Superfamily Gondwanatherioidea
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Mammalia, Dryolestoidea, Meridiolestida) from the Coniacian of Patagonia and New Evidence on Their Early Radiation in South America
AMEGHINIANA - 2012 - Tomo 49 (4): 497 – 504 ISSN 0002-7014 FIRST DRYOLESTOID (MAMMALIA, DRYOLESTOIDEA, MERIDIOLESTIDA) FROM THE CONIACIAN OF PATAGONIA AND NEW EVIDENCE ON THEIR EARLY RADIATION IN SOUTH AMERICA ANALÍA M. FORASIEPI1, 5, RODOLFO A. CORIA2,5, JØRN HURUM3 and PHILIP J. CURRIE4 11CONICET, Museo de Historia Natural de San Rafael, Parque Mariano Moreno s/nº, 5600 San Rafael, Argentina. [email protected] 2CONICET, Subsecretaría de Cultura de Neuquén, Universidad Nacional de Río Negro y Museo Municipal “Carmen Funes”, Av. Córdoba 55, 8318 Plaza Huincul, Argentina. [email protected] 3Natural History Museum, University of Oslo, PO Box 1172, Blindern, NO-0318 Oslo, Norway. [email protected] 4Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada. [email protected] Abstract. We report on a new dryolestoid (Mammalia, Dryolestoidea, Meridiolestida) from the Los Bastos Formation (Coniacian), Neu- quén Province, Patagonia, Argentina, consisting of an edentulous left dentary (MCF-PVPH 412). The alveoli preserved suggest the pre- sence of three incisors, one double-rooted canine, and six double-rooted postcanines (probably three premolars and three molars). Based on comparisons with previously known dentaries and isolated teeth, MCF-PVPH 412 would have been about the same size as Reigitherium Bonaparte. Among Dryolestoidea, MCF-PVPH 412 is assigned to Meridiolestida because there were probably three molars, the roots of the posterior molars are anteroposteriorly compressed, and there is no Meckelian groove. In addition, the penultimate lower premolar would be the largest in the tooth series, which is also true in other meridiolestidans. The position of the mandibular foramen, the probable presence of three premolars, and the outline of the posteroventral part of the jaw suggest affinities with the Mesungulatoidea (e.g., Coloniatherium Rougier, Forasiepi, Hill and Novaceck; Peligrotherium Bonaparte, Van Valen and Kramarz; and Reigitherium). -
Resources Abello, A., Montalvo, C. & Goin, F. 2002
Resources Abello, A., Montalvo, C. & Goin, F. 2002, Marsupiales del Mioceno Superior de Caleufu (La Pampa, Argentina), Ameghiniana 39(4) Agusti, J. & Anton, M. 2002, Mammoths, Sabertooths & Hominids:65 Million Years of Mammalian Evolution in Europe, Columbia University Press, NY Alroy, J. 2002-2003, North American Fossil Mammal Systematics Database-iNet: <http://www.nceas.ucsb.edu/~alroy/nafmsd.html> American Museum of Natural History, 2001-2003, Fossil Database, <http://paleo.amnh.org/fossil/seek.html> American Museum of Natural History, 1994, Mammals & Their Extinct Relatives, American Museum of Natural History, NY Archibald, J. & Averianov, A. 2003, The Late Cretaceous Placental Mammal Kulbeckia, Journal of Vertebrate Paleontology vol 23 #2 Archibald, J. & Averianov, A. 2001,Paranyctoides and allies from the Late Cretaceous of North America and Asia, Acta Palaeontologica Polonica vol 46 #4 Arduini, P. & Teruzzi, G. 1986,Simon & Schusters Guide to Fossils, Simon & Schuster Inc, NY Argot, C. 2004, Evolution of South American mammalian predators (Borhyaenoidea): anatomical & palaeobiological implications, Zoological Journal of the Linnean Society Vol 140 Issue 4 April Argot, C. 2003, Functional adaptations of the Postcranial Skeleton of two Miocene Borhyaenoids (Mammalia, Metatheria), Borhyaena & Prothylacinus, from South America, Palaeontology Vol 46 part 6 Asher, R., McKenna, M., Emry, R., Tabrum, A. & Kron, D. 2002, Morphology & Relationships of Apternodus & other Extinct, Zalambdodont, Placental Mammals, Bulletin of the American Museum of Natural History #273 Astruc, J., Hugueney, M., Escarguel, G., Legendre, S., Rage, J-C., Simon-Coincon, R., Sudre, J. & Sige, B. 2003, Puycelci, a new vertebrate-bearing locality in the Aquitaine molassic basin. Density & continuity of the Paleogene biochronologic record in the Quercy & peripheral basins area, Geobios Vol 36 #6 November-December Averianov, A., Archibald, J. -
