A new herrerasaurid (Dinosauria, Saurischia) from the Upper Triassic Ischigualasto Formation of northwestern Argentina

Abstract Herrerasauridae comprises a basal clade of dinosaurs best known from the Upper Triassic of Argentina and Brazil, which have yielded remains of Herrerasaurus ischigualastensis and Staurikosaurus pricei, respectively. Systematic opinion regarding the position of Herrerasauridae at the base of Dinosauria has varied. Here we describe a new herrerasaurid, Sanjuansaurus gordilloi gen. n., sp. n., based on a partial skeleton from Carnian-age strata of the the Upper Triassic Ischigualasto Formation of northwestern Argentina. The new taxon is diagnosed by numerous features, including long, band-shaped and posterolaterally oriented transverse process on the posterior cervical vertebrae; neural spines of the sixth to eighth dorsal vertebrae, at least, bearing acute anterior and posterior processes; scapula and coracoid with everted lateral margins of the glenoid; and short pubis (63% of the femoral length). Phylogenetic analysis placed Sanjuansaurus within a monophyletic Herrerasauridae, at the base of Theropoda and including Herrerasaurus and Staurikosaurus. The presence of Sanjuansaurus at the base of the Ischigualasto Formation, along with other dinosaurs such as Herrerasaurus, Eoraptor, Panphagia, and Chromogisaurus suggests that saurischian dinosaurs in southwestern Pangea were already widely diversified by the late Carnian rather than increasing in diversity across the Carnian-Norian boundary.

Here we describe a new herrerasaurid from strata near the basal contact of the Ischigualasto Formation. Th e new taxon is based on an associated, partially articulated skeleton recovered from Ischigualasto Provincial Park in 1994.

Geological and palaeontological settings
Th e holotype of the new taxon (PVSJ 605) was found in 1994 during fi eldwork carried out by the Instituto y Museo de Ciencias Naturales of the Universidad Nacional de San Juan. Th e Ischigualasto Formation crops out in northwestern Argentina and forms part of the Ischigualasto-Villa Unión Basin ( Figure 1). It reaches up to 700 m in thickness and comprises fl uvial channel sandstones with sandstones and mudstones deposited on a well-drained fl oodplain. Interlayered volcanic ashes 20 m above the base of the formation provide chronostratigraphic control and have yielded an age of 231.4 Ma, placing them in the Carnian stage Renne et al. 2010).
Th e Ischigualasto Formation is divided into four members (Currie et al. 2009). From the base to the top they are: the La Peña (from the base to 40 m), the Cancha de Bochas (40 to 180 m), the Valle de la Luna (180 to 650 m) and the Quebrada de la Sal (650 to 700 m) members ( Figure 1). Th e La Peña Member consists of multi-story channel sandstones and conglomerates covered by poorly-drained fl oodplain mudstones. Th e Cancha de Bochas Member is composed of thick, well-drained fl oodplain mudstones interbedded with high-sinuosity channel sandstones. Th e Valle de la Luna Member is mostly characterized by amalgamated high-sinuosity channels, abandoned channels and marsh deposits. Finally, the Quebrada de la Sal Member consists of tabular fl uvial deposits.
Th e new fossil was excavated at the La Gallinita locality, which is located in the lowest levels of the Cancha de Bochas Member. It was found 40 m above the base of the formation. Dinosaurs, including several specimens of Herrerasaurus ischigualastensis and Eoraptor lunensis, the holotype of Panphagia protos, and other as yet undescribed species (Martinez et al. 2008), carnivorous and herbivorous cynodonts, rhynchosaurs, and crurotarsan archosaurs were recovered from the same level.

Preservation and preparation
Th e reddish brown bones were covered by a coarse hematite crust, and the entire specimen was embedded in a grey-green, fi ne-grained sandstone matrix. Th e overall preservation of the specimen is good. All the bones are three-dimensionally preserved, and most are complete with the exception of the femora, which are partially distorted and lack fi ne details. Th e incompleteness of the skeleton is attributable to pre-burial processes, although the third, fourth and anterior part of the fi fth dorsal vertebra were lost in the course of preparation. Th e specimen was prepared using a pneumatic air scribe and pin vice.

Terminology
We employ traditional, or "Romerian," anatomical and directional terms rather than their veterinarian alternatives (Wilson 2006). "Anterior" and "posterior", for example, are used as directional terms rather than "rostral" or "cranial" and "caudal". We also follow Wilson's (1999) recommendations regarding the identifi cation of vertebral laminae in saurischians.

Phylogenetic Analysis
In order to asses the phylogenetic position of the new taxon among basal Dinosauria, we added it (Table 1) and the recently described basal sauropodomorph Panphagia (Martinez and Alcober 2009) to the character-taxon matrix published by Langer and Benton (2006). We also modifi ed several character states for these basal taxa following Martínez and Alcober (2009). Th e software used to analyze the phylogenetic relationships was TNT 1.1 (Goloboff et al. 2003).

