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Remains of chironomid larvae from cores of the ancient Lake Faulersee in northern Germany were examined. Pollen, radiocarbon datings, and geochemical data were used to develop the chronology of the Late-Glacial Period in Lake Faulersee and to validate interpretations made by chironomid data. Factors influencing the composition of the subfossil chironomid assemblages were assessed. Our data indicate fluctuations of temperature, lake-level, and trophic state in the Late-Glacial. Furthermore, we explain a discontinuous sequence found in the cores of Lake Faulersee pertaining to a refilling event about 5,800 cal years before present (BP).
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
117--127
Opis fizyczny
Bibliogr 34 poz.
Twórcy
autor
- Heineckeweg 3, D-38173 Evessen, Germany
autor
- Universität Göttingen, Institute for Palynology and Quaternary Science, Wilhelm-Weber-Str. 2, D-37075 Göttingen, Germany
autor
- UFZ – Umweltforschungszentrum Leipzig-Halle GmbH, Brückstr. 3a, D-39114 Magdeburg, Germany
autor
- Dept. Hydrogeology, Theodor-Lieser-Straße 4, D-06120 Halle, Germany
Bibliografia
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- Walker I.R. 1988a. Late-Quaternary palaeoecology of Chironomidae (Diptera: Insecta) from lake sediments in British Columbia. Ph.D. Thesis. Simon Fraser University, Burnaby.
- Walker I.R. 1988b. Late-Quaternary fossil Chironomidae (Diptera) from Hippa Lake, Queen Charlotte Islands, British Columbia, with special reference to Corynocera Zett. Canadian Entomologist 120, 739–751.
- Walker I.R., Levesque A.J., Cwynar L.C., Lotter A.F. 1997. An expanded surface-water palaeotemperature inference model for use with fossil midges from eastern Canada. Journal of Paleolimnology 18, 165–178.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BPW9-0007-0032