Wolayer area, Mt Seewarte, Pedavis pesavis zone, sample Se/02/11/04: Lochkovian, Austria

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Conodonta - Prioniodontida
Pseudooneotodus beckmanni (Bischoff and Sannemann 1958)
5 specimens
Conodonta - Prioniodontida - Icriodontidae
20 specimens
Conodonta - Ozarkodinida - Spathognathodontodae
Ozarkodina excavata (Branson and Mehl 1933)
5 specimens
recombined as Hindeodella excavata
Conodonta - Belodellida - Belodellidae
Belodella resima (Philip 1965)
75 specimens
Dvorakia sp. Klapper and Barrick 1983
1 specimen
Conodonta - Panderodontida - Panderodontidae
Panderodus sp. Ethington 1959
4 specimens
see common names

Geography
Country:Austria
Coordinates: 46.6° North, 12.9° East (view map)
Paleocoordinates:50.6° South, 57.2° East
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period:Devonian Epoch:Early/Lower Devonian
Stage:Lochkovian 10 m.y. bin:Devonian 1
Key time interval:Lochkovian Conodont zone: Pedavis pesavis
Age range of interval:419.20000 - 410.80000 m.y. ago
Stratigraphy
Formation:Rauchkofel
Stratigraphic resolution:group of beds
Lithology and environment
Primary lithology: packstone
Secondary lithology: grainstone
Lithology description: Peloidal pack- to grainstone
Environment:shallow subtidal indet.
Geology comments: Grainstones were found to range from bioclasts with little or no micritisation to coated grains wherein the rim is extensively micritized around the entire grain. The first of these accords with rather rapid cementation of components after breakage and deposition. Components are crinoid stem plates with subordinate skeletal grains of brachiopods and bryozoans. Peloids are sparse or even lacking.Grainstones were found to range from bioclasts with little or no micritisation to coated grains wherein the rim is extensively micritized around the entire grain. The first of these accords with rather rapid cementation of components after breakage and deposition. Components are crinoid stem plates with subordinate skeletal grains of brachiopods and bryozoans. Peloids are sparse or even lacking.
Taphonomy
Modes of preservation:body
Size of fossils:mesofossils,microfossils
Collection methods and comments
Reason for describing collection:taxonomic analysis
Metadata
Database number:141040
Authorizer:W. Kiessling Enterer:M. Krause
Modifier:M. Krause Research group:marine invertebrate
Created:2013-03-20 23:22:55 Last modified:2013-03-20 15:13:49
Access level:authorizer only Released:2013-06-20 23:22:55
Creative Commons license:CC BY
Reference information

Primary reference:
45614. T. J. Suttner. 2007. Conodont Stratigraphy, Facies-Related Distribution Patterns and Stable Isotopes (Carbon and Oxygen)of the Uppermost Silurian to Lower Devonian Seewarte Section(Carnic Alps, Carinthia, Austria). Abhandlungen der Geologischen Bundesanstalt (59)1-111 [W. Kiessling/M. Krause]