Search results for "LYN"

showing 10 items of 910 documents

Two-dimensional Banach spaces with polynomial numerical index zero

2009

We study two-dimensional Banach spaces with polynomial numerical indices equal to zero.

/dk/atira/pure/subjectarea/asjc/2600/2608/dk/atira/pure/subjectarea/asjc/2600/2607Eberlein–Šmulian theoremBanach manifoldFinite-rank operatorPolynomialMatrix polynomialFOS: MathematicsDiscrete Mathematics and Combinatorics/dk/atira/pure/subjectarea/asjc/2600/2602C0-semigroupLp spaceMathematicsMathematics::Functional AnalysisNumerical AnalysisBanach spaceAlgebra and Number TheoryMathematical analysisFunctional Analysis (math.FA)Mathematics - Functional Analysis46B04 (Primary) 46B20 46G25 47A12 (Secondary)Polynomial numerical indexInterpolation space/dk/atira/pure/subjectarea/asjc/2600/2612Geometry and TopologyNumerical rangeMonic polynomialLinear Algebra and its Applications
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Symmetric and finitely symmetric polynomials on the spaces ℓ∞ and L∞[0,+∞)

2018

We consider on the space l∞ polynomials that are invariant regarding permutations of the sequence variable or regarding finite permutations. Accordingly, they are trivial or factor through c0. The analogous study, with analogous results, is carried out on L∞[0,+∞), replacing the permutations of N by measurable bijections of [0,+∞) that preserve the Lebesgue measure.

010101 applied mathematicsCombinatoricsMathematics::CombinatoricsLebesgue measureSymmetric polynomialGeneral Mathematics010102 general mathematics0101 mathematicsInvariant (mathematics)Bijection injection and surjection01 natural sciencesMathematicsMathematische Nachrichten
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Changements environnementaux survenant à la limite Oligocène/Miocène du bassin des Limagnes (Massif central, France).

2018

16 pages; International audience; Continental environments are very sensitive to climatic variations. A unique opportunity to study the climate changes around the Oligocene/Miocene boundary is offered by the Limagne graben Basin (France) where this stage boundary is well constrained by fossils. Indeed, some localities of the Limagne Graben Basin are so rich in mammal remains that they have become a European reference for mammal biostratigraphy. The dominant sedimentary facies of the lacustrine deposits in the northern part of the Limagne Graben Basin are composed of poorly cemented marls and calcarenites containing various plants and animals remains (e.g. algae, fish bones and teeth, gastro…

010504 meteorology & atmospheric sciencesContext (language use)Biostratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrycarbonates lacustresMarl14. Life underwaterstromatolitebassin des Limagnes0105 earth and related environmental sciencesPalynologygeographygeography.geographical_feature_categoryLimagne Basinisotopes de l’oxygènebiologylimite oligo-miocèneoxygen isotopeslcsh:QE1-996.5GeologyMassif15. Life on landbiology.organism_classificationlacustrine carbonateGrabenlcsh:GeologyStromatolite13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyapatitePeriod (geology)Oligocene/Miocene boundarybiozoneGeologyBSGF - Earth Sciences Bulletin
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Environmental change during the Early Cretaceous in the Purbeck-type Durlston Bay section (Dorset, Southern England): a biomarker approach.

2007

20 pages; International audience; The Purbeck-type section (Durlston Bay, Dorset, UK) exhibits littoral lagoonal to lacustrine facies. It shows a gradual climatic/environmental change from semi-arid conditions associated with evaporites at the Jurassic–Cretaceous transition, to a more humid climate at the end of the Berriasian. Though generally organic-poor (total organic carbon, TOC, <1.3%), the Durlston Bay section shows an organic-rich episode (TOC up to 8.5%) located at the transition from evaporitic to more humid facies. A biomarker study was performed in order to determine the origin of the organic matter (OM) in the section and see if changes in organic sources accompanied the genera…

010504 meteorology & atmospheric sciencesEnvironmental change[SDE.MCG]Environmental Sciences/Global ChangesBotryococcus010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeBottom waterSteranechemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry0105 earth and related environmental sciencesTotal organic carbonbiologyEcology15. Life on landbiology.organism_classification[SDE.MCG.CPE]Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry6. Clean waterCretaceousPalynofacies[ SDE.MCG ] Environmental Sciences/Global Changeschemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBayGeology
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Occurrence of fossil organic matter in modern environments: optical, geochemical and isotopic evidence

2011

International audience; This study relates to the input and fate of fossil organic matter (FOM) in the modern environment, and focuses on two experimental watersheds overlying Jurassic marls: Le Laval and Le Brusquet (1 km(2) in area), located near Digne, Alpes-de-Haute-Provence, France. Considering that FOM delivery is mainly a result of different processes affecting sedimentary rocks [(bio)chemical and mechanical weathering], samples from different pools were collected: bedrocks, weathering profiles, soils and riverine particles. The samples were examined using complementary techniques: optical (palynofacies methods), geochemical (Rock-Eval 6 pyrolysis, C/N ratio), molecular (gas chromato…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesMineralogyWeatheringatmospheric carbon010502 geochemistry & geophysics01 natural sciencesstorageGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarlEnvironmental ChemistryOrganic matterglobal carbon balance0105 earth and related environmental scienceschemistry.chemical_classificationvariabilitysedimentary-rocks[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryerosionPollutionPalynofaciesALPES DE HAUTE PROVENCE[ SDE.MCG ] Environmental Sciences/Global Changesmarine-sedimentschemistry13. Climate actionSoil waterrock-eval pyrolysis[SDE]Environmental SciencesErosionSedimentary rockmodern soilshaute-provencePyrolysisGeology
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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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Pollen and non-pollen palynomorph evidence of medieval farming activities in southwestern Greenland

