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  • The sea level in the last interglacial
  • Sangamon and pre-sangamon interglaciations in the Hudson Bay lowlands of Manitoba in The Last? Interglaciation in Canada : Le dernier (?) interglaciaire au Canada.
  • This paper reviews what is known about the last and penultimate interglaciations in northern Manitoba, concentrating on an inventory of the interglacial sites, including diagrammatic descriptions of each site, and more detailed descriptions
  • of the interglacial units. The Manitoba non-glacial units are correlated with similar deposits from other parts of the Hudson Bay Lowlands and some conclusions about the Sangamonian climate and paleogeography are drawn.
  • Comparison of soils in midwestern United States and western Europe with the interglacial record
  • Paleosols that formed primarily before the last glaciation cannot be adequately explained by a model of Holocene like interglacial periods of about 10,000 yr in length. Available data on soils formed during the middle and late Pleistocene from
  • Western Europe and midwestern United States are best explained by relatively long interglaciations or the development of composite soils over a number of temperate periods. Climatic contrasts between the interglaciations appear to have been overemphasized
  • : widespread assumptions regarding greater warmth in interglaciations prior to the present one are generally unproven.
  • Aminostratigraphy of European marine interglacial deposits
  • Interglacial beds at Toronto, Ontario in The Last? Interglaciation in Canada : Le dernier (?) interglaciaire au Canada.
  • The interglacial of Frechen I/Rheinland a section of the Tiglian A-Type
  • Palynological investigations of earliest Pleistocene deposits at Frechen, some ten kilometers West of Cologne permit the dating of these sediments in terms of the Dutch biostratigraphic scale. Of special interest is a newly discovered interglacial
  • period, termed the Frechen I Interglacial, which indicates a more complicated development of vegetation during the early Tiglian than was hitherto thought. (AIS).
  • High-resolution paleotemperature proxy record for the last interglaciation based on norwegian speleothems
  • Chronostratigraphy ; Interglacial ; Isotope analysis ; Karst ; Norway ; Oxygen 18 ; Palaeoclimatology ; Palaeotemperature ; Quaternary ; Uranium
  • The purpose of this paper is to present high-latitude, U-series dated paleoclimatic proxy data from last interglacial speleothems that approach the time resolution reported in ice-core records.
  • Correlation problems of interglacial deposits in Finnish Lapland in Glaciations quaternaires dans l'Hémisphère Nord.
  • Based on the pollen content six different types of interglacial deposits have been recognized. The pollen stratigraphy obtained is very similar to that described from the Leveäniemi Interglacial deposit in northern Sweden.
  • Review on the age and distribution of marine terraces since the last interglacial
  • Review on the about age and distribution of marine terraces since the last interglacial in 22 areas of the world excluding Japan.
  • Paleoecology of organic deposits of probable last interglacial age in northern Ontario in The Last? Interglaciation in Canada : Le dernier (?) interglaciaire au Canada.
  • This paper will review the published palynological and macrofossil results for various deposits and present new data that relate to the character and stratigraphy of pre-Late Wisconsinan nonglacial episodes, particularly the last interglacial
  • Interglacial climates : advances in our understanding of warm climate episodes
  • Antarctica ; Europe ; Fluvial terrace ; Holocene ; Interglacial ; Mediterranean States ; Palaeo-environment ; Palaeoclimate ; Quaternary ; Stratigraphy
  • In this progress report, the AA. review the basis for interglacial complexity, drawing upon the evidence from long continuous terrestrial records in the Mediterranean, Antarctic ice cores and river terrace sequences in western Europe, before using
  • the details of the British Quaternary interglacial record as an example of how marine and terrestrial records can be linked.
