Backbone Limestone

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Lithostratigraphy: Hunton Limestone Megagroup >>Backbone Limestone
Chronostratigraphy: Paleozoic Erathem >>Devonian System >>Lower Devonian Series
Allostratigraphy: Tippecanoe 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)

Charles Collinson and Elwood Atherton

Name

Original description

The Backbone Limestone (Savage, 1920, p. 169-178).

Derivation

Named for an isolated ridge called the Backbone along the Mississippi River north of Grand Tower, Jackson County.

Other names

History/background

Type section

Type location

The type section of the Backbone Formation is in a quarry at the south end of the ridge (SE SW SW 24, 10S-4W), where only the upper 38 feet of the formation, overlain by the Clear Creek Chert, is exposed.

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

The Backbone Limestone overlies the Grassy Knob Chert.

Extent and thickness

The Backbone Limestone appears to be as much as 200 feet thick where it rims the deep part of the Illinois Basin, but it becomes thinner within the deeper part and in places is absent (Collinson et al., 1967a). In the outcrop area in Jackson and Union Counties, the Backbone Limestone is about 100 feet thick, but it thins southward and is absent (or becomes cherty and is not recognized) in the Devonian outcrop area in Alexander County.

Lithology

The Backbone Limestone consists of light gray, massive, crystalline, pure limestone that commonly contains many large crinoid stems and a few scattered chert nodules.

Core(s)

Photograph(s)

Contacts

Well log characteristics

Fossils

The Backbone has a large fauna that is dominated by brachiopods, notably Acrospirifer murchisoni and Costispirifer arenosus, but gastropods, bryozoans, conodonts, and trilobites are common.

Age and correlation

The fossils indicate a correlation with the Oriskany in New York. The Backbone is continuous with the Little Saline Limestone in Missouri.

Environments of deposition

Economic importance

Remarks

References

COLLINSON, CHARLES, L. E. BECKER, G. W. JAMES, J. W. KOENIG, and D. H. SWANN, 1967a, Illinois Basin, in International symposium on the Devonian System: Alberta Society of Petroleum Geologists, v. 1, p. 940-962; Illinois State Geological Survey Reprint 1968-G.
SAVAGE, T. E., 1920, Devonian formations of Illinois: American Journal of Science, v. 49, p. 169-182.

ISGS Codes

Stratigraphic Code Geo Unit Designation
6190
Dbb