Lowery-Leckie 2014 Eagle Ford.Pdf
PALAEO-06957; No of Pages 17 Palaeogeography, Palaeoclimatology, Palaeoecology xxx (2014) xxx–xxx Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Foraminiferal and nannofossil paleoecology and paleoceanography of the Cenomanian–Turonian Eagle Ford Shale of southern Texas Christopher M. Lowery a,⁎, Matthew J. Corbett b,R.MarkLeckiea,DavidWatkinsb, Andrea Miceli Romero c,ArisPramuditod a Univeristy of Massachusetts, Dept. of Geosciences, 233 Morrill Science Center, 611 N. Pleasant St., Amherst, MA 01003, USA b University of Nebraska, Dept. of Earth and Atmospheric Sciences, 214 Bessey Hall, PO Box 80330, Lincoln, NE 68588, USA c University of Oklahoma, School of Geology and Geophysics, 100 East Boyd St., Room 710, Norman, OK 73019, USA d BP, 501 Westlake Park Blvd., Houston, TX 77079, USA article info abstract Article history: The Upper Cretaceous of central Texas is dominated by a broad, shallow carbonate platform called the Comanche Received 3 July 2013 Platform that occupies an important gateway between the epeiric Western Interior Seaway (WIS) of North Received in revised form 21 July 2014 America to the open-marine Gulf of Mexico/Tethys. We investigated the Cenomanian–Turonian Eagle Ford Accepted 23 July 2014 Shale on and adjacent to the Comanche Platform to determine whether the Eagle Ford Shale has an affinity Available online xxxx with the Western Interior, and if so, determine where the transition from Western Interior to open ocean is located. We were also interested in the relationship, if any, between the organic-rich facies of the Eagle Ford Keywords: OAE2 and Oceanic Anoxic Event 2 (OAE2).
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