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Tytuł artykułu

Geochronology of vegetation stages of south-east Baltic coast (Kaliningrad region) during the middle and Late Holocene

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The raised bog sediments that have been continuously accumulated over time represent the most suitable natural object which enables us to reconstruct Late Glacial and Holocene vegetation and palaeoclimates. Bog peat consists of organic carbon formed in situ. It contains moss, plant fragments and microfossils that are necessary for the study of palaeovegetation and palaeoclimate. However, a successful study of palaeoenvironment can be carried out on the basis of investigation of a great quan-tity of samples along the whole peatbog thickness. In the present paper, the authors present the results of palynological, botanical investigations and radiocarbon dating of 31 peat samples taken from the raised bog Velikoye, located in the eastern part of Kaliningrad Region. The data obtained have ena-bled us to reconstruct the palaeovegetation, reveal the evolution of the bog and determine rate of peat formation at different evolutional stages over the last 7500 cal BP.
Wydawca
Czasopismo
Rocznik
Strony
172--181
Opis fizyczny
Bibliogr. 15 poz., rys.
Twórcy
autor
autor
autor
autor
autor
autor
autor
  • Faculty of Geography and Geoecology, St. Petersburg State University, V.O., 10-Line, 33, 199178, St. Petersburg, Russia, arslanovkh@mail.ru
Bibliografia
  • Arslanov KhA, Tertychnaya TV and Chernov SB, 1993. Problems and methods of dating low-activity samples by liquid scintillation couting. Radiocarbon 35(3): 393-398.
  • Arslanov KhA, Savelieva LA, Gey NA, Klimanov VA, Chernov SB, Chernova GM, Kuzmin GF, Tertychnaya TV, Subetto DA and Denisenkov VP, 1999. Chronology of vegetation and palaeoclimatic stages of Northwestern Russia during the Late Glacial and Holocene. Radiocarbon 41(1): 25-45.
  • Arslanov KhA, Savelieva LA, Klimanov VA, Chernov SB, Maksimov FE, Tertychnaya TV and Subetto DA, 2001. New data on chronology of landscape palaeoclimatic stages in Northwestern Russia during the Late Glacial and Holocene. Radiocarbon 43(2): 545-558.
  • Bronk Ramsey C, Dee M, Lee S, Nakagawa T, Staff RA, 2010. Developments in the calibration and modeling of radiocarbon dates. Radiocarbon 52(3): 953-961.
  • Dolukhanov PM, 1977. The Holocene history of the Baltic Sea and ecology of prehistoric settlement. Baltica 6: 227-244.
  • Dolukhanov PM, Shukurov AM, Arslanov KhA, Subetto DA, Zaitseva GI, Djinoridze EN, Kuznetsov DD, Ludikova TV and Savelieva LA, 2007. Evolution of Waterways and Early Human Settlements in the Eastern Baltic Area. Radiocarbon 49(2): 527-542.
  • Grichuk VP and Zaklinskaya ED, 1948. Analysis of fossil pollen and spores and its application in palaeogeography. Moscow: 223 pp. (in Russian).
  • Grimm E, 1991. TILIA and TILIAGRAPH. Illinois State Museum, Springfield.
  • Elina GA, Araslanov KhA and Klimanov VA, 1996. Development stages of Holocene vegetation in Southern and Eastern Karelia. Botanical Journal 81(3): 1-17 (in Russian).
  • Kabailene M, 1977. About reconstruction of the forests history Lithuania durin the Holocene on evidence derived from palynlogical analysis. Baltica (6): 216-224.
  • Klimanov VA, 1976. On the procedure of reconstruction of quantitative climatic characteristics of the past. Vestnik of Moscow State University. Geographical Series 2: 92-98.
  • Kuzmin GF, 1993. Peatbogs and their application. Publication of All Russian Research Institute of Peat Industry, 200 pp (in Russian).
  • Ralska-Jasiewiczowa M and Starkel L, 1994. Changes of vegetation in Poland during Holocene. [In:] Velichko AA, Starkel L, eds., Palaeogeographical bases of recent landscapes. Moscow, Nauka: 205 pp (in Russian).
  • Reimer P.J. et al., 2009. IntCal09 and Marine09 radiocarbon age calibration curves, 0-50,000 yrs cal BP. Radiocarbon 51(4): 1111-1150.
  • Stuiver M, Reimer PJ, Bard E et al., 1998. INTCAL 98 Radiocarbon calibration, 24,000-0 cal BP. Radiocarbon 40(3): 1041-1083.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BWMA-0003-0009
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