Where: Quebec, Canada (49.7° N, 63.7° W)
• Paleocoordinates: 21.3° S, 88.2° W (Wright 2013)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Ozarkodina strena zone, Becscie Formation, Rhuddanian to Rhuddanian (443.4 - 438.5 Ma)
• lower half of the Llandovery (Lower Silurian) succession of Rhuddanian-
•early Aeronian age
• bed-level stratigraphic resolution
Environment/lithology: deep subtidal; mudstone
•lenticular intrarudstone. The Becscie Formation was interpreted as deposited on a low-energy, muddy, carbonate to argillaceous ramp subject to short-lived, episodic, highenergy storms.
Size classes: mesofossils, microfossils
Primary reference: S. Zhang and C. R. Barnes. 2002. A New Llandovery (Early Silurian) Conodont Biozonation and Conodonts from the Becscie,Merrimack, and Gun River Formations, Anticosti Island, Québec. Memoir (The Paleontological Society) [W. Kiessling/M. Krause]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 142676: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 15.04.2013
Creative Commons license: CC0 (CC0)
Taxonomic list
Conodonta | |
Ozarkodina strena conodont | |
Panderodus unicostatus Branson and Mehl 1933 conodont | |
Rexroadus nathani McCracken and Barnes 1981 conodont |