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showing 10 items of 57859 documents

Globorotalia truncatulinoides in Central - Western Mediterranean Sea during the Little Ice Age

2020

Abstract Globorotalia truncatulinoides oscillations have been recorded from different marine sediment cores collected in the central and western Mediterranean Sea. The abundances of this species over the last 500 yrs. demonstrates its potential value as bio-indicator of particular oceanographic condition during the Maunder Minimum (MM) event of the Little Ice Age (LIA). The comparison between the G. truncatulinoides abundance patterns of the Balearic Basin, central and south Tyrrhenian Sea and central and eastern Sicily Channel allows to highlight a similar response of this species during the MM event in the central-western Mediterranean Sea. The ecological meanings of this species and its …

010506 paleontology010504 meteorology & atmospheric sciencesMaunder MinimumMixed layerGloborotalia trucatulinoidesStructural basinOceanography01 natural sciencesMediterranean seaGloborotalia truncatulinoides Little Ice Age Maunder minimum Mediterranean Sea Mixed layerAbundance (ecology)Mixed layer14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryAdvectionPaleontologySedimentSettore GEO/01 - Paleontologia E PaleoecologiaGloborotalia truncatulinoidesOceanographyProductivity (ecology)13. Climate actionMediterranean seaLittle Ice AgeGloborotalia truncatulinoides; Maunder minimum; Little Ice AgeGeologyChannel (geography)
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Late glacial-postglacial North African landscape and forestmanagement : Palynological and anthracological studies in the caves of Kaf Taht el-Ghar an…

2021

This work presents the anthracological and archeopalynological results obtained within the project AGRIWESTMED (ERC AdG 230561), which has involved a comprehensive retrieval of archeobiological remains based on a systematic sampling strategy, beyond the recovery of the usual archeological materials. These surveys were conducted on three sites located in the North of Morocco: the cave of Kaf Taht-el-Ghar, 8 km southeast from Tetuan, and two caves within the El Khil complex, close to Tanger. Both plant micro- and macro-remains (charred wood) were studied through palynological and anthracological analyses, respectively.

010506 paleontology010504 meteorology & atmospheric sciencesPaleolític01 natural sciencesGrazing pressureCavePaleolithicAbies pinsapoGlacial periodNeolithicEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesPalynologyEpipaleolithicgeography.geographical_feature_categorybiologyEpipaleolithicPaleontologyVegetation15. Life on landbiology.organism_classificationNorthern MoroccoArchaeologyGeographyCharcoalPollenJuniper
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The response of a shallow lake and its catchment to Late Glacial climate changes — A case study from eastern Poland

2015

In this study we investigate how climate fluctuation in the Late Glacial period influenced the development of a lake and its catchment located in the East European Plain. We analyzed the sediments of the lake for pollen, subfossil Cladocera, macrofossils and chemical composition. We aimed at disentangling: (1) the climate changes and their limno-ecological responses, (2) temperature dynamics with the use of Cladocera-based transfer function (MJT) and macrofossil-based reconstruction of mean minimum July temperature (MMJT), (3) timing of the response of different proxies to environmental changes. The results of multiproxy analyses explicitly suggest that the main driver for changes in aquati…

010506 paleontology010504 meteorology & atmospheric sciencesta1171lake sedimentsDrainage basinClimate change01 natural sciencesAllerød oscillationGlacial periodYounger Dryas0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorySubfossilMacrofossil15. Life on landcatchment developmentsubfossil cladocera13. Climate actionClimatologylate glacialmulti-proxy analysista1181Terrestrial ecosystemPhysical geographyEast European plainGeology
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Winter climate signal in boreal clastic-biogenic varves : a comprehensive analysis of three varved records from 1890 to 1990 AD with meteorological a…

2017

Clastic-biogenic varves are widely used for reconstructing past climate: in boreal environments, the accumulation of minerogenic clasts on the lake floor is generally considered a proxy for past variations in spring floods reflecting previous winter conditions. However, the physical mechanisms behind this winter climate sensitivity and the influence of catchment type on the varve formation are not fully investigated. Here, we present a winter climate record inferred from the clastic laminae of three lakes located on the region of fine-grained tills in Eastern Finland spanning from AD 1890 to 1990. The minerogenic varve data are compared with instrumental meteorological and hydrological time…

010506 paleontology010504 meteorology & atmospheric sciencesta1172ta1171Drainage basinlake sedimentsNorthern Europecatchment dynamics01 natural sciencesProxy (climate)clastic-biogenic varvesta2180105 earth and related environmental sciencesgeographyVarvegeography.geographical_feature_categoryPaleontologyGeology15. Life on landRadiative forcingSubarctic climateclimate forcingBoreal13. Climate actionClastic rockClimatologyfine-grained tillsClimate sensitivityGeologyboreal climateGFF
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The paramount power of selection: From Darwin to Kauffman

1995

For approximately two decades now, the Darwinian interpretation of evolution has now been challenged in many ways. Modern criticisms make it difficult, even for the staunchest Darwinians, not to take a distance from Darwin’s bold phrases on the “power” of natural selection. Let me remind you of some famous declarations of Darwin on the subject: “It may be said that natural selection is daily and hourly scrutinising, throughout the world, every variation, even the slightest; rejecting that which is bad, preserving and adding up all that is good; silently and insensibly working, whenever and wherever opportunity offers, at the improvement of each organic being in relation to its organic and i…

