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Variable isostatic uplift patterns during the holocene in southeast Sweden, based on high-resolution ams radiocarbon dating of lake isolations - a preliminary interpretation

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EN
Abstrakty
EN
To describe changes in shoreline configuration in northern Uppland, south-east Sweden, the isolations of 17 present and overgrown lakes have been interpreted from diatom analysis and AMS radiocarbon dates on terrestrial macrofossils. The sites studied are spread c. 60 km in east-west and c. 70 km in north-south direction. The oldest isobase direction, representing the "Neolithic Sea", extends in more or less north-south direction. The present day isobase system shows a clear east-west trend. The results indicate a complicated pattern of isostatic uplift during the late Holocene. We have defined five different shore displacement curves denoted A–E. It is obvious that the present day east-western isobase system is not valid for the investigated sites. Instead, the north-south isobases for the "Neolithic Sea" should to a relatively high degree explain the geographic distribution of sites. It is suggested that a re-direction of the isostatic uplift pattern has occurred sometime during the last c. 5000 years. This shift could have taken place as a slow deformation of the bedrock and/or as neotectonic movements along existing fault lines.
Rocznik
Tom
Strony
77--80
Opis fizyczny
bibliogr. 23 poz., rys., wykr.
Twórcy
autor
autor
autor
  • Department of Physical Geography and Quaternary Geology, Stockholm University, SE-106 91 Stockholm, Sweden, jan.risberg@geo.su.se
Bibliografia
  • AXBERG S., 1980 - Seismic stratigrahpy and bedrock geology of the Bothnian Sea, northern Baltic. Stockholm Contr. Geol., 36: 153-213.
  • BATTARBEE R.W., 1986 - Diatom analysis. In: Handbook of Holocene palaeoecology and palaeohydrology (ed. B.E. Beglund): 527-570. Wiley & Sons, Chichester.
  • BERGSTRÖM E., 2001 - Late Holocene distribution of lake sediment and peat in NE Uppland, Sweden. Swedish Nuclear Fuel and Waste Management Co (SKB). Report R-01-12.
  • BJÖRCK S., WOHLFARTH B., 2001 - Chronostratigraphic techniques in paleolimnology. In Tracking Environmental Change Using Lake Sediments, Vol 1: Basin Analysis, Coring and Chronological Techniques (red. W.M. Last, J.P. Smol): 205-238. Kluwer Academic Publishers, Dordrecht, The Netherlands.
  • DE GEER G., 1925 - Förhistoriska tidsbestämningar. Ymer, 45: 1-34.
  • EKMAN M., 1996 - A consistent map of the postglacial uplift of Fennoscandia. Terra Nova, 8: 158-165.
  • GRIMM E.C., 1987 - CONISS: a Fortran 77 program for stratigraphically constrained cluster analysis by the method of international sum of sequences. Computer & Geosciences, 13: 13-35.
  • GRIMM E.C., 1992 - Tilia and Tilia Graph: pollen spreadsheets and graphics programs. Program and Abstracts: 56. 8th International Palynological Congress. Aix-en Provence, September 6-12, 1992.
  • HEDENSTRÖM A., RISBERG J., 2003 - Shore displacement in northern Uppland during the last 6500 calender years. Swedish Nuclear Fuel and Waste Management Co (SKB). Report TR-03-17.
  • KRAMMER K., LANGE-BERTALOT H., 1986 - Bacillario-phyceae 1. Teil Naviculaceae. In: Süsswasserflora von Mittel-europa 2/1, (eds H. Ettl, J. Gerloff, H. Heynig, D. Mollenhauser). Gustav Fischer Verlag, Stuttgart.
  • KRAMMER K., LANGE-BERTALOT H., 1988 - Bacillariophyceae 2. Teil Bacillariaceae, Epithemiaceae, Surirellaceae. In: Süsswasserflora von Mitteleuropa 2/2, (eds H. Ettl, J. Gerloff, H. Heynig, D. Mollenhauser). Gustav Fischer Verlag, Stuttgart.
  • KRAMMER K., LANGE-BERTALOT H., 1991a - Bacillariophyceae 3. Teil Centrales, Fragilariaceae, Eunotiaceae. In: Süss-wasserflora von Mitteleuropa 2/3, (eds H. Ettl, J. Gerloff, H. Heynig, D. Mollenhauser). Gustav Fischer Verlag, Stuttgart.
  • KRAMMER K., LANGE-BERTALOT H., 1991b - Bacillariophyceae 4. Teil Achnanthaceae. Kritishe Ergänzungen zu Navicula (Lineolate) und Gomphonema. In Süsswasserflora von Mitteleuropa 2/4, (eds H. Ettl, J. Gerloff, H. Heynig, D. Mollen-hauser). Gustav Fischer Verlag, Stuttgart
  • JOHANSSON M., OLVMO M., LIDMAR-BERGSTRÖM K., 2001 Inherited landforms and glacial impact of different palaeosurfaces in southwest Sweden. Geografiska Annaler, 83, 1: 67-89.
  • LENNGREN M., 2003 - AMS dateringar av terrestra makrofossilfrån Stensjöns isolering indikerar ojämn isostasi i central Uppland, södra Sverige, efter ca 4400 C-14 år BP. Diploma work in Quaternary Geology. Stockholm University, Department of Physical Geography and Quaternary Geology. Diploma work K-3.
  • LIDMAR-BERGSTRÖM K., 1995 - Relief and saprolites through time on the Baltic shield. Geomorphology, 12: 45-61.
  • LIDMAR-BERGSTRÖM K., 1996 - Long term morphotectonic evolution in Sweden. Geomorphology, 16: 33-59.
  • MILLER U., HEDIN K., 1988 - The Holocene development of the landscape and environment in south-east Mälaren valley, with special reference to Helgö. KungligaVitterhets Historie och Antikvitets Akademien.
  • MÖLDER K., TYNNI R., 1967-1973 - Über Finnlands rezente und subfossile Diatomeen I-VI. Compt. Rendus Soc. géol. Finlande, 39: 199-217 (1967), Bull. Geol. Soc. Finland 40: 151-170 (1968), 41: 235-251 (1969), 42: 129-144 (1970), 43: 203-220 (1971), 44: 141-149 (1972), 45: 159-179 (1973).
  • RISBERG J., 1999 - Strandförskjutningen i nordvästra Uppland under subboreal tid. Appendix 4. In: Bälinge mossar. Kustbor i Uppland under yngre stenåldern. Doctoral thesis (ed. A. Segerberg): 233-241. Department of Archaeology and Ancient History, Uppsala University, Uppsala, Aun 26.
  • RISBERG J., ALM G., GOSLAR T., 2005 - Variable isostatic uplift patterns during the Holocene in southeast Sweden, based on high-resolution AMS radiocarbon datings of lake isolations. The Holocene, 15, 6: 849-859.
  • ROBERTSSON A.M., PERSSON CH., 1989 - Biostratigraphical studies of three mires in northern Uppland, Sweden. Sverig. Geol. Unders. (SGU), ser. C, 821.
  • TYNNI R., 1975-1980 - Über Finnlands rezente und subfossile Diatomeen VIII-XI. Geol. Surv. Finland Bull., 274 (1975), 284, (1976), 296 (1978), 312 (1980).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS6-0020-0025
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