Search results for "last interglacial"

showing 8 items of 8 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
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Millenial-scale paleoenviromental changes in the central Mediterranean during the Last Interglacial: comparison with European and North Atlantic reco…

2010

Abstract The environment of the central Mediterranean Sea is investigated on the basis of high-resolution planktonic foraminifera and calcareous nannofossil data (mean sampling resolutions of about 80 and 160 yr, respectively). MIS 5 is characterized by warm, oligotrophic and stratified waters, while coccolithophore communities developed a vertical zonation that, in today's oceans, is typical of the low-latitude gyres. The temperate-subtropical configuration of planktonic foraminifera and calcareous nannofossil assemblages is repeatedly transformed into a temperate-subpolar one during the suborbital cooling episodes C25-C18. A comparison with European pollen sequences and North Atlantic cor…

Planktonic foraminiferageographygeography.geographical_feature_categorybiologyNorthern HemispherePaleontologybiology.organism_classificationLast InterglacialForaminiferaCentral MediterraneanOceanographyMediterranean seaSpace and Planetary ScienceOcean gyrePaleoceanographyCalcareous nannofossilsInterglacialPaleoclimatologySuborbital climatic fluctuationsQuaternaryGeology
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Fires at Neumark-Nord 2, Germany: An analysis of fire proxies from a Last Interglacial Middle Palaeolithic basin site

2016

Few sites with evidence for fire use are known from the Last Interglacial in Europe. Hearth features are rarely preserved, probably as a result of post-depositional processes. The small postglacial basins (

010506 paleontologyArcheologyHearthEemianStructural basinHeated flint01 natural sciencesLast InterglacialBurned bone0601 history and archaeologyCharcoalheated flint0105 earth and related environmental sciencesFire usegeographyEemiangeography.geographical_feature_category060102 archaeology06 humanities and the artsSedimentary basinArchaeologysedimentary basinsburned bonevisual_artCharcoalInterglacialvisual_art.visual_art_mediumGeologycharcoal
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Surface and deep water conditions in the Sicily channel (central Mediterranean) at the time of sapropel S5 deposition

2011

New centennial-scale data of benthic foraminifera assemblages and of stable isotopes of foraminifera shells from the Sicily Channel, representative of surface and bottom waters, over the interval between about 140 and 110 kyr BP, are presented. During this period anoxia developed on the eastern Mediterranean basin and sapropel S5 deposited. Although anoxic sediments have not been deposited in the Sicily Channel, this area is strategic to study the character of intermediate waters, whose chemical-physical properties strongly precondition the eastern Mediterranean deep water formation. So far, no data from these water masses have been obtained, apart from the isotopic composition of shells of…

Mediterranean climateWater massbiologyPleistoceneSicily ChannelBenthic foraminiferaPaleontologySapropelLate QuaternaryOceanographybiology.organism_classificationLast InterglacialForaminiferaMediterranean seaOceanographyStable IsotopeBenthic zoneSapropel S5Surface waterEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesStable isotopes
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Millennial-scale paleoenvironmental changes in the central Mediterranean during the Last Interglacial: comparison with European and Mediterranean rec…

2008

Paleoceanography last interglacial Sicily ChannelPaleoceanography MIS 5 Mediterranean
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The Grotta Grande of Scario (Salerno, Italy): Archaeology and environment during the last interglacial (MIS 5) of the Mediterranean region

2011

Abstract Archeological and paleo-environmental researches carried on the Grotta Grande site illustrate the importance of a multidisciplinary approach among archeologists, palynologists and paleontologists. The archaeology, fauna, pollen and micro-charcoal recovered in two short sedimentary successions (trenches A, F) located close to the entrance of the cave are discussed. The cave opens directly on the Tyrrhenian Sea, 2 km from Scario (Salerno, Campania, Southern Italy). The morphology of the cave and sedimentary processes were controlled by eustatic fluctuations during the late Middle Pleistocene and the early Late Pleistocene. The sea repeatedly occupied the cave. The cave was frequented…

Mediterranean climatePalinologyPleistoceneGrotta Grande (Scario)FaunamammalFaunal and pollen remainsLast InterglacialMiddle Palaeolithic; Southern Italy; Faunal and pollen remains; Grotta GrandePaleontologyCaveMiddle PalaeolithicGlacial periodfaunaEarth-Surface ProcessesPalynologygeographygeography.geographical_feature_categorybiologyarchaeologyGrotta GrandeSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationArchaeologyArcgaeologyStraight-tusked elephantItalyInterglacialSouthern ItalyenvironmentGeologyGrotta Grande (Scario); archaeology; fauna; pollen and micro-charcoalpollen and micro-charcoalQuaternary International
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Markers of the last interglacial sea level high stand along the coast of Italy: Tectonic implications.

2006

A compilation of the Marine Isotope Substage (MIS) 5.5 high stand (similar to 125Ka) sites spanning the coastline of Italy allows a picture of the vertical displacement pattern affecting the Central Mediterranean coasts since the Late Pleistocene to be drawn. For each of the 246 listed sites, the accurate elevation of the high stand is defined through well-known markers. Coupled with a refilled age assessment locally Supported by new radiometric dating, these markers provide robust constraints oil deformation. Significant alongshore differences in site elevation between + 175 and - 125 m a.s.l. resulted from the interplay of regional and local tectonic processes, including faulting and volc…

See front matterlast interglacialPleistoceneSettore GEO/03 - Geologia Strutturaletectonics; last interglacial ; sea level; italySubsidencehighstandsea levellast interglacial; highstand; Italy; tectonic phenomenaMIS 5.5neotectonicTectonicsGeographieDelamination (geology)italyInterglacialtectonicsVertical displacementtectonic phenomenaItalian coastGeomorphologyForeland basinGeologySea levelEarth-Surface Processes
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Direct terrestrial–marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe

2011

AbstractAn interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 ± 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial–marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e ‘peak’ in the marine record and the start of the last interglacial in this region.

010506 paleontologyEemiangeographyPaleomagnetismgeography.geographical_feature_category010504 meteorology & atmospheric sciencesAardwetenschappenBlake EventMIS 5ePalaeomagnetismLast interglacialTime lagLate onsetEemianSedimentary basin01 natural sciencesSequence (geology)PaleontologyArts and Humanities (miscellaneous)InterglacialShort PaperGeneral Earth and Planetary SciencesGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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