| Imo Formation | |
| Type: | Formation |
| Age: | Carboniferous |
| Namedfor: | Imo, Searcy County, Arkansas |
| Namedby: | Mackenzie Gordon Jr.[1] |
| Region: | Arkansas |
| Country: | United States |
| Unitof: | Pitkin Formation |
| Underlies: | Hale Formation |
The Imo Formation, or Imo Shale, is a geologic unit in northern Arkansas that dates to the Chesterian Series of the late Mississippian. The Imo is considered to be a member of the upper Pitkin Formation, and is the most recent Mississippian age rock in Arkansas. The Imo Shale unconformably underlies the Pennsylvanian age Hale Formation
The stratigraphic placement of this interval has long been debated. It was introduced in 1964 as the "Imo Formation," representing an interval of shale that was presumably of Mississippian and possibly of Pennsylvanian age. However, in a footnote in the first publication to use this designation, the author noted that the shale interval had been mapped into the Pennsylvanian Cane Hill Member of the Hale Formation and revoked use of the name "Imo Formation".
The name was reintroduced in 1973 as the "Imo Shale",[2] and in 2010 was classified as a member of the Mississippian age Pitkin Formation.[3]
A. discus[4]
C. mapesi[4]
D. bressoni[4]
E. imoense[4]
E. richardsoni[4]
F. bransoni[4]
F. friscoense[4]
M. saundersi[4]
P. ornatum[4]
R. miseri[4]
S. cadiconiformisj[4]
S. involutum[4]
S. imprimis[4]
S. tenuis
E. explicata[5]
E. rugosa[5]
Z. discoidea[5]