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Proc Biol Sci. 2006 May 7; 273(1590): 1045–1048.
Published online 2006 January 25. doi:  10.1098/rspb.2005.3426
PMCID: PMC1560254

Extreme convergence in the body plans of an early suchian (Archosauria) and ornithomimid dinosaurs (Theropoda)


Living archosaurs comprise birds (dinosaurs) and crocodylians (suchians). The morphological diversity of birds and stem group dinosaurs is tremendous and well-documented. Suchia, the archosaurian group including crocodylians, is generally considered more conservative. Here, we report a new Late Triassic suchian archosaur with unusual, highly specialized features that are convergent with ornithomimid dinosaurs. Several derived features of the skull and postcranial skeleton are identical to conditions in ornithomimids. Such cases of extreme convergence in multiple regions of the skeleton in two distantly related vertebrate taxa are rare. This suggests that these archosaurs show iterative patterns of morphological evolution. It also suggests that this group of suchians occupied the adaptive zone that was occupied by ornithomimosaurs later in the Mesozoic.

Keywords: convergent evolution, Effigia, Shuvosaurus, suchian, Triassic, archosaur

1. Introduction

The specimens were discovered in unprepared blocks originally excavated in the 1940s by American Museum of Natural History field parties from the famous Ghost Ranch Coelophysis Quarry (also known as Whitaker Quarry). Until recently, this quarry was thought to represent a nearly monospecific death assemblage of the early theropod Coelophysis (Colbert 1989). However, many different kinds of reptiles have recently been reported (Long & Murry 1995; Clark et al. 2000; Harris & Downs 2002). Several specimens are referred to the new taxon. The skull has edentulous jaws, an enlarged orbit, a posteroventrally rotated squamosal and an anteroventrally angled quadrate. All of these features are identical to those of derived ornithomimid dinosaurs. Additional derived features of the pelvis, tail and vertebrae are convergent features that diagnose nested clades within Theropoda.

2. Systematic paleontology

Archosauria (Cope 1869)

Suchia (Krebs 1974 sensu Benton & Clark 1988) Effigia okeeffeae gen. et sp. nov.

(a) Etymology

The generic name is derived from the Latin word effigia (ghost). The specific name is in honour of Georgia O'Keeffe for her numerous paintings of the badlands at Ghost Ranch and her interest in the Coelophysis Quarry when it was discovered.

(b) Holotype

An articulated skeleton including a nearly complete skull, American Museum of Natural History Fossil Reptiles (AMNH FR) 30587.

(c) Referred specimens

AMNH FR 30588, articulated pelvis, femur and caudal vertebrae; AMNH FR 30589, a partial skull with associated cervical vertebrae and partial hindlimb; AMNH FR 30590, femur.

(d) Horizon and locality

Ghost Ranch, central New Mexico. From the Coelophysis Quarry in the ‘siltstone member’ (Norian–?Rhaetian) of the Chinle Formation (Stewart et al. 1972).

(e) Diagnosis

A suchian archosaur distinguishable from all other suchians except Shuvosaurus by the presence of an edentulous premaxilla, maxilla and dentary, a posteriorly long anterodorsal process of the premaxilla, a long preacetabular process of the ilium that connects to the posterior process by a large thin flange and a pubic boot that is 33% as long as the pubic shaft. Distinguished from Shuvosaurus by the presence of a dorsal and posterior process of the maxilla, small posterior process of the premaxilla, fossa on the posterior side of the lacrimal, absence of posterior process of the squamosal and a fossa on the posterior side of the squamosal.

(f) Description

AMNH FR 30587 (figure 1) includes a nearly complete skull missing only the quadratojugal and parts of the braincase. The premaxilla, maxilla and dentary are unusual in being edentulous, and are covered by an extensive system of foramina that suggests the presence of a horny beak or rhamphotheca. The premaxilla bears a long posterior nasal process that meets the nasal dorsally and forms the internarial bar. The premaxillae are separated from the nares dorsally by anterior narial processes of the nasals. Ventrally, the premaxillae meet to form a small secondary palate that contacts the anterior palatal shelves of the maxillae. The reduced maxilla has both a dorsal process that separates the external naris from the antorbital fenestra and a tapered posterior process that contacts the jugal anterior to the antorbital bar. A pronounced, raised external rim forms the anterior and ventral margin of the antorbital fossa on the lateral surface of the maxilla. The ventral edge of the premaxilla and only the anterior half of the maxilla occlude with the dentary. The length of the posteriorly shortened and attenuated dentary corresponds to the beak-like premaxilla and anterior part of maxilla. The dentaries meet at the midline to form a posteriorly expanded symphysis that corresponds to the area created by the premaxillae. This area of the dentary is also covered with nutrient foramina, again suggesting a rhamphotheca. A huge mandibular fenestra is bounded dorsally and posteriorly by the surangular, ventrally by the angular and anteriorly (only slightly) by the dentary. A large surangular foramen is present on the posterolateral side just anterior to the quadrate shaft. The distal articular end of the anteroventrally projected quadrate articulates with the largely convex articular. A slightly dorsolaterally expanded area of the surangular also articulates with the quadrate (also an unambiguous synapomorphy of Ornithomimosauria; Makovicky et al. 2004).