2010

International audience; Radiocarbon dating, pollen and non-pollen palynomorph analyses from a lake core were used to establish the timing and effects of farming activities around Lake Igaliku, Eastern Settlement, Greenland. The absence of agro-pastoral impact before the medieval colonization by Europeans provides an opportunity to understand the development of farming activity in a pristine landscape. The results show that the first phase of clearance and grazing pressure, without the expansion of the Norse apophyte (native plant, in habitats created by humans) Rumex acetosa type, could have occurred in the 9–10th century A.D. The presence of Norse settlers and livestock is clearly recorded…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesGreenlandPlant ScienceRanunculusmedicine.disease_cause01 natural sciencesGrazing pressurelaw.inventionlawPollenGrazingmedicineColonizationRadiocarbon datingNon-pollen palynomorphsCoprophilous fungi0105 earth and related environmental sciencesPalynologybiologyEcologyPaleontology15. Life on landbiology.organism_classificationPalynology[SDE.ES]Environmental Sciences/Environmental and SocietyNon-pollen palynomorphs Palynology Grazing pressure Greenland13. Climate actionGrazing pressure[SDE.ES] Environmental Sciences/Environmental and SocietyGeology[ SDE.ES ] Environmental Sciences/Environmental and Society
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Land use change, soil erosion and alluvial dynamic in the lower Doubs Valley over the 1st millenium AD (Neublans, Jura, France)

2003

International audience; Geochemical and particle size analyses, surface scanning magnetic susceptibility, microscopic charcoal counting and pollen analysis, have been carried out on two cores from the lower Doubs valley in order to reconstruct the land use history. The interpretation of anthropogenic pollen indicators and micro-charcoal deposits is discussed in relation to the lithological variation of sedimentary accumulation and evolution of the settlement. The environmental changes which occurred during the 1st and the 6th century AD reflect the impact of human activities on the landscape in the immediate surroundings of the site. Multiproxy indicators indicate that soil erosion as a con…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencespalaeogeographymedicine.disease_cause01 natural sciences[ SHS.ENVIR ] Humanities and Social Sciences/Environmental studies[SHS.ENVIR] Humanities and Social Sciences/Environmental studiesPollenmedicineLand use land-use change and forestryCharcoalpalynologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesHydrologyLand useSurface scanningsedimentology15. Life on landerosionPerturbation (geology)1st millenium ADvisual_art[SHS.ENVIR]Humanities and Social Sciences/Environmental studiesvisual_art.visual_art_mediumAlluviumSedimentary rockPhysical geographyFranceGeologyfire
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Roman Rhine settlement dynamics evidenced by coin distribution in a fluvial environment (Oedenburg, Upper Rhine, France).

2008

International audience; On the basis of archaeological and alluvial records, this paper presents the first spatial analysis of artefacts in relation to the evolution of the Rhine River, at the Gallo-Roman site of Oedenburg, during the first four centuries AD. The dataset consisted of several thousand Roman artefacts found by pedestrian prospecting over the last twenty years, over half of which were coins. This dataset was used together with high-resolution topography and geomagnetic mapping, to reconstruct settlement evolution, both on the terrace and in the floodplain. A comprehensive monetary chart has been compiled for the Oedenburg site, which highlights four major phases of settlement.…

010506 paleontologyArcheologyFloodplain[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryTerrace (agriculture)Water tableFluvialContext (language use)01 natural sciences[SHS]Humanities and Social Sciences[ SHS ] Humanities and Social SciencesClimate change0601 history and archaeologyGeoarchaeology0105 earth and related environmental sciencesPalynologygeographygeography.geographical_feature_category060102 archaeologyRhine River06 humanities and the artsRoman Period15. Life on landArchaeologyFluvial impact[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryPeriod (geology)AlluviumCoin distribution
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Morphometry of Middle Bronze Age palstaves. Part II - spatial distribution of shapes in two typological groups, implications for production and expor…

2013

10 pages; International audience; For archaeologists, metallic artifacts are key materials to assess Middle Bronze Age production areas and cultural exchanges. Here, a set of 629 bronze palstaves excavated in northern France, belonging to Breton and Norman typological groups, was treated by (open) outline-based morphometrics with orthogonal polynomial regression. Using robust statistics developed for outlier detection, these Norman and Breton palstave outlines can be divided into two groups: those for which the shape fluctuates close to the standard shape, called "congruent" axes, and those which are far enough from this standard to be considered as "non-congruent", although they possess mo…

010506 paleontologyArcheologyHistory[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryOrthogonal polynomialsengineering.materialSpatial distribution01 natural sciencesBronze Age0601 history and archaeologyBronzeOpen contour0105 earth and related environmental sciencesMorphometricsAxe060102 archaeologyExportation06 humanities and the artsArchaeologyShape analysisTypologyArchaeology[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryengineeringMorphometricsPalstave
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