Search results for "PLEISTOCENE"

showing 10 items of 298 documents

Major palaeohydrographic changes in Alpine foreland during the Pliocene - Pleistocene

2008

International audience; The changing palaeogeographical pattern of Alpine deposits across the European forelands can be traced by identifying mineral assemblages and establishing the chronology of Pliocene-Pleistocene deposits in Alpine foreland. In the late Miocene, the upper courses of the Rhine and the Aar flowed east from the Swiss molasse plain towards the Danube. In the early Pliocene (Brunssumian, 5-3.2 Ma), these same rivers headed north-wards towards the Rhine Graben of Alsace. In the early Reuverian, these streams were captured south of the Rhine Graben by the Doubs. They ceased their northward flow and headed west to feed the Bresse Graben. This phase is dated to the Lower and Mi…

Archeologygeographygeography.geographical_feature_category[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010504 meteorology & atmospheric sciencesPleistoceneSchistGeologyMassifLate Miocene010502 geochemistry & geophysics01 natural sciencesMolasseGrabenPaleontology13. Climate actionForeland basinEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesChronologyBoreas
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Late Pleistocene Eifel eruptions: insights from clinopyroxene and glass geochemistry of tephra layers from Eifel Laminated Sediment Archive sediment …

2019

Arts and Humanities (miscellaneous)PleistoceneEarth and Planetary Sciences (miscellaneous)GeochemistryPaleontologySedimentTephraGeologyJournal of Quaternary Science
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Redécouverte d'une faune pléistocène dans les remplissages karstiques de Tam Hang au Laos : premiers résultats.

2008

12 pages; The discovery of a Pleistocene fauna in karstic fills at TamHang in Laos: preliminary results. TamHang, located in northeastern Laos, in the Hua Pan province, is a reference site not only for its numerous archaeological and human remains, but also for its two faunal assemblages, whose composition suggests different dating in the Pleistocene. Discovered in 1934 by Jacques Fromaget, a new excavation of the site has been undertaken in 2003. During this campaign, at Tam Hang south, 575 isolated teeth of mammals were extracted from a deep layer of calcareous breccia. This assemblage corresponds to that one described by Arambourg and Fromaget [C. Arambourg, J. Fromaget, Le gisement quat…

Asie du Sud-Est continentale010506 paleontologyPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryBiostratigraphy010502 geochemistry & geophysicsSouth-East Asia mainland01 natural sciencesTam HangSoutheast asiaPhanerozoicMilieu karstiqueKarstic system0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeneral Engineering15. Life on landArchaeologyPleistoceneLaos[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryClastic rockQuaternary[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCenozoicGeology
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Investigating the influence of climate changes on rodent communities at a regional-scale (MIS 1-3, southwestern France).

2016

25 pages; International audience; Terrestrial ecosystems have continuously evolved throughout the Late Pleistocene and theHolocene, deeply affected by both progressive environmental and climatic modifications, aswell as by abrupt and large climatic changes such as the Heinrich or Dansgaard-Oeschgerevents. Yet, the impacts of these different events on terrestrial mammalian communities arepoorly known, as is the role played by potential refugia on geographical species distributions.This study examines community changes in rodents of southwestern France between50 and 10 ky BP by integrating 94 dated faunal assemblages coming from 37 archaeologicalsites. This work reveals that faunal distributi…

Atmospheric ScienceGeologic Sediments010504 meteorology & atmospheric sciencesStratigraphylcsh:MedicineSocial SciencesEcological succession01 natural scienceslaw.inventionGeographical LocationsPleistocene EpochlawRadiocarbon datinglcsh:ScienceHolocene[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyMammalsClimatologyMultidisciplinaryFossilsEcologyGeologyRadioactive Carbon DatingEuropeGeographyArchaeologyVertebratesTerrestrial ecosystemFrance[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyResearch Article010506 paleontologyPleistoceneClimate ChangeClimate changeRodentiaRodentsAllerød oscillationPaleoclimatologyAnimalsPaleoclimatology0105 earth and related environmental sciences[ SDE.BE ] Environmental Sciences/Biodiversity and Ecologylcsh:RVolesOrganismsBiology and Life SciencesPaleontologyGeologic Time15. Life on land13. Climate actionArchaeological DatingPeople and PlacesEarth SciencesCenozoic Eralcsh:Q[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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The Calabrian Stage redefined

2008

The name Calabrian was introduced in the geological literature by the French stratigrapher Maurice Gignoux in 1910, and later described in his important monograph (633 pages) "Les formations marines pliocènes et quaternaires de l'Italie du sud et de la Sicile" published in 1913. Detailed data were provided on several sections (Santa Maria di Catanzaro, Caraffa, Monasterace, Palermo) and on their fossil content. The Calabrian Stage has commonly been used for over fifty years as the oldest subdivision of the Quaternary, notably in the time scales of Berggren & van Couvering (1974) and Haq & Eysinga (1987). However, after the GSSP for the Pliocene/Pleistocene boundary (P/P) was approved by INQ…

BIOSTRATIGRAFIAPleistoceneQUATERNARIOMAGNETOSTRATIGRAFIABiostratigraphyStratigraphy Quaternary calcareous plankton biostratigraphyCRONOSTRATIGRAFIA STANDARDGlobal Boundary Stratotype Section and PointPaleontologyStratotypeStage (stratigraphy)ISOTOPI STABILICalabrian Stage redefinedIce ageGeneral Earth and Planetary SciencesQuaternaryGeologyMagnetostratigraphyEpisodes
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Chemical composition of modern and fossil hippopotamid teeth and implications for paleoenvironmental reconstructions and enamel formation – Part 2: A…

