Sobre uma coluna vertebral de um titanossaurídeo (Dinosauria, Sauropoda) do grupo Bauru, Neocretáceo do Brasil

A new titanosaurid dinosaur from the Late Cretaceous continental deposits of the Bauru Group is described. Trigonosaurus pricei n.gen., n.sp., is based on two specimens, both collected at the Caieira Quarry near Peirópolis, Minas Gerais. The holotype consists of the five most posterior cervical vertebrae, 10 dorsals, six sacrals and the left ilium (MCT 1488-R). The second specimen (paratype) consists of 10 caudal vertebrae that according to a quarry map, were found isolated but show a similar morphology and compatible size suggesting that they belonged to one individual (MCT 1719-R). Trigonosaurus pricei is diagnosed by a combination of characters such as elongated cervicals and middorsals, dorsal vertebrae 9 and 10 with incipient postzygodiapophyseal lamina and transverse processes well developed throughout the sequence formed by anterior and medial caudals. The occurrence of this new taxon indicates a higher diversity of titanosaurids in the Brazil during the Cretaceous period.Um novo titanossaurídeo procedente dos depósitos continentais do grupo Bauru (Neocretáceo) é descrito. Trigonosaurus pricei n.gen., n.sp. é baseado em dois exemplares coletados na localidade Caieira na região de Peirópolis, Minas Gerais. O holótipo é composto das últimas cinco vértebras cervicais, 10 vértebras dorsais, seis sacrais e o ílio esquerdo (MCT 1488-R). O segundo exemplar (parátipo) é formado por 10 vértebras caudais que, de acordo com um mapa da escavação, foram encontradas isoladas, mas apresentam o mesmo padrão morfológico e um tamanho compatível, sendo, deste modo, consideradas como pertencentes a um mesmo indivíduo (MCT 1719-R). Trigonosaurus pricei é diagnosticado por uma combinação de caracteres tais como vértebras cervicais e dorsais médias alongadas, vértebras dorsais 9 e 10 com uma incipiente lâmina diapopós-zigapofisiária e processos transversos bem desenvolvidos por toda seqüência anterior e média da série caudal. A ocorrência deste novo táxon demonstra a existência de uma maior diversidade de titanosaurídeos no Brasil durante o período Cretáceo

Palaeohistology and palaeopathology of an Aeolosaurini (Sauropoda: Titanosauria) from Morro do Cambambe (Upper Cretaceous, Brazil)

