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  • Maastricht-Belvédère : stratigraphy, palaeoenvironment and archaeology of the Middle and Late Pleistocene deposits.
  • Archéologie ; Géographie de l'Europe ; Paléo-environnement ; Paléolithique ; Pays-Bas ; Pléistocène ; Quaternaire zones moyennes ; Saalien ; Stratigraphie
  • An exceptionally thick Middle Pleistocene tephra layer from Epirus, Greece
  • Domaine méditerranéen ; Eruption volcanique ; Europe ; Grèce ; Italie ; Pléistocène ; Quaternaire ; Stratigraphie ; Téphrochronologie
  • Europe ; Greece ; Italy ; Mediterranean area ; Pleistocene ; Quaternary ; Stratigraphy ; Tephrochronology ; Volcanic eruption
  • This paper reports the discovery of an exceptionally thick ash deposit of Middle Pleistocene age in western Epirus, Greece. This ash layer has not been reworked and has a chemical composition that links it to an Italian volcanic source 750 km
  • distant. The deposit must have been produced by one of the largest Mediterranean eruptions of the past 400,000 yr and should form a distinctive marker horizon in Pleistocene deposits of southern Italy, mainland Greece, and the Aegean Sea.
  • New discoveries at the Middle Pleistocene Acheulian site of Gesher Benot Ya'aqov, Israel
  • Archéologie ; Biostratigraphie ; Israël ; Paléo-environnement ; Pléistocène ; Quaternaire ; Site archéologique
  • Archaeology ; Archeological site ; Biostratigraphy ; Israel ; Paleo-environment ; Pleistocene ; Quaternary
  • opportunity to study large assemblages of in situ Acheulian artifacts, a rare phenomenon in the middle Pleistocene Levantine record. In addition, the organic materials will facilitate paleoenvironmental reconstructions from an ecological floral perspective.
  • Ice-pushed Lower and Middle Pleistocene deposits near Rhenen (Kwintelooijen): sedimentary-structural and lithological/granulometrical investigations
  • Glaciaire ; Granulométrie ; Géographie de l'Europe ; Lithologie ; Marge proglaciaire ; Moraine de poussée ; Pays-Bas ; Pléistocène ; Quaternaire zones moyennes ; Rhenen ; Structure sédimentaire ; Sédimentologie ; Utrecht
  • Lower Pleistocene deposits fluvial middle Pleistocene deposits and fluvial mass flow and alluvial fan Saalian deposits are involved. The most complete thrust sheets are up to 25 m thick.
  • Middle-Late Pleistocene uplift of Puglia: an anomaly in the Apenninic foreland
  • Adriatique mer ; Appennino ; Géologie régionale ; Géomorphologie structurale ; Géophysique ; Italie ; Mouvement vertical ; Pléistocène ; Puglia ; Subduction
  • Adriatic Sea ; Appennino ; Geophysics ; Italy ; Pleistocene ; Puglia ; Regional geology ; Structural geomorphology ; Subduction ; Vertical movement
  • Geochronology of Middle and Upper Pleistocene loess sections in Hungary
  • Géochronologie ; Hongrie ; Loess ; Méthodologie ; Paléosol ; Pléistocène ; Quaternaire ; Stratigraphie ; Thermoluminescence
  • Geochronology ; Hungary ; Loess ; Methodology ; Palaeosol ; Pleistocene ; Quaternary ; Stratigraphy ; Thermoluminescence
  • Pleistocene glaciation of the King Valley, Western Tasmania, Australia
  • Australie ; Glaciation ; Paléogéographie ; Pléistocène ; Quaternaire ; Stratigraphie ; Tasmania
  • Australia ; Glaciation ; Paleogeography ; Pleistocene ; Quaternary ; Stratigraphy ; Tasmania
  • The objectives of this study were to describe the character and extent of the Pleistocene deposits, to establish the number and periods of glaciation, to reevaluate the existing Pleistocene stratigraphy, and to compare the glacial events with those
  • known in other Southern Hemisphere middle latitude areas.