Figure 1
Skull reconstruction of Effigia okeeffeae (AMNH FR 30587). (a, b) Lateral view, (c) reconstruction, (d, e) dorsal view and (f) reconstruction. Abbreviations: an, angular; d, dentary; f, frontal; j, jugal; l, lacrimal; m, maxilla; mf, mandibular fenestra; ...

Other specializations of the skull include an enlarged orbit and external naris. The crescentic postorbital forms both the posterior and part of the ventral and dorsal border of the orbit. A long ventral process of the postorbital and a large orbit are also found in derived ornithomimids (Makovicky et al. 2004). The elongate jugal creates most of the ventral border of the upper skull and forms part of the postorbital bar. It lacks an anterior dorsal process, so the lacrimal forms all of the antorbital bar. The dorsal surface of the skull is completely smooth and includes an enlarged frontal and prefrontal, but clearly lacks a postfrontal. The parietals form a sagittal crest and articulate with posteroventrally directed squamosals. As with Shuvosaurus, the parabasisphenoid is anteriorly elongated as in theropods (Rauhut 1997, 2003).

In the axial skeleton, the posterior cervical vertebrae bear posteriorly directed processes on each diapophysis (only in Ornithomimus and Archaeornithomimus; Makovicky et al. 2004). Cervical and dorsal vertebrae are anteroposteriorly elongated and have complicated transverse processes. The anterior cervical vertebrae have true pleurocoels on the posterior half of the centrum (Britt 1997). The posterior caudal vertebrae bear long prezygapophyses that overlap the adjacent vertebra.

The large scapula (figure 2) is long and triangular with a blunt posterior apex, and the coracoid is equally anteroposteriorly wide. The humerus, radius and ulna are about the same size and are unreduced; the distal ends of both the radius and ulna taper. Although the manus is incomplete, the preserved elements are extremely reduced (2 cm metacarpals), yet retain the relative proportions of a typical Crocodylus manus (Mook 1921).

Figure 2
AMNH FR 30587. (a) Skeletal reconstruction of Effigia okeeffeae. The bones in grey are unknown. (b) Posterior caudal vertebrae (AMNH FR 30589) with overlapping prezygapophyses in lateral view. Arrow indicates anterior direction for the vertebrae only. ...

The elongated, posteriorly concave pubis has a large boot that projects posteriorly. The appressed left and right ischium are laterally compressed. The ilium bears a thin dorsal flange that connects an elongated preacetabular process to a large postacetabular process. The ilium is oriented vertically and the acetabulum is closed medially. The supra-acetabular rim covers the head of the femur on both the dorsal and part of the lateral sides. The sacrum consists of four centra fused into a stiff rod. All of the sacral neural arches are fused.

The proximal portion of the femur bears two medial condyles; the anteromedial condyle is knob-like and hooks posteriorly, a condition reminiscent of the offset proximal head of a dinosaurian femur. However, the ‘head’ of the femur articulates anteriorly as in crocodylians and not medially as in dinosaurs. The shafts of the femur, tibia and fibula are thin-walled and hollow. The astragalus and calcaneum articulate in a crocodile-normal configuration and their morphology is similar to Alligator. The pes consists of five metatarsals. The recurved ungual is dorsoventrally compressed.

3. Discussion

Chatterjee (1993) named Shuvosaurus on the basis of a skull from the Miller (Post) Quarry; the specializations of its skull led him to attribute it to an ornithomimid dinosaur. Later, it was argued (Long & Murry 1995; Hunt et al. 1998) that the skull of Shuvosaurus belongs with the postcrania of Chatterjeea, a suchian archosaur found in the same quarry, although no overlapping elements had been found. The articulated cranial and skeletal material of Effigia strongly suggests that the skull of Shuvosaurus belongs to the postcrania of Chatterjeea. Therefore, Chatterjeea is very probably a junior subjective synonym of Shuvosaurus. The fully developed crocodile-normal ankle, crocodylomorph-like pes and articulation between the femur and ilium clearly place Effigia as more closely related to crocodiles than to birds. Effigia and Shuvosaurus were inserted into a modified version of Benton's (1999) basal archosaur phylogenetic analysis (see electronic supplementary material). The resultant analysis (figure 3a) produced a single tree that placed Effigia and Shuvosaurus within derived suchians. The characters that Chatterjee (1993) used to assign the skull of Shuvosaurus to the Ornithomimidae are now understood to be convergent, according to the phylogenetic analysis presented here. The postcrania of Effigia also contain characters that are convergent with those of theropods at more general taxonomic levels (figure 3b). This is particularly apparent in the pelvis, where Effigia shares the following characters with theropods: at least four sacral vertebrae are fused into a stiffened rod, the preacetabular process of the ilium is enlarged, a thin flange of bone connects the preacetabular process to the ischiadic wing of the ilium and the pubic boot is large and posteriorly expanded.

Figure 3
(a) Phylogenetic positions of Effigia and Shuvosaurus among basal archosaurs. Unique tree shown (81 characters, length=156, RI=0.8320, CI=0.5897). The placement of Effigia within Theropoda requires the addition of 27 steps and the placement sister to ...

