Is echinoid-bearing formation above Annona chalk in southwest AR. Is shown (fig. 1) to correlate with Neylandville marl in TX and with Mount Laurel sand in NJ. Biostratigraphic dating on basis of the echinoid CARDIASTER DECIPER Cooke collected from the Saratoga at USGS localities 13539 and 13550, Clark Co, AR in the Ouachita tectonic belt province. Age is early Maestrichtian (Late Cretaceous). Division of the Maestrichtian into three parts (early, middle, and late) is arbitrary. It signifies merely relative position.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Paleomagnetic (a.f. demagnetized) data indicates the Upper Cretaceous Saratoga Chalk in the Arkla basin in southwest AR possesses a weak remanent magnetization of normal magnetic polarity. The normal polarity is assumed to be primary magnetization, and is interpreted to represent deposition during the Gubbio (Italy) normal polarity zone B+ (Campanian to early Maestrichtian).
Source: GNU records (USGS DDS-6; Denver GNULEX).
Lower member in southwest AR, Arkla basin, has an ammonite fauna of the NOSTOCERAS (NOSTOCERAS) HYATTI zone of late Campanian age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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