A PRELIMINARY REPORT ON AN UNUSUALLY LARGE METOPOSAURID FROM THE SALITRAL FORMATION (UPPER TRIASSIC: CARNIAN) ON LANDS BELONGING TO THE PUEBLO OF JEMEZ

The lands belonging to the Pueblo of Jemez in north-central New Mexico include sedimentary strata ranging in age from Mississippian to Pleistocene, although limited detailed descriptions of these various exposures currently exist. Strata of the Salitral Formation of the Chinle Group (Upper Triassic: Carnian) are present in the southeastern corner of the Jemez Reservation in an area that is filled with complex faulting. Material pertaining to a metoposaurid amphibian was recovered from a grayish-purple paleosol horizon in the lower Salitral Formation, approximately 7-8 meters above the underlying Shinarump (=Agua Zarca) Formation. The fossil bearing horizon is comprised primarily of a poorly consolidated conglomeritic lens dominated by calcareous nodules from 1-10 cm in diameter. This unit also contains moderately abundant fragments of metoposaur and phytosaur material. Metoposaurid material includes cranial and shoulder girdle elements and teeth. Phytosaur material includes teeth and osteoderms with a characteristically high dorsal ridge. The metoposaurid specimens, though fragmentary, are significant for their extraordinary size. A partial interclavicle is conservatively reconstructed as well over 450 cm in width. The largest specimen reported from Texas is 430 cm, whereas the largest known from New Mexico is 400 cm in width. Published sizes of metoposaurid interclavicles from the Chinle Formation of New Mexico and the Dockum Formation of Texas average 307 cm and 313 cm respectively. Thus, the Jemez metoposaur is one of the largest ever reported, approximately 47-48 % larger than those published averages, and approximately 5% larger than the largest one yet reported. Although measurements of the thickness of dermal elements of the pectoral girdle are not commonly available, the Jemez metoposaur also appears remarkable in this regard, measuring over 2.5 cm from deep to superficial surfaces.