Skip to main content
Log in

Long-term vegetation dynamics and the infilling process of a former lake (Švarcenberk, Czech Republic)

  • Published:
Folia Geobotanica Aims and scope Submit manuscript

Abstract

Natural lakes are a rare phenomena within extraglacial areas of Central Europe. Almost all have been completely terrestrialized during the Holocene. This paper deals with one such former lake, located in southern Bohemia. Its extensive lacustrine and peat deposits were subjected to a multidisciplinary study that resulted in high-resolution pollen, macrofossil, algal and sediment-chemistry data interpreted in terms of past climate, geomorphology, soil, and regional vegetation development over the last 16,000 years. Against the background of these large-scale processes, local development took place, comprising the lake’s ontogeny from an arctic-type ecosystem hosting pioneer aquatic communities, through a highly diversified mosaic of eutrophic hydrosere habitats (shallow pools,Phragmites andCarex fen, alder carr), towards an oligotrophic mire that started to dome over the terrestrialized lake. At every individual development stage, specific processes characterized ecosystem function and composition: during the Late-Glacial with its rapid climatic changes, external forces induced the major stresses; while during the Holocene, autogenic changes of the wetland ecosystem played the most important role.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Aaby B. &Berglund B.E. (1986): Characterisation of peat and lake deposits. In:Berglund B.E. (ed.),Handbook of Holocene palaeoecology and palaeohydrology, John Wiley & Sons, Chichester, pp. 231–246.

    Google Scholar 

  • Ammann B. &Lotter A.F. (1989): Late-glacial radiocarbon and palynostratigraphy of the Swiss Plateau.Boreas 18: 109–126.

    Article  Google Scholar 

  • Ammann B. (1989): Response times in bio- and isotope-stratigraphies to Late-glacial climatic shifts — an example from lake deposits.Eclog. Geol. Helv. 82/1: 183–190.

    Google Scholar 

  • Backman A.L. (1951):Najas minorAll. in Europa. Einst und Jetzt.Acta Bot. Fenn. 48: 3–32.

    Google Scholar 

  • Bos H. (1998):Aspects of the Lateglacial — Early Holocene vegetation development in western Europe (Palynological and palaeobotanical investigations in Brabant, the Netherlands and Hessen, Germany). LPP Contributions Series No. 10, LPP Foundation, Utrecht.

    Google Scholar 

  • Bottema S. (1974): The interpretation of pollen spectra from prehistoric settlements (with special attention toLiguliflorae).Palaeohistoria 17: 18–35.

    Google Scholar 

  • Culek M., Grulich V. &Povolný D. (eds.) (1995):Biogeografické členění České republiky (Biogeographical subdivision of the Czech Republic). Enigma, Praha.

    Google Scholar 

  • Dansgaard W. (1980): Palaeoclimatic studies on ice cores. In:Oeshger H., Messerli B. &Svilar M. (eds.),Das Klima. Analysen und Modelle, Geschichte und Zukunft. Springer, Berlin, Heidelberg, New York, pp. 237–245.

    Google Scholar 

  • de Gans W. (1988): Pingo scars and their identification. In:Clark M.J. (ed.),Advances in periglacial geomorphology, John Wiley & Sons, Chichester, pp. 299–324.

    Google Scholar 

  • Dearing J.A. (1991): Lake sediment record of erosional processes.Hydrobiologia 214: 99–106.

    Article  Google Scholar 

  • Demek J. (ed.) (1987):Hory a nížiny. Zeměpisný lexikon ČSR (Mountains and lowlands. Geographical lexikon of the ČSR). Academia, Praha.

    Google Scholar 

  • Ellenberg H. (1996):Vegetation Mitteleuropas mit den Alpen. Ed. 5. Eugen Ulmer GmbH & Co., Stuttgart.

    Google Scholar 

  • Engstrom D.R. &Wright H.E. Jr. (1984): Chemical stratigraphy of lake sediments as record of environmental change. In:Haworth E.Y. &Lund J.G.W. (eds.),Lake sediments and environmental history, Leicester University Press, Leicester, pp. 11–67.

    Google Scholar 

  • Faegri K. &Iversen J. (1989):Textbook of pollen analysis. J. Wiley, Chichester.

    Google Scholar 

  • Frenzel B. (1983): Mires — repositories of climatic information or self-perpetuating ecosystems? In:Gore A.J.P. (ed.),Mires: swamp, bog, fen and moor, General studies, Ecosystems of the world 4A, Elsevier, Amsterdam, Oxford, New York, pp. 35–65.

    Google Scholar 

  • Gams H. (1926):Hydrocaryaceae. In:Hegi (ed.),Flora von Mitteleuropa V/2, München, pp. 882–894.

  • Hammarlund D. &Buchardt B. (1996): Composite stable isotope records from a Late Weichselian lacustrine sequence at Graenge, Lolland, Denmark: evidence of Alleröd and Younger Dryas environments.Boreas 25: 8–22.

