Articles | Volume 6, issue 2
https://doi.org/10.1144/jm.6.2.35
https://doi.org/10.1144/jm.6.2.35
01 Nov 1987
 | 01 Nov 1987

Palynological evidence for a diachronous low-salinity event in the C–T boundary clay at Stevns Klint, Denmark

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.
L. W., Alvarez, W., Alvarez, F., Asaro and H. W., Michel: Current status of the impact theory for the terminal Cretaceous extinction, Geol. Soc. Amer. Spec. Pap, 305-317, 1982.
L. W., Alvarez, W., Alvarez, F., Asaro and H. W., Michel: The end of the Cretaceous: Sharp boundary or gradual transition?, Science, 223, 1183-1186, 1987a.
W., Alvarez, E. G., Laufman, F., Surlyk, L. W., Alvarez, F., Asaro and H. W., Michel: Impact theory of mass extinctions and the invertebrate fossil record, Science, 223, 1135-1141, 1984b.
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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