Lower Danian bivalves, Stevns Klint, Denmark: continuity across the K/T boundary

Author:

Heinberg C.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference58 articles.

1. Abdel-Gawad, G.I., 1986. Maastrichtian non-cephalopod molluscs (Scaphopoda, Gastropoda and Bivalvia) of the Middle Vistula Valley, Central Poland. Acta Geol. Pol. 36 (1–3), 224 pp.

2. Extraterrestrial cause for the Cretaceous–Tertiary mass extinction;Alwarez;Science,1980

3. The terminal Cretaceous extinction in Boreal shelf seas — a multicausal event;Birkelund;Geol. Soc. Am. Spec. Pap.,1982

4. Bromley, R., 1979. Chalk and bryozoan limestone: Facies, sediments and depositional environments. In: Birkelund, T., Bromley, R.G. (Eds.), Cretaceous–Tertiary Boundary Events, University of Copenhagen, Copenhagen, pp. 16–32.

5. Fabric of the Cretaceous–Tertiary marina macrofaunal transition at Braggs, Alabama;Bryan;Palaeogeogr., Palaeoclimatol., Palaeoecol.,1989

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