Results 161 to 170 of about 4,167 (219)
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The Late-Weichselian flora of the Isle of Man
Philosophical Transactions of the Royal Society of London. B, Biological Sciences, 1970Abstract The last glacial deposits of the Ballaugh-Kirkmichael area in the north-east of the Isle of Man have been investigated by analysis of pollen and macroscopic fossils and by radiocarbon dating. Assemblages totalling over 160 taxa of vascular plants and mosses have been recorded from strata referred to LateWeichselian zones I ...
C A, Dickson +2 more
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Multiproxy climate reconstructions for the Eemian and Early Weichselian
Journal of Quaternary Science, 1998Palaeobotanical, coleopteran and periglacial data from 106 sites across northwestern Europe have been analysed in order to reconstruct palaeoclimatic conditions during the Eemian and Early Weichselian. Three time slices in the Eemian and four in the Early Weichselian have been considered.
Aalbersberg, G., Litt, T.
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Late Weichselian Palaeomagnetic Reversal
Nature Physical Science, 1971AS part of the joint European work on the establishment of a world standard section for the Pleistocene/Holocene boundary, an oriented core 14.5 m long was taken with the Swedish foil piston corer in the Botanical Garden of Gothenburg (south-west Sweden).
N.-A. MÖRNER, J. P. LANSER, J. HOSPERS
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Weichselian Convolution Phenomena and processes in fine sediments.
Boreas, 1982In three excavations in the southern Netherlands and northern Belgium, the Weichselian convolutions in fine sand, silt and clay deposits were investigated, and an attempt was made towards a semi‐quantitative approach to some sediment parameters.
Vandenberghe, Jef, Van den Broek, P.
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Boreas, 2008
Core material obtained from three boreholes was studied from the Ruunaa area, Finnish northern Karelia, in order to reveal the Late Pleistocene environmental history of eastern Finland. Conventional litho‐ and biostratigraphical methods were used and suitable sediment samples were dated using quartz optically stimulated luminescence.
Lunkka, J.P. +2 more
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Core material obtained from three boreholes was studied from the Ruunaa area, Finnish northern Karelia, in order to reveal the Late Pleistocene environmental history of eastern Finland. Conventional litho‐ and biostratigraphical methods were used and suitable sediment samples were dated using quartz optically stimulated luminescence.
Lunkka, J.P. +2 more
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Weichselian chronostratigraphy and correlations
Boreas, 1981The glacial history of the Fennoscandian ice cap beyond some 20,000 years B.P. is fairly poorly known because of the absence of a reliable dating control. The Eemian Interglacial of Europe is not dated at all. The Weichselian Glaciation seems to be characterized by three main glaciation maxima separated by two main interstadial periods (of quite ...
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Sedimentary features of a Weichselian glaciolacustrine delta
Boreas, 1981Inclined beds of sand, granules, pebbles and cobbles resembling a glacio‐tectonically tilted sequence were shown by sedimentological studies to constitute the 10–12 m thick foreset beds of a glaciolacustrine Gilbert‐type delta in Kyndby, North Sjælland, Denmark.
Clemmensen, Lars B +1 more
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Weichselian palaeoenvironments at Kobbelgård, Møn, Denmark
Boreas, 1991Lithostratigraphical and palynological investigations of a coastal cliff section at Kobbelgård, Møn (Denmark) reveal a sedimentary sequence of Weichselian age. Bedded clayey sediments are overlain by stratified silt, sand and occasional beds of clay and gravel.
Kolstrup, E., Houmark-Nielsen, M.
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Eemian and Weichselian stratigraphy in South Sweden
Boreas, 1981The stratigraphy of Pleistocene sequences within three main areas of the province of Skane, South Sweden, is discussed. The traditional stratigraphy is revised. New lithostratigraphic units are deficned and named according to international stratigraphic terminology.
BJÖRN E. BERGLUND, ERIK LAGERLUND
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Weichselian in Sweden before 15,000 B.P.
Boreas, 1981A brief summary is given of the present state of knowledge about the Weichselian glaciations and interstadials in sweden. The following stages are discussed: (1) The first Weichselian glaciation (W1). This glaciation has not been identified. Probably only northern Sweden was ice‐covered. (2) The Jämtland Interstadial, dated at > 50,000 B.P.
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