Titlebook: Climatic Changes on a Yearly to Millennial Basis; Geological, Historic N.-A. M?rner,W. Karlén Book 1984 Springer Science+Business Media Dor

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978-90-481-8399-9Springer Science+Business Media Dordrecht 1984

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,Kritische Würdigung und Ausblick, 13,000–10,000 yrs B.P., in SW Sweden (H?kulls Mosse, province of Sk?ne) are interpreted against the two dominant palaeoclimatic models: the palaeobotanical model (Iversen) and the palaeoentomological model (Coope). An important time lag is found in the vegetation response to climatic improvement af

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https://doi.org/10.1007/978-3-8350-9496-300 yr B.P. With litho-, bio- and chronostratigraphic investigations combined with various physical and chemical analyses a picture of the Late Weichselian/Early Holocene glacial, vegetational and, climatic history has been obtained. In the later part of the rather warm Allenz?d Chronozone the Baltic

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