Search results for "vel"

showing 10 items of 36904 documents

Occurrence of organic-matter-rich beds in Early Cretaceous coastal evaporitic setting (Dorset, UK): a link to long-term palaeoclimate changes?

2009

11 pages; International audience; In Dorset (southern U.K.), the Durlston Bay and Lulworth Cove sections expose lowermost Cretaceous coastal marine and non-marine partly evaporitic sediments (the so-called Purbeckian facies). An interval with organic matter (OM)-rich layers is recognized in both sections. This OM-rich interval is 20 m thick in the middle of the Durlston Bay section. Within these beds, a large OM accumulation is recorded, with total organic carbon (TOC) of up to 8.5 wt%. High hydrogen index (HI) values (up to 956 mgHC/gTOC) point to a Type I OM, generally considered as derived from algal-bacterial biomass. This contrasts with the OM present in the underlying and overlying in…

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesClimate changeJurassic[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPalynofaciesDeposition (geology)CretaceousPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterCoveSea level0105 earth and related environmental sciencesTotal organic carbonCretaceous.geographygeography.geographical_feature_categoryPaleontology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousPalynofaciesBotryococcus-type algae[ SDE.MCG ] Environmental Sciences/Global ChangesOceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPurbeckian faciesOrganic matterBayGeology
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The Mid-Cenomanian Event in southeastern France: evidence from palaeontological and clay mineralogical data.

2013

16 pages; International audience; Reconstruction of main palaeoenvironmental conditions across the Mid-Cenomanian Event (MCE I) in the hemipelagic Tethyan section of Blieux (Southeast France, Vocontian Basin) is proposed. Quantitative analyses of calcareous nannofossil, ammonoid and clay mineral assemblages have been made and compared with respect to sea level changes and the carbon cycle perturbations. The nannofossil primary productivity, as recorded by nannofossil fluxes and relative abundances of meso-eutrophic taxa, is low just below and during the MCE Ia, then slightly increases in the interval including the MCE Ib. The clay assemblages mainly consist of illite/smectite mixed-layers w…

010506 paleontology[SDE.MCG]Environmental Sciences/Global Changesengineering.material[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesClimatic conditionsPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySchloenbachiaCalcareous nannofossilsKaoliniteRelative species abundanceSea level[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesMiddle CenomanianbiologyAmmonoidsPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.organism_classificationCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringPrimary productivityCenomanianClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Radial Symmetry, the Anterior/Posterior Axis, and Echinoderm Hox Genes

2008

20 pages; International audience; The strangeness of echinoderm pentaradiality results from superposition of radial symmetry onto ancestral deuterostome bilaterality. The Extraxial- Axial Theory shows that echinoderms also have an anterior/posterior (A/P) axis developed independently and ontogenetically before radiality. The A/P axis is first established via coelomic stacking in the extraxial region, with ensuing development of the pentamerous hydrocoel in the axial region. This is strongly correlated with a variety of gene expression patterns. The echinoid Hox cluster is disordered into two different sets of genes. During embryogenesis, members of the posterior class demonstrate temporal, …

010506 paleontology[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyphylogeny01 natural sciencesHomology (biology)03 medical and health sciencesmorphologyextraxial-axial theoryHox geneEcology Evolution Behavior and Systematics030304 developmental biology0105 earth and related environmental sciences0303 health sciencesDeuterostomeEcologybiology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]Symmetry in biologyevo-devoAnterior Posterior AxishomologyAnatomybiology.organism_classification[ SDV.BID.EVO ] Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]EchinodermEvolutionary developmental biologySymmetry (geometry)[ SDV.BID.SPT ] Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyAnnual Review of Ecology, Evolution, and Systematics
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Dyke failures in the Province of Groningen (Netherlands) associated with the 1717 Christmas flood: a reconstruction based on geoscientific field data…

