Virginia Zurriaguz and Jaime Powell

Saltasaurus loricatus is a derived form of sauropod dinosaur from the Upper Cretaceous of northern Argentina. In this work, we expand the information of the presacral vertebral column of Saltasaurus loricatus, including a detailed description of neural laminae, fossae and pneumatic foramina of the neural arch, and establish a comparative analysis with closely related taxa (Neuquensaurus australis and Rocasaurus muniozi). Our data does not support previous phylogenetic hypothesis in which S. loricatus is more closely related to R. muniozi than N. australis. A conservative pattern of distribution of pneumatic foramina in the neural arch of cervical vertebrae cannot be recognized. Although variation in the pneumatic foramina distribution is also present in dorsal vertebrae, these structures are more commonly observed in certain regions (within the postzygapophyseal spinodiapophyseal fossa and spinoprezygapophyseal fossa + prezygapophyseal spinodiapophyseal fossa and in the dorsal border of the spinodiapophyseal lamina). Our data reveal that, despite its value in paleobiological and systematic studies, the presence and distribution pattern of pneumatic foramina in neural arches of presacral vertebrae appears to be underestimated in previous anatomical studies.

Zurriaguz, V. and Powell, J. 2015. New contributions to the presacral osteology of Saltasaurus loricatus (Sauropoda, Titanosauria) from the Upper Cretaceous of northern Argentina. Cretaceous Research 50: 283-300.

 
 
Desde hace unos días, en el laboratorio del MAU, se dio comienzo a la preparación del cráneo completo de un dinosaurio saurópodo titanosaurio. Este dinosaurio fue hallado casi al finalizar la última campaña realizada en la localidad de La Invernada en noviembre del 2014. Por tal motivo, sólo pudo ser retirado solamente su cráneo. El mismo fue hallado completo y articulado en posición natural al cuello del animal. Cuando se realizó su rescate, se pudo comprobar que se encontraba articulado al cuello, del que se llegó a contabilizar unas seis vértebras cervicales articuladas. No obstante, las vértebras continuaban dentro de la roca por lo que se estima que el resto del ejemplar también se ha preservado. Durante el presente año, se espera poder continuar con las excavaciones en La Invernada, teniendo como prioridad este magnífico ejemplar.

Merry Christmas and Happy New Year!!



 Hasta el momento, se sospechaba que los huesos de varios de los ejemplares de saurópodos titanosaurios hallados en la excavación principal en La Invernada, correspondían a una especie ya conocida para la zona, Overosaurus paradasorum. Este hecho revestía relevancia ya que se podría conocer aún mejor a dic...ha especie. No obstante, los nuevos materiales de estos ejemplares que se encuentran bajo preparación en el laboratorio del Museo, están contando una historia diferente. Los huesos están mostrando una serie de características no esperadas, que lo diferencian claramente por lo que finalmente, estos dinosaurios pertenecerían a una nueva especie de titanosaurio, la cual habría convivido con Overosaurus en los mismos niveles de la Formación Bajo de la Carpa, de la cual provienen los materiales recuperados.



Juan Martín Leardi, Lucas E. Fiorelli, and Zulma Gasparini

Fragmentary remains of Microsuchus schilleri (Crocodyliformes: Mesoeucrocodylia) from the Bajo de La Carpa Formation (Santonian, Late Creteceous) of northern Patagonia, Argentina, are decribed and reevaluated taxonomically. The type specimen is an articulated individual with hindlimb and axial remains. Microsuchus has several traits that allow to recognize it as a valid taxon (the presence of bulge lateral to the prezygapophyses of the second sacral vertebra; elongated posterior zeugopodia; proximal caudal centra with triangular cross section). Microsuchus was originally assigned as a goniopholidid based on the platycely of its vertebral centra, a character that is widely distributed among fossil crocodyliforms. A phylogenetical analysis using an expanded data matrix focusing on postcranial data was performed in which Microsuchus and another long-limbed crocodyliform from the same location, Neuquensuchus, were included. Microsuchus is depicted in a politomy as a basal mesoeucrocodylian, with its position as a neosuchian or notosuchian supported by a single synapomorphy on the different most parsimonious trees. Additionaly, Neuquensuchus is well nested among notosuchians, in contrast to previous hypothesis. These findings further increase the crocodyliform diversity of the Bajo de la Carpa Formation and emphasize the relevance of its fauna in studies of the diversification of mesoeucrocodylians and notosuchians. Furthermore, the occurrence of both Microsuchus and Neuquensuchus gives evidence of a basal stock of mesoeucrocodylians with elongated limbs that was not previously reported for northern Patagonia.

Leardi, J.M, Fiorelli, L.E. and Gasparini, Z. 2015.Redescription and reevaluation of the taxonomical status of Microsuchus schilleri (Crocodyliformes: Mesoeucrocodylia) from the Upper Cretaceous of Neuquen, Argentina. Cretaceous Research 52 (2015) 153e166

 


Durante los días 11 y 12 de noviembre, el equipo del MAU (Museo Argentino Urquiza) conjuntamente con personal de la empresa ExxonMobil y un equipo cinematográfico especializado proveniente de Estados Unidos, llevaron adelante escenas de campo y en las instalaciones del museo, para una documental solicitada por dicha empresa. Este documental resume las dos campañas realizadas en el área La Invernada, la cual se ubica a pocos kilómetros al sur de la localidad de Rincón de los Sauces, en el norte de la Provincia de Neuquén, Argentina.


 
Cecilia Apaldetti, Ricardo N. Martinez, Diego Pol and Thibaud Souter

The cranial anatomy of the basal sauropodomorph Coloradisaurus brevis from the upper levels of the Norian Los Colorados Formation is here redescribed and comparisons made based on the holotype skull and mandible. Coloradisaurus brevis is diagnosed by most of the features proposed in the original description and an additional set of autapomorphies, such as presence of circular upper temporal fenestrae, laminae on the ventrolateral margins of a ventral fossa of the basisphenoid and on the ventral region of the parasphenoid, and tab-like medial process at the posteromedial end of the mandible. Coloradisaurus is placed within Massospondylidae, as in recent analyses. This position is supported primarily by postcranial characters, but some cranial features identified in this study provide additional evidence supporting this position (e.g., jugal contribution to the antorbital fenestra, frontal proportionately longer than nasals). However, the cranial anatomy of Coloradisaurus also bears several characters that are shared with plateosaurids (e.g., low mandibular articulation, broad maxillary wall on the anterior margin of antorbital fossa, broad prefrontals, projection of infratemporal fenestra behind the orbit, stepped braincase, robust septum between basipterygoid processes). Thus, Coloradisaurus is interpreted as a massospondylid that has convergently acquired characters that are otherwise only known in plateosaurids, highlighting the conflicting pattern of character distribution among basal sauropodomorphs.

Cecilia Apaldetti, Ricardo N. Martinez, Diego Pol & Thibaud Souter (2014) Redescription of the Skull of Coloradisaurus brevis (Dinosauria, Sauropodomorpha) from the Late Triassic Los Colorados Formation of the Ischigualasto-Villa Union Basin, northwestern Argentina, Journal of Vertebrate Paleontology, 34:5, 1113-1132.

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