Articles | Volume 5, issue 1
https://doi.org/10.1144/jm.5.1.37
https://doi.org/10.1144/jm.5.1.37
01 Apr 1986
 | 01 Apr 1986

Danian dinoflagellate zonation, the C-T boundary and the stratigraphical position of the fish clay in southern Scandinavia

Stefan U. Hultberg

Cited articles

L. W., Alvarez, W., Alvarez, F., Asaro and H. V., Michel: Extraterrestrial cause for the Cretaceous-Tertiary extinction, Science, 208, 1095-1108, 1980.
W., Alvarez, L. V., Alvarez, F., Asaro and H. V., Michel: The end of the Cretaceous: sharp boundary or gradual transition, Science, 223, 1183-1186, 1983.
J. P., Bujak and E. H., Davies: Modern and fossil Peridiniineae, Am. Assoc. Strat. Palynol., Contr, 13, 1-203, 1983.
A. H., Cheetham: Functional morphology and biofacies distribution of Cheilostome Bryozoa in the Danian Stage (Paleocene) of southern Scandinavia, Smithsonian Contrib. Paleobiol, 6, 81-1971.
L., Christensen, S., Fregerslev, A., Simonsen and J., Thiede: Sedimentology and depositional environment of Lower Danian Fish Clay from Stevns Klint, Denmark, Bull. geol. Soc. Denmark, 2, 192-212, 1973.
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