Search results for " Geologia"

showing 10 items of 570 documents

Reconstruction of the paleoenvironmental changes around the Miocene-Pliocene boundary along a W-E transect across the Mediterranean

2006

Abstract In order to reconstruct the environmental changes at the end of the Messinian salinity crisis, a multidisciplinary study has been carried out with a high sampling resolution of the late Messinian–early Zanclean (Zone MPl 1) sediments along a West–East Mediterranean transect. The studied examples comprise sections from southern Spain (Vera/Almanzora), Balearic Basin (ODP Site 975), Tyrrhenian Basin (ODP Site 974), Sicily (Eraclea Minoa), Zakynthos (Kalamaki), Corfu (Aghios Stefanos), Crete (Aghios Vlasis). Previously analyzed sections from the Levantine Basin (Cyprus and ODP Sites 968 and 969) are used for comparison. The sections have been correlated using planktonic foraminiferal …

Mediterranean climate010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OStratigraphy[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesMediterranean areaPlanktonic foraminiferMiocene–Pliocene transitionPaleontologyStratotype14. Life underwaterSedimentologyTransect0105 earth and related environmental sciencesSettore GEO/06 - Mineralogiaδ13CbiologyGeologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationStable isotope6. Clean waterSettore GEO/08 - Geochimica E VulcanologiaAmmonia tepida13. Climate actionFaciesGeology
researchProduct

Palaeogeographical evolution of the Egadi Islands (western Sicily, Italy). Implications for late Pleistocene and early Holocene sea crossings by huma…

2019

Abstract The continental shelf morphology offshore of western Sicily suggests that during the Last Glacial Maximum (LGM, 20 ka cal BP), two of the Egadi Islands, Favignana and Levanzo, were connected to Sicily by a wide emerged plain, while Marettimo was only separated from the other islands by a narrow channel. We studied the relative sea-level variation from the LGM until today, focussing on two important time slices: the Mesolithic (9.5–13 ka cal BP) and the Neolithic (6.5–7.5 ka cal BP). In this research, we discuss a sea-level rise model by means of geomorphological, archaeological and geophysical observations and new radiocarbon dating of marine and terrestrial fossil fauna. The resul…

Mediterranean climatePalaeoshorelineDwarf elephantsSettore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesPleistoceneSettore GEO/03 - Geologia StrutturaleFaunaDwarf elephants; Egadi archipelago; Food remains; Mammals; Marine geological data; Mediterranean voyaging; Palaeogeographical reconstruction; Palaeoshorelines; Vertical tectonic movements010502 geochemistry & geophysics01 natural sciencesMammallaw.inventionPaleontologylawVertical tectonic movementMediterranean voyagingRadiocarbon datingPalaeoshorelinesMesolithicHolocene0105 earth and related environmental sciencesMammalsgeographygeography.geographical_feature_categoryContinental shelfLast Glacial MaximumFood remainDwarf elephantPalaeogeographical reconstructionGeneral Earth and Planetary SciencesFood remainsMarine geological dataEgadi archipelagoEarth and Planetary Sciences (all)Vertical tectonic movementsEarth-Science Reviews
researchProduct

Sea level and climate forcing of the Sr isotope composition of late Miocene Mediterranean marine basins

2014

Sr isotope records from marginal marine basins track the mixing between seawater and local continental runoff, potentially recording the effects of sea level, tectonic, and climate forcing in marine fossils and sediments. Our 110 new Sr-87/Sr-86 analyses on oyster and foraminifera samples from six late Miocene stratigraphic sections in southern Turkey, Crete, and Sicily show that Sr-87/Sr-86 fell below global seawater values in the basins several million years before the Messinian Salinity Crisis, coinciding with tectonic uplift and basin shallowing. 87Sr/86Sr from more centrally located basins (away from the Mediterranean coast) drop below global seawater values only during the Messinian S…

Mediterranean climateSettore GEO/02 - Geologia Stratigrafica E SedimentologicaEvaporitelate MioceneMediterraneanStructural basinLate Miocenegroundwater residenceForaminiferaTectonic upliftGeochemistry and Petrologysea level changesSea levelLower Evaporitesbiologymediterranean groundwater residenceAmbientaleSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classification87Sr/86SrSettore GEO/08 - Geochimica E VulcanologiaGroundwater effects on river and basin water geochemistry are likely importantGeophysicsOceanographygroundwater residence; sea level changes; late Miocene; lower evaporites; mediterranean; mediterranean groundwater residence; 87Sr/86SrSeawaterInstitut für GeowissenschaftenSr isotope excursions primarily correspond to sea level fall or basin upliftgroundwater residence; late Miocene; Lower Evaporites; Mediterranean; sea level changes; Geophysics; Geochemistry and PetrologyNegative Sr isotope excursions in Miocene Mediterranean marine sedimentGeologyGeochemistry, Geophysics, Geosystems
researchProduct

The end of the Messinian Salinity Crisis in the western Mediterranean: insights from the carbonate platforms of south-eastern Spain.