Altres ajuts: CAISEP (Comisión de Ayudas a la Investigación de la Sociedad Española de Paleontología) project #2018-07153A recent publication of fossil bones of titanosaurs assigned to Aeolosaurini from the Morro do Cambambe site (Mato Grosso state, Brazil, Upper Cretaceous) reported anomalous growth in some of them. Here, we present osteohistological sections of elements to understand not only the microstructure and growth of such bones, but also the nature of those anomalies. The primary bone of all specimens consisted of a variation of the fibrolamellar complex, with the inner cortex being rich in woven bone with dispersed longitudinal canals, while the outer cortex was parallel-fibred with rows of longitudinal canals, interlayered by Lines of Arrested Growth (LAGs). We identified a maximum of two LAGs in the cervical rib and haemal arch, and four in the dorsal rib. The haemal arch shows an External Fundamental System (EFS) in most sections. The advanced remodelling and variation of the fibrolamellar bone in the cortex suggests that all the specimens represent individuals that reached sexual maturity. However, the haemal arch was distinct due to the wide distribution of EFS. The dorsal rib exhibited periosteal and endosteal outgrowth. Such microstructure was assigned to a reactive bone due to an intra-thoracic infection (a pneumonia, probably related to a tuberculosis), which is the first report in a non-avian dinosaur. The microstructure resembles the medullary bone recovered in dinosaurs, which suggests that further studies of medullary bone in thoracic bones should also regard the pathological cases.En una reciente publicación de los huesos fósiles de titanosaurios asignados al clado Aeolosaurini provenientes del yacimiento de Morro do Cambambe (estado de Mato Grosso, Brasil, Cretácico Superior), se reconocieron anormalidades en el crecimiento de algunos de ellos. En el presente trabajo presentamos cortes osteohistológicos de elementos para entender no sólo la microestructura y crecimiento de los mismos, sino también la naturaleza de aquellas anomalías. Entre ellos, seleccionamos una costilla cervical y una costilla dorsal media posterior, así como un arco hemal. El hueso primario de todos los especímenes comprendía una variación del complejo fibrolamelar, siendo la corteza interna rica en tejido reticular óseo con canales longitudinales dispersos, mientras que la corteza externa tenía fibras paralelas con hileras de canales longitudinales, intercaladas por líneas de crecimiento detenido. Identificamos un máximo de dos líneas de crecimiento detenido tanto en la costilla cervical como en el arco hemal, y cuatro en la costilla dorsal. El arco hemal muestra un Sistema Externo Fundamental en la mayoría de las secciones. La remodelación avanzada y la variación del hueso fibrolamelar en la corteza, se sugiere que todas los especímenes alcanzaron la madurez sexual. Sin embargo, el arco hemal fue distinto debido a la amplia distribución de Sistema Externo Fundamental. Con base en la microestructura, identificamos un semaforonte subadulto, y probablemente a un adulto. La costilla dorsal mostró una excrecencia perióstica y endosteal. Dicha microestructura se ha identificado con un hueso reactivo a una infección intratorácica (una neumonía, probablemente relacionada con una tuberculosis), que es el primer informe de un dinosaurio no aviano. La microestructura se asemeja al hueso medular recuperado en los dinosaurios, lo que sugiere que los estudios posteriores del hueso medular en los huesos torácicos también deberían considerar los casos patológicos

New Crocodyliform specimens from Recôncavo-Tucano Basin (Early Cretaceous) of Bahia, Brazil

ABSTRACT In 1940, L.I. Price and A. Oliveira recovered four crocodyliform specimens from the Early Cretaceous Bahia Supergroup (Recôncavo-Tucano Basin). In the present work, we describe four different fossil specimens: an osteoderm, a fibula, a tibia, and some autopodial bones. No further identification besides Mesoeucrocodylia was made due to their fragmentary nature and the reduced number of recognized synapomorphies for more inclusive clades. With exception of the fibula, all other specimens have at least one particular feature, which with new specimens could represent new species. The new specimens described here increase the known diversity of Early Cretaceous crocodyliforms from Brazil. This work highlights the great fossiliferous potential of Recôncavo-Tucano Basin with regard to crocodyliform remains

Caninemys, a New Side-Necked Turtle (Pelomedusoides: Podocnemididae) from the Miocene of Brazil

Meylan, Peter A., Gaffney, Eugene S., De Almeida Campos, Diogenes (2009): Caninemys, a New Side-Necked Turtle (Pelomedusoides: Podocnemididae) from the Miocene of Brazil. American Museum Novitates 3639: 1-26, DOI: 10.1206/608.1, URL: http://www.bioone.org/doi/abs/10.1206/608.

Hongshanopterus lacustris Wang, Campos, Zhou & Kellner, 2008, sp. nov.

