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A review of the systematic position of the dinosauriform archosaur Eucoelophysis baldwini Sullivan & Lucas, 1999 from the Upper Triassic of New Mexico, USA Martín D. EZCURRA Laboratorio de Anatomia Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Av. Angel Gallardo 470, Buenos Aires (1405) (Argentina) [email protected] Ezcurra M. D. 2006. — A review of the systematic position of the dinosauriform archosaur Eucoelophysis baldwini Sullivan & Lucas, 1999 from the Upper Triassic of New Mexico, USA. Geodiversitas 28 (4) : 649-684. Abstract Eucoelophysis baldwini Sullivan & Lucas, 1999 is represented by several post- cranial elements from the Petrified Forest Formation (Norian), New Mexico, USA. Eucoelophysis Sullivan & Lucas, 1999 was widely considered as a coelo- physoid dinosaur by several authors, but the hindlimb anatomy of this genus clearly indicates that it belongs to neither of these groups. The following fea- tures exclude Eucoelophysis from Neotheropoda: absence of oblique ligament groove on caudal surface of femoral head, femoral medial epicondyle small and smoothly rounded, absence of caudal cleft between medial part of the proximal end of the tibia and fibular condyles, cnemial crest low, and fibular crest absent. Moreover, Eucoelophysis lacks dinosaurian synapomorphic characters, but has a plesiomorphic slightly inturned femoral head that prevents its assignment to Dinosauria. Interestingly, the morphology of the femur of Eucoelophysis is extremely similar to that of the basal dinosauriform Silesaurus opolensis Dzik, Key words Dinosauriformes, 2003 from the Late Triassic of Poland. In order to determine the phylogenetic Coelophysoidea, position of Eucoelophysis, a cladistic analysis was carried out, which depicts Eu- Eucoelophysis, coelophysis as a non-dinosaurian dinosauriform. Thus reinterpreted,Eucoelophysis Chinle Group, Upper Triassic, constitutes the youngest record of a non-dinosaurian dinosauriform, indicating New Mexico. their survival into the Norian, being co-eval with early dinosaurs. GEODIVERSITAS • 2006 • 28 (4) © Publications Scientifiques du Muséum national d’Histoire naturelle, Paris. www.geodiversitas.com 649 Ezcurra M. D. Résumé Une révision de la position systématique de l’archosaure dinosauriforme Eucoelo- physis baldwini Sullivan & Lucas, 1999 du Trias supérieur du Nouveau Mexique, États-Unis. Eucoelophysis baldwini Sullivan & Lucas, 1999 est connu d’après plusieurs élé- ments postcraniaux qui proviennent de la Formation Petrified Forest (Norien) au Nouveau Mexique (États-Unis). Eucoelophysis Sullivan & Lucas, 1999 fut généralement considéré comme un théropode coelophyside. Cependant, l’ana- tomie du membre postérieur de ce genre indique clairement que ce n’est ni un neothéropode, ni un coelophyside. Les caractéristiques suivantes excluent ce taxon des Neotheropoda : absence de rainure du ligament oblique sur la surface caudale de la tête fémorale, épicondyle fémoral intermédiaire petit et réguliè- rement arrondi, absence de fissure caudale sur la partie intermédiaire entre l’extrémité proximale fibulaire du tibia et le condyle fibulaire, la crête cnémiale est réduite, et la crête fibulaire absente. De plus, aucune des synapomorphies des dinosaures n’existe chez Eucoelophysis, et le partage d’un caractère primitif (tête fémorale légèrement tournée vers l’intérieur) ne permet pas de rapporter ce taxon aux dinosaures. Par ailleurs, la morphologie du fémur d’Eucoelophysis est très semblable à celle du dinosauriforme basal Silesaurus opolensis Dzik, 2003 Mots clés Dinosauriformes, du Trias supérieur de Pologne. Afin de déterminer la position phylogénétique Coelophysoidea, d’Eucoelophysis, une analyse cladistique a été réalisée, qui positionne Eucoelophysis Eucoelophysis, comme un Dinosauriformes non-dinosaurien. Ainsi ré-interprété, Eucoelophysis groupe Chinle, Trias supérieur, représente le plus jeune Dinosauriformes non-dinosaurien connu, indiquant leur Nouveau Mexique. survivance dans le Norien et leur co-existence avec les premiers dinosaures. INTRODUCTION Coelophysis bauri Cope, 1887 and C. rhodesiensis Raath, 1969 in lacking a well developed posterior Sullivan & Lucas (1999) described Eucoelophysis femoral notch below the femoral head (Fig. 4B, H), baldwini on the basis of an incomplete