Annales de la Société géologique de Belgique

0037-9395 2295-7227

 

ya que 05 febrero 2011 :
Vista(s): 566 (3 ULiège)
Descargar(s): 1028 (2 ULiège)
print        
Dieter Korn

The ammonoid faunal change near the Devonian-Carboniferous boundary

(Volume 115 (1992) — Fascicule 2 - Devonian-Carboniferous boundary)
Article
Open Access

Documento adjunto(s)

Anexidades

Abstract

The Upper Famennian ammonoid fauna is characterized by the predominance of the clymeniids, which became extinct in the topmost Devonian. The Hangenberg Black Shale marks the incision of ammonoid diversity. Survivors are only Mimimitoceras, Wocklumeria, Lissoclymenia and Cymaclymenia, which in two sections (Müssenberg, Drewer) occur in beds above the Hangenberg Blach Shale together with species of Acutimitoceras in the prorsum Zone. The Gattendorfia Stufe fauna evolved rapidly after the extinction of the clymeniids. The new taxa Globimitoceras gen. nov., Nicimitoceras gen. nov., and Mimimitoceras hoennense sp. nov. are proposed.

Para citar este artículo

Dieter Korn, «The ammonoid faunal change near the Devonian-Carboniferous boundary», Annales de la Société géologique de Belgique [En ligne], Fascicule 2 - Devonian-Carboniferous boundary, Volume 115 (1992), 581-593 URL : https://popups.uliege.be/0037-9395/index.php?id=3015.

Acerca de: Dieter Korn

Institut und Museum für Geologie und Paläontologie, Sigwartstrasse 10, D-7400 Tübingen.