Hongshanopterus lacustris sp. nov. Etymology. The specific name comes from the Latin word lacustris, ‘lacustrine’, in reference to the depositional environment of some layers of the Jiufotang Formation. Holotype. A skull, atlas, axis and three other cervical vertebrae embedded in a shale slab, housed at the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences, Beijing, China (IVPP V 14582; Figs. 1–11). Type locality and horizon. Dapingfang, Chaoyang, western Liaoning, China. Jiufotang Formation, Aptian, Lower Cretaceous (He et al. 2004). Diagnosis. An istiodactylid pterosaur distinguished from all other members of this clade by the following combination of characters: comparative large number of upper teeth (34–38) more than in any other istiodactylid); dentition present until a little over half of the skull length (pm-sq); presence of teeth with the crown distinctively directed posteriorly; pterygoid with a ventral anterolateral directed ridge (Figs. 1–11). Description. Generalities and taphonomy. The specimen, embedded in a beige colored shale slab, is composed of the skull and five isolated cervical vertebrae (including the atlas and axis) that due to their close association are regarded as belonging to the same animal (Fig. 1). The skull can only be seen in palatal view. It was compressed dorsoventrally during the fossilization process, causing a deformation from left to right, with some cranial bones displaced to the left side. Due to this displacement, the internal surface of some elements of the skull roof can be seen inside the choana, subtemporal and postpalatinal fenestrae of the left side (Figs. 2, 3). The atlas-axis complex together with two cervical vertebrae was displaced close to the right anterior tip of the skull. The atlas-axis overlies the posterior part of one cervical vertebra. A fifth cervical vertebra is found posterior to the occipital region of the skull and is not well preserved. The bone surface in most elements is broken in tiny pieces, reminding of the crackled shale of a broken egg, which is commonly observed in pterosaur specimens. This is particularly true for the anterior palatal region that contrasts with the comparatively better preserved bone surface of the posterior portion of the skull (Figs. 4, 5). Based on the observations above, it is not clear if the carcass reached the bottom of the water column as one piece or if it was dismembered somewhere else. In any case, at least part of the neck and the skull of this pterosaur reached the bottom of the water column and remained exposed for some time, with soft tissue rotting away and bones being dismembered and displaced from their original anatomical position (e.g., atlas+ axis and other cervical vertebrae). The disposition of the bones and the fact that the cervical vertebrae were not carried away is suggestive of a low-energy environment. Skull and cranial openings. The skull is long, a typical feature of pterosaurs and terminates in a pointed end, lacking any lateral expansion. The orbit and nasoantorbital fenestra are not visible due to crushing but the left upper and lower temporal fenestra are partially preserved (Figs. 1–3). The upper temporal fenestra is the smallest and judging from the preserved portion is oriented dorsally with a rounded outline. The lower temporal fenestra, although taphonomically deformed, is quite elongated, more than in the Anhangueridae (e.g., Kellner & Tomida 2000) and Pteranodon (Bennett 2001). The choanae are elongated, reaching approximately 27.8% of the skull length measured from the tip of the premaxillae to the posterior margin of the squamosal (pm-sq; see Table 1). They are the largest openings in the palate, with the anterior and part of the lateral margin formed by the palatine and the lateroposterior margin formed by the pterygoid. The choanae are separated from each other by thin vomers. The postpalatinal fenestra is much smaller and shows a rather sub-triangular outline. It is perforated by a developed lateral process of the pterygoid. The interpterygoid opening is well developed. Length from the tip of premaxilla to the squamosal—243.5 Length from quadrate to premaxilla—206.7 Length choana (right side)—67.7 Length premaxilla to the anterior margin of the choana (right side)—119.2 Length of postpalatinal fenestra—26.5 Length of subtemporal fenestra—21.2 Width over quadrates (over the ventral part of the lateral articulation surfaces)—39.8 Premaxilla and maxilla. There is no suture visible between the premaxilla and maxilla and the exact number of premaxillary teeth cannot be established. The anterior portion of the upper jaw is pointed and lacks any lateral expansion (Fig. 4). The tooth bearing margin, better preserved on the left side, is formed by thick bone raised in respect to other palatal elements. The limit of maxilla with the palatine is marked by a deep sulcus, but the posterior boundaries of this bone cannot be established. Based on the presence of a developed sulcus on the medial surface of the right jugal, it is possible that the maxilla