Gerstenhübel-Bank

Back to Effingen-Member

Representation and status

Color CMYK
cf. Effingen-Member
Color RGB
R: 190 G: 195 B: 185
Rank
lithostratigraphic Bed
Validity
Unit is in Use
Status
informal term
Status discussion

Nomenclature

Deutsch
Gerstenhübel-Bank
Français
Banc du Gerstenhübel
Italiano
Strato del Gerstenhübel
English
Gerstenhübel Bed
Origin of the Name

Gerstenhübel, Veltheim (AG)

Historical Variants
Gerstenhübelkalk (Jäckli 1966, Hantke 1967), Gerstenhübel-Schicht (Gygi 1969), Gerstenhübel Beds (Gygi 2000b, Gygi 2000c), Gerstenhübel-Kalkschicht
Nomenclatorial Remarks
Schon von F. Mühlberg ausgeschieden. Hübel = Hügel, Berg, Erhebung

Description

Description
Wohlgeschichtete (in Bänken von 20 cm bis 30 cm), leicht mergelige Kalksteine mit spärlichem Vorkommen von Fossilien. Eine rund 10 m mächtige, feingeschichtete Mergelkalkbankabfolge wird im Steinbruch Jakobsberg von Gygi (1969) als Gerstenhübel-Bank 1) bezeichnet und mit dem Riffgürtel der Günsberg-Formation weiter im Westen korreliert (Gygi 2000). Innerhalb des insgesamt 230 m mächtigen Effingen-Members der Bohrung Küttigen-1 (Ref. 3) identifizieren Albert et al. (2007) eine 28 m mächtige Kalkbankabfolge, welche rund 88 m über der Basis einsetzt, als Gerstenhübel-Bank.
Geomorphology
Prominente morphologische Rippe innerhalb des Effingen-Members.
Thickness
Bis 12 m; 16 m (Wetzel & Strasser 2001) ; 13,4 m an der Typlokalität (Gygi 1973)

Components

Fossil Content
  • protists
Coccolithen (Gygi 1969)

Hierarchy and sequence

Superordinate unit
Units at roof
Units at floor

Age

Age at top
  • middle Oxfordian
Age at base
  • middle Oxfordian
Dating Method
Bifurcatus-Zone : Amoeboceras cf. serratum (Sowerby) (Atrops et al. 1993, Gygi 2000b)

Geography

Geographical extent
Erlinsbach - Holderbank - Chestenberg - Villigen (AG).
Type area
Nördlicher Kt. Aargau
Type locality
  • Gerstenhübel (AG)
    Site particularities
    • Obergrenze
    • Untergrenze
    • typische Fazies
    Site accessibility
    • Steinbruch, Tongrube
    Coordinates
    • (2654100 / 1252500)
    Note
    • Steinbruch Jakobsberg, N von Wildegg (Gygi 1969 S.66 Pl.17 Profil RG37, Gygi 2000c)
Type profile
  • Gerstenhübel (AG)
    Site particularities
    • Obergrenze
    • Untergrenze
    • typische Fazies
    Site accessibility
    • Steinbruch, Tongrube
    Coordinates
    • (2654100 / 1252500)
    Note
    • Steinbruch Jakobsberg, N von Wildegg (Gygi 1969 S.66 Pl.17 Profil RG37, Gygi 2000c)

Palaenography and tectonic

  • Malm of the Jura Mountains
Paleogeography
Argovian Basin
Tectonic unit (resp. main category)
Kind of protolith
  • sedimentary
Sequence
The onset of the 16 m thick limestone deposits of the Gerstenhübel Beds represents a flooding followed by highstand sedimentation with increased carbonate production. A few metres above the top of the Gerstenhübel Beds, a 5 - 10 cm thick mudstone bed is capped by a limonite/pyrite crust up to 3 mm thick. Burrows and borings in this hardground suggest a multiphase formation. The sequence-stratigraphic significance of this horizon is debatable; Pittet (1996) interepreted it as maximum-flooding surface, whereas Allenbach (2001c) suggested a type II sequence boundary (SB Ox6) and sediment by-passing. (Wetzel & Strasser 2001)
Metamorphism
non metamorphic

References

Definition
Gygi R. A. (1969) : Geologische Beschreibung des Aargauer-Jura und der nördlichen Gebiete des Kantons Zürich.
Definition
Gygi R. A. (2000) : Annotated index of lithostratigraphic units currently used in the Upper Jurassic of northern Switzerland. Eclogae geol. Helv. 93/1, 125-146

p.130: Gerstenhübel Beds (Gygi 1969) ; Thick limestone succession within the Effingen Member of the Wildegg Formation The Gerstenhübel Beds (Gerstenhübel-Schicht) were named by Gygi (1969. p. 66). The type locality is the hill called Gerstenhübel (coordinates 654.100/252.500) 2 km south-southeast of Veltheim. Canton Aargau. LK 1089. Aarau. where the unit was quarried for some time. The names Veltheim and Gerstenhübel are not indicated on the map LK 1089, Aarau. The Gerstenhübel Beds are the succession no. 37 in section RG 37 of Gygi (1969. Pl. 17). This is the type section. The Gerstenhübel Beds are a well-bedded succession of

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