...TALIA KARIM; STEPHEN R. WESTROP Abstract In south-central Oklahoma, the Pooleville Member of the Bromide Formation is a shallowing upward sequence recorded by distal to more proximal storm-influenced shelf facies. The deepest subtidal facies contains horizons of dense clusters of a single species...

... (Harris’ Corbin Ranch Limestone; equivalent to the upper 20 ft or 6 m of the Pooleville Member of the Bromide Formation). The correlation may well prove to be correct, although present biostratigraphic evidence bearing on this conclusion is meager. In 1963 Templeton and Willman (p. 134–135, 192) proposed...

...FIGURE 11 —Schematic diagram showing survival and regional extinction of trilobite genera in shallow subtidal facies between the upper Bromide (Pooleville Member) and Viola Springs formations. Most of the genera recorded from shallow subtidal facies of the Pooleville disappear with the appearance...

...Figure 2. Stratigraphic section (TQ) in the Pooleville Member of the Bromide Formation, arrows denote horizons collections were taken from. See Sprinkle (1982 , p. 363) for a measured section of the RC locality. Key to abbreviations: ms  =  mudstone, ws  =  wackestone, ps  =  packestone, gs...

... members of the Pontotoc series are absent. The conglomerates near Berwyn, formerly called Franks, are assigned to the Pontotoc series, and a correlation made across the mountains by J. T. Richards on the basis of some concentric-ringed pebbles which have been banded by algae. It is suggested...

... horizons ( Karim and Westrop, 2002 , fig. 5) in an approximately six-meter interval at the top of the Bromide ( Carlucci et al., 2010 , fig. 2). These strata have been assigned to the youngest Pooleville Member of the Bromide in most previous work (e.g., Shaw, 1974 ; Karim and Westrop, 2002 ; Carlucci...

...FIGURE 1— Clustered Homotelus bromidensis (Esker, 1964) from the Pooleville Member, Bromide Formation, Upper Ordovician Sandbian Stage, Criner Hills near Ardmore, Oklahoma; more than 45 articulated prone and 6 enrolled specimens shows evidence of minor decay and dissociation prior to burial...

... collected from the Pooleville Limestone Member of the Bromide Formation, 8 m below the contact with the overlying Viola Springs Formation at an abandoned quarry near the north end of Criner Hills (SW1;cl4, SE1;cl4, sec. 9, T 5S, R 1E, Carter County; Decker, 1935 , and Finney, 1988 ). The Illinois...

..., a square mile or less in area. The larger outcrops occur on the southwest side of the Arbuckle anticline in narrow strips from the vicinity of Pooleville almost to Ravia, two on either side of Washita River northwest of Dougherty, one east of Dougherty between Crusher and the Nebo Store, one at Lawrence...

...., about 17 miles southeast of Ada. Three other sections have been restudied, one east of Pooleville in Sec. 6, T. 2 S., R. 1 W., on West Spring Creek, and two southwest of Ardmore at the north and south ends of the Criner Hills in Sees. 16 and 35, T. 5 S., R. 1 E. In this restudy several changes have been...

... late in Wewoka time, and To all geologists, the term “Arbuckle Mountains” means the entire area in which the lower Paleozoic rocks crop out, and this area is roughly triangular, with the apex at Ada, one angle at Pooleville, and the other at Boggy Depot ( Fig. 2 ). Powers 10 recognized...

... lacking pinnules. Pinnulate crinoids account for almost half of the echinoderms from the Pooleville Member, which was deposited in deeper and quieter water (BA 4). Pinnulate camerates dominate the Girardeau Limestone of Illinois and Missouri, another BA 4 habitat ( Brower, 1973 ; Brett et al., 1997...

... and Sample 2 at Burr Oak and it is possible that these organisms may have competed for food and space. Other examples of Upper Ordovician crinoids in which competition for space and substrates was probably important are known. Examples are: the archaeocrinid beds in the Pooleville Member of the Bromide...

.... Paratypes are from the Pooleville Member, Bromide Formation, Turian Stage, Late Ordovician, Geological Enterprises Quarry, Criner Hills, Oklahoma (see Sprinkle, 1982 ). In addition to the illustrated specimens, several hundred small fragments are reposited at the Prairie Research Institute...

... steinheimerae n. sp. is most like other species of Abludoglyptocrinus , particularly A. pustulosus from the Upper Ordovician Forreston Member of the Grand Detour Formation, Illinois and A. laticostatus from the Upper Ordovician (Sandbian) Pooleville Member of the Bromide Formation, Oklahoma. All three...

... Llandovery crinoids into faunas (e.g., crinoids from the Pooleville Member of the Bromide Formation, the Brassfield Formation). We then used Webster's (2002) compilation to evaluate all species for validity and correct genus assignment. Similarly, we assessed the validity of all genera. In some instances...

... laticardinalis and Cremacrinus ramifer occur in the Mountain Lake and Pooleville members of the Bromide Formation in which the former member was deposited in more shallow and agitated water ( Longman, 1982 ; statistics in Table 3 , eqs. 8, 9). The Student's t values for the logarithms of the initial...