Nomenclatural Acts
Th is published work and the nomenclatural acts it contains have been registered in ZooBank, the proposed online registration system for the ICZN. Th e ZooBank LSIDs (Life Science Identifi ers) can be resolved and the associated information viewed through any standard web browser by appending the LSID to the prefi x "http://zoo-bank.org/". Th e LSID for this publication is: urn:lsid:zoobank.org:pub:FB2AE660-C3EE-4348-BF9F-F4311C47E853.

Institutional abbreviations:
PVSJ Instituto y Museo de Ciencias Naturales, San Juan 5400, Argentina. right pubis, both femora and tibiae, right fi bula, right astragalus and calcaneum, and left metatarsal II. Type locality: Th e specimen was found in the Cancha de Bochas Member (Currie et al. 2009), 40 m above the base of Ischigualasto Formation. Th e type locality, informally called "Herrera de la base", is located 3 km northwestern of "Cancha de Bochas" locality, Ischigualasto Provincial Park, San Juan, Argentina ( Figure 1).

Systematic
Horizon and age: 40 m above the base of the Ischigualasto Formation, Late Triassic, Carnian (ca. 231.4 Ma), Ischigualasto-Villa Unión Basin Renne et al. 2010). Th e type horizon lies at approximately the same level as the dated ash, which implies a late Carnian age for the specimen.
Diagnosis: Diagnosed by the following autapomorphies: shelf-like, posterolaterally directed transverse processes on the posterior cervical vertebrae; neural spines of the sixth to eighth dorsal vertebrae, at least, bearing acute anterior and posterior processes; everted lateral margins of the glenoid; short pubis (63% of the femoral length); and pronounced, rugose scar on the medial surface of the femur at the level of the fourth trochanter.

Description
Although some bones of Sanjuansaurus gordilloi were disarticulated, the proximity of all elements, found in an area of only one square meter, their complementary size, and the absence of any duplicated elements suggest that they represent a single individual ( Figure 2). In size and general proportions ( Table 2, 3), the new specimen ( Figure 3A) is comparable to a medium-sized Herrerasaurus ( Figure 3B), and slightly larger than the only known specimen of Staurikosaurus ( Figure 3C).
Cranium. Th e left maxilla is the only cranial bone preserved ( Figure 4A). It exhibits the anteroposteriorly elongated dorsal process and transversely narrow antorbital fossa as in Herrerasaurus ( Figure 4B, C) but unlike the wide fossa of Eoraptor : Fig. 2A). Th e anterodorsal border of the antorbital fossa shows a slit-shaped promaxillary fenestra as in Herrerasaurus, some coelophysoids, Zupaysaurus, and most tetanurans (Welles 1984;Witmer 1997;Arcucci and Coria 2003;Sereno 2007). Th e anterior border of the maxilla is slightly convex and preserves the posterior border of the subnarial foramen as in other saurischians. Breakage of the dorsal portion makes it impossible to determine whether there is an oval fenestra between the premaxilla and maxilla as in Herrerasaurus (Sereno and Novas 1994). Th e dorsal border of the jugal process below the antorbital fenestra is horizontal ( Figure 4). In specimens of Herrerasaurus, this suture is either horizontal (PVSJ 053, holotype of "Frenguellisaurus ischigualastensis") or posteroventrally inclined (PVSJ 407) (Sereno and Novas 1994: Fig. 1).
Axial skeleton. Th e cervical vertebrae are preserved from the incomplete atlas to the last vertebra of the series ( Figure 5A, B). Sanjuansaurus has nine cervical vertebrae. Th e last cervical vertebra diff ers from the fi rst dorsal vertebra in the presence of a ventral keel and being nearly 30% longer, with the paraphophysis being more anteriorly located and the capitulum of the associated rib being more slender (Figure 2, 3, 5A). Although ten cervical vertebrae have been reported in Herrerasaurus (Sereno and Novas 1994), the cervicodorsal transition is not well preserved on any of the known specimens.
Th e atlas is represented only by its centrum, the odontoid ( Figure 5A), which is completely co-ossifi ed with the axial centrum. It is subcircular in dorsal view with a pointed median projection as in Herrerasaurus (Sereno and Novas 1994). It is semilunar in outline in anterior view. Th e dorsal and ventral surfaces are concave and convex, respectively, as in Herrerasaurus.
Th e axial intercentrum ( Figure 5A) is fused to the axial centrum. It is much broader than the anterior end of the axial centrum as in Herrerasaurus. In lateral view it is subquadrangular rather than triangular as in Herrerasaurus (Sereno and Novas 1994). Its anteroposterior length is one-half that of the axis, resembling that in large specimens of Herrerasaurus (PVSJ 053), but proportionately longer than that in the small ones (e.g, PVSJ 407), where it equals one-third of axial centrum length. As in Herrerasaurus the axial intercentrum is deeply cupped anteriorly.
