CHONDRICHTHYAN ASSEMBLAGES FROM THE SURPRISE CANYON (LATE MISSISSIPPIAN, SERPUKHOVIAN) AND WATAHOMIGI (LATEST MISSISSIPPIAN/EARLY PENNSYLVANIAN, SERPUKHOVIAN/BASHKIRIAN) FORMATIONS OF THE WESTERN GRAND CANYON, NORTHERN ARIZONA
The chondrichthyan assemblage from the Latest Mississippian Surprise Canyon Formation is remarkably diverse with a total of thirty-one taxa, identified from teeth and dermal elements. These include four new euselachian taxa; two protacrodontids, a group best known from the late Devonian, and two anachronistids, with ties to the modern sharks. This assemblage best compares with the Bear Gulch Limestone assemblage from central Montana. The Surprise Canyon assemblage provides a range extension of the paraselachians Srianta and Heteropetalus, which previously were only known from the Bear Gulch Limestone assemblage. However, the Surprise Canyon assemblage differs from the Bear Gulch assemblage in its greater number of euselachian taxa and the presence of the xenacanthimorph Bransonella nebraskensis and the elasmobranch Clairina sp.
The succeeding early Bashkirian Watahomigi Formation represents open marine deposition and contains only two taxa: a new xenacanth, and the holocephalan Deltodus. The relationship between the Surprise Canyon and Watahomigi chondrichthyan assemblages and other significant coeval chondrichthyan assemblages suggest that there may have been an eastern and western distinction between the Euamerican assemblages during the Serpukhovian.