Mammals from the Mesozoic of Mongolia
Mammals from the Mesozoic of Mongolia Introduction and Simpson (1926) dcscrihed these as placental (eutherian) insectivores. 'l'he deltathcroids originally Mongolia produces one of the world's most extraordi- included with the insectivores, more recently have narily preserved assemblages of hlesozoic ma~nmals. t)een assigned to the Metatheria (Kielan-Jaworowska Unlike fossils at most Mesozoic sites, Inany of these and Nesov, 1990). For ahout 40 years these were the remains are skulls, and in some cases these are asso- only Mesozoic ~nanimalsknown from Mongolia. ciated with postcranial skeletons. Ry contrast, 'I'he next discoveries in Mongolia were made by the Mesozoic mammals at well-known sites in North Polish-Mongolian Palaeontological Expeditions America and other continents have produced less (1963-1971) initially led by Naydin Dovchin, then by complete material, usually incomplete jaws with den- Rinchen Barsbold on the Mongolian side, and Zofia titions, or isolated teeth. In addition to the rich Kielan-Jaworowska on the Polish side, Kazi~nierz samples of skulls and skeletons representing Late Koualski led the expedition in 1964. Late Cretaceous Cretaceous mam~nals,certain localities in Mongolia ma~nmalswere collected in three Gohi Desert regions: are also known for less well preserved, but important, Bayan Zag (Djadokhta Formation), Nenlegt and remains of Early Cretaceous mammals. The mammals Khulsan in the Nemegt Valley (Baruungoyot from hoth Early and Late Cretaceous intervals have Formation), and llcrmiin 'ISav, south-\vest of the increased our understanding of diversification and Neniegt Valley, in the Red beds of Hermiin 'rsav, morphologic variation in archaic mammals. which have heen regarded as a stratigraphic ecluivalent Potentially this new information has hearing on the of the Baruungoyot Formation (Gradzinslti r't crl., phylogenetic relationships among major branches of 1977). -
First Ornithopod Remains from the Bajo De La Carpa Formation (Santonian, Upper Cretaceous), Northern Patagonia, Argentina
Cretaceous Research 83 (2018) 182e193 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes First ornithopod remains from the Bajo de la Carpa Formation (Santonian, Upper Cretaceous), northern Patagonia, Argentina * Penelope Cruzado-Caballero a, , Leonardo S. Filippi b, Ariel H. Mendez a, Alberto C. Garrido c, d, Ignacio Díaz-Martínez a a Instituto de Investigacion en Paleobiología y Geología (CONICET-UNRN), Av. Roca 1242, General Roca, Río Negro, Argentina b Museo Municipal Argentino Urquiza, Jujuy y Chaco s/n, Rincon de los Sauces, Neuquen, Argentina c Museo Provincial de Ciencias Naturales “Prof. Dr. Juan Olsacher”, Direccion Provincial de Minería, Etcheluz y Ejercito Argentino, Zapala, Neuquen, Argentina d Departamento Geología y Petroleo, Facultad de Ingeniería, Universidad Nacional del Comahue, Buenos Aires 1400, Neuquen, Argentina article info abstract Article history: In the last decades, the Argentinian ornithopod record has been increased with new and diverse bone Received 29 March 2017 remains found along all the Upper Cretaceous. Most of them are very incomplete and represent taxa of Received in revised form different size. As result, the studies about the palaeobiodiversity of the Ornithopoda clade in South 24 July 2017 America are complex. In this paper, new postcranial remains of an indeterminate medium-sized Accepted in revised form 30 July 2017 ornithopod from the Santonian Bajo de la Carpa Formation (Rincon de los Sauces, Neuquen province) Available online 12 August 2017 are presented. They present diagnostic features of the Ornithopoda clade, and several characters that relate them with other Argentinian ornithopods, especially with the medium-sized members of the Keywords: Ornithischia Elasmaria clade sensu Calvo et al. -
