. Bulletins of American paleontology. OsAGEAN Type Sections: Lane et al. 185 EUROPEAN SERIES VISEAN (part) (0 a z < < z (£. O LLI I- < -J r < a. LU ~ NORTH AMERICAN SERIES Z < LU O < o m I- < IT < UJ KINDERHOOK- lAN (part) FORAMINIFERAL ASSEMBLAGES (MIDCONTINENT) Lower Warsaw- Keokuk faunas (Brenckle etal., 1974. 1982; Kammer 1990) Endothyra-"Priscella" Rectogranuliferella godini- Mametella chautauquae Gllmore City faunas (Brenckle & Groves, 1987; Woodson, 1993) Septaglomospiranella- Prochernyshinella? CONODONT ZONES texanus bulbosus c Q C â s lane
. Bulletins of American paleontology. OsAGEAN Type Sections: Lane et al. 185 EUROPEAN SERIES VISEAN (part) (0 a z < < z (£. O LLI I- < -J r < a. LU ~ NORTH AMERICAN SERIES Z < LU O < o m I- < IT < UJ KINDERHOOK- lAN (part) FORAMINIFERAL ASSEMBLAGES (MIDCONTINENT) Lower Warsaw- Keokuk faunas (Brenckle etal., 1974. 1982; Kammer 1990) Endothyra-"Priscella" Rectogranuliferella godini- Mametella chautauquae Gllmore City faunas (Brenckle & Groves, 1987; Woodson, 1993) Septaglomospiranella- Prochernyshinella? CONODONT ZONES texanus bulbosus c Q C â s lanei latus multistriatus communis carinus punctatus isosticha Upper crenulata CONODONT FAUNAL UNITS 4B 4A 3B 3A 1G 1F TYPE OSAGE Lower Warsaw- Keokuk Burlington Burlington Sedalia MISSISSIPPI RIVER VALLEY. Chouteau Text-figure 2.âOsagean microfossil zones/assemblages and their relation to North American Midcontineni formations and western European series. Diagnostic conodonts. belonging to the multistriatus Zone, are limited to the lower part of the Burlington Limestone in the type Osage. The upper part of the Burlington in this area is placed within the laiitiis and lanei conodont zones (Faunal Units 4A and 4B) by stratigraphic position. The Gilinore City foraminifers are assumed to fit within the hiatus at the Kinderhookian-Osagean boundary in the Mississippi River Valley (Brenckle and Groves, 1987). even though this assemblage cannot be correlated directly to either the Mississippi River Valley or the type Osage because there are no diagnostic foraminifers in common. The Septaglomospiranella-Prochernyshinellal foraminiferal assemblage comes from occurrences listed in Lane and Brenckle (in press, fig. 8); the Rectogranuliferella godini-Mametella chautauquae assemblage from occurrences discussed in this paper; and the Endothyra-"Priscella" assemblage is from Witzke et al. (1990) and Lane and Brenckle (in press, fig. 8). sured sections are located within the quarry a
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