Th e axial centrum ( Figure 5A) is twice as long as it is deep and bears a pronounced ventral keel as in Herrerasaurus (Sereno and Novas 1994). Th e diapophyses are short and face dorsolaterally as in Herrerasaurus, although they are located more anteriorly and are level with the axial intercentrum. In Herrerasaurus the diapophyses do not extend beyond the anterior articular surface of the centrum. Damage to the neural spine and the postzygapophyses preclude description of their structure.
Th e postaxial cervical centra are spool-shaped, amphicoelous, and have pronounced ventral keels. In Herrerasaurus, by contrast, the lateral and ventral sides of the centrum are less concave, and the ventral keel diminishes progressively in more distal vertebrae (Sereno and Novas 1994). Th e second to the sixth cervical centra are approximately parallelogram-shaped in lateral view whereas the seventh to the ninth centra are subrectangular. Th e third cervical vertebra is longer than the axis, and centrum length increases posteriorly up to the sixth cervical centrum ( Figure 5A) as in Herrerasaurus (Sereno and Novas 1994). Th is condition is diff erent from Staurikosaurus, in which the third or fourth centrum is the longest (Galton 1977;Bittencourt and Kellner 2009). Th e parapophyses of the anterior cervical vertebrae of Sanjuansaurus protrude ventrally beyond the ventral margin of the centrum in lateral view, in contrast to the condition Measured along ventral edge excluding anterior convexity of centrum when present. in Herrerasaurus, where they are located slightly dorsal to the ventral border of the centrum. Posteriorly, from the seventh vertebra, the parapophyses are displaced progressively backwards and upwards. All the cervical neural spines are broken at their bases. From the third to the ninth vertebra, the prezygapophyses extend one third of the centrum length beyond the anterior border of the body. Th e postzygapophyses are high and do not project behind the level of the posterior face of the centrum. As in Herrerasaurus (Sereno and Novas 1994), the epipophyses are pointed and extend beyond the postzygapophyses ( Figure 5A). On the sixth cervical vertebra, anterior and posterior centrodiapophyseal, postzygodiapophyseal, and prezygodiapophyseal laminae are present and become more prominent on successive cervical vertebrae. From the fi fth cervical vertebra onwards, the transverse processes increase in both anteroposterior width and transverse length and project posteroventrolaterally ( Figure 5B), an unusual shape among theropods. Th e transverse processes are triangular in Herrerasaurus (Sereno and Novas 1994) and Staurikosaurus (Galton 1977). Th e dorsal vertebrae are articulated. Only the third, fourth and anterior half of the fi fth vertebra are lacking and were accidentally lost during preparation . Th us we can say with confi dence that there are 14 dorsal vertebrae as in Herrerasaurus (Sereno 2007, contra Novas 1994, in contrast to 15 in Staurikosaurus (Galton 1977;Bittencourt and Kellner 2009). Th e dorsal vertebrae are characterized by anteroposteriorly short centra and tall neural arches as in Herrerasaurus and Staurikosaurus (Novas 1994;Colbert 1970;Bittencourt and Kellner 2009). Th ey diff er in having more distinctly spool-shaped centra ( Figure 5C). Th e ventral concavity is very conspicuous in the fi rst to eleventh dorsal vertebrae, decreasing slightly in the twelfth  to fi fteenth. Centrum length decreases from the fi rst to the second dorsal, increases from the sixth to the twelfth, and decreases again to the fi nal dorsal vertebra ( Table 2). A ventral keel is absent on all dorsal vertebrae although a prominent keel is present on the last cervical vertebra. Th e parapophyses are prominent and oval in lateral view. On the fi rst and second dorsals, they are located at mid-length of the centrum. In more posterior dorsal vertebrae, they are displaced anterodorsally. On the twelfth dorsal vertebra, the parapophyses and diapophyses are located at the same level. Th e parapophyses of the fi rst and second dorsal vertebrae are shared between the centrum and neural arch. In the sixth vertebra (the fi rst completely preserved vertebra posterior to the second), the parapophyses are located entirely on the neural arch ( Figure  5B). Th e neural arches are anteroposteriorly short and dorsoventrally deep. Pre-and postzygapophyses are anteroposteriorly short, the former are slightly longer than the latter and extend beyond the anterior centrum face as in Herrerasaurus (Novas 1994). Pre-and postzygapophyses are separated by an interzygapohpyseal sulcus, which extends onto the anterior and posterior edges of the neural spine as in Herrerasaurus and Staurikosaurus (Novas 1994;Bittencourt and Kellner 2009). Th e second dorsal vertebra, which is disarticulated from the posterior part of the vertebral column, has a well developed hyposphene similar to that present in Herrerasaurus (Novas 1994). Th e remaining dorsals presumably also had hyposphene-hypantrum articulations, but these are obscured by the tight articulation between vertebrae. Th e anterior neural spines are broken off with the exception of those on the sixth and eighth dorsal vertebrae. Th ese have distinctive pointed processes extending anteriorly and posteriorly from the apex of the spine ( Figure 5C, D). Th e distal end of the neural spine of the last dorsal vertebrae also bears a spine table, which is similar to that in Herrerasaurus (Novas 1994). All the dorsal vertebrae have well developed anterior and posterior centrodiapophyseal, postzygodiapophyseal, and prezygodiapophyseal laminae. Th ese laminae bound three subtriangular spaces the infraprezygapophyseal, infradiapophyseal and infrapostzygapophyseal fossae ( Figure 5C). Th ese fossae converge below a horizontal roof formed by the diapophysis and pre-and postzygodiapophyseal laminae as in Herrerasaurus.
