Search results for " facies analysis"

showing 4 items of 4 documents

From sepulchre to butchery-cooking: Facies analysis, taphonomy and stratigraphy of the Upper Palaeolithic post burial layer from the San Teodoro Cave…

2020

Abstract The San Teodoro Cave is considered the most significant witness of the first, Epigravettian, human colonization of Sicily from the Italian continent. Furthermore the site is a paradigmatic horizon in the Pleistocene faunal record, demonstrating a progressive transition from mega faunas to smaller-sized, Boreal, faunas. The site has been repeatedly studied and excavated, with different aims and approaches, leading to an interpretation of Epigravettian burial site and daily attendance. Here we propose a reappraisal of the study of the stratigraphy of the site, and in particular of the bone-rich layer (PAL) accumulated over the red ochre layer that apparently sealed all the different …

ArcheologygeographyTaphonomygeography.geographical_feature_categoryHorizon (archaeology)PleistoceneMediterranean Late Upper Palaeolithic Epigravettian Taphonomy Butchering Facies analysis AMS dating San Teodoro CaveSettore BIO/08 - AntropologiaArchaeologyQuartz areniteStratigraphyCaveFaciesPeriod (geology)GeologyJournal of Archaeological Science: Reports
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Facies stacking and extinctions across the Triassic–Jurassic boundary in a peritidal succession from western Sicily

2017

An uppermost Triassic–lowermost Jurassic carbonate platform succession, which is 430 m thick, in northwestern Sicily is described with the aim to provide new data on the sedimentological and biological variations across the Triassic–Jurassic boundary in peritidal environments. The studied succession belonged to the rimmed carbonate shelf that developed during the upper Triassic along the margins of the Ionian Tethys. The peritidal sediments consist of metre-scale shallowing-upward cycles formed by subtidal, intertidal and supratidal facies. Three main informal units are differentiated along the section on the basis of the variations recorded by the subtidal facies. The lower and middle unit…

Extinction event010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyFaunaPaleontologyGeologyEcological succession010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundPaleontologychemistryTriassic-Jurassic boundary mass extinction foraminiferal biostratigraphy peritidal carbonates facies analysis SicilyBenthic zoneFaciesCarbonateSedimentologyGeology0105 earth and related environmental sciencesFacies
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Lithostratigraphy of Sicily

2018

This book offers as comprehensive an overview as possible of the lithostratigraphy of the Italian region of Sicily, taking into account the multiplicity of formational and terminological variability developed over more than a century of studies and publications. It presents stratigraphic terminology, the geological lexicon and the main stratigraphic subdivisions that are not familiar to Sicilian geologists. The new stratigraphic methods and the use of formations as mapping units have prompted the acquisition of new lithostratigraphic data, and a review of the previous units and their comparison with the new collected data, enabling the definition of a number of new lithostratigraphic units.…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSedimentology Paleogeography Chronostratigraphy Stratigraphic Methods Plate-tectonic History Micropaleontology Facies Analysis Macro- and Micro-Facies Biostratigraphy Carbonate Deposits Evaporite Deposits
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Facies, architecture and genetic controls of carbonate ramp aprons development

Cool-water Carbonate Ramp Aprons (CRA) are depositional systems in which skeletal sand and gravel are redistributed basinwards on a ramp, off a shallow carbonate platform by tractive currents as a result of flow funnelling in between topographic highs. These deposits are different and should not be confused with the carbonate apron models proposed by of Mullins and Cook (1986) who describe either carbonate deep water turbiditic systems accumulated at the base of the slope or talus cones formed at the margins of carbonate build ups. A key example of CRA facies assemblages is represented by the Early Pleistocene, Favignana Calcarenite where bimodal depositional processes, occurring in a water…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicacarbonate ramp aprons facies analysis Egadi Islands
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