sends a posterior ramus that takes part in the lateral margin of the subtemporal fenestra. On the left side there are at least 17 alveoli and possibly two more, indicating the presence of 17 to 19 teeth on each side of the upper jaw (see dentition). The alveoli are elongated anteroposteriorly. They tend to be projected and show thickened borders. The alveoli are overall evenly spaced and the spacing in most cases is larger than the longest axis of the adjacent alveolus. The ventral surface of two elongated bones can be observed inside the left choana (Figs. 2, 3). Based on their position, they are interpreted as the premaxilla and nasal from the right side. This portion of the premaxilla suggests that the nasoantorbital fenestra is well developed. Nasal. A strip-like bone is observed inside the left choana and is interpreted as the right nasal (Figs. 2, 3). This bone contacts the premaxilla ventrolaterally but, despite being elongated, probably did not reach the most anterior portion of the nasoantorbital fenestra. The posterior portion of the nasal cannot be observed. Squamosal. The squamosal is not well preserved (Figs. 2, 3, 6). If forms the lateral margin of the posterior end of the skull, the posterolateral margin of the upper temporal fenestra and the posterodorsal margin of the lower temporal fenestra. The suture between this bone and the jugal is marked by a line on the left side. Jugal. The right jugal is the best preserved of the two and was displaced medially, inside the posterior end of the nasoantorbital fenestra (Figs. 2, 3, 5, 7). The lacrimal process has a broad base, and it is not clear if it thins upward and is posteriorly inclined in the same fashion as observed in other istiodactylids (Wang et al. 2005; Andres & Ji 2006). The right jugal shows a well developed sulcus on the medial surface, possible to receive the jugal ramus of the maxilla. The jugal has a strong postorbital process, which can be seen on the left side. In this region, a small portion of the postorbital is observable. Quadratojugal. The quadratojugal on the left side is better preserved than on the right (Figs. 2, 3, 6). It is a small bone that forms the ventral margin of the lower temporal opening, contacting the jugal dorsally and the quadrate ventrally. On both sides this bone is partially fused with the jugal and the quadrate and only a faint line indicates the sutures. In its ventral portion, the quadratojugal exhibits an odd ‘knob-like’ protuberance positioned close to the quadrate articulation (Fig. 5). The pterodactyloid Dsungaripterus (IVPP V 64045 - 9) also shows a protuberance in this region, but is more developed and placed more ventrally. Quadrate. This bone is well preserved on both sides (Figs. 2, 3, 5). It is a long rod-like element that has a wide base for the mandibular articulation. It sends a thick medial process that articulates with the basipterygoid process of the basisphenoid and the pterygoid. On the right side, the quadrate shows a faint laminar bone, indicating the presence of a shallow embayment (e.g. quadrate flange), such as reported in anhanguerids (Kellner & Tomida 2000) and other more derived pterodactyloids (e.g., Dsungaripterus, Pteranodon, Thalassodromeus). The articulation with the mandible has suffered some compression that has somewhat altered its shape (compare the right and left quadrates on Fig. 7). The better preserved one is the right (Fig. 5). The articulation surface is formed by two concavities separated by a small ridge. The lateral concavity is larger and the medial one very shallow. This is similar to the condition reported in Anhanguera araripensis and Pteranodon (Wellnhofer 1985; Eaton 1910), which differ from the Chinese specimen by having the medial concavity more developed than the lateral one. This structure is commonly called the helical jaw joint (Eaton 1910; Bennett 2001). Apparently the lower jaws of Liaoningopterus (originally regarded as the wing phalanges, Wang & Zhou 2003) also have a helical jaw joint, similar to Anhanguera (Campos & Kellner 1985). Basisphenoid. The occipital region has suffered severely from compression and only some elements can be observed. The best preserved one is the basisphenoid (Figs. 2, 3) that forms a thin and fragile anteriorly directed bony plate. It bears short and broad lateroventrally processes (the basipterygoid processes) that contact the quadrate and the pterygoid. Although it is not possible to establish the exact length of this bone, it appears to be comparatively short. Basioccipital and exoccipital. The basioccipital forms the rounded occipital condyle, and has strong depression below it (Figs. 2, 3, 6). The exoccipital is made of relatively thick bone and forms at least the lower half of the occipital region. An eye-shaped opening is observed on the right side, totally surrounded by this bone. Palatine. The limits between the palatine and the surrounding bones cannot be determined easily in this specimen due to fusion (Figs. 2, 3). The suture with the maxilla is formed by a distinct groove