POSSIBLE SECONDARILY TERRESTRIAL LIFESTYLE IN THE EUROPEAN PHYTOSAUR NICROSAURUS KAPFFI (LATE TRIASSIC, NORIAN): A PRELIMINARY STUDY

Size: px
Start display at page:

Download "POSSIBLE SECONDARILY TERRESTRIAL LIFESTYLE IN THE EUROPEAN PHYTOSAUR NICROSAURUS KAPFFI (LATE TRIASSIC, NORIAN): A PRELIMINARY STUDY"

Transcription

1 306 Tanner, L.H., Spielmann, J.A. and Lucas, S.G., eds., 2013, The Triassic System. New Mexico Museum of Natural History and Science, Bulletin 61. POSSIBLE SECONDARILY TERRESTRIAL LIFESTYLE IN THE EUROPEAN PHYTOSAUR NICROSAURUS KAPFFI (LATE TRIASSIC, NORIAN): A PRELIMINARY STUDY JULIEN KIMMIG Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, Saskatchewan, S7N 5E2, Canada, j.kimmig@usask.ca Abstract The Late Triassic (Norian) phytosaurs Nicrosaurus kapffi and Mystriosuchus planirostris appear at about the same time in central Europe. Both have very distinctive snout shapes and are thought to occupy different ecological niches. The depositional environment and post-cranial morphology suggest a secondarily terrestrial lifestyle for Nicrosaurus. Some phytosaurs might have exploited coastal habits based on fossils occuring in saline water deposits, whereas most are found in fresh to brackish water deposits. INTRODUCTION Phytosaurs are Late Triassic (Carnian to Rhaetian) archosaurs, with a body plan similar to modern crocodilians (Fig. 1). They are primarily known from the United States and Europe, but have also been found in Africa, South America and Asia. The deposits in which phytosaurs occur range from marine to swamp-like deposits, but most species are found in semi-aquatic environments (Long and Murry, 1995; Kimmig and Arp, 2010). Phytosaurs are considered to be close to the base of the crocodilian branch of evolution (Hutchinson, 2001; Irmis et al., 2007; Brusatte et al., 2010), the closest relatives being aetosaurs, rauisuchians and members of the Ornithosuchidae. Even though more recent phylogenetic analyses reinforce this relationship, there is no consensus on the precise origin of phytosaurs (Ballew, 1989; Hungerbühler, 2002). Given that the taxonomy of the Phytosauria is based on cranial characters and that most of the postcranial material has not been found associated with skulls, research on phytosaur postcrania is spare (Parrish, 1986a, b) and mostly reduced to comparisons with other archosaurs (Hutchinson, 2001; Holliday et al., 2010; Padian et al., 2010). Due to their resemblance to crocodilians, a lifestyle similar to that of extant crocodiles has long been suggested for phytosaurs ( Parrish, 1986b; Hunt, 1989). This led to the popular image of phytosaurs as semi-aquatic animals, which may be true for most taxa, although data analyzed here suggest that a more terrestrial lifestyle developed in at least one species. The first support for this conclusion came from an analysis of the European phytosaur-bearing deposits, which indicated that Nicrosaurus lived in swamp-like environments and spent less time in the water than did Mystriosuchus or most other phytosaurs. A similar habitat was suggested for the North American Redondasaurus (Heckert et al., 2001; Kimmig and Arp, 2010). To evaluate the lifestyles of various phytosaurs an analysis of the most commonly-preserved postcranial bones (ilia, femora, and humeri) of all available species was undertaken. The results of this analysis support the idea of the Early Norian phytosaur Nicrosaurus as primarily terrestrial, not semi-aquatic. In contrast, Mystriosuchus from the same deposits developed a lifestyle more aquatic than all other phytosaurs, a conclusion reinforced by the recovery of the remains of Mystriosuchus from marine strata in Austria, Italy and Switzerland (Buffetaut, 1993; Renesto and Paganoni, 1998). Institutional abbreviations: BMNH, The Natural History Museum, London, United Kingdom; NMMNH, New Mexico Museum of Natural History and Science, Albuquerque, NM, USA; Staatliches Museum fur Naturkunde Stuttgart, Stuttgart, Germany; UCMP, University of California Museum of Paleontology, Berkeley, CA, USA; ZPAL, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland. FIGURE 1. Comparison of the skeletons of A, Leptosuchus crosbiensis (after Long and Murry 1995), and B, Crocodylus niloticus (after Lydekker, 1879). MATERIAL AND METHODS For this study, phytosaur postcrania (ilia, femora and humeri) were compared to their closest relatives: aetosaurs, rauisuchians, and other archosaurs. The comparison was primarily based on published material, but also included some museum specimens. These three elements were chosen, because they are the portions of the phytosaur postcrania most commonly referred to the species-level. The published literature on crocodilian locomotion was used for reconstructing phytosaur locomotion. TAXONOMIC BACKGROUND Phytosaur taxonomy is highly debated and it is unlikely that a consensus opinion will be reached in the near future (Long and Murry, 1995; Hungerbühler, 2002; Stocker, 2010). In this paper I use the taxonomy of Hungerbühler (2002) and Kimmig (2009), which provides the most recent revision of the entire group. This revision concludes that all derived phytosaurs demonstrate sexual dimorphism, which is mainly based on the presence of a cranial crest in the male specimens. Phytosaurs are close to the base of the archosaurian tree (Fig. 2), but still a member of the crown Archosauria (Irmis et al., 2007; Brusatte et al., 2010). CROCODILIAN ECOLOGY All extant crocodilians are semi-aquatic animals, which has led to the general assumption that phytosaurs were also semi-aquatic. However, over the long history of the crocodilian order there were a variety of species that were terrestrial. Indeed, the earliest crocodylomorphs were terrestrial, and throughout crocodile evolution terrestrial forms evolved several times (e.g., Brochu, 2001).

2 FIGURE 2. Archosaur phylogeny based on Brusatte et al. (2010) and phytosaur phylogeny based on Hungerbühler (2002). Crocodilians are known for their crawling locomotion on land, but they can also move in a more mammal-like high walk by which they reach speeds of up to 5 kph (Guggisberg, 1972). The fastest method of moving is the gallop, where crocodiles can reach a speed of up to 17 kph (Webb and Gans, 1982). The high walk and the gallop are supposedly inherited from their ancestors, so it is likely that other members of the Crurotarsi also had the ability to perform these locomotion styles. Crocodilians feed on everything from fish and crustaceans to large mammals (Ross and Magnusson, 1989). This variation in feeding is mainly expressed by the snout form, which can partly provide an analog for phytosaurs (Hunt, 1989). ECOLOGICAL INDICATORS OF A TERRESTRIAL LIFESTYLE IN NICROSAURUS Hungerbühler (2002) mentioned that most phytosaur fossils of the Stubensandstein are found in sheet-flood sandstones at the transition from distal alluvial plain to playa lake. As phytosaur specimens in these sediments are mostly restricted to disarticulated specimens, it is likely that the fossils were subject to fluvial transport. Considering that most Mystriosuchus specimens outside of the Stubensandstein were found in saltwater deposits, it is likely that the carcasses were transported within the basin and that the animals lived close to the place where they were buried (Renesto and Paganoni, 1998; Hungerbühler, 2002; Kimmig and Arp, 2010). Nicrosaurus, in contrast, is mostly found in reworked palaeosols (Salzgitter) and marginal-lacustrine sandstones or breccias resting on sub-aerial exposure planes (Çal Dag; Krähenberg). This indicates that the animals spent a large amount of time on land and most likely lived in swamps or similar areas (Kimmig and Arp, 2010). Unfortunately most of the German basin outcrops from which the phytosaur fossils were collected are no longer accessible, so modern facies analysis is not possible. Another factor suggesting different lifestyles for these two phytosaur genera is the skull shape and the dentition. Nicrosaurus has a 307 very massive skull with a tripartite dentition, which is similar to the skull of modern crocodiles and suggests predation on larger animals with robust bones or even bony osteoderms. Mystriosuchus, in contrast, has a very slender skull with a bipartite dentition, similar to modern gavials, which is more suited for hunting fish and smaller tetrapods. PREVIOUS RESEARCH ON PHYTOSAUR LOCOMOTION Locomotion studies on phytosaurs are restricted to Leptosuchus (also referred to as Rutiodon: Parrish, 1986a, b). These studies compared them with several other archosaurs, but as Leptosuchus happens to be found in semi-aquatic deposits it is no surprise that it shows strong similarities to extant crocodilians (Mehl, 1928; Doyle and Sues, 1995). As there are at least nine genera of phytosaurs (Hungerbühler, 2002; Stocker, 2010), and some are found in marine or playa lake deposits (Gozzi and Renesto, 2003; Kimmig and Arp, 2010), it is surprising that functional analyses have not been performed for other genera. Some research on the functional morphology of the Polish Paleorhinus angustifrons material is in progress (Bronowicz, personal commun.) and supposedly this analysis will indicate a semi-aquatic lifestyle, which is consistent with the habitat (Dzik and Sulej, 2007). The advantage is that there is a large amount of P. angustifrons cranial and postcranial material available from this locality (Dzik, 2001; Dzik and Sulej, 2007), similar to the Pseudopalatus material from the Snyder quarry in New Mexico, USA (Zeigler, 2003; Zeigler et al., 2003). In their paper on Apatopus tracks, Padian et al. (2010) concluded that phytosaurs are the likely trackmaker of this ichnotaxon and that they must have been capable of a high walk. Achieving a high walk is the first step towards a terrestrial lifestyle and supports the possibility of a secondarily terrestrial lifestyle. In the case of Apatopus, these tracks were likely produced by Rutiodon, as they are primarily known from New Jersey, and Rutiodon is the only phytosaur known from the eastern United States (Long and Murry, 1995). PHYTOSAUR POSTCRANIAL ANATOMY Humerus (Fig. 5) The humerus of phytosaurs is not very variable. The major variation is in the diaphysis, which is slender in Paleorhinus (Fig. 4A) and Pseudopalatus (Fig. 4D) and thickened in the other phytosaurs. The proximal end of the humerus is similar in all phytosaurs where the humerus is known, except for Nicrosaurus (Fig. 4C), in which it is flattened. All derived phytosaurs have a well-developed crest that covers half of the humerus from the postero-distal end to the middle of the diaphysis. The distal end displays more variation than the proximal end. Paleorhinus, Leptosuchus (Fig. 4B), Pseudopalatus and Nicrosaurus have humeri with a rounded distal end. In contrast, the humerus of Mystriosuchus (Fig. 4E) has a flattened distal end and is thicker overall (more robust) than the other humeri. The humerus of Mystriosuchus is different from that of the other phytosaurs, especially the more massive shape and the flattened top. A more extreme form of this is found in marine reptiles, for example, placodonts, nothosaurs and marine crocodiles. Overall, the variation is smaller than in the hind limb, but it indicates a different lifestyle of Nicrosaurus, Redondasaurus and Mystriosuchus when compared to other phytosaurs. Ilium (Fig. 3) The ilium is known for all phytosaur genera except Angistorhinus talainti (Hunt, 1994) and is one of the most primitive ilia of all archosaurs (Benton and Clark, 1988). Phytosaur ilia are characterized by a low and long, sub-horizontally oriented iliac blade, a horizontal acetabulum and a pubis that attaches to the antero-ventral face. The iliac blade is oriented slightly inwards (medially), as seen in articulated specimens of Angistorhinus (Lucas et al., 2002).