Th e sacrum ( Figure 5C, D) of Sanjuansaurus comprises three vertebrae. Th e fi rst is a dorsosacral whereas the second and third represent the primordial sacral pair as in Herrerasaurus (Sereno 2007, contra Novas 1994. In Staurikosaurus the sacrum is composed of two primordial sacrals, with some uncertainty concerning the presence of a dorsosacral or caudosacral (Bittencourt and Kellner 2009). Given the degree of neurocentral coossifi cation in other parts of the axial column and the fusion of the sacral ribs to their respective centra, it is surprising that the sacral centra are not co-ossifi ed.
Th e fi rst sacral vertebra is 10% longer than the last dorsal vertebra, and the position of the infradiapophyseal laminae and the transverse processes are somewhat different. Th e posterior centrodiapophyseal lamina is displaced anteriorly toward the anterior centrodiapophyseal lamina, so that ventral to the transverse process they both extend nearly vertically ( Figure 5C, D). Th e transverse process is not a single fl at process as on the posterior dorsal vertebrae but rather is composed of two laminae, one horizontal and the other one vertical, which join to form an inverted L-shape near the contact with the ilium. Th is confi guration is similar to that shown on dorsal vertebra 15 in Herrerasaurus (Novas 1994 : Fig. 1). Th e addition of the ventral lamina presumably strengthened the transverse process. Th e latter expands posterolaterally toward its distal end, which is broken away. Th e form of the process and its distal expansion suggest that it probably contacted the preacetabular process of the ilium, but this contact or the distal articular surface is not preserved. Th e distal end of the neural spine is expanded to form a spine table as in Herrerasaurus (Novas 1994). Th e anterior and posterior borders of the neural spine have median sulci that extend between the preand postzygapophyses, respectively.
Th e second sacral vertebra is 25% longer than the fi rst and is the longest in the sacrum ( Figure 5C, D). Th is is true for one individual of Herrerasaurus (PVSJ 373), whereas in another (PVL 2566) the third sacral vertebra is longest (Novas 1994). Th e centrum is transversally narrower and dorsoventrally fl atter, and the neural spine is broader than in the fi rst sacral vertebrae as in Herrerasaurus (Novas 1994). Th e spine table and anterior and posterior median sulci are twice the transverse width of the corresponding features on the fi rst and third sacral vertebrae. Th e ribs are extensively fused to the anterodorsal portion of the centrum.
Th e third sacral vertebra, the most robust of the sacrum, is dorsolaterally fl attened and transversally expanded as in Herrerasaurus (Novas 1994) (Figure 5C, D). As on the second sacral vertebra, robust sacral ribs are fused to the centrum. Th e ventral border of the rib is located at the same level as the ventral surface of the centrum, in contrast to the condition in Herrerasaurus, in which the rib is off set dorsally (Novas 1994). Th e neural spine is equal in height to the second sacral but is lateromedially narrower.
Th e sacral ribs of the second and third sacral vertebrae have broad distal attachment surfaces that are continuous and, in lateral view ( Figure 5D) form a C-shape that opens dorsally. Large subcircular openings are present between the articular ends of the sacral ribs and the centra as in Herrerasaurus (Novas 1994).
