Grove Church Shale
Lithostratigraphy: Pope Megagroup >>Grove Church Shale
Chronostratigraphy: Paleozoic Erathem >>Mississippian Subsystem >>Chesterian Series >>Elviran Stage
Allostratigraphy: Kaskaskia Sequence
Primary source
Willman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.
Contributing author(s)
Elwood Atherton, Charles Collinson, and Jerry A. Lineback
Name
Original description
Grove Church Shale (Swann, 1963, p. 44-45).
Derivation
Named for Cedar Grove Church, Johnson County.
Other names
History/background
Type section
Type location
The type section for the Grove Church is in a roadcut and near-by gullies, 1.25 miles east of Lick Creek (W line NE NW 31, 11S-2E), where the formation is 16 feet thick.
Type author(s)
Type status
Reference section
Reference location
Reference author(s)
Reference status
Stratigraphic relationships
The Grove Church Shale is the uppermost formation in the Chesterian Series in Illinois.
Extent and thickness
The formation has been largely eroded from Illinois by pre-Pennsylvanian erosion, and it occurs only in patches in Johnson, Pope, and Saline Counties, and probably in parts of adjacent counties. The maximum known thickness is 67 feet in the northern half of Johnson County.
Lithology
The Grove Church is a gray, fossiliferous shale and includes interbedded fossiliferous limestone. It was originally part of the Kinkaid Formation, but it was split off because it is dominantly shale. As a result, the Kinkaid is a dominantly limestone formation.
Core(s)
Photograph(s)
Contacts
Well log characteristics
Fossils
It has a distinctive fauna; some species have affinities to Pennsylvanian fossils, particularly the fusuline Millerella and some ostracodes (Cooper, 1947). The conodont fauna differs strikingly from that of the Kinkaid (Rexroad and Burton, 1961). The genus Streptognathodus comprises over one-third of the fauna of the Grove Church and there is a marked decrease in Cavusgnathus. Transitional forms show that the change is evolutional, rather than being a migratory influx.
Age and correlation
Environments of deposition
Economic importance
Remarks
References
COOPER, C. L., 1947, Upper Kinkaid (Mississippian) microfauna from Johnson County, Illinois: Journal of Paleontology, v. 21, p. 81-94; Illinois State Geological Survey Report of Investigations 122.
REXROAD, C. B., and R. C. BURTON, 1961, Conodonts from the Kinkaid Formation (Chester) in Illinois: Journal of Paleontology, v. 35, p. 1143-1158; Illinois State Geological Survey Reprint 1962-B.
SWANN, D. H., 1963, Classification of Genevievian and Chesterian (Late Mississippian) rocks of Illinois: Illinois State Geological Survey Report of Investigations 216, 91 p.
ISGS Codes
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