From the Adamantina Formation, Bauru Group, Upper Cretaceous of Brazil and the Phylogenetic Relationships of Aeolosaurini
Zootaxa 3085: 1–33 (2011) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2011 · Magnolia Press ISSN 1175-5334 (online edition) A new sauropod (Macronaria, Titanosauria) from the Adamantina Formation, Bauru Group, Upper Cretaceous of Brazil and the phylogenetic relationships of Aeolosaurini RODRIGO M. SANTUCCI1 & ANTONIO C. DE ARRUDA-CAMPOS2 1Universidade de Brasília - Faculdade UnB Planaltina, Brasília-DF, 73300-000, Brazil. E-mail: [email protected] 2Museu de Paleontologia de Monte Alto, Praça do Centenário, s/n. Monte Alto-SP, 15910-000, Brazil. E-mail: [email protected] Table of contents Abstract . 1 Introduction . 2 Historical background . 2 Geological setting . 4 Systematic Palaeontology . 4 DINOSAURIA Owen, 1842 . 4 SAURISCHIA Seeley, 1887 . 4 SAUROPODA Marsh, 1878 . 4 MACRONARIA Wilson and Sereno, 1998. 4 TITANOSAURIFORMES Salgado, Coria and Calvo, 1997b. 4 TITANOSAURIA Bonaparte and Coria, 1993 . 4 AEOLOSAURINI Franco-Rosas, Salgado, Rosas and Carvalho, 2004 . 5 Aeolosaurus Powell, 1987 . 5 Aeolosaurus rionegrinus Powell, 1987 . 5 Aeolosaurus maximus sp. nov. 6 Phylogenetic analysis . 17 Comparison and discussion . 19 Conclusions . 25 Acknowledgements . 25 References . 26 APPENDIX 1. 29 APPENDIX 2. 29 Abstract Remains of a new titanosaur, Aeolosaurus maximus sp. nov., from the Adamantina Formation (Upper Cretaceous), Bauru Group, São Paulo State of Brazil are described. The new species is represented by a single partially articulated skeleton and is characterized by having a well-developed posterior protuberance below the articular area on the anterior and middle haemal arches and a lateral bulge on the distal portion of the articular process of the mid-posterior haemal arches. It shares with other Aeolosaurus species the presence of prezygapophyses curved downward on anterior caudal vertebrae and hae- mal arches with double articular facets set in a concave posterodorsal surface. -
Paleontological Discoveries in the Chorrillo Formation (Upper Campanian-Lower Maastrichtian, Upper Cretaceous), Santa Cruz Province, Patagonia, Argentina
Rev. Mus. Argentino Cienc. Nat., n.s. 21(2): 217-293, 2019 ISSN 1514-5158 (impresa) ISSN 1853-0400 (en línea) Paleontological discoveries in the Chorrillo Formation (upper Campanian-lower Maastrichtian, Upper Cretaceous), Santa Cruz Province, Patagonia, Argentina Fernando. E. NOVAS1,2, Federico. L. AGNOLIN1,2,3, Sebastián ROZADILLA1,2, Alexis M. ARANCIAGA-ROLANDO1,2, Federico BRISSON-EGLI1,2, Matias J. MOTTA1,2, Mauricio CERRONI1,2, Martín D. EZCURRA2,5, Agustín G. MARTINELLI2,5, Julia S. D´ANGELO1,2, Gerardo ALVAREZ-HERRERA1, Adriel R. GENTIL1,2, Sergio BOGAN3, Nicolás R. CHIMENTO1,2, Jordi A. GARCÍA-MARSÀ1,2, Gastón LO COCO1,2, Sergio E. MIQUEL2,4, Fátima F. BRITO4, Ezequiel I. VERA2,6, 7, Valeria S. PEREZ LOINAZE2,6 , Mariela S. FERNÁNDEZ8 & Leonardo SALGADO2,9 1 Laboratorio de Anatomía Comparada y Evolución de los Vertebrados. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina - fernovas@yahoo. com.ar. 2 Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina. 3 Fundación de Historia Natural “Felix de Azara”, Universidad Maimonides, Hidalgo 775, C1405BDB Buenos Aires, Argentina. 4 Laboratorio de Malacología terrestre. División Invertebrados Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 5 Sección Paleontología de Vertebrados. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 6 División Paleobotánica. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Avenida Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina. 7 Área de Paleontología. Departamento de Geología, Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria (C1428EGA) Buenos Aires, Argentina. 8 Instituto de Investigaciones en Biodiversidad y Medioambiente (CONICET-INIBIOMA), Quintral 1250, 8400 San Carlos de Bariloche, Río Negro, Argentina. -
