«Unterer Seewerkalk»
Back to Seewen-FormationRepresentation and status
- Color CMYK
- N/A
- Color RGB
- R: 125 G: 125 B: 125
- Rank
- lithostratigraphic unit
- Validity
- Unit is not in Use
- Status
- incorrect name (though informally used)
- Status discussion
Nomenclature
- Deutsch
- «Unterer Seewerkalk»
- Français
- «Calcaire inférieur de Seewen»
- Italiano
- «Calcare inferiore di Seewen»
- English
- «Lower Seewen Limestone»
- Historical Variants
-
Unterer Seewen Kalk (Paulcke 1906), unterer Seewerkalk (Herb 1965), Calcaires sublithographiques en bancs (Villars 1992)
Hierarchy and sequence
- Subordinate units
- Upper boundary
-
Roter Seewerkalk
- Lower boundary
-
Garschella-Formation
Age
- Age at top
-
- Turonian
- Age at base
-
- Cenomanian
Geography
- Geographical extent
- Amden (Herb 1965) + Bornes, Aravis, Platé (Villars 1992).
Palaenography and tectonic
- Tectonic unit (resp. main category)
- Kind of protolith
-
- sedimentary
-
Untere Götzis-Bank
- Name Origin
- Götzis (Österreich)
- Rank
- lithostratigraphic Bed
- Status
- incorrect name (though informally used)
- In short
- Resedimentierte glaukonitisch-sandige Einschaltungen («Grünsand») im unteren, gebankten Teil der Seewen-Formation (direkt über den OAE-2). Im proximalen Bereich häufig mit Lithoklasten aus der Garschella-Formation.
- Age
- Latest Cenomanian
-
Bonarelli level (OAE-2)
- Name Origin
-
Named after the Italian geologist Guido Bonarelli (1871-1951).
- Rank
- Oceanic Anoxic Event
- Status
- valid
- In short
-
Oceanic anoxic event at the Cenomanian/Turonian boundary (around 93 Ma ago) with a major impact on the chemistry of the oceans worldwide. This event correlates with a marine extinction event.
- Age
- Late Cenomanian