Redefinition of the Osagean-Meramecian boundary in the Mississippian stratotype region
- West Virginia Univ., Morgantown (USA)
- Amoco Production Co., Tulsa, OK (USA)
- Carnegie Museum of Natural History, Pittsburgh, PA (USA)
- Ohio State Univ., Columbus (USA)
Analysis of fossil occurrences in late Osagean-early Meramecian stratotype beds of the upper Mississippi River Valley shows that major faunal changes occur within the Warsaw Formation, not at the underlying Keokuk-Warsaw formational contact where the Osagean-Meramecian serial boundary is presently placed. Relying on this evidence, the authors propose raising this boundary to the base of the informal upper Warsaw member described herein. The boundary is recognized by the first occurrence of the brachiopods Warsawia lateralis, Planalvus densa, Crossacanthia perlamellosa, Setigerites altonensis, and Tetracamera subcuneata, the blastoid Pentremites conoideus, and the calcareous foraminifer Globoendothyra baileyi. Use of these fossil appearances provides a more rigorous definition of the serial boundary and permits correlation beyond the Mississippi River Valley. Foraminifers suggest that the boundary falls within the middle Visean of western Europe. The stratotype section for the proposed boundary is located near the type locality of the Meramecian Series at Meramec Highlands, St. Louis County, Missouri. The lithostratigraphy of the late Osagean and early Meramecian is reviewed in key areas within the Mississippi River Valley and a new member, the Peerless Park, is proposed for a shoaling unit within the middle of the Keokuk Limestone.
- OSTI ID:
- 5504633
- Journal Information:
- Palaois; (United States), Vol. 5:5
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
02 PETROLEUM
CARBONIFEROUS PERIOD
BOUNDARY CONDITIONS
GEOLOGIC FORMATIONS
PALEONTOLOGY
STRATIGRAPHY
MISSISSIPPI RIVER BASIN
FORAMINIFERA
FOSSILS
INVERTEBRATES
MISSOURI
SEDIMENTARY ROCKS
ANIMALS
DEVELOPED COUNTRIES
FEDERAL REGION VII
GEOLOGIC AGES
GEOLOGY
MICROORGANISMS
NORTH AMERICA
PALEOZOIC ERA
PROTOZOA
ROCKS
SARCODINA
USA
WATERSHEDS
580000* - Geosciences
020200 - Petroleum- Reserves
Geology
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