By Nils-Axel Mörner (auth.), N.-A. Mörner, W. Karlén (eds.)
Nils-Axel Marner &Wibjarn Karlen Organizers of the Stockholm Symposium in 1983 Stockholm college, Sweden This publication is the lawsuits of the second one NORDIC SYMPOSIUM ON CLIMATIC alterations AND similar difficulties held in Stockholm, Sweden, could 16-20, 1983 (Frydendahl et al., 1983; Marner, 1983). This was once "an foreign interdisciplinary symposium with particular refe rence to Nordic files and their relation to international climatic changes". the 1st NORDIC SYMPOSIUM ON CLIMATIC alterations AND similar difficulties used to be held in Copenhagen in 1978 ( Frydendahl, 1978) and had a truly vast medical application. the second one NORDIC SYMPOSIUM was once particularly directed to convinced difficulties, time levels and assets of knowledge, as mentioned lower than. Scandinavia is a classical sector for the examine of climatic fluctuations over the past 20,000 years . a big a part of the elemental info for the overseas theories and synthesis originate from Scandinavian info. this is applicable, for instance, to: (1) The drastic climatic fluctuations in reference to the re cession of the land-ice giving upward push to the alternation of inter stadials (warm classes with fast ice recession) and stadials (cold sessions with readvances or retardations within the ice recession). (2) The climatic alterations throughout the Holocene with its famous sub-division in line with the Blytt-Sernander approach (nowadays getting used some distance outdoor the boreal quarter for which it used to be origi nally defined). (3) The Holocene climatic optimal and the next climatic de terioration at round 2500 BP (well-established already at the start of this century).
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Extra info for Climatic Changes on a Yearly to Millennial Basis: Geological, Historical and Instrumental Records
1977. Fossil coleopteran assemblages as sensitive indicators of climatic changes during the Devensian (Last) cold stage. Phil. Trans. R. Soc. Lond. B. 280, 313-340. R. , 1972 . Late Glacial environmental changes indicated by a coleopteran succession from North Wales. Boreas 1, 97-142 . Davis, M. B. , 1978. Climatic i nt er pret ati on of pollen in Quaternary sediments. In: Walker, D. C. (eds Biology and Quaternary Environments. Austral. Acad. , Canberra. 35-51. A. , III, 1983 . Dynamic plant ecology: The spectrum of vegetational change in space and time.
E. 10,262 varves BP (Marner, 1977) and in 20 B. E. -A . MORNER the area north of Mt. Billingen (Marner, 1970). According to the new results of Bjarck and Digerfeldt (this volume), there was a final "drainage" of the Baltic Ice Lake at about 10,500 BP. Bjarck and Digerfeldt (1982) have shown that there was a very rapid, not to say "instantaneous", drop in relative sea level in the Hunneberg area at about 10,200 radiocarbon years BP. (Note the fact, that this occurred west of Mt. Billingen and must, hence, not be confused with any "drainage" of the Baltic Ice Lake).
Climatic i nt er pret ati on of pollen in Quaternary sediments. In: Walker, D. C. (eds Biology and Quaternary Environments. Austral. Acad. , Canberra. 35-51. A. , III, 1983 . Dynamic plant ecology: The spectrum of vegetational change in space and time. Quaternary Science Reviews 1, 153-175. van Geel, B. , 1978. Tentative explanation of the Late Glacial and Early Holocene climatic changes in NorthWestern Europe. Geologie En Mijnbouw 57,87-89. , 1954. The Late-Glacial flora of Denmark and its relation to climate and soil.