  • Tephrostratigraphy of the Bedded Tuff Member (Kapthurin Formation, Kenya) and the nature of archaeological change in the later middle Pleistocene
  • Acheuléen ; Adaptation ; Homme fossile ; Kenya ; Pléistocène ; Quaternaire ; Site archéologique ; Téphrochronologie
  • Acheulean ; Adaptation ; Archeological site ; Fossil man ; Kenya ; Pleistocene ; Quaternary ; Tephrochronology
  • The AA. emphasize here data from the Kapthurin Formation of Kenya and detail a stratigraphic framework for a succession of volcanic tephra and archaeological sites that provides the means to assess temporal change across the Acheulian Middle Stone
  • Middle Pleistocene climate change recorded in fossil mammal teeth from Tarija, Bolivia, and upper limit of the Ensenadan land-mammal age
  • Analyse isotopique ; Bolivie ; Carbone ; Chronostratigraphie ; Dent ; Mammifère ; Oxygène 18 ; Paléo-environnement ; Pléistocène ; Quaternaire ; Variation climatique
  • Bolivia ; Carbon ; Chronostratigraphy ; Climatic variation ; Isotope analysis ; Mammal ; Oxygen 18 ; Palaeo-environment ; Pleistocene ; Quaternary
  • Fossiliferous middle Pleistocene sediments of the Tarija basin of southern Bolivia contain a classic Ensenandan land-mammal fauna. New carbon isotopic data reported here for 5 specimens of the grazing mammals Equus (horse) and Cuvieronius (mastodon
  • ), documented from 8 stratigraphic levels at Tarija, vary significantly in the C 13 values of their teeth. These new isotopic data are used here to identify warm-cold paleoclimatic cycles during the middle Pleistocene and clarify the upper limit
  • Middle-Late Pleistocene evolution of the Adriatic coastline of Southern Apulia (Italy) in response to relative sea-level changes
  • Faille ; Géomorphologie littorale ; Italie ; Littoral ; Niveau marin ; Pléistocène ; Puglia ; Quaternaire ; Sédiment marin
  • Coastal environment ; Coastal geomorphology ; Fault ; Italy ; Marine sediment ; Pleistocene ; Puglia ; Quaternary ; Sea level
  • The Adriatic coastal area stretching from Monopoli to Brindisi in Apulia is characterised by landforms and marine/coastal deposits of Middle-Upper Pleistocene age. An E-W striking fault system, roughly corresponding to the geographic “Soglia
  • Messapica”, is also present. This area shows the effects of different phases of coastal evolution. During the Middle Pleistocene, north of the Soglia Messapica, thin coastal deposits accumulated and abrasion surfaces were cut whereas, to the south, marine
  • Pleistocene stages in the Middle Dnieper basin by evidence of spore-pollen analysis of loesses in Lithology and stratigraphy of loess and paleosols.
  • Dnepr ; Géographie de l'Europe ; Loess ; Palynologie ; Paléobiogéographie ; Pléistocène ; Quaternaire zones moyennes ; URSS d'Europe ; Variation climatique
  • Karstic landscape evolution of southern Apulia foreland during the Pleistocene
  • by Middle Pleistocene terrigenous sediments has been recognized. Presently, the Salento Peninsula landscape shows at its inner and western parts wide karstic surfaces, remnants of the middle Pleistocene sedimentary cover, and morphostructural ridges. - (NF)
  • The Salento area is a narrow peninsula composed of Cretaceous and Neogenic carbonatic rocks constituting the southernmost part of the emerged Apulian foreland. A karstic landscape shaped on Upper Cretaceous - Lower Pleistocene rocks and covered
  • Dating early and middle Pleistocene glaciations in central Yukon by tephrochronology
  • Canada ; Datation ; Datation K/Ar ; Glaciation ; Paléo-environnement ; Pléistocène ; Quaternaire ; Thermoluminescence ; Téphrochronologie ; Yukon
  • Canada ; Dating ; Glaciation ; K/Ar dating ; Palaeo-environment ; Pleistocene ; Quaternary ; Tephrochronology ; Thermoluminescence ; Yukon
  • on the timing of extensive Pleistocene glaciations that affected this area. This approach relies on the tephrochronological method, augmented by glass-fission-track, K-Ar, and TL (thermoluminescence) ages, which are supported at some localities by paleomagnetic
  • Documents palynologiques du Pléistocène moyen dans le Sud-Ouest de la France
  • France ; France du Sud-Ouest ; Géographie physique ; Palynologie ; Pléistocène moyen ; Quaternaire zones moyennes
  • Some Middle Pleistocene deposits and palynological diagrams were discovered in South-West of France. The floras of these phases are poorly known in Europa, especially for the beginning of the Middle Pleistocene. In South-West of France, some
  • Palaeoenvironments and sedimentology of the Middle Pleistocene Olorgesailie Formation, southern Kenya Rift Valley in Palaeoecology of Africa and the surrounding islands-Vol 13.