Th e fi rst 15 caudal vertebrae of PVSJ 605 are preserved in articulation. Th e posterior end of the fi fteenth vertebra and all the hemal arches are lacking ( Figure 5E). Th e preserved centra are strongly constricted, or spool-shaped, more so than in Herrerasaurus (Novas 1994 : Fig. 4). As in Herrerasaurus and Staurikosaurus (Bittencourt and Kellner 2009), the centra lack ventral keels. Th e fi rst caudal centrum is 10% shorter than that of the last sacral, and this length is maintained with minor variation along the preserved series, despite the decreasing height of the centra ( Table 2). Th e neural arches are very tall with zygapophyses located far from the transverse process as in Herrerasaurus (Novas 1994). Th e subhorizontal transverse processes are situated in the middle of the centrum and project laterally and slightly posteriorly. In section the transverse processes are dorsoventrally fl attened, in contrast to the semicircular section evident in Herrerasaurus (Novas 1994) and Staurikosaurus (Bittencourt and Kellner 2009). Th e only preserved neural spines, the third and fourth, are tall and near vertical, as is the case with the proximal caudal spines in Herrerasaurus. Th e caudal neural spines lack the anterior and posterior sulci present on the dorsal and sacral spines, and on the anterior caudals of Herrerasaurus (Novas 1994). Th e prezygapophyses extend beyond the anterior centrum face, whereas the postzygapophyses terminate fl ush with the posterior centrum face. Appendicular Skeleton. Each scapula is fi rmly fused to its respective coracoid. Th e anterior margin is broken away on both scapulae, although its curved margin can be restored. Th e acromial process diverges from the blade at an angle slightly greater than 90°, as in Herrerasaurus (Sereno 1994). Th e glenoid is shared unevenly between the scapula and coracoid, the former contributing a smaller portion of the articulation, as in Herrerasaurus. Th e margin, or lip, of the glenoid protrudes laterally in a conspicuous manner, which does not seem to be an artifact of preservation ( Figure 6A). Th e scapular blade is straplike with narrow proportions in lateral view ( Figure 6A, B). Th e minimum width of the blade (near the base) is 54% the width of the acromial margin. Th is ratio is smaller than that found in either small (83%; PVSJ 407) or very large individuals (60%; PVSJ 053, "Frenguellisaurus") of Herrerasaurus. Th e dorsal margin of the acromion is thin in contrast to the thickened border in Herrerasaurus (Sereno 1994). Th e lateral surface of the scapular blade has a distinct crest along the proximal two thirds of its length as in Herrerasaurus (Sereno 1994). In lateral view the blade is gently arched posteriorly in contrast to the nearly straight blade in Herrerasaurus.
Th e semicircular, plate-shaped coracoid ( Figure 6A, B) is broader anteroposteriorly than dorsoventrally as in Herrerasaurus (Sereno 1994). It is gently concave medially. As in Herrerasaurus, the coracoid foramen is located anteroventral to the glenoid, opening anterolaterally entirely within the coracoid. Th e margin of the glenoid is particularly prominent laterally, forming a shelf ( Figure 6A). Th e hook-shaped posteroventral pro-cess of the coracoid is long and pointed ( Figure 6B), similar to that in ornithomimids such as Gallimimus (Osmólska and Barsbold 1990: Fig. 4). When the scapular blade is held vertically it is seen to extend far posterior to the glenoid. Th e process is considerably shorter in Herrerasaurus (Brinkman and Sues 1987: Fig. 2-10). Th e glenoid is separated from the posteroventral process by a notch marked by a deep depression ( Figure 6A).
Th e ulna is more gracile than that of Herrerasaurus (Sereno 1994), but otherwise similar in shape. Th e proximal end bears a prominent olecranon process and a concave articular surface ( Figure 6C-E). Th e lateral surface of the proximal end has a distinct protuberance that contributes to a concave articular surface for the proximal end of the radius as in Herrerasaurus (Sereno 1994). In Sanjuansaurus the ulnar protuberance is more acute. Th e medial surface of the proximal end is slightly concave, in contrast to the convex surface of Herrerasaurus, although this diff erence may be due to postmortem deformation in Sanjuansaurus. Th e distal half of the ulnar shaft shows a gentle medial curvature and has longitudinal ridges on its anterior, lateral and medial surfaces as in Herrerasaurus (Sereno 1994). Th e ulnar shaft of Sanjuansaurus appears to be more slender than in Herrerasaurus. Th e distal end of the ulna exhibits several diff erences to that of Herrerasaurus. It is expanded to a lesser degree than in small individuals of Her- rerasaurus (e.g, PVSJ 373;Sereno 1994). Th e articular surface for the ulnare is concave and faces anteromedially ( Figure 6D, E) in contrast to the convex surface of Herrerasaurus. Anterolateral to this articular facet, there is a protuberance that extends distally ( Figure 6C-E). Th is protuberance may be homologous with a subtriangular ligament rugosity in Herrerasaurus (Sereno 1994).
Of the manus only one manual ungual ( Figure 6F, G) is preserved. Th e ungual has been crushed transversely. Its curvature and transversely narrow proportions (Figure 6F) identify it as pertaining the the manus rather than the pes. Its small size, short and deep proportions, and ventral position of the attachment groove suggest that it is probably the fourth (terminal) phalanx of the third digit. Th e ungual has a well developed fl exor tubercle more deeply grooved on the left side ( Figure 6G). Although we considered that it is the smaller ungual of the hand, it is still small compared to individuals of Herrerasaurus (PVSJ 373) smaller in overall size than Sanjuansaurus.
