Search results for "Magnetostratigraphy"

showing 3 items of 13 documents

Bio-chronostratigraphic calibration of the Upper Carnian-Lower Norian magnetostratigraphic scale at Pizzo Mondello (Sicani Mountains, Sicily).

2010

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicamagnetostratigraphy bio-chronostratigraphy Upper Carnian-Lower Norian Pizzo Mondello
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Chronology for the Cueva Victoria fossil site (SE Spain): Evidence for Early Pleistocene Afro-Iberian dispersals

2014

Cueva Victoria has provided remains of more than 90 species of fossil vertebrates, including a hominin phalanx, and the only specimens of the African cercopithecid Theropithecus oswaldi in Europe. To constrain the age of the vertebrate remains we used paleomagnetism, vertebrate biostratigraphy and (230)Th/U dating. Normal polarity was identified in the non-fossiliferous lowest and highest stratigraphic units (red clay and capping flowstones) while reverse polarity was found in the intermediate stratigraphic unit (fossiliferous breccia). A lower polarity change occurred during the deposition of the decalcification clay, when the cave was closed and karstification was active. A second polarit…

Theropithecus010506 paleontologyEarly PleistocenePleistoceneved/biology.organism_classification_rank.speciesBiostratigraphy010502 geochemistry & geophysics01 natural sciencesTheropithecusPaleontologyAfrica NorthernCaveAnimalsEcology Evolution Behavior and SystematicsMagnetostratigraphy0105 earth and related environmental sciencesMammalsgeographygeography.geographical_feature_categoryFossilsved/biologyHominidaeBiological EvolutionCavesSpainAnthropologyAnimal MigrationTheropithecus oswaldiGeologyAcheuleanJournal of Human Evolution
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Magnetostratigraphy and biostratigraphy of the Carnian/Norian boundary interval from the Pizzo Mondello section (Sicani Mountains, Sicily)

2001

The 146.5 m-thick Upper Triassic limestone section at Pizzo Mondello in the Sicani Mountains of western Sicily is characterized by high quality of exposure, accessibility, and stratigraphic continuity. Magnetostratigraphic results delineate 12 normal and reverse polarity magnetozones, labelled successively from the base upwards as PM1n, PM1r, PM6n, PM6r. The Carnian/Norian boundary, based on conodont biostratigraphy, falls somewhere in the PM3n to PM5n interval which corresponds to the E14n to E16n magnetozone interval in the Newark reference sequence of polarity reversals. Comparison of magnetobiostratigraphic data from the Newark basin, Pizzo Mondello and other Late Triassic marine sectio…

biologySedimentary GeologyPaleontologyBiostratigraphyStructural basinOceanographybiology.organism_classificationPaleontologySection (archaeology)ConodontSouthern HemisphereEcology Evolution Behavior and SystematicsMagnetostratigraphyGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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