The Glen Dean Formation

The Glen Dean Formation (Glen Dean Limestone) was named for the village of Glen Dean in southern Breckinridge Co., Kentucky. It is Chester age, Late Mississippian, and is bracketed by the Hardinsburg Sandstone below and the Tar Springs Sandstone above. It includes limestone and shale in varying proportions. The thickness of the Glen Dean varies between 40 – 50 feet northwest of Bowling Green (Warren County), Kentucky and in southern Illinois, reaching a maximum of 180 feet in western Breckinridge Co., Kentucky.

The Glen Dean has been documented in Hardin and Pope Counties of southern Illinois (see Butts, 1917) as well as south-central Indiana (Crawford, Dubois, Martin, Orange, and Perry Counties). Horowitz (1965) considers this formation as having abundant, highly diversified marine fauna which existed in clear, shallow agitated water and in quieter water where muds were deposited.

E.O. Ulrich (in Butts, 1917) considered this formation to be the most fossiliferous of the Chester series by volume, although the Golconda (now Haney Formation in Kentucky) has more species. Fifteen fossils are considered index fossils, restricted to this formation. The most common phylum is bryozoans, with just under 70 of the 162 species listed by Ulrich (pages 226 – 230).

Table 1 shows number of species of phyla in Ulrich’s list. This does not show later species, such as Perry and Horowitz (1963) and Utgaard & Perry (1960), nor trace fossils.

Phylum                 Species      Notes

Corals                          1          Zaphrentites spinulosa (Edwards & Haime) and, noted by myself and others, Amplexus geniculatus (Worthen)

Echinoderms               55        22 Pentremites blastoids, over-split according to the late Dr. Alan Horowitz (pers. com.)

Bryozoans                   67

Brachiopods                17

Worms                        1

Mollusks                      7

Arthropods                  11        One species of trilobite, rest ostracods

            Vertebrate fossils include typical Chesterian shark teeth, spines, and dermal plates. They were not included in Butt’s or Ulrich’s lists, but have been found by the writer and other collectors.

Index species in Ulrich’s list (refer to comments above about Pentremites)

Pentremites brevis

P. canalis

P. elegans

P. fohsi

P. lyoni

P. robustus

P. robustus hemisphericus

P. subplanus

Pterotocrinus acinus

P. bifurcatus

Anisotrypa symmetrica

Eridotrypa macrostoma

Chilotrypa hispida

Meekopora clausa

Tabulipora ramosa (Stenopora in 1917)

References

Charles Butts, 1917 – The Mississippian Formations of Western Kentucky

Horowitz, Alan S., 1965, Crinoids from the Glen Dean Limestone (Middle Chester) of Southern Indiana and Kentucky

Perry, T.G. and Horowitz, A.S. 1963, Bryozoans from the Glen Dean Limestone (Middle Chester) of southern Indiana and Kentucky: Indiana Geol. Survey Bull. 26, 51 p. (This is not on-line yet).

Utgaard, J. & Perry, T.G. ,1960, Fenestrate Bryozoans of the Glen Dean Formation of Southern Indiana

See my fossil pages for many photos of Glen Dean specimens.

Cheilotrypa hispida bryozoan,  3 cm view
Cheilotrypa hispida bryozoan, 3 cm view