010506 paleontology0303 health sciencesNatural selectionbusiness.industryInterpretation (philosophy)Subject (philosophy)selectionEnvironmental ethics01 natural sciencesPower (social and political)[SHS.HISPHILSO]Humanities and Social Sciences/History Philosophy and Sociology of Sciences03 medical and health sciencesDarwin (ADL)DarwinismArtificial intelligenceForm of the GoodRelation (history of concept)business030304 developmental biology0105 earth and related environmental sciencesMathematics
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La co-subjectivité soignant–famille–psychologue : soutenir la vie psychique du patient en réanimation. À propos de l’article de B. Golse et S. Misson…

2020

Resume Objectifs et champ de connaissances explore En reanimation, la question du lien se pose avec acuite lorsque le patient n’est plus conscient, est sedate, intube, qu’il semble absent psychiquement a la relation. Peut-on alors parler d’intersubjectivite supposant une forme d’interaction dynamique avec le patient ? Methode L’enjeu est ici de montrer a partir du texte de B. Golse et S. Missonnier que les dimensions intrapsychiques se trouvent du cote du soignant et de la famille et qu’il est possible en passant par l’intersubjectivite du soignant et de la famille de reinscrire le patient dans sa fonction de sujet. Ce texte a pour objectif de questionner la nature des espaces therapeutique…

010506 paleontology060302 philosophy06 humanities and the arts0603 philosophy ethics and religion01 natural sciencesComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences3. Good health[SHS]Humanities and Social Sciences
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Evidence of aerial volcanic activity during the Valanginian along the northern Tethys margin.

2009

7 pages; International audience; Stratigraphic measurement and sampling on three sections (Vergol, La Charce, and Montclus) through Valanginian deposits from the Vocontian Basin (southeastern France) reveals the occurrence of centimetre thick ochre-coloured layers, which can be correlated from one section to another. At least twelve of these are identified in sediments dated from the Pertransiens to Furcillata ammonite Zones. These horizons appear similar to previously described Oxfordian and Aptian bentonites, also from the Vocontian Basin. Clay-mineralogical and geochemical data are similar in the Valanginian ochre horizons and their enclosing marls except in one of these that shows a cla…

010506 paleontologyAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesBentonite.PaleontologyVolcanismPassive margin[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesAmmoniteHorizon (geology)geographygeography.geographical_feature_categoryPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageCretaceousVocontian BasinVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyValanginianlanguageBentoniteGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Environmental and climatic controls of the clay mineralogy of Albian deposits in the Paris and Vocontian basins (France)

2020

18 pages; International audience; High-resolution clay mineral analyses were performed on lower and middle Albian deposits from the Paris and Vocontian basins in order to specify the weathering conditions that prevailed at that time. The clay mineral assemblages are composed of small proportions of chlorite and vermiculitic clays associated with abundant illite, R0 type illite-smectite mixed-layers (smectite) and kaolinite. Clay minerals originated from the physical alteration and chemical weathering of rocks and soils outcropping on the Variscan massifs bordering the studied areas. In the Paris Basin, the covariation of illite and kaolinite suggests the reworking of these latter minerals f…

010506 paleontologyAptianOutcropGeochemistryWeatheringengineering.materialPalaeoclimate010502 geochemistry & geophysics01 natural sciencesParis BasinKaoliniteMortoniceras0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyPaleontologyAlbianMassifbiology.organism_classificationClay mineralsVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringClay mineralsGeologyCretaceous Research
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Inter-site variability in the season of shellfish collection on the central coast of British Columbia

2013

High-resolution stable oxygen isotope analysis of the bivalve Saxidomus gigantea from shell midden sites was applied to identify seasonal patterns of resource procurement on the central coast of British Columbia, Canada. A total of 90 archaeological shells were examined from eight distinct sites spanning a 4500-year period. Combining micro-growth pattern analysis with high-resolution stable oxygen isotope sampling allows for a precise season of collection to be determined in estuarine bivalves recovered from archaeological sites. The results of the stable oxygen isotope analysis provide insights into seasonally structured harvest of S. gigantea (butter clam), which is associated with differ…

010506 paleontologyArcheology01 natural sciencesIsotopes of oxygenSclerochronologymedicine0601 history and archaeology14. Life underwaterComputingMilieux_MISCELLANEOUSShellfish0105 earth and related environmental sciencesgeographygeography.geographical_feature_category060102 archaeologybiologyEstuary06 humanities and the artsSeasonalitymedicine.diseasebiology.organism_classificationSaxidomus giganteaMiddenFisheryOceanography[SDE]Environmental SciencesPeriod (geology)GeologyJournal of Archaeological Science
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A mitogenome sequence of an Equus hydruntinus specimen from Late Quaternary site of San Teodoro Cave (Sicily, Italy)

2020

Abstract Equus hydruntinus was a small equid that ranged from the Iberian Peninsula to Middle East. In Italy it has been considered present from the Middle Pleistocene to its extinction in the Middle-Late Holocene. E. hydruntinus shares plesiomorphic traits with other known Pleistocene equids. As a consequence, its classification has always been problematic. Genetic analyses on few fossil remains from Iran and Crimea have revealed that E. hydruntinus was more closely related to extant hemiones. To further investigate its systematic position, using target-enrichment capture and next-generation sequencing, we reconstructed a near complete mitogenome of a specimen from San Teodoro Cave from Si…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPleistoceneWestern EuropeSettore BIO/08 - Antropologia01 natural scienceslaw.inventionEquus hydruntinuSan Teodoro CaveQuaternaryPaleontologyGlaciationRefugium (population biology)CaveMitochondrial genomelawRadiocarbon datingGlacial periodEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary Changegeography.geographical_feature_categoryAncient DNAGeologyLGMGeographyAncient DNAQuaternary
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