Multituberculate Mammals from the Cretaceous of Uzbekistan
Multituberculate mammals from the Cretaceous of Uzbekistan ZOFIA KIELAN- JAWOROWSKA and LEV A. NESSOV Kielan-Jaworowska, 2. & Nessov, L. A. 1992. Multituberculate mammals from the Cretaceous of Uzbelustan. Acta Palaeontologica Polonica 37, 1, 1- 17. The first western Asian multituberculates found in the Bissekty Formation (Co- niacian) of Uzbekistan are described on the basis of a lower premolar (p4), a fragment of a lower incisor, an edentulous dentary, a proximal part of the humerus and a proximal part of the femur. Uzbekbaatar kizylkumensis gen. et sp. n. is defined as having a low and arcuate p4. possibly without a posterobuccal cusp; it presumably had two lower premolars, as inferred from the presence of a triangular concavity at the upper part of the anterior wall of p4, and p3 less reduced in relation to p4 than in non-specialized Taeniolabidoidea and Ptilodontoidea. Uzbek- baatar is placed in the Cimolodonta without indicating family and infraorder. It might have originated from the Plagiaulacinae or Eobaatarinae. Key words : Multituberculata, Marnmalia, Cretaceous, Coniacian, Uzbekistan. Zofia Kielan-Jaworowska. Paleontologisk Museum, Universitetet i Oslo, Sars Gate 1, N-0562 Oslo, Norway. flec A. Hecoc, kf~cmumym3exnoiL Kopbl, Ca~~m-nemep6ypzc~uiiYnueepcumem, 199 034 Ca~~m-l7emep6ypz,Poccun (Lev A. Nessov, Institute of the Earth Crust, Sankt-Peters- burg University, 199 034 St. Petersburg. Russla]. Introduction The Multituberculata is the first mammalian order to have adapted to herbivorous niches, although many may have been omnivorous (Krause 1982). Known from the Late Triassic to the Early Oligocene (Hahn & Hahn 1983), this order of mammals was dominant throughout the Mesozoic in most of the local faunas studied. -
Masticatory Musculature of Asian Taeniolabidoid Multituberculate Mammals
Masticatory musculature of Asian taeniolabidoid multituberculate mammals PETR P. GAMBARYAN & ZOFIA KIELAN-JAWOROWSKA* Gambaryan, P.P. & Kielan-Jaworowska, 2. 1995. Masticatory musculature of Asian taeniolabidoid multituberculate mammals. Acta Palaeontologica Polonica 40, 1, 45-108. The backward chewing stroke in multituberculates (unique for mammals) resulted in a more anterior insertion of the masticatory muscles than in any other mammal group, including rodents. Multituberculates differ from tritylodontids in details of the masticatory musculature, but share with them the backward masticatory power stroke and retractory horizontal components of the resultant force of all the masticatory muscles (protractory in Theria). The Taeniolabididae differ from the Eucosmodontidae in having a more powerful masticatory musculature, expressed by the higher zygomatic arch with relatively larger anterior and middle zygomatic ridges and higher coronoid process. It is speculated that the bicuspid, or pointed upper incisors, and semi-procumbent, pointed lower ones, characteristic of non- taeniolabidoid mdtitliberculates were used for picking-up and killing insects or other prey. In relation to the backward power stroke the low position of the condylar process was advantageous for most multituberculates. In extreme cases (Sloanbaataridae and Taeniolabididae), the adaptation for crushing hard seeds, worked against the benefit of the low position of the condylar process and a high condylar process developed. Five new multituberculate autapomorphies are rec- ognized: anterior and intermediate zygomatic ridges: glenoid fossa large, flat and sloping backwards (forwards in rodents), arranged anterolateral and standing out from the braincase; semicircular posterior margin of the dentary with condylar process forming at least a part of it; anterior position of the coronoid process; and anterior position of the masseteric fossa. -