3 308 FIGURE 3. A, Left ilium of Leptosuchus crosbiensis (UCMP 27200). B, Left ilium of Pseudopalatus buceros (NMMNH P-58352). C, Right ilium of Redondasaurus gregorii (NMMNH P-25662). D, Left ilium of Nicrosaurus kapffi (BMNH 38063). Parrish (1987) noted that the ilium of primitive archosaurs is characterized by a shallow, imperforate acetabulum and the lack of any anterior extension of the blade. In contrast, more derived archosaurs have a deeper acetabulum and an anterior extension of the blade. Phytosaurs have this more derived type of ilium (Fig. 3). All phytosaurs have an anterior extension of the iliac blade As can be seen in Figure 3, the more derived phytosaurs (Leptosuchus, Pseudopalatus and Redondasaurus) have a dorso-ventrally compressed ilium, whereas Nicrosaurus has a non-compressed ilium. The ratio of the length of the iliac blade to the width of the ilium is about 1.85:1 in Leptosuchus, Redondasaurus, Pseudopalatus and Angistorhinus. In contrast the ratio in Nicrosaurus is 1.5:1. The ratio is smaller in Erythrosuchus (1.3:1) and Stagonolepis (1.4:1). The ilium of Parasuchus, the most primitive among phytosaurs (Chatterjee, 1978), is characterized by a shorter iliac blade than in all other phytosaurs and no dorso-ventral compression. Indeed, it looks very similar to the ilium of the aetosaur Stagonolepis. The ilium of Angistorhinus, much like Parasuchus, is not dorso-ventrally compressed, but the iliac posterior process is elongated and the tip of the process is ventrally oriented. In Parasuchus, this tip has a dorsal orientation (Chatterjee, 1978). Both genera have a highly-developed acetabular crest that covers half of the acetabulum and shows an elongated anterior process. The ilia of Leptosuchus (Fig. 3A) and Rutiodon (McGregor, 1906) are very similar. Both are dorso-ventrally compressed, and have a slightly convex dorsal margin. The blade is posteriorly elongated and has a short anterior process. Compared with Leptosuchus, the ilium of Pseudopalatus (Fig. 3B) is dorso-ventrally compressed and has a flat ankle between the pubis and the ischium. The ilium of Redondasaurus (Fig. 3C) is similar to that of Pseudopalatus, but in contrast the iliac blade is more robust and has a shorter anterior process. As described by Brusatte et al. (2010), there are three different forms of the dorsal margin of the ilium. The first one is a straight margin, which can be found in Pseudopalatus and Redondasaurus. A convex dorsal margin is known in Angistorhinus, Rutiodon, Leptosuchus and Nicrosaurus, whereas Paleorhinus has a concave and saddle shaped one. In terrestrial archosaurs and archosauriforms the ilium tends to have a straight or convex dorsal margin. Nicrosaurus (Fig. 3D) has the most distinctive ilium of all phytosaurs. Like all derived phytosaurs it is characterized by a posteriorly elongated blade and a short anterior process, but in contrast to the ilia of other phytosaurs it is dorso-ventrally elongated and more closely resembles the ilia of the erythrosuchian Erythrosuchus africanus (Romer, 1923). The angle between the pubis and ischium is steeper than that of Leptosuchus. Due to dorso-ventral elongation the acetabulum is longer than in the other phytosaurs (Fig. 3) and the posterior blade is more massive than in Leptosuchus or Pseudopalatus. The acetabular crest is well developed, but not as strong as in rauisuchians, e.g., Batrachotomus kupferzellensis. Femur (Fig. 4) Parrish (1987) notes that the femur in erect archosaurs developed a medially-directed head, lost the adductor fossa, developed the fourth trochanter on the retractor surface of the femur and developed femoral condyles. This is true for the more derived archosaurs, but basal archosauromorphs such as Proterosuchus did not have these developments and were still able to walk in an erect gait. All formerly analyzed phytosaur femora - Leptosuchus, Rutiodon, Mystriosuchus and Paleorhinus (Parrish, 1986a; Brusatte et al., 2010) are femora with the typical s-shape. This s-shape is also found in extant crocodilians and is common in sprawling and semi-erect animals. More elongated femora indicate an erect gait. For taxa with femoral heads, decreased torsion of the femur correlates with a tendency towards erect gait (Parrish, 1986a). Parrish (1986a) suggested a sprawling or semi-erect locomotion for all phytosaurs because the torsion of the femoral head to the shaft is approximately 70 degrees. By reconsidering the torsion of the femur in phytosaurs a similar result to Brusatte et al.

4 309 FIGURE 4. A, Left femur of Leptosuchus crosbiensis (UCMP 27200) in lateral and medial view. B, Left femur of Pseudopalatus buceros (NMMNH P-56268) in lateral and medial view. C, Right femur of Redondasaurus gregorii (NMMNH P-25665) in lateral and medial view. D, Right femur of Nicrosaurus kapffi (BMNH 38054) in lateral and medial view. Abbreviations: cr, crest; faa, facies articularis antotrochanterica; ftd, fourth trochanter depression; lc, lateral condyle; mc, medial condyle; ve, ventral emargination.

5 310 FIGURE 5. A, Left humerus of Paleorhinus arenaceus (ZPAL AbIII 1516). B, Right humerus of Leptosuchus (UCMP 27094). C, Left humerus of Nicrosaurus kapffi (SMNS unnumbered). D, Left humerus of Pseudopalatus buceros (NMMNH P-20852). E, Left humerus of Mystriosuchus planirostris (SMNS 10260). (2010, character 133) was achieved and suggests that it is less than 45 degrees. The femur of Mystriosuchus planirostris has a thicker shaft and its distal end is more strongly curved than other phytosaur femora. It also demonstrates less torsion. A similar femur is known in the marine crocodile Metriorhynchus. The fibular condyle on phytosaur femora is not present, whereas all more derived members of the Crurotarsi possess it. Terrestrial animals of similar size, i.e., Proterosuchus and Erythrosuchus, are also missing the fibular condyle. This makes it a possible systematic tool, but not a necessity for an erect gait. A very small fourth trochanter can be seen in Paleorhinus, Redondasaurus and Nicrosaurus, but it is not as well developed as in more derived archosaurs. Like the ilium, the femur is known for all phytosaur genera except Angistorhinus, and the femur shows the highest degree of variation of all the postcranial bones of phytosaurs. The femur of Pseudopalatus (Fig. 3B) is very similar to that of Crocodylus niloticus. The most significant difference is a longer crest and a stronger development of the lateral condyle and medial condyle in Crocodylus. Considering the similarity between the two animals and the sediments in which Pseudopalatus is found, a similar lifestyle can be assumed. The facies articularis antotrochanterica shows strong variation in the different phytosaur taxa. The femur of Leptosuchus (Fig. 3A) is characterized by a high and nearly pointed shape and a short tip, whereas Nicrosaurus and Redondasaurus (Fig. 3C) have a high, rounded shape and a short tip. Pseudopalatus has a rounded, low facies articularis antotrochanterica and a long tip. The crest is more strongly developed in Nicrosaurus and Redondasaurus than in the other genera, as are the medial and lateral condyles. In contrast to Leptosuchus and Pseudopalatus, the femora of Redondasaurus and Nicrosaurus (Fig. 3D) show a straighter overall shape. This is not due to deformation, as there is no evidence of it on the specimens. This shape is reminiscent of that of basal terrestrial archosaurs (e.g. Nesbitt et al., 2009). Next to this the torsion in Nicrosaurus was reduced, which is an indication of animals with an erect gait (Parrish, 1986a, 1987). The femur of Mystriosuchus (Gozzi and Renesto, 2003) is very curved, even more so than in Pseudopalatus. The crest is very short, and the facies articularis antotrochanterica is flat and has a long tip (Gozzi and Renesto, 2003). DISCUSSION All derived phytosaurs have an ilium with an elongated blade and a short anterior process, but three basic forms characterize the derived phytosaur ilium. The first one, represented by Pseudopalatus and Redondasaurus, is dorso-ventrally compressed and shows a flat angle between the pubis and the ischium. Leptosuchus and Rutiodon show an intermediate form. Nicrosaurus shows similarities to terrestrial archosaurs, which is less compressed than others and is able to keep the femur closer to the body. Overall, the diversity of form in derived phytosaurs suggests that they adapted better to the lifestyle of the animal and that there must have been differences in the different genera. Three different types of femora characterize phytosaurs: a crocodile-like femur, a much straighter more basal dinosaurian or rauisuchianlike femur and the extremely curved femur of Mystriosuchus. The straighter femur is found in Nicrosaurus and Redondasaurus. This means that the ilium and femur of Nicrosaurus more resemble those of terrestrial archosaurs than those of semi-aquatic archosaurs such as extant crocodilians. In general, the hind-leg morphology gives clues to the lifestyle of animals and suggests different lifestyles in the different genera. Straight shapes of femora and ilia similar to phytosaur ilia are known in aetosaurs and rauisuchians (Long and Murry, 1995; Gower and Schoch, 2009). Both of these animals were terrestrial, and the similarity of postcrania supports a secondary terrestrial lifestyle of Nicrosaurus and Redondasaurus. The different shape of the Mystriosuchus femur from that of all other phytosaurs speaks in favor of a different lifestyle. In addition to the postcranial anatomy, several other arguments