that can be followed until the postpalatinal fenestra. No limits are discernible with the premaxillae or with the vomers. The limits with the pterygoid are also not very clear and in some parts are indicated by a faint groove. The palatine surrounds the anterior part of the choanae and also at least part of the postpalatinal fenestrae but appears not to contact the ectopterygoid. Anteriorly, a palatal ridge starts between the level of the 3 rd and 4 th alveoli (Fig. 4), gets more pronounced at the level of the 10 th alveolus and decreases from there until fading away between the level of the 13 th- 14 th alveoli. Pterygoid. Both pterygoids are relatively well preserved (Figs. 2, 3). They form the posterior margin of the choanae, are unfused and meet at the midline forming two small anteriorly projected processes that are overlain by the vomers. The anteriorly tapering palatinal process forms the lateral margin for over the half length of the choana and part of the medial margin of the postpalatinal fenestra. Posteriorly this bone is connected with the quadrate and basisphenoid. The posterior processes diverge leaving a comparatively wide interpterygoid opening. Laterally this bone shows a well developed process that penetrates the subtemporal fenestra. A well developed anterolaterally directed ridge (Fig. 5), followed by a marked anteroposteriorly directed sulcus can be observed on both pterygoids (Fig. 7). Ectopterygoid. The ectopterygoid is better preserved on the left side. This bone shows a marked sulcus and makes the boundary between the postpalatinal and subtemporal fenestrae (Figs. 2, 3, 7). Vomer. The vomers are thin medial elements that posteriorly join the pterygoids and anteriorly the palatines. They divide the choanae, are thinnest at their middle point and gradually get wider posteriorly and anteriorly (Figs. 2, 3). Teeth. Several alveoli show remains of teeth but only four are preserved enough to be described (Fig. 4, 8). Only part of the crown of the second tooth from the left side (likely from the premaxilla) is preserved indicating that this (and perhaps also the first) was short and more rounded compared to the others. The remaining three are all from the left side: two isolated (possible the fourth and seventh) and the eight, still in the alveolus (Fig. 8). All three teeth are strongly labiolingually compressed with pointed triangular crows. There is no marked constriction separating the crown from the root. The seventh has the crown curved posteriorly. In all these teeth the crown is rather smooth and lacks carinae. As far observation is possible, the roots are subequal in size with the crown. The dentition extends after the anterior margin of the choanae. Cervical Vertebrae. In total, five cervical vertebrae were found (Fig. 1). The atlas and axis were displaced over the posterior end of an anterior cervical (Fig. 9). The atlas is apparently fused to the axis and the limits of those elements cannot be established (Fig. 10). The combined length of the centrum is about 11 mm. There are some broken bone parts anterior to the neural spine of the axis and partially displaced inside the neural canal; it is not clear if they belong to the axis or the atlas. The anterior surface of the atlas shows a well developed rounded concavity that receives the occipital condyle. A blunt knob-like projection is observed on the right anterolateral surface, lateral to the neural canal and might be a region where the neural spine of the atlas is fused to the axis. The axis is a strong element that has a well developed neural spine whose dorsal surface is broken. The postzygapophysis is strong and directed lateroposteriorly. The postexapophyses are also strongly developed. A well developed pneumatic foramen pierces the lateral side of this bone. The remaining cervical vertebrae show basically the same morphology but vary in size. The largest one is in contact with the axis (Fig. 9) and has its lateral right side exposed (length between prezygapophysis and postexapophysis ~ 27 mm). It shows a high spike-like neural spine. The lateral side of the centrum is pierced by an eye-shaped pneumatic foramen. Another cervical vertebra is positioned between the previous ones and the skull and is exposed in ventral view (Fig. 1). It is smaller (length of the centrum = 21.5 mm), clearly procoelic and shows a well developed hypapophysis ventral to the cotyle (Fig. 11). Despite being dorsoventrally compressed, the lateral surfaces show evidence of a pneumatic foramen. The last preserved cervical vertebra is located close to the left rear end of the skull (Fig. 1). It is exposed in dorsal view and is the smallest element of all (estimated length of the centrum = 14 mm). None show evience of cervical ribs.Published as part of Wang, Xiaolin, Campos, Diogenes De Almeida, Zhou, Zhonghe & Kellner, Alexander W. A., 2008, A primitive istiodactylid pterosaur (Pterodactyloidea) from the Jiufotang Formation (Early Cretaceous), northeast China, pp. 1-18 in Zootaxa 1813 on pages 2-8, DOI: 10.5281/zenodo.27434