articulated and also from C. bauri in having a tibia that has a leg, pelvic girdle, and other incomplete postcranial distinct appressed surface along the distal two-thirds elements (Figs 1B; 2B, G, H; 4B, H; 5B, C, F; 6D). of the bone and lacks a fibular crest (Fig. 2G, H). Its type material was found in the Petrified Forest Eucoelophysis was diagnosed by the presence of an Formation (Norian; Lucas & Hunt 1992; Lucas ischio-acetabular groove and a sulcus on the proximal 1998) directly associated with phytosaur bones articular surface of the femur (Fig. 1B) (Sullivan & and some unidentified elements within a square Lucas 1999). However, several features mentioned meter area (Sullivan & Lucas 1999). Sullivan & above are plesiomorphic traits of Dinosauria Owen, Lucas (1999) originally assigned Eucoelophysis to 1842 and Neotheropoda Bakker, 1986 (Novas a monophyletic Ceratosauria Marsh, 1884 (sensu 1996; Sereno 1999; Holtz 2000; Rauhut 2003). Rowe & Gauthier 1990) on the basis of triangular Additionally, no dinosaurian synapomorphic traits and caudally directed transverse processes of its are present in Eucoelophysis, preventing its assign- dorsal vertebrae and a prominent trochanteric shelf ment to the Dinosauria. On the other hand, the on the lesser trochanter of the femur. They also in- anatomy of Eucoelophysis is more congruent with terpreted the postcranial elements as belonging to the dinosaurian close relative Silesaurus opolensis a coelophysoid theropod. Sullivan & Lucas (1999) Dzik, 2003. Moreover, several autapomorphic traits also pointed out that Eucoelophysis differs from support the validity of the genus Eucoelophysis, 650 GEODIVERSITAS • 2006 • 28 (4) The systematic position of Eucoelophysis (Dinosauriformes) distinguishing it from Silesaurus and other basal stated by Padian et al. (1999) (see Langer 2004), Dinosauriformes Novas, 1992. Herrerasauridae is considered to lie outside Thero- The type material of Eucoelophysis has already poda, being the sister-taxon of Eusaurischia, and been described in detail and excellently documented Averostra is used for the Ceratosauria + Tetanurae with photographs by Sullivan & Lucas (1999), clade (see Paul 2002). The coelophysoid species and a new description is not necessary. The main “S.” rhodesiensis is here considered to belong to purpose of this paper is to discuss the systematic the genus Coelophysis Cope, 1889, i.e. Coelophysis position of this interesting taxon testing its status rhodesiensis, following Tykoski (2005) and Ezcurra as a coelophysoid theropod, and determining its & Novas (2006). phylogenetic relationships. SYstematics Methods Ornithodira Sereno, 1991 The re-evalutation of the systematic position of Dinosauromorpha Benton, 1975 Eucoelophysis baldwini was carried out on basis of Dinosauriformes Novas, 1992 unpublished photographs of its type material and the published data. Throughout the text, materials Genus Eucoelophysis Sullivan & Lucas, 1999 indicated by their respective collection numbers cor- respond to studied materials, casts, or unpublished TYPE SPECIES. — Eucoelophysis baldwini Sullivan & photographs of dinosaurian materials. Lucas, 1999. STRATIGRAPHIC DISTRIBUTION. — Petrified Forest For- INSTITUTIONAL ABBREVIATIONS mation, Chinle Group, Upper Triassic (Norian; Lucas & AMNH American Museum of Natural History, Hunt 1992; Lucas 1998; Sullivan & Lucas 1999). New York; HMN BM Humboldt Museum für Naturkunde, Ber- GEOGRAPHIC DISTRIBUTION. — Ghost Ranch Quad- lin; rangle, Rio Arriba County, New Mexico, USA (Sullivan MCZ Museum of Comparative Zoology, Cam- & Lucas 1999). bridge, Massachusetts; MLP Museo de La Plata; NMMNH New Mexico Museum of Natural History Eucoelophysis baldwini Sullivan & Lucas, 1999 and Science, Albuquerque; PULR Paleontología, Universidad Nacional de La (Figs 1B; 2B, G, H; 4B, H; 5B, C, F; 6D) Rioja; PVL Fundación “Miguel Lillo”, Universidad HOLOTYPE. — NMMNH P-22298, incomplete postcra- Nacional de Tucumán, San Miguel de nial material consisting of two dorsal and four incomplete Tucumán; caudal vertebrae, nearly complete right pubis, partial right PVSJ Museo de Ciencias Naturales, Universidad ischium, ilum fragment?, fragmentary femora, proximal Nacional de San Juan; half of the left tibia, incomplete right metatarsal II and UCMP University of California Museum of Pale- IV, and