6 speak in favor of a secondary terrestrial lifestyle in Nicrosaurus. The tripartite dentition of Nicrosaurus in combination with the massive skull suggests predation on larger prey: The morphology of the posterior maxillary dentition of Nicrosaurus kapffi is unique among carnivorous archosaurs. It may well indicate a unique mode of food processing among archosaurs, and can be interpreted as an excellent tool for dismembering large prey items (Hungerbühler, 2000, p. 46). As terrestrial vertebrates such as Sellosaurus mainly represent larger prey in the Stubensandstein, Nicrosaurus would have had to wait for the prey as living crocodilians do. This is difficult to explain as the presence of a second definitely semiaquatic to aquatic phytosaur in Mystriosuchus planirostris makes it improbable that two phytosaurs lived in the same environment. If Hungerbühler s taxonomy is considered it would even indicate that four phytosaurs lived in the same environment at the same time (Hungerbühler and Hunt, 2000; Hungerbühler, 2002). SUMMARY Research on phytosaur ecology and locomotion is still in its early stages and it will take a large amount of research on existing and new material to completely understand these animals. Whereas the ecology of the early (Carnian to early Norian) phytosaurs has been analyzed in the past or is being analyzed at the moment, the more derived genera have not had a lot of attention apart from their systematic position. Further investigation including in-depth functional morphology analyses of phytosaurs have to be made to understand the movement of the different species. Also, muscle reconstructions as far as possible will help to understand how far the femur and humerus were flexible to switch into high gait and to what extent a gallop movement might be possible in these animals. Reconstructing the ecology of phytosaurs is complicated, because postcranial material is rarely preserved with the skulls on which the taxonomy is based. Due to this, the material that can be used for postcranial studies is restricted and not always well preserved. 311 The fore- and hind limbs of phytosaurs show the highest adaptation to their environment and speak in favor of three different lifestyles in phytosaurs. The first one is a relatively generalist, semi-aquatic lifestyle that is known from Parasuchus, Paleorhinus, Pseudopalatus and Leptosuchus. The limbs of these four genera resemble those of extant members of the genus Crocodylus and support a similar, semi-aquatic lifestyle. A terrestrial lifestyle is definitely supported in Nicrosaurus and is partly supported for Redondasaurus. Due to the phylogenetic relationships of both genera this secondary terrestrial lifestyle must have developed somewhere between the Late Carnian and Early Norian. This may be due to the aquatic niche having been occupied by a better-developed predator; in the case of Nicrosaurus this could be Mystriosuchus. Overall, the similarities between the ilia and femora of Nicrosaurus and those of other archosaurs represent a less primitive condition than in other phytosaurs. The similarities also suggest a non-sprawling walking style and an erect walking style that has mostly been associated with a terrestrial lifestyle. In contrast to Nicrosaurus and Redondasaurus, the limbs of Mystriosuchus are evidence of a more aquatic lifestyle. This is indicated by a more s-like femur and extremely widened proximal and distal ends compared to the other phytosaurs. As documented by Kimmig and Arp (2010), Mystriosuchus remains are always found in marine or playa lake deposits. This and the fact that the remains are always found far away from the coast also support a fully aquatic lifestyle. As all close phytosaur relatives represent terrestrial animals, a secondary terrestrial lifestyle would certainly represent reversals of the semi-aquatic lifestyle back to a terrestrial lifestyle, whereas the more aquatic lifestyle of Mystriosuchus would represent a more derived state. ACKNOWLEDGMENTS I thank Justin Spielmann and Spencer G. Lucas for their reviews and comments. Sandra Chapman (BMNH), Rainer Schoch (SMNS), Pat Holroyd (UCMP), Daniel Brinkman (YPM), Robert Bronowicz (Warsaw University), Justin Spielmann (NMMNH) and William G. Parker (PEFO) are thanked for access to their collections. REFERENCES Ballew, K.L., 1989, A phylogenetic analysis of Phytosauria from the Late Triassic of the Western United States; in Lucas, S.G., and Hunt, A.P., eds., Dawn of the age of dinosaurs in the American Southwest: New Mexico Museum of Natural History and Science, Albuquerque, p Benton, M.J., and Clark, J.M., 1988, Archosaur phylogeny and the relationships of the Crocodylia; in Benton, M.J. ed., The Phylogeny and Classification of Tetrapods. Volume 1 Amphibians, Reptiles, Birds: Clarendon Press, Oxford, p Brochu, C.A., 2001, Progress and future directions in archosaur phylogenetics: Journal of Paleontology, v. 75, p Brusatte, S.L., Benton, M.J., Desojo, J.B., and Langer, M.C., 2010, The higher-level phylogeny of Archosauria (Tetrapoda: Diapsida): Systematic Palaeontology, v. 8, p Buffetaut, E., 1993, Phytosaurs in time and space: Paleontologia Lombarda, v. 2, p Chatterjee, S., 1978, A primitive parasuchid (phytosaur) reptile from the Upper Triassic Maleri Formation of India: Palaeontology, v. 21, p Doyle, K.D., and Sues, H.D., 1995, Phytosaurs (Reptilia: Archosauria) from the Upper Triassic New Oxford Formation of York County, Pennsylvania: Journal of Vertebrate Paleontology, v. 15, p Dzik, J., 2001, A new Paleorhinus fauna in the early Late Triassic of Poland: Journal of Vertebrate Paleontology, v. 21, p Dzik, J., and Sulej, T., 2007, A review of the early Late Triassic Krasiejów biota from Silesia, Poland: Palaeontologia Polonica, v. 64, p Gower, D.J., and Schoch, R.R., 2009, Postcranial anatomy of the rauisuchian archosaur Batrachotomus kupferzellensis: Journal of Vertebrate Paleontology, v. 29, p Gozzi, E., and Renesto, S., 2003, A complete specimen of Mystriosuchus (Reptilia, Phytosauria) from the Norian (Late Triassic) of Lombardy (Northern Italy): Rivista Italiana Di Paleontologia E Stratigrafia, v. 109, p Guggisberg, C.A.W., 1972, Crocodiles. Their Natural History, Folklore and Conservation: David and Charles (Publishers) Limited, Newton Abbot, 200 p. Heckert, A.B., Lucas, S.G., Hunt, A.P., and Harris, J.D., 2001, A giant phytosaur (Reptilia, Archosauria) skull from the Redonda Formation (Upper Triassic, Apachean) of east-central New Mexico: New Mexico Geological Society, Guidebook 52, p Holliday, C.M., Ridgely, R.C., Sedlmayr, J.C., and Witmer, L.M., 2010, Cartilaginous epiphysis in extant archosaurs and their implications for reconstructing limb function in dinosaurs: PLos ONE, v. 5, e Hungerbühler, A., 2000, Heterodonty in the European phytosaur Nicrosaurus kapfii and its implications for the taxonomic utility and funtional morphology of phytosaur dentitions: Journal of Vertebrate Paleontology, v. 20, p Hungerbühler, A., 2002, The Late Triassic phytosaur Mystriosuchus westphali, with a revision of the genus: Palaeontology, v. 45, p