2012

Abstract. For reconstructing environmental change in terrestrial realms the geochemistry of fossil bioapatite in bones and teeth is among the most promising applications. This study demonstrates that alkaline earth elements in enamel of Hippopotamids, in particular Ba and Sr are tracers for water provenance and hydrochemistry. The studied specimens are molar teeth from Hippopotamids found in modern and fossil lacustrine settings of the Western Branch of the East African Rift system (Lake Kikorongo, Lake Albert, and Lake Malawi) and from modern fluvial environments of the Nile River. Concentrations in enamel vary by ca. two orders of magnitude for Ba (120–9336 μg g−1) as well as for Sr (9–21…

BasaltProvenancePleistoceneEnamel paintArcheanlcsh:QE1-996.5lcsh:LifeGeochemistryMineralogyWeatheringlcsh:Geologylcsh:QH501-531ddc:560Aridificationlcsh:QH540-549.5East African Riftvisual_artvisual_art.visual_art_mediumlcsh:EcologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesBiogeosciences
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Source area determination of aeolian sediments at Jandia Isthmus (Fuerteventura, Canary Islands)

2010

Abstract The Jandia Isthmus (Fuerteventura, Canary Islands) is a complex aeolian system composed of Pliocene and Pleistocene marine deposits, which are partially covered of carbonate crusts, palaeosols and sand sheets. The area has been greatly influenced by climate changes during the Quaternary. Nowadays this area presents an arid landscape dominated by the aeolian processes. Grain size, mineralogical and micropalaeontological analyses have been carried out to identify the source area of these wind-blown materials, considering five possible sources: windward beaches, Pliocene dune cliffs, Upper Pleistocene aeolian deposits, carbonate crusts and basaltic outcrops. Each one of these analyses…

BasaltbiologyPleistoceneOutcropGeochemistryAquatic ScienceOceanographybiology.organism_classificationForaminiferachemistry.chemical_compoundchemistryErosionAeolian processesCarbonateQuaternaryGeomorphologyEcology Evolution Behavior and SystematicsGeologyJournal of Marine Systems
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Millstones as indicators of relative sea-level changes in northern Sicily and southern Calabria coastlines, Italy

2011

Abstract New data are presented for late Holocene relative sea-level changes in two coastal sites of Sicily and Calabria, southern Italy. Reconstructions are based on precise measurements of submerged archaeological remains that are valuable indicators of past sea-level position. The archaeological remains are millstone quarries carved on sandstone coastal rocks and nowadays partially submerged which, to the authors’ knowledge, are used for the first time as sea-level markers. Millstones of similar typology are located on the coast of Capo d’Orlando (northern Sicily) and Capo dell’Armi (southern Calabria). When the archeologically-based sea-level position is compared with the shoreline elev…

BeachrockShoregeographygeography.geographical_feature_categoryHolocenePleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaElevationtectonic movements; sea level changes; Holocene;tectonic movementArchaeologyMillstoneTectonicsgeoarcheologyPhysical geographysea level changeSicily and CalabriaSea levelHoloceneGeologyrelative sea-level changeEarth-Surface Processes
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A multiproxy record of palaeoenvironmental conditions at the Middle Palaeolithic site of Abric del Pastor (Eastern Iberia)

2019

This paper presents a multiproxy palaeoenvironmental study from Abric del Pastor (Alcoy, Spain), a rock shelter which has yielded evidence for Middle Palaeolithic human occupation. The sedimentary sequence has been analysed for lipid biomarker n-alkane abundances (ACL, CPI), compound specific leaf wax δH and δC, and bulk organic geochemistry (TOC, %N, %S), providing a record of past climate and local vegetation dynamics. Site formation processes have been reconstructed through the application of soil micromorphology. Analyses of anthracological, microvertebrate and macrofaunal assemblages from selected subunits are also presented here. Our data indicates that a variable climate marked by pr…

Biotope010506 paleontologyArcheologyNeanderthal010504 meteorology & atmospheric sciencesPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryMiddle palaeolithicStratigraphic unit01 natural sciencesSoil micromorphologybiology.animalOrganic geochemistryEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesNeanderthalsStable isotopesGlobal and Planetary Changegeography.geographical_feature_categorybiologyGeology15. Life on landArchaeologyPleistoceneEuropeGeographyArchaeologyLipid biomarkersSedimentary rockIberiaRavinePalaeoenvironment reconstructionRock shelter
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Sourcing african ivory in chalcolithic Portugal

2009

A recent review of all ivory from excavations in Chalcolithic and Beaker period Iberia shows a marked coastal distribution – which strongly suggests that the material is being brought in by sea. Using microscopy and spectroscopy, the authors were able to distinguish ivories from extinct Pleistocene elephants, Asian elephants and, mostly, from African elephants of the savannah type. This all speaks of a lively ocean trade in the first half of the third millennium BC, between the Iberian Peninsula and the north-west of Africa and perhaps deeper still into the continent.

Bronze ageArcheologyProvenancegeography.geographical_feature_categoryPleistocenePortugalGeneral Arts and HumanitiesChalcolithicIvoryAncient historyArchaeologyChalcolithicMaritimeGeographyBronze AgeBeakerPeninsulaOceansPeriod (geology)TradeBeaker periodIberia
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