Hongshanopterus Wang, Campos, Zhou & Kellner, 2008, gen. nov.

<i>Hongshanopterus</i> gen. nov. <p> <b>Etymology.</b> The generic name is derived from the Hongshan culture whose archaeological sites are mainly found in western Liaoning Province and in neighboring southeastern Inner Mongolia. <b>Diagnosis.</b> As for the type species.</p>Published as part of <i>Wang, Xiaolin, Campos, Diogenes De Almeida, Zhou, Zhonghe & Kellner, Alexander W. A., 2008, A primitive istiodactylid pterosaur (Pterodactyloidea) from the Jiufotang Formation (Early Cretaceous), northeast China, pp. 1-18 in Zootaxa 1813</i> on page 2, DOI: <a href="http://zenodo.org/record/274343">10.5281/zenodo.274343</a&gt

A new Abelisauroid from the Upper Cretaceous of Brazil

Although important dinosaur specimens have been recently described from Brazil, the theropod record in this county is still rather scarce, particularly from Cretaceous strata. Here we describe a complete right tibia (MCT 1783-R) from the Marília Formation (Maastrichtian, Bauru Basin) near Peirópolis (Uberaba, Minas Gerais). This is the best theropod specimen recovered from this unit after five decades of collecting. MCT 1783-R shows a well developed cnemial crest with a lobular distal end, that projects significantly above the proximal articular surface, features that are characteristic of the Abelisauroidea. It further shows unique characters such as a marked asymmetry of lateral and medial condyles in posterior view, and a very deep triangular articular face for the astragalus, suggesting that it represents a new taxon.A pesar de que importantes especímenes de dinosaurios de Brasil se han descrito recientemente, el registro de terópodos en este país es todavía bastante escaso, especialmente en los estratos del Cretácico. Aquí reportamos una tibia derecha completa (MCT 1783-R) de la Formación Marília (Maastrichtiano, Cuenca Bauru) en el área de Peirópolis (Uberaba, Minas Gerais). Este es el mejor material de terópodo recuperado de esta unidad en cinco décadas de recolección. MCT 1783-R muestra una cresta cnemial bien desarrollada con un extremo distal lobular, proyectado significativamente por encima de la superficie articular proximal, los cuales son rasgos característicos de Abelisauroidea. Muestra, además, algunas características únicas, como una marcada asimetría de los cóndilos medial y lateral en el lado posterior y una cara triangular articular muy profunda por el astrágalo, sugiriendo que representa un nuevo taxón

<i>Sahitisuchus fluminensis</i> gen. et sp. nov. (MCT 1730-R), in ventral view.

<p>A, photo; B, illustration. For abbreviations see <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0081386#pone-0081386-g001" target="_blank">Figure 1</a>. Scale bar: 100 mm.</p