7 312 Hungerbühler, A., and Hunt, A.P., 2000, Two new phytosaur species (Archosauria, Crurotarsi) from the Upper Triassic of southwest Germany: Neues Jahrbuch für Geologie und Paläontologie. Monatshefte, v. 2000, p Hunt, A.P., 1989, Cranial morphology and ecology among phytosaurs; in Lucas, S.G., and Hunt, A.P., eds., Dawn of the age of dinosaurs in the American Southwest: Albuquerque, New Mexico Museum of Natural History and Science, p Hunt, A.P., 1994, Vertebrate paleontology and biostratigraphy of the Bull Canyon Formation (Chinle Group, Upper Triassic), east-central New Mexico with revisions of the families Metoposauridae (Amphibia: Temnospondyli) and Parasuchidae (Reptilia: Archosauria) [Ph.D. dissertation]: Albuquerque, The University of New Mexico, 404 p. Hutchinson, J.R., 2001, The evolution of femoral osteology and soft tissues on the line to extant birds (Neornithes): Zoological Journal of the Linnean Society, v. 131, p Irmis, R., Nesbitt, S., Padian, K., Smith, N.D., Turner, A.H., Woody, D., and Downs, A., 2007, A Late Triassic dinosauromorph assemblage from New Mexico and the rise of dinosaurs: Science, v. 317, p Kimmig, J., 2009, Functional morphology and systematic palaeontology of the Phytosauria (Archosauria; Crurotarsi) and the development of their Late Triassic habitats [M.S. dissertation]: London, Imperial College London, 118 p. Kimmig, J., and Arp, G., 2010, Phytosaur remains from the Norian Arnstadt Formation (Leine Valley, Germany), with reference to European phytosaur habitats: Palaeodiversity, v. 3, p Long, R.A., and Murry, P.A., 1995, Late Triassic (Carnian and Norian) tetrapods from the southwestern United States: New Mexico Museum of Natural History and Science, Bulletin 4, 254 p. Lucas, S.G., Heckert, A.B., and Kahle, R., 2002, Postcranial anatomy of Angistorhinus, a Late Triassic phytosaur from West Texas: New Mexico Museum of Natural History and Science, Bulletin 21, p Lydekker, R., 1879, Indian pre-tertiary vertebrata, fossil Reptilia and Batrachia: Palaeontologia Indica, 4th series, v. 1, p McGregor, J.H., 1906, The Phytosauria, with special reference to Mystriosuchus and Rhytidodon: Memoirs of the American Musuem of Natural History, v. 9, p Mehl, M.G., 1928, Pseudopalatus pristinus, a new genus and species of phytosaurs from Arizona: University of Missouri Studies, v. 3, p Meyer, H.v., 1861, Reptilien aus dem Stubensandstein des oberen Keupers: Palaeontographica, v. 7, p Nesbitt, S.J., Irmis, R.B., Parker, W.G., Smith, N.D., Turner, A.H., and Rowe, T., 2009, Hindlimb osteology and distribution of basal dinosauromorphs from the Late Triassic of North America: Journal of Vertebrate Paleontology, v. 29, p Padian, K., Li, C., and Pchelnikova, J., 2010, The trackmacker of Apatopus (Late Triassic, North America): Implications for the evolution of archosaur stance and gait: Palaeontology, v. 53, p Parrish, J.M., 1986a, Locomotor adaptations in the hindlimb and pelvis of the Thecodontia: Hunteria, v. 1, p Parrish, J.M., 1986b, Structure and function of the tarsus in the phytosaurs (Reptilia; Archosauria); in Padian, K., ed., The beginning of the age of dinosaurs; faunal change across the Triassic-Jurassic boundary: Cambridge, Cambridge University Press, p Parrish, J.M., 1987, The origin of crocodilian locomotion: Paleobiology, v. 13, p Renesto, S., and Paganoni, A., 1998, A phytosaur skull from the Norian (Late Triassic) of Lombardy (northern Italy): Rivista Italiana Di Paleontologia E Stratigrafia, v. 104, p Romer, A., 1923, The pelvic musculature of saurischian dinosaurs: Bulletin of the American Museum of Natural History, v. 48, p Ross, C.A., and Magnusson, W.E., 1989, Crocodiles and Alligators: New York, Weldon Owen Pty Limited, 240 p. Stocker, M., 2010, A new taxon of phytosaur (Archosauria: Pseudosuchia) from the Late Triassic (Norian) Sonsela Member (Chinle Formation) in Arizona, and a critical reevaluation of Leptosuchus Case, 1922: Palaeontology, v. 53, p Webb, G.J.W., and Gans, C., 1982, Galloping in Crocodylus johnstoni - a reflection of terrestrial activity: Records of the Australian Museum, v. 34, p Zeigler, K.E., 2003, Taphonomic analysis of the Snyder Quarry; a firerelated Upper Triassic vertebrate fossil assemblage from north-central New Mexico: New Mexico Museum of Natural History and Science, Bulletin 24, p Zeigler, K.E., Heckert, A.B., and Lucas, S.G., 2003, An illustrated atlas of the phytosaur (Archosauria, Parasuchidae) postcrania from the Upper Triassic Snyder Quarry (Petrified Forest Formation, Chinle Group): New Mexico Museum of Natural History and Science, Bulletin 24, p

KATE E. ZEIGLER, ANDREW B. HECKERT and SPENCER G. LUCAS. New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, NM

KATE E. ZEIGLER, ANDREW B. HECKERT and SPENCER G. LUCAS. New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, NM Zeigler, K.E., Heckert, A.B., and Lucas, S.G., eds., 2003, Paleontology and Geology of the Snyder Quarry, New Mexico Museum of Natural History and Science Bulletin No. 24. AN ILLUSTRATED ATLAS OF THE PHYTOSAUR

More information

MANDIBLES OF JUVENILE PHYTOSAURS (ARCHOSAURIA: CRUROTARSI) FROM THE UPPER TRIASSIC CHINLE GROUP OF TEXAS AND NEW MEXICO, USA

MANDIBLES OF JUVENILE PHYTOSAURS (ARCHOSAURIA: CRUROTARSI) FROM THE UPPER TRIASSIC CHINLE GROUP OF TEXAS AND NEW MEXICO, USA 228 Tanner, L.H., Spielmann, J.A. and Lucas, S.G., eds., 2013, The Triassic System. New Mexico Museum of Natural History and Science, Bulletin 61. MANDIBLES OF JUVENILE PHYTOSAURS (ARCHOSAURIA: CRUROTARSI)

More information

REVISION OF REDONDASUCHUS (ARCHOSAURIA: AETOSAURIA) FROM THE UPPER TRIASSIC REDONDA FORMATION, NEW MEXICO, WITH DESCRIPTION OF A NEW SPECIES

REVISION OF REDONDASUCHUS (ARCHOSAURIA: AETOSAURIA) FROM THE UPPER TRIASSIC REDONDA FORMATION, NEW MEXICO, WITH DESCRIPTION OF A NEW SPECIES Harris et al., eds., 2006, The Triassic-Jurassic Terrestrial Transition. New Mexico Museum of Natural History and Science Bulletin 37. REVISION OF REDONDASUCHUS (ARCHOSAURIA: AETOSAURIA) FROM THE UPPER

More information

THE LATE TRIASSIC AETOSAUR PARATYPOTHORAX

THE LATE TRIASSIC AETOSAUR PARATYPOTHORAX Harris et al., eds., 2006, The Triassic-Jurassic Terrestrial Transition. New Mexico Museum of Natural History and Science Bulletin 37. THE LATE TRIASSIC AETOSAUR PARATYPOTHORAX 575 SPENCER G. LUCAS 1,

More information

TOPOTYPES OF TYPOTHORAX COCCINARUM, A LATE TRIASSIC AETOSAUR FROM THE AMERICAN SOUTHWEST

TOPOTYPES OF TYPOTHORAX COCCINARUM, A LATE TRIASSIC AETOSAUR FROM THE AMERICAN SOUTHWEST Lucas, S.G. and Spielmann, J.A., eds., 2007, The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41. TOPOTYPES OF TYPOTHORAX COCCINARUM, A LATE TRIASSIC AETOSAUR FROM THE AMERICAN

More information

Are the dinosauromorph femora from the Upper Triassic of Hayden Quarry (New Mexico) three stages in a growth series of a single taxon?

Are the dinosauromorph femora from the Upper Triassic of Hayden Quarry (New Mexico) three stages in a growth series of a single taxon? Anais da Academia Brasileira de Ciências (2017) 89(2): 835-839 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201720160583

More information

New Mexico Geological Society

New Mexico Geological Society New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/56 Vertebrate fauna of the Upper Triassic Mesa Montosa Member (Petrified Forest Formation, Chinle Group), Chama

More information

A GIANT SKULL, ONTOGENETIC VARIATION AND TAXONOMIC VALIDITY OF THE LATE TRIASSIC PHYTOSAUR PARASUCHUS

A GIANT SKULL, ONTOGENETIC VARIATION AND TAXONOMIC VALIDITY OF THE LATE TRIASSIC PHYTOSAUR PARASUCHUS 222 Lucas, S.G. and Spielmann, J.A., eds., 2007, The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41. A GIANT SKULL, ONTOGENETIC VARIATION AND TAXONOMIC VALIDITY OF THE LATE

More information

New Mexico Geological Society

New Mexico Geological Society New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/56 Definition and correlation of the Lamyan: A new biochronological unit for the nonmarine Late Carnian (Late

More information

Lucas, S.G. and Spielmann, J.A., eds., 2007, The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41.

Lucas, S.G. and Spielmann, J.A., eds., 2007, The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41. Lucas, S.G. and Spielmann, J.A., eds., 2007, The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41. BIOSTRATIGRAPHIC UTILITY OF THE UPPER TRIASSIC AETOSAUR TECOVASUCHUS (ARCHOSAURIA:STAGONOLEPIDIDAE),

More information

Postilla PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY NEW HAVEN, CONNECTICUT, U.S.A.