2020

AbstractThe 1717 Christmas flood is one of the most catastrophic storm surges the Frisian coast (Netherlands and Germany) has ever experienced. With more than 13,700 casualties it is the last severe storm surge with a death toll of this order. At the same time, little is known about the hydrodynamic conditions and the morphological effects associated with this storm surge.In this study, 41 potential dyke failures in the Province of Groningen (Netherlands) associated with the 1717 Christmas flood were systematically reconstructed and mapped by using historical maps and literature and by analysing the recent topography in search of typical pothole structures and sediment fans. The dimensions …

010506 paleontologyeducation.field_of_studyCoastal hazards010504 meteorology & atmospheric sciencesFlood mythPopulationStorm surgeSedimentGeology01 natural sciencesWater levelCurrent (stream)Physical geographyElectrical resistivity tomographyeducationGeology0105 earth and related environmental sciencesNetherlands Journal of Geosciences
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The Last Deglaciation of the Southeastern Sector of Scandinavian Ice Sheet

2006

The Scandinavian Ice Sheet (SIS) was an important component of the global ice sheet system during the last glaciation, but the timing of its growth to or retreat from its maximum extent remains poorly known. We used 115 cosmogenic beryllium-10 ages and 70 radiocarbon ages to constrain the timing of three substantial ice-margin fluctuations of the SIS between 25,000 and 12,000 years before the present. The age of initial deglaciation indicates that the SIS may have contributed to an abrupt rise in global sea level. Subsequent ice-margin fluctuations identify opposite mass-balance responses to North Atlantic climate change, indicating differing ice-sheet sensitivities to mean climate state.

010506 paleontologygeographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesClimate change01 natural sciencesIce-sheet modelOceanography13. Climate action[SDE]Environmental SciencesPaleoclimatologyDeglaciationGlacial periodClimate statePhysical geographyIce sheetComputingMilieux_MISCELLANEOUSSea levelGeology0105 earth and related environmental sciences
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Sandy fan‐like forms in the central‐eastern mazovian lowland (central poland): textural record and chronology

2016

A unique, continuous, fan-shaped belt of sandy landforms in the central-eastern Mazovian Lowland, Central Poland has been investigated using a multiproxy dataset of sediment physical properties and chronological framework. Although there are several previous studies of similar fan-like forms elsewhere in Central Poland, this central-eastern part has not been investigated in detail. A combined methodological approach, using grain-size distributions, the roundness, surface character and microtexture of quartz grains, and the mineral composition of the light and heavy fractions, indicate a predominantly aeolian origin for the fan-like forms. Overlying them are dunes, the sediment within which …

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesPleistoceneLandformGeography Planning and DevelopmentGeochemistrySedimentGeologyRoundness (geology)01 natural sciencesAeolian processesGlacial periodYounger DryasGeomorphologyGeology0105 earth and related environmental sciencesChronologyGeografiska Annaler: Series A, Physical Geography
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Depositional mechanism of the upper Pliocene-Pleistocene shelf-slope system of the western Malta Plateau (Sicily Channel)

2021

Abstract A high resolution seismic stratigraphic study of the western edge of the Malta Plateau (central Mediterranean Sea) was conducted to reconstruct the depositional mechanisms of the shelf-slope system since the end of the Messinian salinity crisis (MSC; 5.3 Ma). The accurate interpretation of a large grid of variable-resolution seismic reflection profiles (multichannel and Sub Bottom) allows us to identify and map a Plio-Quaternary sedimentary sequence overlying the Messinian evaporites. The stratal pattern of this sequence is the result of a clinoform prograding system that constitutes the internal structure of a sedimentary shelf developed in a ramp about 2° slope with bathymetries …

010506 paleontologygeographygeography.geographical_feature_categoryPlateauMessinian salinity crisisEvaporiteContinental shelfStratigraphyPlio-QuaternaryGeologySubsidence010502 geochemistry & geophysics01 natural sciencesSedimentary depositional environmentPaleontologySedimentary rockContinental shelf; Malta Plateau; Messinian salinity crisis; Plio-Quaternary; SicilyProgradationContinental shelfSicilyMalta PlateauGeologySea level0105 earth and related environmental sciences
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Sea–land geology of Marettimo (Egadi Islands, central Mediterranean sea)