A fragment of the left ilium comprises the distal portion of the pubic peduncle ( Figure 7D). It is fused with the proximal end of the pubis, and preserved in articulation with the left femur (although the latter is dorsally rotated from its natural position). Medially it is also fused to a distal fragment of the second sacral rib. Th e pubic peduncle is stout, anteroventrally directed and forms the anterior border of a wide perforate acetabulum as in Herrerasaurus (Novas 1994). Th e supra-acetabular crest forms the straight lateral edge of the pubic peduncle, extending posterodorsally over the acetabulum as in Herrerasaurus.
Th e pubis is relatively short, its proximodistal length comprising only 63% the length of the femur ( Figure 7A-C). By contrast, in Herrerasaurus and Staurikosaurus, the length of the pubis equals 91% (PVL 2566) and 70% the length of the femur, respectively. Th e two proximal articular surfaces are set at an angle of 130°. Th e fi rst faces posteriorly and articulates with the ischium whereas the second faces posterodorsally and includes an acetabular section and an articular facet for the ilium. A marked prominence, more distinct than that seen in Herrerasaurus (Novas 1994), is located on the anterolateral margin of the pubis near the iliac peduncle and is presumed to represent the insertion site for the ambiens muscle. Th e oval obturator foramen is large, its anteroposterior diameter measuring 34% of the anteroposterior width of the proximal end. In Sanjuansaurus the pubis shaft lacks the strong proximal curvature characteristic of Herrerasaurus (Novas 1994), although the lateral margin of the shaft has a similar sinuous curvature in anterior view. Th e distal portion of the pubis expands and is turned posteriorly to form a pubic "foot" as in Herrerasaurus and Staurikosaurus (Novas 1994;Bittencourt and Kellner 2009). Th e anteroposterior width of the pubic "foot" is 40% of pubic length, which is slightly less than in Herrerasaurus (43% and 48% in small and large individuals, respectively) (Novas 1994), but greater than in Staurikosaurus (26%).
Both femora are poorly preserved ( Figure 7D-H). Th e left femur is complete and articulated with the ilium, although rotated dorsally from its natural articulation ( Figure 7D). Only the proximal and distal ends of the right femur are preserved ( Figure 7E). Th e femur is sigmoid in lateral and anterior views ( Figure 7D, E). Th e anteromedially projecting head lies at an angle of approximately 65° to the transverse axis of the distal end. Th is is slightly more divergent than in Herrerasaurus (55°;Novas 1994). Th e size of the head is smaller and narrower transversally than in small individuals of Herrerasaurus (PVSJ 373) that are smaller in overall size than Sanjuansaurus. In proximal view the head is kidney-shaped ( Figure 7F), and its proximal surface is smoothly convex as in Herrerasaurus (Novas 1994), although Sanjuansaurus lacks the facies articularis antitrochanterica present in the latter (Novas 1994). Th e anterior surface of the femoral neck lacks the pronounced anterior trochanter present in Herrerasaurus (Novas 1994). Although partially obscured by deformation Abbreviations: aa, acetabular area; ao, abnormal outgrowth in posteroventral process; cc, cnemial crest; ctf, crista tibiofi bularis; 4t, fourth trochanter; fc, fi bular condyle; fh, femoral head; gt, greater trochanter; Isaf, ischium articular facet; Il, illium; Isaf, ischium articular facet; lc, lateral condyle; mae, ambiens muscle eminence; mCFLs, scars for attachment of muscle caudifemoralis longus; of, obturator foramen; pf, pubic foot; pv, posteroventral process; rP, right pubis; sac, supraacetabular crest; tc, tibial condyle; ts, trochanteric shelf. Scale bar equals 5 cm. and adhering hematite, the trochanteric shelf is present on the lateral surface of the femur ( Figure 7E). Th e shaft of the left femur appears to be more robust than that of Herrerasaurus, although this may be an artifact of preservation. Anteriorly, it has a pronounced keel that extends from the level of the trochanteric shelf proximally to the distal quarter of the femur. Th e fourth trochanter is semi-elliptical in lateral view and located on the proximal third of the femur ( Figure 7E), similar to the condition in Chindesaurus (Long and Murry 1995: Fig. 184). It is longer (one fourth of femoral length), thinner, and seemingly more symmetrical than in Herrerasaurus. A very large, pronounced and rugose protuberance is present on the medial surface of the femur at the level of the fourth trochanter, presumably for the insertion of M. caudifemoralis longus ( Figure 7G). In Herrerasaurus this protuberance is relatively small and smooth. Th e distal end of the femur is expanded. Th e anterior surface is convex transversally, lacks an intercondylar groove, and has a large attachment scar that extends laterally as in Herrerasaurus (Novas 1994). Th e posterior surface has a deeper popliteal fossa than in Herrerasaurus (Novas 1994). Th e crista tibiofi bularis is separated by a sulcus from the fi bular condyle and projects farther posteriorly than the tibial condyle (Figure 7H). Th e articular surface of the distal end has a concavity extending from the popliteal fossa medially to the groove between the crista tibiofi bularis and the fi bular condyle as in Herrerasaurus.