Postilla PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY NEW HAVEN, CONNECTICUT, U.S.A. Postilla PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY NEW HAVEN, CONNECTICUT, U.S.A. Number 117 18 March 1968 A 7DIAPSID (REPTILIA) PARIETAL FROM THE LOWER PERMIAN OF OKLAHOMA ROBERT L. CARROLL REDPATH

More information

Anatomy. Name Section. The Vertebrate Skeleton

Anatomy. Name Section. The Vertebrate Skeleton Name Section Anatomy The Vertebrate Skeleton Vertebrate paleontologists get most of their knowledge about past organisms from skeletal remains. Skeletons are useful for gleaning information about an organism

More information

The Triassic Transition

The Triassic Transition The Triassic Transition The Age of Reptiles Begins As the Paleozoic drew to a close through the Carboniferous and Permian several important processes were at work. Assembly of Pangea Evolutionary radiation

More information

THE FIRST PHYTOSAUR (DIAPSIDA, ARCHOSAURIFORMES) FROM THE LATE TRIASSIC OF THE IBERIAN PENINSULA

THE FIRST PHYTOSAUR (DIAPSIDA, ARCHOSAURIFORMES) FROM THE LATE TRIASSIC OF THE IBERIAN PENINSULA Journal of Vertebrate Paleontology 34(4):970 975, July 2014 2014 by the Society of Vertebrate Paleontology SHORT COMMUNICATION THE FIRST PHYTOSAUR (DIAPSIDA, ARCHOSAURIFORMES) FROM THE LATE TRIASSIC OF

More information

Title: Phylogenetic Methods and Vertebrate Phylogeny

Title: Phylogenetic Methods and Vertebrate Phylogeny Title: Phylogenetic Methods and Vertebrate Phylogeny Central Question: How can evolutionary relationships be determined objectively? Sub-questions: 1. What affect does the selection of the outgroup have

More information

What is a dinosaur? Reading Practice

What is a dinosaur? Reading Practice Reading Practice What is a dinosaur? A. Although the name dinosaur is derived from the Greek for "terrible lizard", dinosaurs were not, in fact, lizards at all. Like lizards, dinosaurs are included in

More information

A short-snouted, Middle Triassic phytosaur and its implications for the morphological

A short-snouted, Middle Triassic phytosaur and its implications for the morphological Supplementary Information for: A short-snouted, Middle Triassic phytosaur and its implications for the morphological evolution and biogeography of Phytosauria Michelle R. Stocker 1* Li-Jun Zhao 2, Sterling

More information

UPPER TRIASSIC TETRAPODS FROM THE LUCERO UPLIFT, CENTRAL NEW MEXICO

UPPER TRIASSIC TETRAPODS FROM THE LUCERO UPLIFT, CENTRAL NEW MEXICO New Mexico Geological Society Guidebook, 50th Field Conference, Albuquerque Geology, 1999 311 UPPER TRIASSIC TETRAPODS FROM THE LUCERO UPLIFT, CENTRAL NEW MEXICO ANDREW B. HECKERT Department of Earth &

More information

TAXONOMY AND BIOSTRATIGRAPHY OF THE LATE TRIASSIC ARCHOSAUROMORPH TRILOPHOSAURUS

TAXONOMY AND BIOSTRATIGRAPHY OF THE LATE TRIASSIC ARCHOSAUROMORPH TRILOPHOSAURUS Lucas, S.G. and Spielmann, J.A., eds., 2007, Triassic of the American West. New Mexico Museum of Natural History and Science Bulletin 40. TAXONOMY AND BIOSTRATIGRAPHY OF THE LATE TRIASSIC ARCHOSAUROMORPH

More information

KRZYZANOWSKISAURUS, A NEW NAME FOR A PROBABLE ORNITHISCHIAN DINOSAUR FROM THE UPPER TRIASSIC CHINLE GROUP, ARIZONA AND NEW MEXICO, USA

KRZYZANOWSKISAURUS, A NEW NAME FOR A PROBABLE ORNITHISCHIAN DINOSAUR FROM THE UPPER TRIASSIC CHINLE GROUP, ARIZONA AND NEW MEXICO, USA Heckert, A.B., and Lucas, S.G., eds., 2005, Vertebrate Paleontology in Arizona. New Mexico Museum of Natural History and Science Bulletin No. 29. KRZYZANOWSKISAURUS, A NEW NAME FOR A PROBABLE ORNITHISCHIAN

More information

Phytosaur remains from the Norian Arnstadt Formation (Leine Valley, Germany), with reference to European phytosaur habitats

Phytosaur remains from the Norian Arnstadt Formation (Leine Valley, Germany), with reference to European phytosaur habitats Palaeodiversity 3: 215 224; Stuttgart 30 December 2010. 215 Phytosaur remains from the Norian Arnstadt Formation (Leine Valley, Germany), with reference to European phytosaur habitats JULIEN KIMMIG & GERNOT

More information

A new basal sauropodiform dinosaur from the Lower Jurassic of Yunnan Province, China

A new basal sauropodiform dinosaur from the Lower Jurassic of Yunnan Province, China SUPPLEMENTARY INFORMATION A new basal sauropodiform dinosaur from the Lower Jurassic of Yunnan Province, China Ya-Ming Wang 1, Hai-Lu You 2,3 *, Tao Wang 4 1 School of Earth Sciences and Resources, China

More information

d a Name Vertebrate Evolution - Exam 2 1. (12) Fill in the blanks

d a Name Vertebrate Evolution - Exam 2 1. (12) Fill in the blanks Vertebrate Evolution - Exam 2 1. (12) Fill in the blanks 100 points Name f e c d a Identify the structures (for c and e, identify the entire structure, not the individual elements. b a. b. c. d. e. f.

More information

A R T I C L E S STRATIGRAPHIC DISTRIBUTION OF VERTEBRATE FOSSIL FOOTPRINTS COMPARED WITH BODY FOSSILS

A R T I C L E S STRATIGRAPHIC DISTRIBUTION OF VERTEBRATE FOSSIL FOOTPRINTS COMPARED WITH BODY FOSSILS A R T I C L E S STRATIGRAPHIC DISTRIBUTION OF VERTEBRATE FOSSIL FOOTPRINTS COMPARED WITH BODY FOSSILS Leonard Brand & James Florence Department of Biology Loma Linda University WHAT THIS ARTICLE IS ABOUT

More information

BEHAVIORAL AND PALEOENVIRONMENTAL IMPLICATIONS OF REPTILE SWIM TRACKS FROM THE EARLY TRIASSIC OF WESTERN NORTH AMERICA

BEHAVIORAL AND PALEOENVIRONMENTAL IMPLICATIONS OF REPTILE SWIM TRACKS FROM THE EARLY TRIASSIC OF WESTERN NORTH AMERICA Tracy Thomson attended the College of Eastern Utah and then received his B.Sc. in geology from the University of Utah. He is currently attending the University of California-Riverside and Dr. Mary Droser

More information

University of Bristol - Explore Bristol Research

University of Bristol - Explore Bristol Research Benton, M. J. (2016). Palaeontology: Dinosaurs, Boneheads and Recovery from Extinction. Current Biology, 26(19), R887-R889. DOI: 10.1016/j.cub.2016.07.029 Peer reviewed version License (if available):

More information

Comparative biomechanical analysis demonstrates functional. convergence between slender-snouted crocodilians and phytosaurs

Comparative biomechanical analysis demonstrates functional. convergence between slender-snouted crocodilians and phytosaurs 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 Comparative biomechanical analysis demonstrates functional convergence between slender-snouted crocodilians and phytosaurs Robert Lemanis 1*,

More information

Origin and Evolution of Birds. Read: Chapters 1-3 in Gill but limited review of systematics

Origin and Evolution of Birds. Read: Chapters 1-3 in Gill but limited review of systematics Origin and Evolution of Birds Read: Chapters 1-3 in Gill but limited review of systematics Review of Taxonomy Kingdom: Animalia Phylum: Chordata Subphylum: Vertebrata Class: Aves Characteristics: wings,

More information

THE TRACKMAKER OF APATOPUS (LATE TRIASSIC, NORTH AMERICA): IMPLICATIONS FOR THE EVOLUTION OF ARCHOSAUR STANCE AND GAIT

THE TRACKMAKER OF APATOPUS (LATE TRIASSIC, NORTH AMERICA): IMPLICATIONS FOR THE EVOLUTION OF ARCHOSAUR STANCE AND GAIT [Palaeontology, Vol. 53, Part 1, 2010, pp. 175 189] THE TRACKMAKER OF APATOPUS (LATE TRIASSIC, NORTH AMERICA): IMPLICATIONS FOR THE EVOLUTION OF ARCHOSAUR STANCE AND GAIT by KEVIN PADIAN, CHENG LI and

More information

Tuesday, December 6, 11. Mesozoic Life

Tuesday, December 6, 11. Mesozoic Life Mesozoic Life Review of Paleozoic Transgression/regressions and Mountain building events during the paleoozoic act as driving force of evolution. regression of seas and continental uplift create variety

More information

8/19/2013. Topic 5: The Origin of Amniotes. What are some stem Amniotes? What are some stem Amniotes? The Amniotic Egg. What is an Amniote?

8/19/2013. Topic 5: The Origin of Amniotes. What are some stem Amniotes? What are some stem Amniotes? The Amniotic Egg. What is an Amniote? Topic 5: The Origin of Amniotes Where do amniotes fall out on the vertebrate phylogeny? What are some stem Amniotes? What is an Amniote? What changes were involved with the transition to dry habitats?