Characters shared between Effigia and Shuvosaurus are also present in the fragmentary taxon Sillosuchus (Alcober & Parrish 1997) including the presence of a thin supra-acetabular crest, thin dorsal flange of the ilium and similar ischial morphology. From the Late Carnian of Argentina, Sillosuchus indicates that Effigia-like taxa had a larger distribution than just North America and furthermore, Effigia-like taxa were present during most of the Late Triassic.

The Late Triassic is marked by a number of body plans convergent with later dinosaurs. The simple unspecialized bodies of Late Triassic theropods such as Coelophysis contrast strongly with the diversity of coeval crocodile-line archosaurs. An iterative pattern of morphological evolution suggests that some of the Late Triassic suchians may have occupied similar adaptive zones to subsequent clades of dinosaurs. The presence of ornithomimid-like suchians (as well as the carnosaur-like suchians such as Postosuchus (Chatterjee 1985) and ankylosaur-like suchians such as aetosaurs) suggest that only in the Jurassic after most clades of crocodile-line archosaurs became extinct, did dinosaurs begin to explore new adaptive opportunities.


We thank Paul Olsen, Peter Makovicky, Randall Irmis, Kevin Padian and Alan Turner for invaluable help and guidance in preparing this manuscript. We thank Carl Mehling (AMNH) and Sankar Chatterjee (TTM) for access to collections. Technical assistance with figures was provided by Mick Ellison. Preparation of the skull was generously completed by Amy Davidson. This work was supported under a National Science Foundation Graduate Research Fellowship and support from AMNH.

Supplementary Material

Phylogenetic analysis, character list and data matrix:


  • Alcober O, Parrish J.M. A new poposaurid from the upper Triassic of Argentina. J. Vertebr. Paleontol. 1997;17:548–556.
  • Benton M.J. Scleromochlus taylori and the origin of dinosaurs and pterosaurs. Phil. Trans. R. Soc. B. 1999;1388:1423–1446. 10.1098/rstb.1999.0489
  • Benton M.J, Clark J.M. Archosaur phylogeny and the relationship of the Crocodylia. In: Benton M.J, editor. The phylogeny and classification of tetrapods, 1: amphibians, reptiles, birds. Clarendon Press; Oxford: 1988. pp. 295–338.
  • Britt B. B. 1997. Pneumatic postcranial bones in dinosaurs and other archosaurs. Ph.D. dissertation, University of Calgary.
  • Colbert E.H. The Triassic dinosaur Coelophysis. Mus. Northern Arizona Bull. 1989;57:1–160.
  • Chatterjee S. Postosuchus, a new thecodontian reptile from the Triassic of Texas and the origin of tyrannosaurs. Phil. Trans. R. Soc. B. 1985;309:395–460.
  • Chatterjee S. Shuvosaurus, a new theropod. Natl Geogr. Res. Explor. 1993;9:274–285.
  • Clark J.M, Sues H.D, Berman D.S. A new specimen of Hesperosuchus agilis from the upper Triassic of New Mexico and the interrelationships of basal crocodylomorph archosaurs. J. Vertebr. Paleontol. 2000;20:683–704.
  • Harris J.D, Downs A. A drepanosaurid pectoral girdle from the ghost ranch Coelophysis Quarry (Chinle Group Rock Point Formation, Rhaetian), New Mexico. J. Vertebr. Paleontol. 2002;22:70–75.
  • Hunt A.P, Lucas S.G, Heckert A.B, Sullivan R.M, Lockley M.G. Late Triassic dinosaurs from the Western United States. Geobios. 1998;31:511–531. 10.1016/S0016-6995(98)80123-X
  • Long R.A, Murry P.A. Late Triassic (Carnian and Norian) tetrapods from the Southwestern United States New Mexico. Mus. Nat. Hist. Sci. Bull. 1995;4:1–254.
  • Makovicky P.J, Kobayashi Y, Currie P.J. Ornithomimosauria. In: Weishampel D.B, Dodson P, Osmolska H, editors. The Dinosauria. University of California Press; Berkeley, CA: 2004. pp. 137–150.
  • Mook C.C. Notes on the postcranial skeleton in the Crocodilia. The dermo–supraoccipital bone in the Crocodilia. Bull. Am. Mus. Nat. Hist. 1921;44:67–103.
  • Rauhut O.W.M. Zur schadelanatomie von Shuvosaurus inexpectatus. In: Sachs S, Rauhut O.W.M, Weigert A, editors. Treffen der deutschsprachigen palaeoherpetologen. Alfred-Wegener-Stiftung; Germany: 1997. pp. 17–21.
  • Rauhut O.W.M. The interrelationships and evolution of basal theropod dinosaurs. Spec. Pap. Palaeontol. 2003;69:1–215.
  • Stewart J.H, Poole F.G, Wilson R.F. Stratigraphy and origin of the Chinle Formation and related upper Triassic strata in the Colorado plateau region. US Geol. Surv. Prof. Pap. 1972;690:1–336.

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