    Article  Google Scholar 

  • Hoek W. (1997): Palaeogeography of Lateglacial Vegetations. Aspects of Lateglacial and Early Holocene vegetation, abiotic landscape, and climate in the Netherlands.Ned. Geogr. Stud., 230: 1–147.

    Google Scholar 

  • Holčík J. (1977): Changes in fish community of Klicava reservoir with particular reference to Eurasian perch (Perca fluviatilis) 1857–1972.J. Fish. Res. Board Canada, 34: 1734–1747.

    Google Scholar 

  • Huizer A.S. &Izarin R.F.B. (1997): The reconstruction of past climates using multi-proxy evidence: An example of the Weichselian Pleniglacial in northwest and central Europe.Quatern. Sci. Rev. 16: 513–533.

    Article  Google Scholar 

  • Huntley B. &Prentice I.C. (1993): Holocene vegetation and climates of Europe. In:Wright H.E., Kutzbach J.E., Webb T., Ruddiman W.F., Street-Perrot F.A. &Bartlein P.J. (eds.),Global climates since the Last Glacial maximum, University of Minnesota Press, Minneapolis, London, pp. 136–168.

    Google Scholar 

  • Husák Š. &Hejný S. (1978): General characteristics of the Třeboň Basin and Lednice region. In:Dykyjová D. &Květ J. (eds.),Pond littoral ecosystems, Ecological Studies 28, Springer-Verlag, Berlin, pp. 13–95.

    Google Scholar 

  • Iversen J. (1954): The Late-glacial flora of Denmark and its relation to climate and soil.Danmarks Geol. Undersøl. II/80: 87–119.

    Google Scholar 

  • Jankovská V. (1980):Paläogeobotanische Rekonstruktion der Vegetationsentwicklung im Becken Třeboňská pánev während des Spätglazials und Holozäns. Vegetace ČSSR A11, Academia, Praha.

    Google Scholar 

  • Jankovská V. (1983): Palynologische Forschung am ehemaligen Komořany-See (Spätglazial bis Subatlanticum).Věstn. Ústředn. Ústavu Geol. 58: 99–107.

    Google Scholar 

  • Jankovská V. &Komárek J. (1982): Das Vorkommen einiger Chlorokokalalgen in Bömischen Spätglazial und Postglazial.Folia Geobot. Phytotax. 17: 165–195.

    Google Scholar 

  • Jankovská V. &Komárek J. (1995):Pediastrum orientale from subfossil layers.Folia Geobot. Phytotax. 30: 319–329.

    Google Scholar 

  • Jorga W., Pietsch W. &Weise G. (1982): Beiträge zur Ökologie und Bioindication vonTrapa natans L.Limnologica 14: 385–394.

    CAS  Google Scholar 

  • Jowsey P.C. (1966): An improved peat sampler.New Phytol. 65: 245–248.

    Article  Google Scholar 

  • Kac J.N., Kac C.V. &Kipiani M.G. (1965):Atlas i opredelitel’ plodov i semyan vstrechayushchikhsya v chetvertichnykh otlozheniyakh SSSR (An atlas and a key to fruits and seeds found in Quaternary deposits of the Soviet Union). Nauka, Moscow.

    Google Scholar 

  • Karasev G.L. (1987):Ryby Zabaikal’ya (Fish of Zabaikal’e). Nauka, Novosibirsk.

    Google Scholar 

  • Klečka A. (1926): O stáří Českých rašelin (On the age of Bohemian peat bogs).Věda Přír. 7: 305–313.

    Google Scholar 

  • Klečka A. (1928): Agrobotanická studie o rokytských rašelinách (Agrobotanical study on Rokytské peat bog).Sborn. Českoslov. Akad. Zeměd. 3: 195–267.

    Google Scholar 

  • Komárek J. &Jankovská V. (2000):Review of the green algal genus Pediastrum;Implication for pollenanalytical research. Bibliotheca Phycologica, J. Kramer, Berlin, Stuttgart, in press.

    Google Scholar 

  • Kubiak-Martens L. (1996): Evidence for possible use of plant foods in Palaeolithic and Mesolithic diet from the site of Calowanie in the central part of the Polish Plain.Veg. Hist. Archaeobot. 5: 33–38.

    Article  Google Scholar 

  • Lang G. (1994):Quartäre Vegetationsgeschichte Europas. G. Fisher, Jena.

    Google Scholar 

  • Lotter A.F. (1988): Paläeoökologische und paläolimnologische Studie des Rotsees bei Luzern. Pollen-, grossrest-, diatomeen- und sedimentanalytische Untersuchungen.Diss. Bot. 124: 1–187.

    Google Scholar 

  • Lotter A.F. &Juggins S. (1991): POLPROF, TRAN and ZONE Programs for plotting, editing and zoning pollen and diatom data. INQUA-Commission for the Study of the Holocene, Working group.Data-Handling Meth. Newslett. 6: 651–660.

