skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Paleoecology of Eocene Wheelock Member of Cook Mountain Formation in western Houston County, Texas

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:5141498

Sixty-nine foraminifera species and 49 mollusk species were recovered from the Wheelock Member of the Cook Mountain Formation, in the Porter's Springs area of Houston County, Texas, and along the Little Brazos River in Brazos County, Texas. The Wheelock Member is primarily a regressive unit. A thin shell lag deposit at the base of the member, consisting of abraded mollusk fragments and subrounded pebbles of impure fossiliferous limestone, is all that remains of the transgressive part of the sequence. Above the shell lag deposit, the lower part of the member consists dominantly of bioturbated, glauconitic, fossiliferous mudstone. The species composition and diversity of benthic foraminifera and the planktonic/benthic ratio, suggest deposition in a normal marine inner or inner-middle shelf environment. Dominant benthic foraminifera include: Ceratobulimina eximia, Cibicides mauricensis, Eponides mexicanus, Gyroidina octocamerata, Melonis planatum, Siphonina claibornensis, and Spiroplectammina mississippiensis. The mollusk population has a low diversity and is dominated by only a few species. These include: Buccitriton texanum, Mesalia claibornensis, Polinices aratus, Notocorbula texana, Vokesula petropolitana, and Cadulus subcoarevatus. The low diversity and high dominance of the mollusk population suggest deposition in an unstable environment. This instability, however, had little or no effect on the foraminifera. The upper part of the Wheelock Member consists dominantly of regularly layered mudstone and siltstone and contains only a low-diversity assemblage of agglutinated foraminifera. This part of the member was probably deposited in a shallow brackish-water environment with a high sedimentation rate. Dominant agglutinated species include: Haplophragmoides mauricensis, Trochammina claibornensis, and Verneuilina cushmanii.

OSTI ID:
5141498
Report Number(s):
CONF-8910221-; CODEN: AABUD
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (USA), Vol. 73:9; Conference: Gulf Coast Association of Geological Societies and Gulf Coast Section of SEPM meeting, Corpus Christi, TX (USA), 25-27 Oct 1989; ISSN 0149-1423
Country of Publication:
United States
Language:
English

Similar Records

Benthic foraminiferal distribution in deep-water periplatform carbonate environments
Conference · Fri May 01 00:00:00 EDT 1987 · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) · OSTI ID:5141498

Foraminifera from Paleocene Clayton Formation lithostratotype, Barbour Count, Alabama
Conference · Thu May 01 00:00:00 EDT 1986 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:5141498

Foraminiferal biostratigraphy and paleoecology of Wilcox group (Paleocene-Eocene), central Louisiana
Conference · Thu May 01 00:00:00 EDT 1986 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:5141498