New Record of Snakes from the Cretaceous of Patagonia (Argentina)
New record of snakes from the Cretaceous of Patagonia (Argentina) Adriana María ALBINO CONICET, Departamento de Biología, Universidad Nacional de Mar del Plata, Funes 3250, 7600 Mar del Plata (Argentina) [email protected] Albino A. M. 2000. — New record of snakes from the Cretaceous of Patagonia (Argentina). Geodiversitas 22 (2) : 247-253. KEY WORDS Cretaceous, Serpentes, ABSTRACT Madtsoiidae, New remains of snakes from the Late Cretaceous (La Colonia Formation; ?Boidae, Campanian-Maastrichtian) of Argentina increase the record of the earliest incertae sedis, Patagonia, Patagonian snakes. They include the southernmost record of the madtsoiid paleobiogeography. snake Alamitophis, another probable madtsoiid, perhaps a boid, and a snake incertae sedis. MOTS CLÉS RÉSUMÉ Crétacé, serpents, De nouveaux restes de serpents du Crétacé supérieur de Patagonie (Argentine). Madtsoiidae, De nouveaux restes de serpents du Crétacé supérieur (Formation La Colonia ; ?Boidae, Campanien-Maastrichtien) d’Argentine sont décrits. Ils comprennent le incertae sedis, Patagonie, représentant le plus austral du madtsoiidé Alamitophis, un autre probable paléobiogéographie. madtsoiidé, peut-être un Boidae et un serpent incertae sedis. GEODIVERSITAS • 2000 • 22 (2) © Publications Scientifiques du Muséum national d’Histoire naturelle, Paris. www.mnhn.fr/publication/ 247 Albino A. M. 70° 65° 35° s pa ire La Pam s A s o n e u B Neuquen 4 Río Negro CHILE 3 40° 2 1 Chubut 45° N 45° 0 200 km 75 70° 65° 60° FIG. 1. — Localities. 1, eastern slopes between El Buitre Chico and El Buitre hills, La Colonia area, “Comarca Norpatagónica”. Second facies association of the La Colonia Formation (Campanian-Maastrichtian age); 2, Cerro Cuadrado, Arroyo Verde, middle section of the Los Alamitos Formation (Campanian age, Bonaparte 1996); 3-4, other Late Cretaceous Patagonian localities bearing remains of Alamitophis argentinus; 3, El Palomar; 4, Bajo Trapalcó. -
Reassessment of Aeolosaurus Maximus, a Titanosaur Dinosaur from the Late Cretaceous of Southeastern Brazil
Historical Biology An International Journal of Paleobiology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/ghbi20 Reassessment of Aeolosaurus maximus, a titanosaur dinosaur from the Late Cretaceous of Southeastern Brazil Julian C. G. Silva Junior, Agustín G. Martinelli, Fabiano V. Iori, Thiago S. Marinho, E. Martín Hechenleitner & Max C. Langer To cite this article: Julian C. G. Silva Junior, Agustín G. Martinelli, Fabiano V. Iori, Thiago S. Marinho, E. Martín Hechenleitner & Max C. Langer (2021): Reassessment of Aeolosaurus maximus, a titanosaur dinosaur from the Late Cretaceous of Southeastern Brazil, Historical Biology, DOI: 10.1080/08912963.2021.1920016 To link to this article: https://doi.org/10.1080/08912963.2021.1920016 Published online: 29 Apr 2021. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 HISTORICAL BIOLOGY https://doi.org/10.1080/08912963.2021.1920016 ARTICLE Reassessment of Aeolosaurus maximus, a titanosaur dinosaur from the Late Cretaceous of Southeastern Brazil Julian C. G. Silva Junior a,b, Agustín G. Martinelli b,c, Fabiano V. Iorid,e, Thiago S. Marinho b,f, E. Martín Hechenleitner g,h and Max C. Langer a aLaboratório de Paleontologia de Ribeirão Preto, Faculdade de Filosofia, Ciências e Letras de Ribeirão Preto, Universidade de São Paulo, Ribeirão Preto, São Paulo, Brazil; bCentro de Pesquisas Paleontológicas “Llewellyn Ivor Price”, Universidade Federal do Triângulo Mineiro, Uberaba, Peirópolis, Minas Gerais, Brazil; cCONICET-Sección Paleontología De Vertebrados, Museo Argentino De Ciencias Naturales ‘Bernardino Rivadavia’, Buenos Aires, Argentina; dMuseu de Paleontologia Pedro Candolo, Estação Cultura, Praça Farmacêutico Bruno Garisto, Uchoa, São Paulo, Brazil; eMuseu de Paleontologia Prof. -