  • U-series dates for stalagmitic flowstone E (Riss/Würm interglaciation) at Grotte du Lazaret, Nice, France
  • Alpes-Maritimes ; Archaeology ; Dating ; France ; Interglacial ; Isotope ; Palaeogeography ; Palaeozoology ; Provence-Alpes-Côte d'Azur ; Quaternary ; Stratigraphy
  • The results show that this speleothem began to grow about 130,000 yr B.P. and continued to about 70,000 yr B.P., coinciding almost exactly with the last interglaciation. Even though Ensemble E is not in direct stratigraphic relation with the cave
  • deposits, this study shows that the Acheulian artifacts industry and fauna within Lazaret are older than the Riss/Wurm interglaciation.
  • Stable isotope stratigraphy of a late last interglacial speleothem from Rana, northern Norway
  • Climate fluctuation ; Interglacial ; Isotope dating ; Norway ; Oxygen 18 ; Palaeo-environment ; Palaeoclimatology ; Quaternary ; Speleothem ; Stratigraphy ; Uranium
  • The AA. present high-resolution stable oxygen and carbon isotope records from a speleothem from northern Norway, giving details on climatic fluctuations from the late last interglacial and the last interglacial-glacial transition, as well
  • The last (Koy-Yukon) Interglaciation in the northern Yukon : evidence from unit 4 at Ch'ijee's Bluff, Bluefish in The Last? Interglaciation in Canada : Le dernier (?) interglaciaire au Canada.
  • Ch'ijees Bluff is an important datum for study of the last interglaciation in northern North America and because of this it has been designated as one of a number of northern references sites scheduled for detailed study under project CELIA (Climate
  • and Environment of the Last Interglacial in Northern North America). Pollen and fossils data are discussed (plant macrofossils, insect and other arthropod fossils).
  • Loess particle size data indicative of stable winter monsoons during the last interglacial in the western part of the Chinese Loess Plateau
  • Aeolian features ; China ; Grain size distribution ; Interglacial ; Loess ; Monsoon ; Palaeo-environment ; Palaeoclimate ; Palaeosol ; Plateau ; Quaternary ; Winter
  • Particle size data from the western part of the Chinese Loess Plateau do not support the last interglacial correlation, suggested by the data from the central part of the Loess Plateau, between the high dust-influx events in the Loess Plateau
  • and the cool events in the high northern latitudes. The lack of marked oscillations in the particle size of the last interglacial paleosol S1 in the western part of the plateau is interpreted as an indication of stable winter monsoons. It is thus inferred
  • that the teleconnection between the northern high latitudes and the Chinese Loess Plateau evident in the last glacial might not have existed during the last interglacial.
  • Organogenic deposits of the Mazovian Interglacial (Mindel II-Riss I) in the middle Vistula basin, compared to coeval European localities
  • Deposits representative of two climatic optima of the Mazovian Interglacial/Mindel II/Riss I/occur in post-glacial paleolakes/Ferdynandow, Podgorze/and paleovalleys/Syrniki/in the middle Vistula basin. As judged after their paleogeomorphologic
  • and lithostratigraphic analysis, the lower optimum of the Mazovian Interglacial can be correlated with the lower part /Lh/of the Likhvin Interglacial, and the upper optimum with the Holstein Interglacial. Younger organogenic deposits, underlying the till of the Odranian
  • Coastal aminostratigraphy on the Last Interglaciation in southern Australia
  • This report summarizes measurements of the extent of amino racemization in last-interglacial molluscan fossils from a range of coastal sequences in southern Australia. A model is presented that permits dating of fossiliferous strata based
  • Last interglacial sea levels on the south coast of New South Wales
  • Australia ; Dating ; Interglacial ; New South Wales ; Palaeogeography ; Quaternary ; Sea level ; Shoreline ; Thermoluminescence
  • This paper reports the sedimentary and thermoluminescence evidence from barrier beaches dating from the Last Interglacial at Middle Lagoon (also known as Tanja Lagoon) and Gillards Beach, 4-6 km north of the mouth of the Bega River, on the far south
  • Last Interglacial Muir Point Formation, Vancouver Island, British Columbia in The Last? Interglaciation in Canada : Le dernier (?) interglaciaire au Canada.
  • Paleosols of the interglacial climates in Canada in The Last? Interglaciation in Canada : Le dernier (?) interglaciaire au Canada.