Th e left tibia of Sanjuansaurus is complete and well preserved ( Figure 7I-N). Th e right tibia is preserved in articulation with the fi bula. Th e distal ends of these bones as well as the right astragalus and calcaneum exhibit some features that appear to be abnormalities rather than artifacts of postmortem compression or crushing. Th e tibia is slightly shorter than the femur. Th e tibiofemoral ratio is 0.89, which lies within the range recorded for Herrerasaurus (0.87-0.91) (Novas 1994). Th e proximal end of the tibia is subtriangular with its long axis directed anteroposteriorly. Th e cnemial crest projects anteriorly and extends along the proximal one fi fth of the tibia. Th e lateral condyle is posteriorly located as in Herrerasaurus. In cross-section, the proximal half of the shaft is elliptical and the distal half subcircular. In lateral view, the anterior margin of the tibial shaft ventral to the cnemial crest is straight, whereas it is concave in Herrerasaurus (Novas 1994 : Fig. 8B). In distal view the distal end of the tibia is subcircular, rather than quadrangular, more closely resembling the condition in Staurikosaurus (Galton 1977) than in Herrerasaurus. Th e posteroventral process is transversally narrower and dorsoventrally shorter than in Herrerasaurus. Th e distal end of the right tibia, which as mentioned above appears to be pathologic, has an unusual, tab-shaped lateral expansion of the posteroventral process ( Figure 7P).
Th e relatively slender fi bula is subequal to the tibia in length and has transversally fl attened proximal and distal ends, the former twice the anteroposterior width at the mid shaft. Th e shaft is slightly bowed anterolaterally, and has a subtriangular crosssection at mid shaft. Poor surface preservation and breakage of the distal end obscure further details.
Th e astragalus and calcaneum of Sanjuansaurus are fused as in some dinosauromophs (Dromomeron romeri; Irmis et al. 2007), Lagerpeton chanarensis (Romer 1971), heterodontosaurids (Santa Luca 1980, and coelophysoid theropods (Raath 1969). Unlike in many coelophysoids, however, there is no fusion between the crus and proximal tarsals. Whereas the complete fusion of proximal tarsals in Sanjuansaurus might be natural, the distal end of the tibia just above the preserved proximal tarsals appears to be pathologic. Th us we are uncertain whether the observed fusion of the preserved right proximal tarsals is natural or a pathological condition. Th e astragalus is subtriangular in dorsal view, with a rounded posteromedial border, instead of the distinct posteromedial corner present in Herrerasaurus ( Figure 8A, B). Th e ascending process is tabular, extending transversally from the medial border of the astragalus mediolaterally along the entire width of the astragalus ( Figure 8A, B). In Sanjuansaurus, the tip of the ascending process is located at one fi fth the length of the lateral border, as in Herrerasaurus, but is close to the anterior border in the former, whereas in the latter it is close to the posterior border. Lateral to its tip, the ascending process continues as a ridge on the proximomedial surface of the calcaneum ( Figure 8A). Th e anterior surface of the ascending process is pierced by a large foramen near its base, as in Herrerasaurus  (Novas 1994). Th e posterior portion of the astragalus is fl at with a sharp posterior edge that forms a posteriorly projecting shelf ( Figure 8E, F).
A complete left second metatarsal is the only pedal bone preserved. It is straight in dorsal view ( Figure 7O). Th e proximal end is transversely fl attened with the long axis directed anterolaterally as in Herrerasaurus (Novas 1994). A pair of distinct articular surfaces for the fi rst and third metatarsals is present on the medial and lateral sides of the proximal part of the shaft. Th e proximal articular surface is subrectangular in proximal view. Th e narrow shaft is twisted so that, in distal view, proximal and distal ends have undergone a clockwise rotation of 45°. Th e distal end of the metatarsal is asymmetrical, with the lateral condyle extending further distally than the medial condyle. Th e lateral condyle is more developed than the medial and has a deeper collateral ligament fossa. Th e distal end has a transversely broad dorsal extensor depression to accommodate the base of the proximal pedal phalanx. Th e depression is bounded proximally by a ridge, which is more prominent laterally than medially. Th ese features also characterize the second metatarsal of Herrerasaurus (Novas 1994).