Aspects of the Microvertebrate Fauna of the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, Southern England
ASPECTS OF THE MICROVERTEBRATE FAUNA OF THE EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OF THE ISLE OF WIGHT, SOUTHERN ENGLAND By STEVEN CHARLES SWEETMAN M.A. (Oxon.) 1980 F.G.S. A thesis submitted in partial fulfilment of the requirements for the award of the degree of Doctor of Philosophy of the University of Portsmouth School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth, PO1 3QL, U.K. April, 2007 0 Disclaimer Whilst registered for this degree, I have not registered for any other award. No part of this work has been submitted for any other academic award. 1 Acknowledgements At inception of this project there was a significant risk that the Wessex Formation would not yield a microvertebrate fauna. I would, therefore, like to express special thanks to Dave Martill (University of Portsmouth) for his initial support and for securing the research scholarship which made this study possible. I would also like to thank him for his supervision, generous support, encouragement and advice thereafter. Special thanks also to Susan Evans (UCL) for her enthusiastic help and advice on all matters relating to microvertebrates in general, and lizards in particular, and to Jerry Hooker (NHM) for everything relating to mammals; also to Brian Gasson for his support in the field and for the generous donation of many exceptional specimens from his private collection. The broad scope of this study has engendered the help, support and advice of many others and I am grateful to all. At the University -
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Reu. Mus. Argentino C~enc.Nat., n.s. 6(2): 257-305,2004 Buenos A~rca,ISSN 1514-5158 Late Cretaceous vertebrates from Bajo de Santa Rosa (Alien Formation), Rio Negro province, Argentina, with the description of a new sauropod dinosaur ('ll'itanosauridae) Agustin G. MARTINELLI' & Analfa M. FORASIEPI' " 'Museu Argentino de Ciencias Naturales -Bernirrdino Rivadavia., Av A. Gallardo 470, C1405D.m Bilenos Aires, Argentina. [email protected]. zl)epartment of Anatomical Sciences and Neurobioloa, University of Louisville. I,ouisvillo, Kentucky (40292), IJSA, [email protected] ,4bstraet: A large and diverse collection of vertebrate remains from the Campanian-Maastrichtian Allen For- mation (Malargiie Group) at the Bajo de Santa Rosa locality (Rio Negro Province, Argentina) is described hore. The vertebrates arc represented hv: chondrichthvans: di~iomvstidsiluriform. le~isosteid,cf oercichthvid and titanosaurid dinosaurs. A now small salt,asaurinetit&saurid, I3onatitan reigigen. el sp. no"., is described. It is diagnosed by the following association of characters: 1) longitudinal groovo located an the suture between pari- otals that continues posteriorly over the supraoccipital to the foramen magnum; 2) basisphcnoid tubera long and narrow; 3) dorsalto middle caudal vertebrae with deep oval to circular pits present on both sides of the prespinal lamina; 4) anterior caudal vertebra with spino-postzygapophysiat and spino-prezygapophysiai lami- nae; 5) neural arch of anterior caudals with deep interzygapophysial fossae with numerous pits; 6) anterior caudal vertebra with an accessom sub-horizontal lamina extendine" from the antero-ventral oortion of the postzygapophysis to the mid-portion of tho spino-prezygapophysial lamina; and finally, 7) anterior caudal verto- bra with a prominent axial crest on the ventral surftaee of tho cerntrum.