complete metatarsal III, phalanges, unidenti- ontology, Berkeley; fied bone fragments, and probably an incomplete left YPM Yale Peabody Museum, New Haven, Con- scapulocoracoid (Sullivan & Lucas 1999). necticut. EMENDED DIAGNOSIS. — Dinosauriform diagnosable by SYSTEMATIC NOMENCLATURE the following autapomorphies (see Discussion): non-inva- This paper follows the phylogenetic hypothesis sive pleurocoels in the dorsal vertebrae; strongly marked and systematic nomenclature employed by Novas U-shaped ischio-acetabular groove (Sullivan & Lucas 1999); absence of femoral trochanteric shelf; cnemial (1996) for basal Dinosauriformes relationships. crest distinctively offset from the tibial shaft, cranially Regarding saurischian nomenclature, the term straight, and without lateral notch; and probably femoral Eusaurischia is applied following the definition fourth trochanter reduced
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    Distance Hierarchical joiningclustering 3.0 2.5 2.0 1.5 1.0 0.5 Sinosauropteryx Caudipteryx Eoraptor Compsognathus Compsognathus Compsognathus Compsognathus Megaraptora basal Coelurosauria Noasauridae Neotheropoda non-averostran T non-tyrannosaurid Dromaeosauridae basalmost Theropoda Oviraptorosauria Compsognathidae Therizinosauria T A yrannosauroidea Compsognathus roodontidae ves Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Richardoestesia Scipionyx Buitreraptor Compsognathus Troodon Compsognathus Compsognathus Compsognathus Juravenator Sinosauropteryx Juravenator Juravenator Sinosauropteryx Incisivosaurus Coelophysis Scipionyx Richardoestesia Compsognathus Compsognathus Compsognathus Richardoestesia Richardoestesia Richardoestesia Richardoestesia Compsognathus Richardoestesia Juravenator Richardoestesia Richardoestesia Richardoestesia Richardoestesia Buitreraptor Saurornitholestes Ichthyornis Saurornitholestes Ichthyornis Richardoestesia Richardoestesia Richardoestesia Richardoestesia Richardoestesia Juravenator Scipionyx Buitreraptor Coelophysis Richardoestesia Coelophysis Richardoestesia Richardoestesia Richardoestesia Richardoestesia Coelophysis Richardoestesia Bambiraptor Richardoestesia Richardoestesia Velociraptor Juravenator Saurornitholestes Saurornitholestes Buitreraptor Coelophysis Coelophysis Ornitholestes Richardoestesia Richardoestesia Juravenator Saurornitholestes Velociraptor Saurornitholestes
  • An Early Late Triassic Long-Necked Reptile with a Bony Pectoral Shield and Gracile Appendages

    An Early Late Triassic Long-Necked Reptile with a Bony Pectoral Shield and Gracile Appendages

    An early Late Triassic long-necked reptile with a bony pectoral shield and gracile appendages JERZY DZIK and TOMASZ SULEJ Dzik, J. and Sulej, T. 2016. An early Late Triassic long-necked reptile with a bony pectoral shield and gracile appendages. Acta Palaeontologica Polonica 61 (4): 805–823. Several partially articulated specimens and numerous isolated bones of Ozimek volans gen. et sp. nov., from the late Carnian lacustrine deposits exposed at Krasiejów in southern Poland, enable a reconstruction of most of the skeleton. The unique character of the animal is its enlarged plate-like coracoids presumably fused with sterna. Other aspects of the skeleton seem to be comparable to those of the only known specimen of Sharovipteryx mirabilis from the latest Middle Triassic of Kyrgyzstan, which supports interpretation of both forms as protorosaurians. One may expect that the pectoral girdle of S. mirabilis, probably covered by the rock matrix in its only specimen, was similar to that of O. volans gen. et sp. nov. The Krasiejów material shows sharp teeth, low crescent scapula, three sacrals in a generalized pelvis (two of the sacrals being in contact with the ilium) and curved robust metatarsal of the fifth digit in the pes, which are unknown in Sharovipteryx. Other traits are plesiomorphic and, except for the pelvic girdle and extreme elongation of appendages, do not allow to identify any close connection of the sharovipterygids within the Triassic protorosaurians. Key words: Archosauromorpha, Sharovipteryx, protorosaurs, gliding, evolution, Carnian, Poland. Jerzy Dzik [[email protected]], Instytut Paleobiologii PAN, ul. Twarda 51/55, 00-818 Warszawa, Poland and Wydział Biologii Uniwersytetu Warszawskiego, Centrum Nauk Biologiczno-Chemicznych, ul.