Where: Austria (46.6° N, 12.9° E: paleocoordinates 42.5° S, 52.7° E)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Oulodus elegans detorta conodont zone, Megarella Formation, Pridoli (423.0 - 419.2 Ma)
• Pridolian age
• bed-level stratigraphic resolution
Environment/lithology: shallow subtidal; grainstone
•beds have less peloids, with bioclasts forming the major allochthonous components in predominantly sparitic rather than micritic matrix.
•were fragmented crinoids, bryozoans, brachiopods, corals and cephalopods (restricted to this interval).
Size classes: mesofossils, microfossils
Primary reference: 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]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 141073: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 20.03.2013
Creative Commons license: CC BY (attribution)