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Late Serpukhovian Foraminifers Near the Mississippian-pennsylvanian Boundary At South Syncline Ridge, Southern Nevada, Usa: Implications For Correlation
Multichannel systems in an ancient river-dominated delta: case study of the lower Yanchang Formation, southwest Ordos Basin, China
U-Pb Detrital-zircon Geochronology of the Middle Bloyd Sandstone (morrowan) of Northern Arkansas (U.S.A.): Implications For Early Pennsylvanian Sediment Dispersal in the Laurentian Foreland
ONTOGENY AND HETEROCHRONY IN THE MIDDLE CARBONIFEROUS AMMONOID ARKANITES RELICTUS (QUINN, McCALEB, AND WEBB) FROM NORTHERN ARKANSAS
MASONOCERAS , A NEW KARAGANDOCERATID AMMONOID FROM THE LOWER MISSISSIPPIAN (LOWER OSAGEAN) OF KENTUCKY
Morrowan lithistid demosponges and hexactinellids from the Ozark Mountains of northwestern Arkansas
Abstract The localities described here form a transect from the Arkansas River, near Webbers Falls, Muskogee County, eastern Oklahoma, eastward to the Oklahoma/Arkansas boundary area near Evansville, Arkansas (Fig. 1). Detailed location data for each stop on the transect are given in the text.
Abstract The Beaver Dam exposure is reached by taking Arkansas 187 south from its junction with U.S. 62 immediately south of Busch, Arkansas (Fig. 1). Arkansas 187 crosses Beaver Dam and a turnoff to the dam site overlook is located approximately 0.25 mi (0.4 km) south of the dam. Parking maybe found at the overlook. This exposure occupies NW¼Sec.10, T.20N., R.27W., Carroll County, Arkansas.
Abstract Road cut on east side of U.S. 65 beginning directly south of the Peyton Creek Bridge, 0.2 mi (0.3 km) south of the Searcy- Van Buren county line and 3.4 mi (5.5 km) south of Leslie. NE¼, Sec.11 and NW¼, Sec.12, T.13N., R.15W., Van Buren County, Arkansas (Fig. 1).