More information

GLOBAL TRIASSIC TETRAPOD BIOSTRATIGRAPHY AND BIOCHRONOLOGY: 2007 STATUS

GLOBAL TRIASSIC TETRAPOD BIOSTRATIGRAPHY AND BIOCHRONOLOGY: 2007 STATUS Lucas, S.G. and Spielmann, J.A., eds., 2007, The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41. GLOBAL TRIASSIC TETRAPOD BIOSTRATIGRAPHY AND BIOCHRONOLOGY: 2007 STATUS 229

More information

THE VERTEBRATE FAUNA OF THE UPPER TRIASSIC CHINLE FORMATION IN NORTHERN ARIZONA

THE VERTEBRATE FAUNA OF THE UPPER TRIASSIC CHINLE FORMATION IN NORTHERN ARIZONA Guidebook to the Triassic Formations of the Colorado Plateau in northern Arizona: Geology, Paleontology, and History. Sterling J. Nesbitt, William G. Parker, and Randall B. Irmis (eds.) Mesa Southwest

More information

Geo 302D: Age of Dinosaurs LAB 4: Systematics Part 1

Geo 302D: Age of Dinosaurs LAB 4: Systematics Part 1 Geo 302D: Age of Dinosaurs LAB 4: Systematics Part 1 Systematics is the comparative study of biological diversity with the intent of determining the relationships between organisms. Humankind has always

More information

A new species of sauropod, Mamenchisaurus anyuensis sp. nov.

A new species of sauropod, Mamenchisaurus anyuensis sp. nov. A new species of sauropod, Mamenchisaurus anyuensis sp. nov. by Xinlu He, Suihua Yang, Kaiji Cai, Kui Li, and Zongwen Liu Chengdu University of Technology Papers on Geosciences Contributed to the 30th

More information

Origin and Evolution of Birds. Read: Chapters 1-3 in Gill but limited review of systematics

Origin and Evolution of Birds. Read: Chapters 1-3 in Gill but limited review of systematics Origin and Evolution of Birds Read: Chapters 1-3 in Gill but limited review of systematics Review of Taxonomy Kingdom: Animalia Phylum: Chordata Subphylum: Vertebrata Class: Aves Characteristics: wings,

More information

A critical re-evaluation of the Late Triassic dinosaur taxa of North America

A critical re-evaluation of the Late Triassic dinosaur taxa of North America Journal of Systematic Palaeontology 5 (2): 209 243 Issued 25 May 2007 doi:10.1017/s1477201907002040 Printed in the United Kingdom C The Natural History Museum A critical re-evaluation of the Late Triassic

More information

Natural Sciences 360 Legacy of Life Lecture 3 Dr. Stuart S. Sumida. Phylogeny (and Its Rules) Biogeography

Natural Sciences 360 Legacy of Life Lecture 3 Dr. Stuart S. Sumida. Phylogeny (and Its Rules) Biogeography Natural Sciences 360 Legacy of Life Lecture 3 Dr. Stuart S. Sumida Phylogeny (and Its Rules) Biogeography So, what is all the fuss about phylogeny? PHYLOGENETIC SYSTEMATICS allows us both define groups

More information

Oct. 2017 ACTA GEOLOGICA SINICA (English Edition) Vol. 91 No. 5 1529 http://www.geojournals.cn/dzxben/ch/index.aspx of Yumenerpeton and that of all the other bystrowianids. On the other hand, the primitive

More information

Eoraptor: Discovery, Fossil Information, Phylogeny, and Reconstructed Life

Eoraptor: Discovery, Fossil Information, Phylogeny, and Reconstructed Life Williams 1 Scott Williams Dr. Parker IFS 2087 Dinosaur Paper 11-7-15 Eoraptor: Discovery, Fossil Information, Phylogeny, and Reconstructed Life Abstract In 1991 Ricardo Martinez found a fossil of a dinosaur

More information

In North America 1. the Triassic is represented by the thick Newark Group along the east coast, 2. by widespread red-bed and fluvial sediments in the

In North America 1. the Triassic is represented by the thick Newark Group along the east coast, 2. by widespread red-bed and fluvial sediments in the The Triassic System The name Triassic derives from the three parts into which the Triassic is divided on the European platform: 3. Keuper (highest) 2. Muschelkalk 1. Bunter (lowest) In North America 1.

More information

New Carnivorous Dinosaurs from the Upper Cretaceous of Mongolia

New Carnivorous Dinosaurs from the Upper Cretaceous of Mongolia 1955 Doklady, Academy of Sciences USSR 104 (5):779-783 New Carnivorous Dinosaurs from the Upper Cretaceous of Mongolia E. A. Maleev (translated by F. J. Alcock) The present article is a summary containing

More information

A BEAKED HERBIVOROUS ARCHOSAUR WITH DINOSAUR AFFINITIES FROM THE EARLY LATE TRIASSIC OF POLAND

A BEAKED HERBIVOROUS ARCHOSAUR WITH DINOSAUR AFFINITIES FROM THE EARLY LATE TRIASSIC OF POLAND Journal of Vertebrate Paleontology 23(3):556 574, September 2003 2003 by the Society of Vertebrate Paleontology A BEAKED HERBIVOROUS ARCHOSAUR WITH DINOSAUR AFFINITIES FROM THE EARLY LATE TRIASSIC OF POLAND

More information

Exceptional fossil preservation demonstrates a new mode of axial skeleton elongation in early ray-finned fishes

Exceptional fossil preservation demonstrates a new mode of axial skeleton elongation in early ray-finned fishes Supplementary Information Exceptional fossil preservation demonstrates a new mode of axial skeleton elongation in early ray-finned fishes Erin E. Maxwell, Heinz Furrer, Marcelo R. Sánchez-Villagra Supplementary

More information

Edinburgh Research Explorer

Edinburgh Research Explorer Edinburgh Research Explorer Superiority, Competition, and Opportunism in the Evolutionary Radiation of Dinosaurs Citation for published version: Brusatte, SL, Benton, MJ, Ruta, M & Lloyd, GT 2008, 'Superiority,

More information

17.2 Classification Based on Evolutionary Relationships Organization of all that speciation!

17.2 Classification Based on Evolutionary Relationships Organization of all that speciation! Organization of all that speciation! Patterns of evolution.. Taxonomy gets an over haul! Using more than morphology! 3 domains, 6 kingdoms KEY CONCEPT Modern classification is based on evolutionary relationships.

More information

Red Eared Slider Secrets. Although Most Red-Eared Sliders Can Live Up to Years, Most WILL NOT Survive Two Years!

Red Eared Slider Secrets. Although Most Red-Eared Sliders Can Live Up to Years, Most WILL NOT Survive Two Years! Although Most Red-Eared Sliders Can Live Up to 45-60 Years, Most WILL NOT Survive Two Years! Chris Johnson 2014 2 Red Eared Slider Secrets Although Most Red-Eared Sliders Can Live Up to 45-60 Years, Most

More information

8/19/2013. Topic 14: Body support & locomotion. What structures are used for locomotion? What structures are used for locomotion?

8/19/2013. Topic 14: Body support & locomotion. What structures are used for locomotion? What structures are used for locomotion? Topic 4: Body support & locomotion What are components of locomotion? What structures are used for locomotion? How does locomotion happen? Forces Lever systems What is the difference between performance

More information

The early fossil record of dinosaurs in North America: a new neotheropod from the base of the Dockum Group (Upper Triassic) of Texas

The early fossil record of dinosaurs in North America: a new neotheropod from the base of the Dockum Group (Upper Triassic) of Texas http://app.pan.pl/som/app60-nesbitt_ezcurra_som.pdf SUPPLEMENTARY ONLINE MATERIAL FOR The early fossil record of dinosaurs in North America: a new neotheropod from the base of the Dockum Group (Upper Triassic)

More information

POSTCRANIAL ANATOMY OF THE RAUISUCHIAN ARCHOSAUR BATRACHOTOMUS KUPFERZELLENSIS

POSTCRANIAL ANATOMY OF THE RAUISUCHIAN ARCHOSAUR BATRACHOTOMUS KUPFERZELLENSIS Journal of Vertebrate Paleontology 29(1):103 122, March 2009 # 2009 by the Society of Vertebrate Paleontology ARTICLE POSTCRANIAL ANATOMY OF THE RAUISUCHIAN ARCHOSAUR BATRACHOTOMUS KUPFERZELLENSIS DAVID

More information

Geo 302D: Age of Dinosaurs. LAB 7: Dinosaur diversity- Saurischians

Geo 302D: Age of Dinosaurs. LAB 7: Dinosaur diversity- Saurischians Geo 302D: Age of Dinosaurs LAB 7: Dinosaur diversity- Saurischians Last lab you were presented with a review of major ornithischian clades. You also were presented with some of the kinds of plants that

More information

Dominique; Bustamante, Rogelio; Cirks, Leah; Lopez, Martin; Moncada, Adriana; Ortega,

Dominique; Bustamante, Rogelio; Cirks, Leah; Lopez, Martin; Moncada, Adriana; Ortega, An unusual archosauromorph tooth increases known archosauromorph diversity in the lower portion of the Chinle Formation (Late Triassic) of southeastern Utah, USA Lopez, Andres; St. Aude, Isabella; Alderete,

More information

Test one stats. Mean Max 101

Test one stats. Mean Max 101 Test one stats Mean 71.5 Median 72 Max 101 Min 38 30 40 50 60 70 80 90 100 1 4 13 23 23 19 9 1 Sarcopterygii Step Out Text, Ch. 6 pp. 119-125; Text Ch. 9; pp. 196-210 Tetrapod Evolution The tetrapods arose

More information

AGE AND CORRELATION OF LATE TRIASSIC TETRAPODS FROM SOUTHERN POLAND

AGE AND CORRELATION OF LATE TRIASSIC TETRAPODS FROM SOUTHERN POLAND Annales Societatis Geologorum Poloniae (2015), vol. 85: 627 635. doi: http://dx.doi.org/10.14241/asgp.2015.024 AGE AND CORRELATION OF LATE TRIASSIC TETRAPODS FROM SOUTHERN POLAND Spencer G. LUCAS New Mexico