2016

We present a 1:10,000 scale geological map of Marettimo Island and its offshore (Egadi Archipelago, central Mediterranean Sea). The map was achieved by integrating a new geological survey with data from recent, marine, geological and geophysical surveys acquired along the adjacent continental shelf. The island is composed of a Mesozoic, mostly carbonate platform succession, which is overlain by continental to coastal marine Quaternary deposits. Extensional tectonics have affected the carbonate platform since the Late Triassic producing an initial increase of accommodation space that was filled by interbed breccias, marls and calcareous marls. During the Jurassic, a NE-SW-directed normal fau…

010506 paleontologygeographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaContinental shelfCarbonate platformSettore GEO/03 - Geologia StrutturaleGeography Planning and Developmentstratigraphy010502 geochemistry & geophysics01 natural sciencestectonicPaleontologyTectonicsMediterranean seaArchipelagoMarlEarth and Planetary Sciences (miscellaneous)Egadi IslandExtensional tectonicsGeological surveyGeological Map geological survey stratigraphy tectonics Egadi IslandsQuaternaryGeology0105 earth and related environmental sciences
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Seismites resulting from high-frequency, high-magnitude earthquakes in Latvia caused by Late Glacial glacio-isostatic uplift

2016

Abstract Geologically extremely rapid changes in altitude by glacial rebound of the Earth crust after retreat of the Scandinavian Ice Sheet at the end of the last Weichselian glaciation influenced the palaeogeography of northern Europe. The uplift of the Earth crust apparently was not gradual, but shock-wise, as the uplift was accompanied by frequent, high-magnitude earthquakes. This can be deduced from strongly deformed layers which are interpreted as seismites. Such seismites have been described from several countries around the Baltic Sea, including Sweden, Germany and Poland. Now similarly deformed layers that must also be interpreted as seismites, have been discovered also in Latvia, a…

010506 paleontologygeographygeography.geographical_feature_categorySoft-sediment deformation structures (SSDS) SeismitesGeography Planning and DevelopmentMagnitude (mathematics)PaleontologyPost-glacial rebound010502 geochemistry & geophysics01 natural sciencesLatviaQE701-760PaleontologyTectonic upliftAltitudeEarthquake recurrence timeGlacio-isostatic reboundGlacial periodIce sheetWeichselian glaciationPalaeogeographySeismologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Palaeogeography
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Geological Setting and Paleoecology of the Upper Cretaceous Bench 19 Marine Vertebrate Bonebed at Bentiaba, Angola

2014

AbstractThe Bench 19 Bonebed at Bentiaba, Angola, is a unique concentration of marine vertebrates preserving six species of mosasaurs in sediments best correlated by magnetostratigraphy to chron C32n.1n between 71.4 and 71.64 Ma. The bonebed formed at a paleolatitude near 24°S, with an Atlantic width at that latitude approximating 2700 km, roughly half that of the current width. The locality lies on an uncharacteristically narrow continental shelf near transform faults that controlled the coastal outline of Africa in the formation of the South Atlantic Ocean. Biostratigraphic change through the Bentiaba section indicates that the accumulation occurred in an ecological time dimension within …

010506 paleontologygeographygeography.geographical_feature_categorybiologyContinental shelfFaunaGeology010502 geochemistry & geophysicsbiology.organism_classificationMosasaur01 natural sciencesCretaceous/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterPaleontologyMarine vertebratePrognathodonPaleoecology14. Life underwaterSDG 14 - Life Below WaterGeologyMagnetostratigraphy0105 earth and related environmental sciencesNetherlands Journal of Geosciences = Geologie en Mijnbouw
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