  • Afrique ; Diatomée ; Formation d'Olorgosailie ; Géographie de l'Afrique ; Kenya ; Limnologie ; Paléo-environnement ; Paléobiogéographie ; Paléohydrologie ; Pléistocène moyen ; Quaternaire zone chaude ; Rift africain ; Sédiment fluviatile ; Sédiment
  • A detailed account is presented of the sediments and diatoms of the Middle Pleistocene Olorgesailie Formation. Facies distributions suggest a lake that was centred on the Koora Graben and which periodically expanded over an area to the north of Mt
  • phases in the evolution of the palaeolake can be inferred. The palaeogeography of the southern Kenya Rift and Middle Pleistocene palaeoclimate are briefly considered.
  • Schwermineralverteilung und Alter pleistozäner mariner Sedimente in Mittelitalien. (Heavy mineral distribution and age of Pleistocene marine sediments in middle Italy)
  • Beach rock ; Géographie physique ; Italie ; Lazio ; Minéraux lourds ; Pléistocène ; Quaternaire marin ; Sédiment marin ; Sédimentologie ; Terrasse ; Terrasse marine
  • In the Maremma, Alto Lazio, Middle Italy, heavy mineral studies were used to differentiate several types of beachrock and other marine sediments which are attributed to marine terraces of different age. (L'A.).
  • Middle Pleistocene (Early Toringian) carnivore remains from northern Israel
  • Carnivore ; Faune fossile ; Israël ; Montagne ; Paléobiogéographie ; Paléontologie ; Pléistocène ; Quaternaire ; Refroidissement climatique ; Variation climatique
  • Climatic cooling ; Climatic variation ; Fossil fauna ; Israel ; Mountain ; Palaeobiogeography ; Palaeontology ; Pleistocene ; Quaternary
  • Study of seventy well-preserved fossil remains from deposits of an eroded karstic cave in the Upper Galilee of northern Israel. This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). The AA. correlate the carnivore faunule
  • with some Near Eastern and southern Levantine sites and assume that only a severe cold phase could have shifted these species over the Taurus-Zagros mountain chain this far to the south. This faunule elucidates Pleistocene biotic exchanges between Europe
  • Le gisement pléistocène à grands mammifères à Rotselaar (Brabant, Belgique)
  • Belgique ; Brabant ; Gisement ; Mammifère ; Paléo-environnement ; Paléo-écologie ; Paléoclimat ; Pléistocène ; Quaternaire
  • Belgium ; Brabant ; Geological field;Site;Deposits ; Mammals ; Paleo-ecology ; Paleo-environment ; Paleoclimate ; Pleistocene ; Quaternary
  • The presence of cave lion and the evolutionary stage of the horse and mammoth remains, dates the fauna back to the middle of the last glacial period. Paleoecological and paleoclimatological information is given. - (LW)
  • Interregional paleopedological Pleistocene correlation of the USSR loess regions in Lithology and stratigraphy of loess and paleosols.
  • Géographie de l'Europe ; Paléopédologie ; Paléosol ; Pléistocène ; Quaternaire ; Stratigraphie ; URSS
  • Investigations were carried out in the Don, Upper Oka, Middle Volga basins, the Ural Foreland, souther part of the West-Siberian plain and in Soviet Central Asia and Georgia. 15 Pleistocene stages are identified with the corresponding stratigraphic
  • Stratigraphy and sedimentology at Bir Sahara, Egypt : environments, climate change and the Middle Paleolithic
  • Archéologie ; Artefact ; Changement climatique ; Désert ; Egypte ; Géoarchéologie ; Paléo-environnement ; Paléolithique ; Pléistocène ; Quaternaire ; Stratigraphie ; Sédimentologie
  • Archaeology ; Artifact ; Climatic change ; Desert ; Egypt ; Geoarchaeology ; Palaeo-environment ; Palaeolithic ; Pleistocene ; Quaternary ; Sedimentology ; Stratigraphy
  • Bir Sahara, situated in the eastern Saharan portion of northeast Africa, contains a set of sedimentary sequences that imply episodic changes in climate and environment during the Middle and Late Pleistocene. Some of the stratigraphic contexts
  • are associated with Middle Paleolithic artifact assemblages. The artifact assemblages are typically in sands that underlie deposits composed of high amounts of carbonate or fine clastics (muds) indicative of expanding lakes and wetter climates. The wetter
  • climates may have provided landscapes that were periodically inhabitable by Pleistocene hominids.