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A New Specimen of Acrocanthosaurus Atokensis (Theropoda, Dinosauria) from the Lower Cretaceous Antlers Formation (Lower Cretaceous, Aptian) of Oklahoma, USA

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A New Specimen of Acrocanthosaurus Atokensis (Theropoda, Dinosauria) from the Lower Cretaceous Antlers Formation (Lower Cretaceous, Aptian) of Oklahoma, USA A new specimen of Acrocanthosaurus atokensis (Theropoda, Dinosauria) from the Lower Cretaceous Antlers Formation (Lower Cretaceous, Aptian) of Oklahoma, USA Philip J. CURRIE Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, Alberta T0J 0Y0 (Canada) [email protected] Kenneth CARPENTER Denver Museum of Natural History, Department of Earth Sciences, City Park, Denver, Colorado 80205 (USA) [email protected] Currie P. J. & Carpenter K. 2000. — A new specimen of Acrocanthosaurus atokensis (Theropoda, Dinosauria) from the Lower Cretaceous Antlers Formation (Lower Cretaceous, Aptian) of Oklahoma, USA. Geodiversitas 22 (2) : 207-246. The data matrix is available at http://www.mnhn.fr/publication/matadd/g00n2a3.html ABSTRACT A new skeleton of Acrocanthosaurus atokensis is the most complete specimen collected and has the only known complete skull. Aspects of the new skeleton are described in detail, with special attention directed to the morphology of the skull and forelimb. Although unquestionably one of the largest theropods ever found, it is smaller than Carcharodontosaurus, Giganotosaurus and Tyrannosaurus. Comparison with other theropods suggests that Acrocanthosaurus bears a strong resemblance to these taxa because of charac- KEY WORDS ters that are size determinate, and the evidence suggests Acrocanthosaurus is Dinosaurs, more closely related to Allosauridae than to Carcharodontosauridae. Three theropods, Early Cretaceous, families (Allosauridae, Carcharodontosauridae, Sinraptoridae) are recognized USA. in the Allosauroidea. GEODIVERSITAS • 2000 • 22 (2) © Publications Scientifiques du Muséum national d’Histoire naturelle, Paris. www.mnhn.fr/publication/ 207 Currie P. J. & Carpenter K. RÉSUMÉ Un nouveau specimen d’Acrocanthosaurus atokensis (Theropoda, Dinosauria) du Crétacé inférieur de la Formation Antlers (Crétacé inférieur, Aptien) de l’Oklahoma, États-Unis. Nous décrivons le squelette d’Acrocanthosaurus atokensis le mieux conservé jusqu’ici et possédant un crâne complet. La morphologie des structures incon- nues sont décrites ; l’accent est mis sur la morphologie du crâne et du membre antérieur. Bien que ce théropode soit l’un des plus grands, ses dimensions restent inférieures à celles de Carcharodontosaurus, Giganotosaurus et Tyrannosaurus. Il présente un fort degré de ressemblance morphologique avec ces taxons, MOTS CLÉS dont la nature serait liée à leur taille importante. Une analyse de parcimonie Dinosaures, place Acrocanthosaurus comme plus proche parent des Allosauridae que des théropodes, Crétacé inférieur, Carcharodontosauridae. Trois familles sont identifiées au sein des Allosauroidea : États-Unis. les Allosauridae, les Carcharodontosauridae et les Sinraptoridae. INTRODUCTION Parts of another specimen (two posterior cervical or anterior dorsal centra, ischial fragment, distal end of a femur), described in this paper, were col- Acrocanthosaurus atokensis was described by lected by the Oklahoma Museum of Natural Stovall & Langston (1950) on the basis of two History and were catalogued as OMNH 10168. partial skeletons (one with part of a skull) from Most of the specimen, however, was collected by the Lower Cretaceous Antlers Formation (Trinity Cephis Hall & Sid Love, who retrieved the skull, Group, Aptian-Albian) of Atoka County, about two dozen vertebrae, ribs, chevrons, most of Oklahoma. The holotype is OMNH 10146 the front limbs, pelvic fragments, parts of both (MUO 8-0-S9 of Stovall & Langston 1950) and femora and tibiae, and most of the bones of the the paratype is OMNH 10147 (MUO 8-0-S8). foot. This, the most complete skeleton of Acrocanthosaurus Stovall & Langston, 1950 was Acrocanthosaurus known, also comes from the the top predator of one of the richest faunas Antlers Formation (Trinity Group) of McCurtain known from Early Cretaceous times (Cifelli et al. County, Oklahoma. The unprepared specimen 1997). Although it seems to have been widely was eventually acquired by Allen Graffham of distributed (Lipka 1998) in North America, it Geological Enterprises, Inc., Ardmore, Oklahoma, was not the only large theropod of Aptian-Albian who in turn arranged for the Black Hills Institute times (Harris 1998b). in Hill City, South Dakota, to prepare the speci- Another partial skull and skeleton of men. The preparation was completed at the end of Acrocanthosaurus was “discovered” in 1990 (the the summer of 1996, and the original skeleton specimen was actually noticed for the first time went the following year to the North Carolina State more than 40 years earlier) near Weatherford, Museum of Natural Sciences. Texas in