Büls-Bank

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Darstellung und Status

Farbe CMYK
siehe Betlis-Fm.
Farbe RGB
R: 160 G: 210 B: 120
Rang
lithostratigraphische Bank
Gebrauch
Element ist in Gebrauch
Status
lokaler Begriff (informell)

Nomenklatur

Deutsch
Büls-Bank
Français
Banc de Büls
Italiano
Strato del Büls
English
Büls Bed
Herkunft des Namens

Hinterbüls (SG), Churfristen

Historische Varianten
Büls-Bank (Kuhn 1997), Büls Member (Föllmi et al. 2007)

Beschreibung

Mächtigkeit
Max. 5 m (Föllmi et al. 2007).

Komponenten

Fossilien
  • Ammoniten

Hierarchie und Abfolge

Alter

Alter Top
  • Frühes Valanginien

Bermerkungen zu Top
Stephanophorus Zone / frühe campylotoxus-Zone (Wyssling 1986, Kuhn 1996)
Alter Basis
  • Frühes Valanginien

Bermerkungen zu Basis
späte Pertransiens-Zone
Datierungsmethode
Biostratigraphie (Ammoniten : Wyssling 1986, Kuhn 1996).

Paläogeografie und Tektonik

  • «Neokom»
  • Kreide des Helvetikums
Paläogeografie
North Tethyan Shelf (Helv.) :
marge continentale européenne
Tektonische Einheit (bzw. Überbegriff)
Herkunftstyp
  • sedimentär

Referenzen

Erstdefinition
Kuhn Oliver (1996) : Der Einfluss von Verwitterung auf die Paläozeanographie zu Beginn des Kreide-Treibhausklimas (Valanginian und Hauterivian) in der West-Tethys. Diss. ETH Zürich

Die Phosphoritbildung der neudefinierten Büls-Schichten findet innerhalb der Pertransiens und Stephanophorus-Zone statt (Unter Valanginian), ...
Neubearbeitung
Föllmi Karl B., Bodin Stephane, Godet Alexis, Linder Pascal, van de Schootbrugge B. (2007) : Unlocking paleo- environmental information from Early Cretaceous shelf sediments in the Helvetic Alps: stratigraphy is the key! Swiss J. Geosci. 100, 349-369

p.354: In distal parts of the platform, the lower Betlis Limestone is overlain by an up to 5 m thick and heterogeneous succession, which consists of sandy, glauconitic, hemipelagic carbonates and marl, which include a discrete level of phosphate nodules or a phosphatized hardground (Fig. 2; Fig. 3). This unit is identified both in different regions in Vorarlberg (Austria), as well as in eastern and central Switzerland (Hauswirth 1913; Heim 1910–1916; Haus 1937; Strasser 1979; Felber and Wyssling 1979) and has been defined as “Büls Beds” by Kuhn (1996). The Büls Member is underlain either by sediments of the Vitznau Formation or of the lower Betlis Limestone (Fig. 2) and overlain by sediments of the hemipelagic Sichel Limestone of the Diphyoides Formation. In the case this latter member is absent, the Büls Member bundle with the overlying Gemsmättli Bed and forms a single phosphate-rich bed (Kuhn 1996). This is the case for example at the type locality of the Gemsmättli Bed in the Pilatus region (Wyssling 1986). The Büls Member includes the oldest drowning unconformity within the Helvetic platform succession, and documents a first phase of highly reduced carbonate production on the platform (Föllmi et al. 1994, 2006). Its age is constrained by ammonite biostratigraphy in occurrences in Vorarlberg and eastern Switzerland and encompasses the late pertransiens and early campylotoxus zones (Wyssling 1986; Kuhn 1996).
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