciencesEcosystemUniquenessmediterranean seacoccolithophoresGeology0105 earth and related environmental sciencesOpen Geosciences
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An aeolian or a glaciolacustrine record? A case study from Mieļupīte, Middle Gauja Lowland, northeast Latvia

2017

Abstract In the Middle Gauja Lowland, northeast Latvia, dunes are distributed over a vast glaciolacustrine plain that formed during the retreat of the Fennoscandian ice sheet. Such a direct contact between aeolian and glaciolacustrine sediments can be used to infer depositional settings and decipher to what extent these sediments bear an aeolian component. Our proxies, although preliminary, reveal a limited range of variation in grain-size parameters, a significant presence of quartz grains with silica precipitation and matt-surface grains of various rounding degrees and massive structure combined with horizontal lamination. These are indicative of periglacial-aeolian depositional condition…

010506 paleontologyQE1-996.5Optically stimulated luminescenceEarth sciencequartz grainsGeologyBaltic states010502 geochemistry & geophysicsbaltic states01 natural sciencesduneice-dammed lakelinkuva ice-marginal zoneGeneral Earth and Planetary SciencesAeolian processesLinkuva ice-marginal zoneoptically stimulated luminescenceGeomorphologyGeology0105 earth and related environmental sciencesGeologos
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Ammonite paleobiogeography during the Pliensbachian-Toarcian crisis (Early Jurassic) reflecting paleoclimate, eustasy, and extinctions.

2011

14 pages; International audience; The Pliensbachian-Toarcian crisis (Early Jurassic) is one of the major Mesozoic paleoecological disturbances when ca. 20% of marine and continental families went extinct. Contemporaneously, profound paleobiogeographical changes occurred in most oceanic domains including a disruption of ammonite provincialism during the Early Toarcian. Here, we quantitatively reappraise the structure and evolution of paleobiogeographical patterns displayed by ammonite faunas before, during, and after the biological crisis, over a time-interval including 13 biochronozones. The high-resolution study presented here involves the use of hierarchical Cluster Analyses, non-metric M…

010506 paleontologyRange (biology)Biome010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyPaleoclimatologypaleoclimateprovincialism14. Life underwaterMesozoic0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyExtinction eventAmmoniteGlobal and Planetary ChangeExtinctionammonitesEarly Jurassicpaleobiogeography15. Life on landlanguage.human_languageArctic13. Climate actionlanguagemass extinction[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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