Search results for "PLEISTOCENE"

showing 10 items of 298 documents

Vertical movements in NE Sicily and its offshore: Outcome of tectonic uplift during the last 125 ky

2013

New data in the coastal area between Acquedolci and Patti (northeastern Sicily, Italy) have been collected to calculate vertical tectonic rates in a key sector between the Kabilian-Calabrian and the Sicilian-Maghrebian chain. The comparison among marine geology data (multibeam and seismic reflection profiles) on the continental shelf-slope system and the radiocarbon ages on geomorphological markers collected during a coastal survey, provided new stratigraphic, geomorphological and biological data, contributing to the knowledge of the geological evolution of this sector for the last 125 ky.This coastal area is framed between two main structural features active during the Pleistocene in north…

geographygeography.geographical_feature_categoryPleistoceneHoloceneLast Glacial MaximumSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaMarine geologyLast Glacial MaximumFault (geology)Last Interglaciallaw.inventionTectonicsTectonic upliftlawRelative Sea level changeUplift rateLate Quaternary depositional sequenceRadiocarbon datingGeomorphologyGeologyHoloceneEarth-Surface Processes
researchProduct

Middle-Late Pleistocene marine terraces and fault activity in the Sant’Agata di Militello coastal area (north-eastern Sicily)

2012

Abstract The coastal sector of Sant’Agata di Militello (north-eastern Sicily) is characterized by a flight of raised Middle-Upper Pleistocene marine terraces occurring at different heights with respect to present sea level. In particular, the geomorphological survey and the analysis of stereo-pairs of aerial photographs allowed to recognize at least five main orders of well preserved Quaternary surfaces and relative deposits mostly located at the hanging wall and at the footwall of the Pleistocene northwest-dipping Capo d’Orlando normal fault, which controlled the geomorphological evolution of the coastal area. The marine terraces show an overall good morphological continuity and are formed…

geographygeography.geographical_feature_categoryPleistoceneOSL datingFault (geology)coastal tectonicsPaleontologyTectonicsGeophysicsTerrace (geology)marine terracesRiver terracesSedimentary rockQuaternarycoastal tectonics; marine terraces; OSL datingSea levelGeologyEarth-Surface ProcessesJournal of Geodynamics
researchProduct

Defining the Island Dwarfing Rate of an Extinct Sicilian Elephant Using Ancient DNA

2020

Evolution on islands, and the often extreme phenotypic changes associated with it, has attracted much interest from evolutionary biologists. However, measuring the rate of change of a particular phenotypic trait of extinct animals can be challenging, due to the incompleteness of the fossil record. Here, we use combined molecular and fossil evidence to define the minimum and maximum rate of dwarfing in an extinct Mediterranean dwarf elephant from Puntali Cave (Sicily). Despite the challenges associated with recovering ancient DNA from warm climates, we successfully retrieved a mitogenome from a sample with an estimated age between 147,000 and 50,000 years. Our results suggest that this speci…

geographygeography.geographical_feature_categoryPleistocenePalaeoloxodonbiologyLineage (evolution)Phenotypic traitbiology.organism_classificationlanguage.human_languageDwarfingAncient DNACaveEvolutionary biologylanguageSicilianSSRN Electronic Journal
researchProduct

Palaeogeographical relationships between Alpine and Jura glaciers during the two last Pleistocene glaciations

1992

Abstract Two main moraine complexes are usually defined in the northwestern Alpine piedmont: the External Moraine Complex (EMC) dated to the penultimate glaciation (“Riss” sensu lato) and the Internal Moraine Complex (IMC) dated to the last glaciation (“Wurm”). Until recently the prevalent concept was that these two complexes had been built by glaciers originating in the central Alpine zone. This paper presents a new palaeogeographical diagram, based on mapping and petrographical studies of these two moraine complexes, and especially on the relationships between Alpine and Jura tills. We reach the following conclusions. 1. (1) The Jura glaciers were independent of the Alpine glaciers during…

geographygeography.geographical_feature_categoryPleistocenePaleontologyAlpine climateGlacierOceanographyPaleontologyMoraineGlacial periodGeomorphologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
researchProduct

1999

The Quaternary karstic site of Sierra de Quibas (Abanilla, Murcia, Spain) has provided a wide faunistic list with 53 species distributed among gastropods, myriapods, amphibians, reptiles, birds and mammals. Especially interesting among the gastropods is Palaeoglandina that became extinct in Europe during the Pliocene. It remains as a relict genus in the Pleistocene of the Iberian Peninsula. Two of the birds, Gypaetus barbatus and Geronticus eremita, and a snake, Elaphe cf. E. sealaris, are scarcely represented in the fossil record. For several birds, it is the first record in the Lower Pleistocene of the Iberian Peninsula. Among the mammals, the presence of the Cercopithecine Macaca sylvanu…

geographygeography.geographical_feature_categoryPleistocenebiologyEcologyGeologybiology.organism_classificationEquusPeninsulaGenusArvicolaEliomysQuaternaryGeronticusEstudios Geológicos
researchProduct

Pleistocene Glaciations in Latvia

2011

Abstract During the Pleistocene the territory of Latvia was repeatedly overridden by Scandinavian ice sheets, at least from the Elsterian onwards. Extent limit of all glaciations was located far outside of Latvia. Due to vigorous erosion by subsequent glaciations the Pleistocene record is incomplete. Radiocarbon, cosmogenic nuclide and radiation exposure dating methods have been mainly used only for age determination of the upper part of the Pleistocene sequence. Decay of the Late Weichselian glaciation in Latvia is marked by five major ice-marginal zones

geographygeography.geographical_feature_categoryPleistocenelaw.inventionRadiation exposurePaleontologySequence (geology)lawInterglacialRadiocarbon datingIce sheetCosmogenic nuclideWeichselian glaciationGeology
researchProduct

Rifted margin formation in the South Tyrrhenian Sea: A high resolution profile across the North Sicily passive continental margin.

