Search results for " Late Pleistocene"

showing 4 items of 4 documents

The last of the large-sized tortoises of the Mediterranean islands

2022

Altres ajuts: CERCA Programme/Generalitat de Catalunya Altres ajuts: Operational Programme Research, Development and Education Project (CZ.02.2.69/0.0/0.0/16_027/0008360) Archaeological investigations carried out in the cave Zubbio di Cozzo San Pietro, Bagheria, Sicily, revealed the presence of a few skeletal elements of a large-sized tortoise in a funerary area dating to the Copper/Bronze Age. The tortoise has been AMS-dated revealing an age of 12.5 ± 0.5 kyr BP and therefore it pre-dates the funerary activities. The morphology of the retrieved skeletal elements differs from that of the only native tortoise currently living in Sicily, Testudo hermanni. The tortoise's size significantly exc…

Evolutioninsular faunasancient DNA insular faunas Italy latest Late Pleistocene parsimony Sicily Testudinidae10125 Paleontological Institute and MuseumSettore BIO/08 - AntropologiaparsimonyBehavior and SystematicsAnimaliaInsular faunasChordataancient DNASicilyEcology Evolution Behavior and SystematicsTaxonomyEcologyAncient DNAlatest Late PleistoceneBiodiversitySettore GEO/01 - Paleontologia E PaleoecologiaTestudinidae560 Fossils & prehistoric lifeItalyTestudinesAnimal Science and ZoologyParsimonyLatest Late Pleistocene
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Multi-proxy analysis suggests Late Pleistocene affinities of human skeletal remains attributed to Balzi Rossi

2021

: In two publications from 1967 and 1971, M. Masali described human skeletal remains presumed to have been found in the Balzi Rossi caves (Ventimiglia, Italy), based on a signed note dated to 1908. Since then, the remains - dubbed "Conio's Finds" and preserved at the University of Torino - had not been further studied. We performed a multidisciplinary investigation aimed at clarifying the geographical and chronological attribution of these specimens. Collagen extraction for AMS dating was unsuccessful, but we obtained two direct dates on the best- preserved crania via 231Pa/235U direct gamma-ray spectrometry (10,500±2,000 years BP and 12,500±2,500 years BP). We analyzed the metrics and morp…

Late PleistoceneCraniofacial morphometrics; Cross-sectional geometry; Epigravettian; Gravettian; Grimaldi Caves; Late Pleistocene; U-Pa series dating; Western EuropeGrimaldi CavesU-Pa series datingCraniofacial morphometricsEpigravettianWestern EuropeCross-sectional geometryGravettian
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Variability in the vertical structure of the water column and paleoproductivity reconstruction in the central-western Mediterranean during the Late P…

2008

Abstract A sedimentary sequence spanning Marine Isotope Stage (MIS) 6 to MIS 2 in core LC07, recovered in the central Mediterranean, has been investigated in order to produce a high-resolution paleoceanographic reconstruction. The changes in productivity deduced from calcareous plankton relative abundances and independently confirmed by the Ba XS fluctuations are linked to the stability of the water column which is mainly controlled by the water mass temperature. During glacial intervals, productivity was generally enhanced. Oligotrophic and warmer water masses with a deepened seasonal thermocline can be inferred for most of MIS5. The magnetic properties of the sediment show increased occur…

Marine isotope stageWater massPleistocenePaleontologyMineral dustOceanographyPaleontologyWater columnOceanographyCalcareous Plankton Paleoceanography Late PleistoceneInterglacialGlacial periodThermoclineGeology
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Human settlements in the Mediterranean and the sea level changes from 12 ka to the present

2012

Understanding past sea-level change plays an important role in determining the underlying causes, and also allows the extrapolation of past sea levels to locations and epochs for which there are no instrumental data. A compilation of global sea-level estimates based on deep-sea oxygen isotope ratios at millennial-scale resolution or higher was published since ‘70. These global sea level curves do not take in account isostasy and tectonics. Observed sea level change can be reconstructed from dated fossils, coral reef terraces, speleothems, emerged and forming terraces on coastal areas, archaeological and other markers well connected with sea level. Because of the lack of coral reefs in the M…

Mediterranean climatePalaeoshorelinesea level rise; palaeoshorelines; late pleistocene; palaeoshorelines.; holoceneHoloceneSettore GEO/04 - Geografia Fisica E GeomorfologiaHolocene Late Pleistocene Sea level rise PalaeoshorelinesHolocene; Late pleistocene; Palaeoshorelines; Sea level rise; GeologyGeologyLate pleistoceneSea level riseOceanographyGeographySea level riseLate PleistoceneHuman settlementPalaeoshorelinesHoloceneSea levelPalaeoshorelines.
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