More information

Mesozoic reptiles. Benton: Chapters 6 & 8. G404 Geobiology. Department of Geological Sciences Indiana University

Mesozoic reptiles. Benton: Chapters 6 & 8. G404 Geobiology. Department of Geological Sciences Indiana University Mesozoic reptiles Benton: Chapters 6 & 8 Gait of Plateosaurus (Mallison, 2010, Palaeontologia Electronica 13.2.8A) Lab Tomorrow: Please bring laptop computers if you have them. Lab assignment will use

More information

Video Assignments. Microraptor PBS The Four-winged Dinosaur Mark Davis SUNY Cortland Library Online

Video Assignments. Microraptor PBS The Four-winged Dinosaur Mark Davis SUNY Cortland Library Online Video Assignments Microraptor PBS The Four-winged Dinosaur Mark Davis SUNY Cortland Library Online Radiolab Apocalyptical http://www.youtube.com/watch?v=k52vd4wbdlw&feature=youtu.be Minute 13 through minute

More information

AMERICAN NATURALIST. Vol. IX. -DECEMBER, No. 12. OR BIRDS WITH TEETH.1 OI)ONTORNITHES,

AMERICAN NATURALIST. Vol. IX. -DECEMBER, No. 12. OR BIRDS WITH TEETH.1 OI)ONTORNITHES, AMERICAN NATURALIST. Vol. IX. -DECEMBER, 1875.-No. 12. OI)ONTORNITHES, OR BIRDS WITH TEETH.1 BY PROFESSOR 0. C. MARSH. REMAINS of birds are amono the rarest of fossils, and few have been discovered except

More information

Animal Diversity wrap-up Lecture 9 Winter 2014

Animal Diversity wrap-up Lecture 9 Winter 2014 Animal Diversity wrap-up Lecture 9 Winter 2014 1 Animal phylogeny based on morphology & development Fig. 32.10 2 Animal phylogeny based on molecular data Fig. 32.11 New Clades 3 Lophotrochozoa Lophophore:

More information

May 10, SWBAT analyze and evaluate the scientific evidence provided by the fossil record.

May 10, SWBAT analyze and evaluate the scientific evidence provided by the fossil record. May 10, 2017 Aims: SWBAT analyze and evaluate the scientific evidence provided by the fossil record. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: E.3-Examining

More information

Edinburgh Research Explorer

Edinburgh Research Explorer Edinburgh Research Explorer First record of Mesozoic terrestrial vertebrates from Lithuania Citation for published version: Brusatte, SL, Butler, RJ, Niedwiedzki, G, Sulej, T, Bronowicz, R & Nas, JS 2013,

More information

What are taxonomy, classification, and systematics?

What are taxonomy, classification, and systematics? Topic 2: Comparative Method o Taxonomy, classification, systematics o Importance of phylogenies o A closer look at systematics o Some key concepts o Parts of a cladogram o Groups and characters o Homology

More information

ABSTRACT. Candice M. Stefanic and Sterling J. Nesbitt

ABSTRACT. Candice M. Stefanic and Sterling J. Nesbitt The axial skeleton of Poposaurus langstoni (Pseudosuchia: Poposauroidea) and its implications for accessory intervertebral articulation evolution in pseudosuchian archosaurs Candice M. Stefanic and Sterling

More information

New Mexico Geological Society

New Mexico Geological Society New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/54 Tetrapod footprints from the Middle Triassic (Perovkan-Early Anisian) Moenkopi Formation, west-central New

More information

Biology 340 Comparative Embryology Lecture 12 Dr. Stuart Sumida. Evo-Devo Revisited. Development of the Tetrapod Limb

Biology 340 Comparative Embryology Lecture 12 Dr. Stuart Sumida. Evo-Devo Revisited. Development of the Tetrapod Limb Biology 340 Comparative Embryology Lecture 12 Dr. Stuart Sumida Evo-Devo Revisited Development of the Tetrapod Limb Limbs whether fins or arms/legs for only in particular regions or LIMB FIELDS. Primitively

More information

eschweizerbartxxx author

eschweizerbartxxx author N. Jb. Geol. Paläont. Abh. 2009, vol. 252/3, p. 315 325, Stuttgart, June 2009, published online 2009 The oldest record of drepanosaurids (Reptilia, Diapsida) from the Late Triassic (Adamanian Placerias

More information

Animal Form and Function. Amphibians. United by several distinguishing apomorphies within the Vertebrata

Animal Form and Function. Amphibians. United by several distinguishing apomorphies within the Vertebrata Animal Form and Function Kight Amphibians Class Amphibia (amphibia = living a double life) United by several distinguishing apomorphies within the Vertebrata 1. Skin Thought Question: For whom are integumentary

More information

THE TETRAPOD FAUNA OF THE UPPER TRIASSIC LOWER CHINLE GROUP (ADAMANIAN: LATEST CARNIAN) OF THE ZUNI MOUNTAINS, WEST-CENTRAL NEW MEXICO

THE TETRAPOD FAUNA OF THE UPPER TRIASSIC LOWER CHINLE GROUP (ADAMANIAN: LATEST CARNIAN) OF THE ZUNI MOUNTAINS, WEST-CENTRAL NEW MEXICO I Lucas~ S.G., Estep, }.W., Williamson/ T.E. and Morgan, G.S. eds., 1997, New Mexico's Fossil Record 1. New Mexico Museum of Natural History and Science Bulletin No. 11. 29 THE TETRAPOD FAUNA OF THE UPPER

More information

Field Trip: Harvard Museum of Natural History (HMNH)

Field Trip: Harvard Museum of Natural History (HMNH) Field Trip: Harvard Museum of Natural History (HMNH) Objectives To observe the diversity of animals. To compare and contrast the various adaptations, body plans, etc. of the animals found at the HMNH.

More information

PALEONTOLOGICAL CONTRIBUTIONS

PALEONTOLOGICAL CONTRIBUTIONS THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS August, 1965 Paper 2 A NEW WYOMING PHYTOSAUR By THEODORE H. EATON, JR. [Museum of Natural History, University of Kansas I ABSTRACT The skull of a

More information

CROCODILE 28FT - SALTWATER

CROCODILE 28FT - SALTWATER CROCODILE 28FT - SALTWATER 100097 Crocodile 28ft Saltwater L 888 x W 230 x H 100cm - 270kg The Pawlowski Crocodile. This is a reconstruction of the largest crocodile every reliably recorded in Australia,

More information

Evolution of Tetrapods

Evolution of Tetrapods Evolution of Tetrapods Amphibian-like creatures: The earliest tracks of a four-legged animal were found in Poland in 2010; they are Middle Devonian in age. Amphibians arose from sarcopterygians sometime

More information

Lecture 11 Wednesday, September 19, 2012

Lecture 11 Wednesday, September 19, 2012 Lecture 11 Wednesday, September 19, 2012 Phylogenetic tree (phylogeny) Darwin and classification: In the Origin, Darwin said that descent from a common ancestral species could explain why the Linnaean

More information

A NEW RAUISUCHIAN REPTILE (DIAPSIDA: ARCHOSAURIA) FROM THE LATE TRIASSIC OF POLAND

A NEW RAUISUCHIAN REPTILE (DIAPSIDA: ARCHOSAURIA) FROM THE LATE TRIASSIC OF POLAND Journal of Vertebrate Paleontology 25(1):78 86, March 2005 2005 by the Society of Vertebrate Paleontology A NEW RAUISUCHIAN REPTILE (DIAPSIDA: ARCHOSAURIA) FROM THE LATE TRIASSIC OF POLAND TOMASZ SULEJ

More information

2018 SVP Schedule of Events (subject to change) All events are held at the Albuquerque Convention Center unless otherwise noted with an **

2018 SVP Schedule of Events (subject to change) All events are held at the Albuquerque Convention Center unless otherwise noted with an ** 2018 SVP Schedule of Events (subject to change) All events are held at the Albuquerque Convention Center unless otherwise noted with an ** Tuesday, October 16 3:00pm 7:00pm 7:00pm 9:00pm Special Lecture

More information

Biology 1B Evolution Lecture 11 (March 19, 2010), Insights from the Fossil Record and Evo-Devo

Biology 1B Evolution Lecture 11 (March 19, 2010), Insights from the Fossil Record and Evo-Devo Biology 1B Evolution Lecture 11 (March 19, 2010), Insights from the Fossil Record and Evo-Devo Extinction Important points on extinction rates: Background rate of extinctions per million species per year:

More information

Class Reptilia Testudines Squamata Crocodilia Sphenodontia

Class Reptilia Testudines Squamata Crocodilia Sphenodontia Class Reptilia Testudines (around 300 species Tortoises and Turtles) Squamata (around 7,900 species Snakes, Lizards and amphisbaenids) Crocodilia (around 23 species Alligators, Crocodiles, Caimans and

More information

From Slime to Scales: Evolution of Reptiles. Review: Disadvantages of Being an Amphibian

From Slime to Scales: Evolution of Reptiles. Review: Disadvantages of Being an Amphibian From Slime to Scales: Evolution of Reptiles Review: Disadvantages of Being an Amphibian Gelatinous eggs of amphibians cannot survive out of water, so amphibians are limited in terms of the environments

