Search results for "Conti"

showing 10 items of 3486 documents

Late Quaternary coastal uplift of southwestern Sicily, central Mediterranean sea

2021

Abstract Mapping and luminescence aging of raised marine terraces and aeolian ridges along an ∼90 km coastal stretch in southwestern Sicily provide the first quantitative assessment of vertical tectonic deformation in this region, which spans the frontal part of an active thrust belt. We recognized a staircase of eleven terraces and nine related aeolian ridges. The elevation profile of terraces parallel to the coast shows a >90 km long bell-shaped pattern, onto which shorter-wavelength (∼10 km long) undulations are superimposed. Luminescence ages from terraced beach deposits and aeolian sediments constrain the position of paleoshorelines formed during MIS 5e, 7a and 7c, with a maximum uplif…

010506 paleontologyArcheologyMarine terracesEarly Pleistocene010504 meteorology & atmospheric sciencesPleistoceneLuminescence datingSettore GEO/03 - Geologia StrutturaleFold growth01 natural sciencesMarine terracePaleontologyMediterranean seaContinental marginAeolian ridgeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangegeographyFrontal thrust beltgeography.geographical_feature_categoryThermoluminescence datingBedrockGeologyPleistoceneMediterranean seaAeolian ridgesAeolian processesQuaternaryGeologySouthwestern sicilyQuaternary Science Reviews
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Environmental responses of past and recent agropastoral activities on south Greenlandic ecosystems through molecular biomarkers

2016

Paleoenvironmental studies previously performed on Lake Igaliku revealed two agropastoral phases in south Greenland: the Norse settlement from AD 986 to ca. AD 1450 and the recent installation of sheep farmers, since the 1920s. To improve the knowledge of the timing and magnitude of the Greenlandic agropastoral activities, a lipid inventory was realized and compared with biological and geochemical data. During the 12th century, a major increase in deoxycholic acid (DOC) and coprophilous fungal spores revealed a maximum of herbivores. Synchronously, a minimum of the n-C29/ n-C31 alkane ratio and tree and shrub pollen and a maximum of triterpenyl acetates showed a reduction in the tree and s…

010506 paleontologyArcheologysouth Greenlandved/biology.organism_classification_rank.specieslake sediments010502 geochemistry & geophysicsmedicine.disease_cause01 natural sciencesShrubmolecular biomarkersPollenGrazingmedicine[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentEcosystemRumex[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeHerbivoreEcologybiologyEcologyved/biologyPaleontology15. Life on landbiology.organism_classificationMolecular biomarkersagropastoral activities13. Climate actionPlant speciesNorseGeologyecosystem responses
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Astrochronology of the Valanginian Stage from reference sections (Vocontian Basin, France) and palaeoenvironmental implications for the Weissert Even…

2013

12 pages; International audience; High-resolution gamma-ray measurements performed on five biostratigraphically well-dated reference sections from the Vocontian Basin (south-eastern France) are used to develop a new astrochronology of the Valanginian Stage and its subdivisions (i.e. ammonite and calcareous nannofossil zones and subzones). Spectral analyses show a pervasive dominance of 405-kyr eccentricity cycles with the expression of 100-kyr eccentricity, obliquity and precession. Previous rough estimates of Valanginian Stage duration ranged from 3.9 to 6.5 myr but were generally based on less reliable or indirect methods. This study provides a precise duration of 5.08 myr, tuning the ser…

010506 paleontologyBiozone[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanographyPalaeoclimate01 natural sciencesPaleontologyGeologic time scaleStage (stratigraphy)Ecology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesAmmoniteAstrochronologySeries (stratigraphy)High-resolution gamma-rayParaná-EtendekaPaleontologyCyclostratigraphylanguage.human_languageVocontian BasinStratigraphy13. Climate actionValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguageGeologyWeissert Event
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The relationships between soft-sediment deformation structures and synsedimentary extensional tectonics in Upper Triassic deep-water carbonate succes…

2016

Abstract We describe soft-sediment deformation structures into the Upper Triassic cherty limestone outcropping in the Pizzo Lupo section (Central Sicily, Italy), pertaining to the deep-water palaeodomain of the Southern Tethyan margin. In the study section, mainly consisting of thin-bedded mudstone/marl alternations with bedded chert intercalations, some lithofacies have been separated on the basis of the abundance of the calcium carbonate/clay content and the overall textural features. The deformational structures, displaying different deformational styles as folded and faulted beds, disturbed layers, clastic dikes, and slumps occur mainly in the deformed horizons that involve marl-dominat…

010506 paleontologyDikegeographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphyGeology010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingSoft-sediment deformation structuresSoft-sediment deformation structures Synsedimentary tectonics Upper Triassic deep-water carbonates Central SicilyPaleontologyContinental marginClastic rockMarlExtensional tectonicsSedimentary rockGeology0105 earth and related environmental sciencesSedimentary Geology
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Quaternary marine and continental unconformity-bounded stratigraphic units of the NW Sicily coastal belt

2017

In the coastal sector of NW Sicily, the regional correlation of relevant unconformities recognised within the Quaternary sedimentary successions allowed the mapping of seven unconformity-bounded stratigraphic units (UBSUs). The regional unconformities are marine or subaerial erosional surfaces, as well as non-depositional surfaces, locally marked by paleosoils. The erosional surfaces were produced from marine abrasion, surface water overland/concentrated flow, river erosion, karst solution, mass movement, or wind erosion. The main lithofacies of the Quaternary UBSUs consist of: (a) marine and coastal bioclastic calcarenites, (b) aeolian sandstones, (c) river deposits, (d) colluvial deposits…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaNW Sicilyquaternary continental and marine depositsGeography Planning and DevelopmentGeochemistryquaternary continental and marine deposit010502 geochemistry & geophysics01 natural sciencesUnconformitylcsh:G3180-9980Earth and Planetary Sciences (miscellaneous)tectonicsclimateGeomorphologyUnconformity-bounded stratigraphic unit0105 earth and related environmental sciencesColluviumlcsh:Mapsgeographygeography.geographical_feature_categoryUnconformity-bounded stratigraphic unitsKarsttectonicsea-level changeTectonicsSubaerialErosionSedimentary rocksea-level changesQuaternaryGeologyUnconformity-bounded stratigraphic units; quaternary continental and marine deposits; tectonics; sea-level changes; climate; NW SicilyJournal of Maps
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Geology of Monte Gallo (Palermo Mts, NW Sicily)

2016

The promontory of Monte Gallo (Palermo, NW Sicily) is a spectacular site where Upper Triassic-Eocene carbonate platform rocks and Quaternary continental to marine deposits are well exposed. A Mesozoic-Paleogene rock succession allows the potential visitor to easily detect the features and the evolution of the Panormide carbonate platform, a shallow-water paleogeographic domain of the Southern Tethyan margin. Quaternary deposits, as well many landforms, enable the visitor to directly identify the interplay between climate changes, tectonics and fluctuations of marine level that occurred during the Quaternary Period. A detailed geological map (1:15,000 mapping scale) is presented, accompanied…

010506 paleontologyUpper Triassic-Eocene shallow-water carbonateSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformSettore GEO/04 - Geografia Fisica E GeomorfologiaGeography Planning and Developmentquaternary continental and marine synthemClimate change010502 geochemistry & geophysics01 natural sciencesgeotourismPaleontologyEarth and Planetary Sciences (miscellaneous)GeotourismSicily0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryLandformGeological mapGeologic mapgeositeTectonicsQuaternaryScale (map)Geology
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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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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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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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