Discussion
Sanjuansaurus gordilloi exhibits several features that allow its distinction from all other known basal dinosaurs: similar, the new taxon can be further distinguished from the latter form by three other characters: (1) Th e scapular blade of Sanjuansaurus is straplike in lateral view ( Figure 6A, B), similar in shape than that present in Herrerasaurus, but it is narrower in Sanjuansaurus. Th e minimum width of the blade (near the base) is 54% the width of the acromial margin, less than that found in either small (83%; PVSJ 407) or very large individuals (60%; PVSJ 053) of Herrerasaurus. (2) Th e pubis shaft of Sanjuansaurus lacks the strong proximal curvature characteristic of Herrerasaurus (Novas 1994). (3) In Sanjuansaurus the obturator foramen of the pubis is larger. Th e anteroposterior diameter of the obturator foramen of Sanjuansaurus measures 34% of the anteroposterior width of the proximal end of the pubis, whereas that value is 15% in Herrerasaurus.

Phylogenetic Position
Phylogenetic analysis resulted in a single most parsimonious tree of 190 steps (consistency index 0.553, retention index 0.593). An implicit enumeration search (Goloboff et al. 2003) and jackknifi ng (probability of character removal 0.36, 1,000 resampled matrices) were also performed. Th e topology of the most parsimonious tree is similar to the consensus tree recovered by Martinez and Alcober (2009), diff ering mainly in resolved positions for Silesaurus and Guaibasaurus. In the present analysis Silesaurus was positioned outside Dinosauria, and Guaibasaurus was positioned as a non-eusaurischian saurischian as in the analysis by Langer and Benton (2006).
Th e analysis supports the hypotheses that Dinosauria and Herrerasauridae (Staurikosaurus pricei + Herrerasaurus ischigualastensis + Sanjuansaurus gordilloi) are monophyletic and that Herrerasauridae is positioned at the base of Saurischia outside of Eusaurischia, a result similar to that presented by Langer and Benton (Langer and Benton 2006). Within Herrerasauridae, a polytomy was obtained between Staurikosaurus, Sanjuansaurus and Herrerasaurus.
Seven synapomorphies support the clade Herrerasauridae in the consensus tree (characters 20. 1, 39.1, 45.1, 46.1, 47.1, 69.2, and 77.1). Only four of those (characters 39, 45, 46, and 77) can be scored in all herrerasaurids, and character 20 is the only one that cannot be determined in Sanjuansaurus. Th e unambiguous synapomorphies that unite the herrerasaurids in this analysis are the same as those previously identifi ed (Langer and Benton 2006), and do not modify our understanding of the monophyly of Herrerasauridae, although they clearly recover Sanjuansaurus as herrerasaurid.
Other features that support a grouping Sanjuansaurus + Herrerasaurus, but are ambiguous at present include: a narrow "U" shaped antorbital fossa with a promaxillary fenestra located on the anterodorsal border; centrum of the sixth cervical vertebra longest in the cervical series; spine tables on the distal end of the last dorsal and the sacral neural spines; two sacral vertebrae with the addition of one incipient dorsosacral; strap-shaped scapular blade that forms an angle of more than 90° with the acromion; size and shape of the pubic foot; and sinuous lateral border of the pubis in anterior view. Th ere are a few ambiguous character-states shared by Sanjuansaurus and Staurikosaurus but not with Herrerasaurus: shortness of the pubis relative to the femur and the subcircular distal end of the tibia in distal view. Th e latter character was originally considered as an autapomorphy of Staurikosaurus (Bittencourt and Kellner 2009).
On the other hand, many characters of Sanjuansaurus are unlike those inother herrerasaurids (where known): long band-shaped transverse processes of the distal cervicals; deep lateral and ventral concavity in cervical and dorsal centra; short pubis with wide subcircular obturator foramen; and fused astragalus and calcaneum with a tabular ascending process (if this character-state is not pathological in origin).

Faunal Considerations
Th e co-occurrence in the basal portion of the Ischigualasto Formation, of two herrerasaurids (Sanjuansaurus, Herrerasaurus), a basal saurischian (Eoraptor), and two sauropodomorphs (Panphagia, Chromogisaurus) suggests that saurischian dinosaurs were already highly diversifi ed in southwestern Pangea early in the Late Triassic. Th e new herrerasaurid also represents another large-bodied predatory dinosaur in the Carnianage Ischigualasto fauna, contrasting with the rarity of carnivorous dinosaurs in the successive Norian assemblage of the overlaying Los Colorados Formation. In that richly represented assemblage, only a single specimen of a coelophysoid theropod has been recovered to date (Arcucci and Coria 2003). Carnivorous crurotarsan archosaurs dominate this Norian fauna, underscoring a complex pattern of faunal change. Th e faunal assemblages of Ischigualasto Basin strengthen the theory of a complex early radiation of dinosaurs (Brusatte et al. 2010), controlled by a succession of events developed during the Late Triassic, in opposition to models of gradual dominance by competition (Bonaparte 1982;Charig 1984), rapid diversifi cation in the late Carnian (Padian and May 1993); opportunistic radiation in the Norian and Early Jurassic (Benton 1993;Benton 2006), dinosaurian dominance in the Norian (Novas 1996), or early diversifi cation in the Carnian and increase in diversity and abundance in the Norian (Langer et al. 2010).