    Google Scholar 

  • Mangerud J., Andersen S.T., Berglund B.E. &Donner J.J. (1974): Quaternary stratigraphy of Norden, a proposal of terminology and classification.Boreas 3: 109–127.

    Article  Google Scholar 

  • Moore P.D., Webb J.A. &Collinson M.E. (1991):Pollen analysis. Blackwell, Oxford.

    Google Scholar 

  • Olsen S.R., Cole C.V., Watanabe F.S. & Dean L.A. (1954): Estimation of available phoshorus in soils by extraction with sodium bicarbonate.Circ. U.S.D.A. No. 939. USA

  • Pissart A. (1988): Pingos: an overview of the present state of knowledge. In:Clark M.J. (ed.),Advances in periglacial geomorphology, John Wiley and Sons, Chichester, pp. 279–298.

    Google Scholar 

  • Punt W. (ed.) (1976–1996):The Northwest European pollen flora 1–7. Elsevier, Amsterdam.

    Google Scholar 

  • Rudolph K. &Firbas F. (1922): Pollenanalytische Untersuchungen böhmischer Moore.Ber. Deutsch. Bot. Ges. 47: 393–405.

    Google Scholar 

  • Rudolph K. (1917): Untersuchungen über den Aufbau böhmischer Moore I. Aufbau und Entwicklungsgeschichte südböhmischer Hochmoore.Abh. Königl. Zool. Bot. Ges. Wien 9/4: 1–116.

    Google Scholar 

  • Rybníček K. (1983): The environmental evolution and infilling process of a former lake near Vracov (Czechoslovakia).Hydrobiologia 103: 247–250.

    Article  Google Scholar 

  • Stuiver M., Grootes P.M. &Braziunas T. (1995): The GISP18O climate record of the past 16,500 years and the role of the sun, ocean and volcanoes.Quatern. Res. 44: 341–354.

    Article  CAS  Google Scholar 

  • Štěpánová M. (1930): Une étude de dévélopément des tourbes dans la Bohéme de Sud.Spisy Přír. Fak. Karlovy Univ. 109: 1–36.

    Google Scholar 

  • Törnqvist T.E., de Jong A.F.M., Oosterbaan W.A. &van der Borg K. (1992): Accurate dating of organic deposits by AMS14C measurement of macrofossils.Radiocarbon 34: 566–577.

    Google Scholar 

  • Tallis J.H. (1983): Changes in wetland communities. In:Gore A.J.P. (ed.),Mires: swamp, bog, fen and moor, General studies, Ecosystems of the world 4A, Elsevier, Amsterdam, Oxford, New York, pp. 311–347.

    Google Scholar 

  • Troels-Smith J. (1955): Characterization of unconsolidated sediments.Danmarks Geol. Undersøl. 3/10: 73 pp.

    Google Scholar 

  • Tutin T.G. et al. (eds.) (1964–1980):Flora europaea 1–5. Cambridge University Press, Cambridge.

    Google Scholar 

  • van Geel B., Bohncke S.J.P. &Dee H. (1981): A palaeoecological study of an upper Lateglacial and Holocene sequence from De Borchert, The Netherlands.Rev. Palaeobot. Palynol. 31: 367–448.

    Article  Google Scholar 

  • van Geel B., Coope G.R. &van der Hammen T. (1989): Palaeoecology and stratigraphy of the Lateglacial type section at Usselo (The Netherlands).Rev. Palaeobot. Palynol. 39: 25–129.

    Article  Google Scholar 

  • van Geel B., Hallewas D.P. &Pals J.P. (1983): A Late Holocene deposit under the Westfriese Zeedijk near Enkhuizen (Prov. of Noord-Holland, The Netherlands) palaeoecological and archaeological aspects.Rev. Palaeobot. Palynol. 38: 269–335.

    Article  Google Scholar 

  • Walker D. (1970): Direction and rate in some British Post-glacial hydroseres. In:Walker D. &West R.G. (eds.),Studies in the vegetational history of the British Isles, Cambridge University Press, Cambridge, pp. 117–139.

    Google Scholar 

  • Walker M.J.C. (1995): Climatic changes in Europe during the last glacial/interglacial transition.Quatern. Int. 28: 63–76.

    Google Scholar 

  • Washburn A.L. (1980):Geocryology. A survey of periglacial processes and environments. John Wiley and Sons, New York.

    Google Scholar 

  • Weber C.A. (1908): Aufbau und Vegetation der Moore Norddeutschlands.Bot. Jahrb. 40 (Suppl.): 19–34.

    Google Scholar 

  • Zvelebil M. (1994): Plant use in the Mesolitic and its role in the transition to farming.Proc. Syst. Prehist. Soc. 60: 35–74.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Petr Pokorný.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Pokorný, P., Jankovská, V. Long-term vegetation dynamics and the infilling process of a former lake (Švarcenberk, Czech Republic). Folia Geobot 35, 433–457 (2000). https://doi.org/10.1007/BF02803554

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02803554

Keywords

Navigation