2010

International audience; How the Messinian Salinity Crisis (MSC) ended is still a matter of intense debate. The Terminal Carbonate Complex (TCC) is a late Messinian carbonate platform system that recorded western Mediterranean hydrological changes from the final stages of evaporite deposition till the advent of Lago-Mare fresh- to brackish water conditions at the very end of Messinian times. A multidisciplinary study has been carried out in three localities in south-eastern Spain to reconstruct the history of TCC platforms and elucidate their significance in the MSC. Overall, this study provides evidence that the TCC formed following a regional 4th order water level rise and fall concomitant…

Mediterranean climateWestern Mediterranean010506 paleontologyEvaporiteEnvironmental changeSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyEvaporite deformation and dissolutionMessinian Salinity Crisis010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentMessinian Salinity Crisis Western Mediterranean Carbonate platforms Evaporite deformation and dissolution Eustasy Return to marine conditionschemistry.chemical_compoundReturn to marine conditions14. Life underwaterCarbonate platformsEustasy0105 earth and related environmental sciencesBrackish waterGeologySettore GEO/01 - Paleontologia E PaleoecologiaWater levelOceanographychemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
researchProduct

Surface expression of eastern Mediterranean slab dynamics: Neogene topographic and structural evolution of the southwest margin of the Central Anatol…

2012

The southwest margin of the Central Anatolian Plateau has experienced multiple phases of topographic growth, including the formation of localized highs prior to the Late Miocene that were later affected by wholesale uplift of the plateau margin. Our new biostratigraphic data limit the age of uplifted marine sediments at the southwest plateau margin at 1.5 km elevation to <7.17 Ma, and regional lithostratigraphic correlations imply that the age is <6.7 Ma. Single-grain CA-TIMS U-Pb zircon analyses from a reworked ash within the marine sediments yield dates as young as 10.6 Ma, indicating a maximum age that is consistent with the biostratigraphy. Our structural measurements within the uplifte…

Mediterranean Neogene Turkey TectonicSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E Vulcanologia
researchProduct

Reconstruction of the paleoenvironmental changes around the Messinian-Pliocene boundary along a W-E transect across the Mediterranean

2004

Messinian Pliocene Salinity CrisisSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E Vulcanologia
researchProduct

Clastic vs. primary precipitated evaporites in the Messinian Sicilian basins

2006

Messinian; Salinity Crisis; Sicily; Foraminfera;Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinianSettore GEO/03 - Geologia StrutturaleForaminferaSettore GEO/01 - Paleontologia E PaleoecologiaSicilySalinity Crisi
researchProduct

The role of topography and erosion in the development and architecture of shallow-water coral bioherms (Tortonian-Messinian, Cabo de Gata, SE Spain).

2009

23 pages; International audience; During the Miocene, Mediterranean shallow-water carbonates were rich in scleractinian corals, which thrive in various depositional settings. A Tortonian–Messinian bioherm belt developing in a heterozoan-dominated ramp was investigated along a 1.2 km continuous transect located in the Cabo de Gata region. The interval studied displays four depositional environments from mid-to-inner ramp, dominated by swell waves and storm energy, deposited as a single, large-scale depositional sequence during a 3rd to 4th order transgressive–regressive cycle. The bioherms grew in three phases, and were essentially composed of inplace primary frameworks. Three coral genera w…

Micro-encrusters010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStormsCoralPorites010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentBiohermPaleontologyStormBack-reef erosionPalaeotopography14. Life underwaterTransectEcology Evolution Behavior and SystematicsSea level0105 earth and related environmental sciencesEarth-Surface ProcessesMicro-encrustergeographygeography.geographical_feature_categorybiologyPaleontologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationWaves and shallow waterVolcano[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyErosionCoralGeology
researchProduct

Le pieghe minori nelle Unità Imeresi e Trapanesi dei Monti di Palermo ed il loro significato nell’evoluzione tettonica dell’area

2003

In questo lavoro sono riassunte le osservazioni sulle pieghe minori che interessano i terreni delle Unità Imeresi e Trapanesi del settore orientale dei Monti di Palermo, con l'obbiettivo di: a) descri-vere la geometria e lo stile deformativo delle mesopieghe e stabilirne le relazioni spazio-temporali con le pieghe maggiori e le altre strut-ture minori (clivaggi, joints); b) ricavare, attraverso l'analisi stati-stica dei dati giaciturali, l'orientazione dei campi deformativi asso-ciati alle strutture plicative; c) ricostruire il significato delle pieghe minori nell'evoluzione tettonica dell'area. Nelle Unità Imeresi e Trapanesi, l'analisi statistica dei dati e le osservazioni di campagna han…

Monti di Palermo Sicilia mesopieghe meccanismi di deformazione strutture di interferenzaSettore GEO/03 - Geologia Strutturale
researchProduct

Evaluation of debris flow susceptibility in El Salvador (CA): a comparison between Multivariate Adaptive Regression Splines (MARS) and Binary Logisti…

2018

In the studies of landslide susceptibility assessment, which have been developed in recent years, statistical methods have increasingly been applied. Among all, the BLR (Binary Logistic Regression) certainly finds a more extensive application while MARS (Multivariate Adaptive Regression Splines), despite the good performance and the innovation of the strategies of analysis, only recently began to be employed as a statistical tool for predicting landslide occurrence. The purpose of this research was to evaluate the predictive performance and identify possible drawbacks of the two statistical techniques mentioned above, focusing in particular on the prediction of debris flows. To this aim, an…

Multivariate Adaptive Regression Splines (MARS)hurricane IdaMultivariate adaptive regression splines010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaBinary Logistic Regression (BLR)0208 environmental biotechnologyGeography Planning and Developmentlcsh:G1-92202 engineering and technologyMars Exploration ProgramDebris flowLogistic regression01 natural sciences020801 environmental engineeringDebris flowdebris flowsStatisticsEl SalvadorGeneral Earth and Planetary Scienceslandslide susceptibilitySettore GEO/05 - Geologia Applicatalcsh:Geography (General)Geology0105 earth and related environmental sciencesHungarian Geographical Bulletin
researchProduct