Where: Oklahoma (35.9° N, 95.0° W: paleocoordinates 11.7° S, 36.3° W)
• coordinate based on political unit
• local area-level geographic resolution
When: Chesterian (335.5 - 323.2 Ma)
• The Pitkin Fm. overlies the Fayetteville Fm. This boundary is gradational and for this study was taken to be the point at which shale partings between the limestone beds were not more than several inches thick. The Pitkin limestone ranges in thickness from 0 to over 60ft. in northeastern Oklahoma. The Pitkin is absent north of Wagoner and Cherokee counties due to truncation below lower Pennsylvanian strata. In the study area, the Pitkin represents the uppermost Mississippian and is unconformably overlain by lower Pennsylvanian Morrowan Series.
Environment/lithology: wackestone and mudstone
Primary reference: R. S. F. Fabian. 1987. Relation of Biofacies to Lithofacies in interpreting Depositional Environments in the Pitkin Limestone (Mississippian) in Norhteastern Oklahoma (Part I). Shale Shaker 76-95 [T. Olszewski/M. Gibson]more details
PaleoDB collection 12786: authorized by Tom Olszewski, entered by Melissa Gibson on 16.12.2001
Creative Commons license: CC BY (attribution)
Taxonomic list
Bivalvia | |
Schizodus sp. King 1844 clam | |
Edmondia sp. de Koninck 1841 clam | |
Sphenotus sp. Hall 1884 clam | |
Aviculopecten sp. M'Coy 1851 scallop | |
Rhynchonellata | |
Reticulariina sp. Fredericks 1916 | |
Dielasma sp. Beede and Rogers 1900 | |
Girtyella sp. Weller 1911 | |
Anthracospirifer sp. Lane 1963 | |
Composita sp. Brown 1849 | |
"Camarophoria sp." = Stenoscisma
"Camarophoria sp." = Stenoscisma Conrad 1839 | |
Strophomenata | |
Rugosochonetes sp. Sokolskaja 1950
Eolissochonetes sp. Hoare 1960 | |
Diaphragmus sp. Girty 1910 | |