the Twin Mountain Formation (Trinity The total length of the skeleton (Fig.1) as mounted Group), which correlates with the lower part of for display by the Black Hills Institute is 11.5 m. the Antlers Formation (Harris 1998a). It was col- This would make it one of the largest known lected by a crew from Southern Methodist theropods, comparable in total length with University. SMU 74646 includes about 70% of a Tyrannosaurus rex Osborn, 1905 (the mounted skeleton (Harris 1998a). skeletons of BHI 3033 and MOR 555 are 11.5 m) 208 GEODIVERSITAS • 2000 • 22 (2) Acrocanthosaurus atokensis from Antlers Formation, Oklahoma, USA FIG. 1. — Acrocanthosaurus atokensis. Reconstruction of skeleton. Scale bar: 1 m. and Giganotosaurus Coria & Salgado, 1995 (the GI Paleontological Museum of the mounted skeleton of MUCPv-CH1 is 12.2 m). Geological Institute of Mongolia, We have not attempted to describe the entire Ulaan Baatar; skeleton of Acrocanthosaurus in this paper, but MACN-CH Museo Argentino de Ciencias have focused on new information available from Naturales “Bernardino Rivadavia”, NCSM 14345. This is especially true for the Buenos Aires; skull, pectoral girdle and forelimb and, to a lesser MOR Museum of the Rockies, Bozeman; extent, the hindlimb. The reader is referred to MUCPv-CH Museo de la Universidad Nacional del papers by Stovall & Langston (1950) and Harris Comahue, El Chocón collection, (1998a) for complementary information on the Neuquén, Argentina; palate, braincase, vertebral column and pelvis. A NCSM North Carolina State Museum of more detailed description of the braincase of the Natural Sciences, Raleigh; holotype has been prepared by Welles et al. NMMNH New Mexico Museum of Natural Acrocanthosaurus (Fig. 1) was assigned to the History, Albuquerque; Allosauridae by Stovall & Langston (1950). This OMNH Oklahoma Museum of Natural was generally accepted by other authors until it History, University of Oklahoma, was reassigned to the Carcharodontosauridae Norman; (Sereno et al. 1996). A more thorough analysis by PIN Paleontological Institute of the Russian Harris (1998a) supported the inclusion of Academy of Sciences, Moscow; Acrocanthosaurus within the Carcharodonto- SMU Southern Methodist University, sauridae. Information from the new specimen Dallas; will be used in this paper to re-examine the rela- TMP Royal Tyrrell Museum of Palaeon- tionships of Acrocanthosaurus. tology, Drumheller; USNM United States National Museum of Natural History, Smithsonian Ins- ABBREVIATIONS titution, Washington; BYU Brigham Young University, Provo; UUVP University of Utah, Vertebrate FMNH Field Museum of Natural History, Paleontology Collection, Salt Lake Chicago; City. GEODIVERSITAS • 2000 • 22 (2) 209 Currie P. J. & Carpenter K. A B FIG. 2. — Acrocanthosaurus atokensis NCSM 14345; A, skull in left view; B, skull in right view. Scale bar: 10 cm. SYSTEMATIC PALEONTOLOGY Acrocanthosaurus atokensis Stovall & Langston, 1950 Subclass DINOSAURIA Owen, 1842 MATERIAL. — North Carolina State Museum of Order THEROPODA Marsh, 1881 Natural Sciences, NCSM 14345, nearly complete Suborder CARNOSAURIA von Huene, 1920 skull and most of postcranium. Superfamily ALLOSAUROIDEA LOCALITY AND AGE. — NCSM 14345 was recovered Currie & Zhao, 1993 from the Antlers Formation (Trinity Group, Lower Family ALLOSAURIDAE Marsh, 1878 Cretaceous) of McCurtain County, Oklahoma. 210 GEODIVERSITAS • 2000 • 22 (2) Acrocanthosaurus atokensis from Antlers Formation, Oklahoma, USA A A, B B C DEFG FIG. 3. — Acrocanthosaurus atokensis. Reconstruction of skull; A, dorsal view; B, left lateral view; C, occipital condyle; D-G, denti- cles of maxillary teeth. Scale bars: A, B, 10 cm; C, 2 cm. REVISED DIAGNOSIS. — Large theropod with elongate ing and distortion of the skull, mostly towards neural spines that are more than 2.5 times correspon- the back (Fig. 2). For example, the left postor- ding presacral, sacral and proximal caudal lengths of the centra. Lacrimal contacts postorbital; supraoccipi- bital was broken in at least two places, and had tal expands on either side of the midline to protrude as pulled away from its suture with the frontal, the a double boss behind the nuchal crest; pleurocoelous ventral part rotating medially. Minor crushing fossae and foramina pronounced on all presacral and and distortion are also evident in the posterior sacral vertebrae; cervical neural spines have triangular anterior processes that insert into depressions beneath half of the jaws. overhanging processes on preceding neural spines; The skull (Figs 2; 3) is almost 129 cm long (pre- accessory transverse processes on mid-caudal vertebrae. maxilla to quadrate) with a preorbital length of 85 cm. The height of the skull in front of the DESCRIPTION orbit is 47 cm. Femur length (Table 1) is a rela- NCSM 14345 was found lying on its side, par- tively stable standard of measurement in tially disarticulated. There has been some crush- theropods, and can be used to assess
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