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Oligocence dinoflagellate-cysts in Quaternary freshwater sediments of Eifel maars

  • H. Weiler
Palaeobiology
Part of the Lecture Notes in Earth Sciences book series (LNEARTH, volume 49)

Abstract

Well preserved dinoflagellate-cysts, indicating an oligocene age, were found in young-quarternary fresh water maare-lake sediments. They are the remnants of a former wide spread transgression from the Mainz-Basin into the Eifel-area.

Keywords

Sediment Core Lake Sediment Stratigraphic Range Tertiary Sediment Additional Sediment 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. GRAMOWSKI, E. (1987): Marine, oligozäne Fossilien in jungquartären Sedimenten der Westeifel. Überlegungen zur Paläogeographie.—Diplom-Arbeit der Joh. Gutenberg-Universität, Institut für Geowissenschaften. 150 S., 50 Abb., 10 Ktn., 9 Tab., Mainz.Google Scholar
  2. ROTHAUSEN, K.H. & SONNE, V. (1984): Mainzer Becken. Sammlung geolog. Führer, 79, 203 S., 21 Abb., 24 Taf., Borntraeger, Berlin.Google Scholar
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  4. WEILER, H. (1982): Bestandsaufnahme des Phytoplanktons (Dinoflagellaten-Zysten, Prasinophyceae und Calciodinelloideen) im “prae-aquitanen” Tertiär des Mainzer Beckens.—Mainzer geowiss. Mitt., 10, 13–17, 1 Tab., Mainz.Google Scholar
  5. WEILER, H. (1990): Calcispaeren aus oligozänen Schichten des Mainzer Beckens und des Oberrheingrabens.—Mainzer geowiss. Mitt., 19, 9–48, 89 Abb., 1 Tab., Mainz.Google Scholar

Copyright information

© Springer-Verlag 1993

Authors and Affiliations

  • H. Weiler
    • 1
  1. 1.Geologisches Landesamt Rheinland-PfalzMainz

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