2000

A new, 150 km long seismic line across the continental margin of north Sicily has been acquired and interpreted. The overall structure of the margin is controlled by extension, which caused crustal thinning and widespread normal faulting. Two main thinned zones are observed in the south in correspondence with the Cafalù basin and farther to the north at the continent-ocean transition. Zones of thinned crust coincide with zones of intense normal faulting. Extension began in late Tortonian times and caused the opening of the Cefalù basin controlled by a northward dipping listric fault. Messinian stretching affected most of the future margin and provoked a widening of the Cefalù basin and norm…

geographygeography.geographical_feature_categoryRiftPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCrustFault (geology)Structural basinSouthern Tyrrhenian North Sicily continental margin Rifted Continental Margin Cefalù basin./dk/atira/pure/sustainabledevelopmentgoals/life_below_waterPaleontologyGeophysicsContinental marginGeochemistry and PetrologyLithospherePassive marginSDG 14 - Life Below WaterGeologySeismology
researchProduct

Astronomical dating of two Pliocene alkaline volcanic ash layers in the Capo Rossello area (southern Sicily, Italy): implications for the beginning o…

2009

Key-words. - Sicily Channel rift, Biostratigraphy, Astronomical calibration, Pliocene, Volcanic ash layers. Abstract. - Two volcaniclastic ash layers (AL1 and AL2) are intercalated throughout the middle Pliocene sedimentary sequences of Punta Piccola and Capo Rossello exposed along the south coast of Sicily (Italy). Astronomical calibration of the Punta Piccola section provided an age of 2.676 Ma for the deposition of the AL1 layer. The high-resolution bio-cyclostratigraphy of the Capo Rossello section, in combination with detailed correlations with previously astrono- mically calibrated coeval sequences, provided an age of 2.225 Ma for the deposition of the AL2 layer. Mineralogical, petrog…

geographygeography.geographical_feature_categoryRiftPlioceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaPleistoceneGeochemistryBiostratigraphyPyroclastic rockGeologySicily Channel riftSettore GEO/01 - Paleontologia E PaleoecologiaBiostratigraphyAstronomical calibrationSettore GEO/08 - Geochimica E VulcanologiaVolcanoSicily Channel rift Biostratigraphy Astronomical calibration Pliocene Volcanic ash layersMagmatismVolcanic ash layersSedimentary rockSeismologyGeologyVolcanic ashBulletin de la Société Géologique de France
researchProduct

A catalogue of the vertebrate fossil record from the Guadix-Baza Basin (SE Spain)

2020

In this paper, a catalogue of the vertebrate content of the Guadix-Baza Basin is presented. A total of 93 localities have been reviewed, providing more than 300 vertebrate species. These localities have been included in 11 biochronological units, ranging in age from the late Miocene (MN 13) to the Middle Pleistocene (MmQ 4), including also two MN 10 localities. The best-represented epoch in the Guadix-Baza Basin is the Pliocene (MN 14 to MN 16), with 41 sites. This is followed by the Early Pleistocene (MN17 and MmQ1 to MmQ3) with 30 sites. The vertebrate classes represented in the basin are Actinopterygii, Amphibia, Aves, Reptilia and Mammalia, this last one being the best represented. Amon…

guadix-baza basin pliocene pleistocene mammals reptiles amphibiansEarly PleistocenebiologyPleistoceneEcologyActinopterygiiVertebratePaleontologyLate MioceneStructural basinbiology.organism_classificationQE701-760PaleontologyGroup (stratigraphy)biology.animalGeologyMuridaeSpanish Journal of Palaeontology
researchProduct

The magnesium isotope record of cave carbonate archives

2012

Here we explore the potential of magnesium (δ<sup>26</sup>Mg) isotope time-series data as continental climate proxies in speleothem calcite archives. For this purpose, a total of six Pleistocene and Holocene stalagmites from caves in Germany, Morocco and Peru and two flowstones from a cave in Austria were investigated. These caves represent the semi-arid to arid (Morocco), the warm-temperate (Germany), the equatorial-humid (Peru) and the cold-humid (Austria) climate zones. Changes in the calcite magnesium isotope signature with time are compared against carbon and oxygen isotope records from these speleothems. Similar to other proxies, the non-trivial interaction of a …

lcsh:GE1-350CalciteGlobal and Planetary Changegeographygeography.geographical_feature_categoryPleistocenelcsh:Environmental protectionStratigraphyGeochemistryPaleontologySpeleothemStalagmiteArchaeologyAridchemistry.chemical_compoundlcsh:Environmental pollutionCavechemistrylcsh:TD172-193.5Carbonatelcsh:TD169-171.8lcsh:Environmental sciencesGeologyHoloceneClimate of the Past
researchProduct