Downloaded from http://sp.lyellcollection.org/ at CAPES on May 3, <strong>2013</strong>RAUISUCHIAXilousuchus sapingensis). These well-constrainedages for these ctenosauriscids <strong>al</strong>so double as theoldest confirmed dates for both Pseudosuchia andArchosauria as a whole (<strong>Nesbitt</strong> 2011; <strong>Nesbitt</strong><strong>et</strong> <strong>al</strong>. 2011a; Butler <strong>et</strong> <strong>al</strong>. 2011; Brusatte <strong>et</strong> <strong>al</strong>. 2011).A vari<strong>et</strong>y of other rauisuchians are known fromthe Middle Triassic, including the Anisian ‘Mandasuchustanyauchen’ (Charig 1967), Stagonosuchusnyassicus (Huene 1938a) and possibly ‘P<strong>al</strong>listeriaangustimentum’ from the Manda beds, and Prestosuchuschiniquensis (Huene 1938b) and Decuriasuchusquartacolonia (França <strong>et</strong> <strong>al</strong>. 2011) from theLadinian (Dinodontosaurus Assemblage Zone) partof the Santa Maria Formation. However, the exactages of these rocks are not clear.Youngest recordAn<strong>al</strong>yses of the end-Triassic extinction (e.g. Benton1986b, 1994; Olsen & Sues 1986) have depictedrauisuchians extending to the end of the Triassic.However, the previously presented data have threenotable limitations: (i) the rauisuchians used inthese studies are not monophyl<strong>et</strong>ic; (ii) revisionsin the Triassic timesc<strong>al</strong>e (Muttoni <strong>et</strong> <strong>al</strong>. 2004; Furin<strong>et</strong> <strong>al</strong>. 2006; Mundil <strong>et</strong> <strong>al</strong>. 2010) have changed stratigraphicranges; and (iii) the vertebrate fossil recordin the latest Triassic is poor glob<strong>al</strong>ly (Sues & Fraser2010). Fasolasuchus tenax from the top of the LosColorados Formation was previously thought tobe one of the youngest occurrences from the latestTriassic (Lucas 1998; Arcucci <strong>et</strong> <strong>al</strong>. 2004), butnew magn<strong>et</strong>ostratigraphic data (Santi M<strong>al</strong>nis <strong>et</strong> <strong>al</strong>.2011) suggest a mid-Norian date approximatelyequiv<strong>al</strong>ent to the age of Postosuchus kirkpatricki,c. 217–215 million years ago (mya) (Irmis <strong>et</strong> <strong>al</strong>.2010). The youngest known poposauroid is clearlyEffigia okeeffeae from the late Norian or Rha<strong>et</strong>ianCoelophysis Quarry (<strong>Nesbitt</strong> 2007; Zeigler & Geissman2011). A specimen referred to Postosuchus sp.(CM 73372) was recorded from the same quarry(Long & Murry 1995; Weinbaum 2002; Novak2004; Peyer <strong>et</strong> <strong>al</strong>. 2008), and if it belongs to Postosuchuskirkpatricki it would represent the youngestknown occurrence of Rauisuchidae. Recently,however, <strong>Nesbitt</strong> (2011) hypothesized a crocodylomorphrelationship for this specimen. Clearly, thediscovery and study of latest Triassic rauisuchiansis a pressing area of future research.The only possible early Jurassic record of a rauisuchianbelongs to a single specimen from the upperElliot Formation of South Africa (<strong>Nesbitt</strong> andR. Smith unpublished data). The specimen (SAM383) consists of the posterior portion of a maxillawith portions of five te<strong>et</strong>h from an anim<strong>al</strong> with askull length estimated to be c.1 m. It is unclear ifsome features of the maxilla that it shares with rauisuchians(e.g. Fasolasuchus tenax) are apomorphic(rectangular posterior portion of the maxilla inlater<strong>al</strong> view, fused interdent<strong>al</strong> plates, sh<strong>al</strong>low antorbit<strong>al</strong>fossa, large posteriorly opening foramen onposterior portion maxilla in medi<strong>al</strong> view). Alternatively,it is possible that the maxilla could belongto an early crocodylomorph. Addition<strong>al</strong> materi<strong>al</strong>and a b<strong>et</strong>ter understanding of character evolutionin rauisuchians and early crocodylomorphs areneeded to more confidently identify this intriguingspecimen.Relationships and evolutionRauisuchian taxonomy and evolution have beenpoorly understood because of a number of factors,including poor preservation of specimens, a fragmentaryfossil record, incompl<strong>et</strong>e descriptions, confusionin sorting <strong>al</strong>pha-level taxonomy and anincompl<strong>et</strong>e understanding of Triassic pseudosuchianrelationships. D<strong>et</strong>ails of the tortured taxonomichistory of rauisuchian classification areprovided elsewhere (see Gower 2000; Brusatte<strong>et</strong> <strong>al</strong>. 2010; <strong>Nesbitt</strong> 2011) and will not be repeatedhere. However, the combination of an increasinglymore compl<strong>et</strong>e fossil record with advances in phylogen<strong>et</strong>icm<strong>et</strong>hodologies (e.g. character construction,Sereno 2007; taxon inclusion, Brusatte 2010) instudying early archosaurs has led to a number ofbreakthroughs in understanding rauisuchian systematics.For example, early archosaur phylogenies(e.g. Juul 1994) including rauisuchians often usedcomposite scoring for suprageneric taxa thatassumed the monophyly of groups such as Prestosuchidae.Lately, b<strong>et</strong>ter-sampled archosaur phylogenies(Brusatte <strong>et</strong> <strong>al</strong>. 2010; Butler <strong>et</strong> <strong>al</strong>. 2011;<strong>Nesbitt</strong> 2011) including rauisuchians have usedspecies- or genus-level termin<strong>al</strong> taxa that do notassume the monophyly of Rauisuchia or majorsubgroups of rauisuchians. Even with those m<strong>et</strong>hodologiesin place, however, there is still no consensusabout rauisuchian relationships as a whole,<strong>al</strong>though the framework of one does seem to beemerging. This will, of course, only become clearwith further an<strong>al</strong>yses.The following descriptions of the relationshipsand evolution of rauisuchians follow the recentworks of Brusatte <strong>et</strong> <strong>al</strong>. (2010) and <strong>Nesbitt</strong> (2011)and revised iterations of those matrices in Butler<strong>et</strong> <strong>al</strong>. (2011). These two large an<strong>al</strong>yses disagree onthe fundament<strong>al</strong> relationships of rauisuchians; Brusatte<strong>et</strong> <strong>al</strong>. (2010) found a monophyl<strong>et</strong>ic Rauisuchia(<strong>al</strong>beit with minim<strong>al</strong> support, and overturned by therevised an<strong>al</strong>ysis in Butler <strong>et</strong> <strong>al</strong>. 2011), whereas<strong>Nesbitt</strong> (2011) found a paraphyl<strong>et</strong>ic ‘Rauisuchia’with respect to Crocodylomorpha (Fig. 2). However,<strong>al</strong>though these two an<strong>al</strong>yses differ fundament<strong>al</strong>ly,both works recovered similar relationships
Downloaded from http://sp.lyellcollection.org/ at CAPES on May 3, <strong>2013</strong>S. J. NESBITT ET AL.