More information

Introduction and methods will follow the same guidelines as for the draft

Introduction and methods will follow the same guidelines as for the draft Locomotion Paper Guidelines Entire paper will be 5-7 double spaced pages (12 pt font, Times New Roman, 1 inch margins) without figures (but I still want you to include them, they just don t count towards

More information

Supplementary Figure 1 Cartilaginous stages in non-avian amniotes. (a) Drawing of early ankle development of Alligator mississippiensis, as reported

Supplementary Figure 1 Cartilaginous stages in non-avian amniotes. (a) Drawing of early ankle development of Alligator mississippiensis, as reported Supplementary Figure 1 Cartilaginous stages in non-avian amniotes. (a) Drawing of early ankle development of Alligator mississippiensis, as reported by a previous study 1. The intermedium is formed at

More information

Tetrapod biostratigraphy and biochronology of the Triassic Jurassic transition on the southern Colorado Plateau, USA

Tetrapod biostratigraphy and biochronology of the Triassic Jurassic transition on the southern Colorado Plateau, USA Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242 256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic Jurassic transition on the southern Colorado

More information

REPTILES. Scientific Classification of Reptiles To creep. Kingdom: Animalia Phylum: Chordata Subphylum: Vertebrata Class: Reptilia

REPTILES. Scientific Classification of Reptiles To creep. Kingdom: Animalia Phylum: Chordata Subphylum: Vertebrata Class: Reptilia Scientific Classification of Reptiles To creep Kingdom: Animalia Phylum: Chordata Subphylum: Vertebrata Class: Reptilia REPTILES tetrapods - 4 legs adapted for land, hip/girdle Amniotes - animals whose

More information

Archived version from NCDOCKS Institutional Repository

Archived version from NCDOCKS Institutional Repository Archived version from NCDOCKS Institutional Repository http://libres.uncg.edu/ir/asu/ Revision of the Archosauromorph Reptile Trilophosaurus, With a Description of the First Skull of Trilophosaurus Jacobsi,

More information

Modern Evolutionary Classification. Lesson Overview. Lesson Overview Modern Evolutionary Classification

Modern Evolutionary Classification. Lesson Overview. Lesson Overview Modern Evolutionary Classification Lesson Overview 18.2 Modern Evolutionary Classification THINK ABOUT IT Darwin s ideas about a tree of life suggested a new way to classify organisms not just based on similarities and differences, but

More information

A NEW SPECIES OF THE AETOSAUR TYPOTHORAX (ARCHOSAURIA:STAGONOLEPIDIDAE) FROM THE UPPER TRIASSIC OF EAST-CENTRAL NEW MEXICO

A NEW SPECIES OF THE AETOSAUR TYPOTHORAX (ARCHOSAURIA:STAGONOLEPIDIDAE) FROM THE UPPER TRIASSIC OF EAST-CENTRAL NEW MEXICO Heckert, A.B., and Lucas, S.G., eds., 2002, Upper Triassic Stratigraphy and Paleontology. New Mexico Museum of Natural History and Science Bulletin No. 21. A NEW SPECES OF THE AETOSAUR TYPOTHORAX (ARCHOSAURA:STAGONOLEPDDAE)

More information

Published online: 04 Nov 2014.

Published online: 04 Nov 2014. This article was downloaded by: [Jerzy Dzik] On: 17 November 2014, At: 03:42 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer

More information

With original illustrations by Brian Regal, Tarbosaurus Studio. A'gJ" CAMBRIDGE UNIVERSITY PRESS

With original illustrations by Brian Regal, Tarbosaurus Studio. A'gJ CAMBRIDGE UNIVERSITY PRESS David E. Fastovsky University of Rhode Island David B. Weishampel Johns Hopkins University With original illustrations by Brian Regal, Tarbosaurus Studio A'gJ" CAMBRIDGE UNIVERSITY PRESS Preface xv CHAPTER

More information

8/19/2013. Topic 4: The Origin of Tetrapods. Topic 4: The Origin of Tetrapods. The geological time scale. The geological time scale.

8/19/2013. Topic 4: The Origin of Tetrapods. Topic 4: The Origin of Tetrapods. The geological time scale. The geological time scale. Topic 4: The Origin of Tetrapods Next two lectures will deal with: Origin of Tetrapods, transition from water to land. Origin of Amniotes, transition to dry habitats. Topic 4: The Origin of Tetrapods What

More information

TRUE SKULL ROOF CONFIGURATION OF ICHTHYOSAURUS AND STENOPTERYGIUS AND ITS IMPLICATIONS

TRUE SKULL ROOF CONFIGURATION OF ICHTHYOSAURUS AND STENOPTERYGIUS AND ITS IMPLICATIONS Journal of Vertebrate Paleontology 25(2):338 342, June 2005 2005 by the Society of Vertebrate Paleontology TRUE SKULL ROOF CONFIGURATION OF ICHTHYOSAURUS AND STENOPTERYGIUS AND ITS IMPLICATIONS RYOSUKE

More information

Giant croc with T. rex teeth roamed Madagascar

Giant croc with T. rex teeth roamed Madagascar Giant croc with T. rex teeth roamed Madagascar www.scimex.org/newsfeed/giant-croc-with-t.-rex-teeth-used-to-roam-in-madagascar Embargoed until: Publicly released: PeerJ A fossil of the largest and oldest

More information

These small issues are easily addressed by small changes in wording, and should in no way delay publication of this first- rate paper.

These small issues are easily addressed by small changes in wording, and should in no way delay publication of this first- rate paper. Reviewers' comments: Reviewer #1 (Remarks to the Author): This paper reports on a highly significant discovery and associated analysis that are likely to be of broad interest to the scientific community.

More information

Skulls & Evolution. 14,000 ya cro-magnon. 300,000 ya Homo sapiens. 2 Ma Homo habilis A. boisei A. robustus A. africanus

Skulls & Evolution. 14,000 ya cro-magnon. 300,000 ya Homo sapiens. 2 Ma Homo habilis A. boisei A. robustus A. africanus Skulls & Evolution Purpose To illustrate trends in the evolution of humans. To demonstrate what you can learn from bones & fossils. To show the adaptations of various mammals to different habitats and

More information

On the Discovery of the earliest fossil bird in China (Sinosauropteryx gen. nov.) and the origin of birds

On the Discovery of the earliest fossil bird in China (Sinosauropteryx gen. nov.) and the origin of birds On the Discovery of the earliest fossil bird in China (Sinosauropteryx gen. nov.) and the origin of birds by Qiang Ji and Shu an Ji Chinese Geological Museum, Beijing Chinese Geology Volume 233 1996 pp.

More information

Today there are approximately 250 species of turtles and tortoises.

Today there are approximately 250 species of turtles and tortoises. I WHAT IS A TURTLE OR TORTOISE? Over 200 million years ago chelonians with fully formed shells appeared in the fossil record. Unlike modern species, they had teeth and could not withdraw into their shells.

More information

Earth-Science Reviews

Earth-Science Reviews Earth-Science Reviews 101 (2010) 68 100 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev The origin and early radiation of dinosaurs Stephen

More information

A NEW ANKYLOSAUR FROM THE UPPER CRETACEOUS OF MONGOLIA E.A. Maleev Doklady Akademii Nauk, SSSR 87:

A NEW ANKYLOSAUR FROM THE UPPER CRETACEOUS OF MONGOLIA E.A. Maleev Doklady Akademii Nauk, SSSR 87: translated by Dr. Tamara and F. Jeletzky, 1956 A NEW ANKYLOSAUR FROM THE UPPER CRETACEOUS OF MONGOLIA E.A. Maleev 1952. Doklady Akademii Nauk, SSSR 87:273-276 Armored dinosaurs make a considerable part

More information

Edinburgh Research Explorer

Edinburgh Research Explorer Edinburgh Research Explorer First record of Mesozoic terrestrial vertebrates from Lithuania Citation for published version: Brusatte, SL, Butler, RJ, Niedwiedzki, G, Sulej, T, Bronowicz, R & Nas, JS 2013,

More information

Sauropterygia. Lepidosauromorpha

Sauropterygia. Lepidosauromorpha Sauropterygia Lepidosauromorpha ***cladogram of lepids*** Pachypleurosauridae Nothosauria Pliosauroidea Plesiosauroidea Mosasauridae Thalattosauriformes? Placodontia Pistosauridae Plesiosauria Sauropterygia

More information

Amniote Relationships. Reptilian Ancestor. Reptilia. Mesosuarus freshwater dwelling reptile

Amniote Relationships. Reptilian Ancestor. Reptilia. Mesosuarus freshwater dwelling reptile Amniote Relationships mammals Synapsida turtles lizards,? Anapsida snakes, birds, crocs Diapsida Reptilia Amniota Reptilian Ancestor Mesosuarus freshwater dwelling reptile Reptilia General characteristics

More information

1/9/2013. Divisions of the Skeleton: Topic 8: Appendicular Skeleton. Appendicular Components. Appendicular Components

1/9/2013. Divisions of the Skeleton: Topic 8: Appendicular Skeleton. Appendicular Components. Appendicular Components /9/203 Topic 8: Appendicular Skeleton Divisions of the Skeleton: Cranial Postcranial What makes up the appendicular skeleton? What is the pattern of serial homology of the limbs? Tetrapod front limb morphology

More information

A new carnosaur from Yongchuan County, Sichuan Province

A new carnosaur from Yongchuan County, Sichuan Province A new carnosaur from Yongchuan County, Sichuan Province by Dong Zhiming Institute of Vertebrate Palaeontology and Palaeoanthropology, Academia Sinica Zhang Yihong, Li Xuanmin, and Zhou Shiwu Chongqing

More information