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| | A NEW HEXACTINELLID SPONGE FROM THE REEF TRAIL MEMBER OF THE UPPER GUADALUPIAN BELL CANYON FORMATION, GUADALUPE ... |
 | | The hexactinellid sponge was collected from 0.3 m below the lowest zone of scaphopod lenses and 0.7 m above a distinctive stratigraphie unit, about 3.7 mm thick, which is bounded above and below by a pair of coarse-grained packstone debris flows that range from 0.3 to 1.35 m thick. |
 | | The new hexactinellid sponge, and a somewhat younger suite of calcareous sponges currently under study, were collected from very near or at King's (1948) Strigogoniatites fountaini locality (USGS locality 7663, King, 1948, pi. |
 | | The Toomeyospongia Rigby, Horrocks, and Cys, 1982, described here, is equivalent in age to the youngest ammonites known from the Permian Basin of Texas and New Mexico and occurs within the latest Guadalupian fusulinid zone of Paraboultonia Skinner and Wilde, 1954. |
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