New Early Cretaceous Multituberculate Fossils from the Iberian Peninsula
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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). -
Replica a Los Comentarios De Canudo Et Al. a «Asociacion
Estudios Geol., 60: 53-59 (2004) REPLICA A LOS COMENTARIOS DE CANUDO ET AL. A «ASOCIACION FAUNISTICA DE VERTEBRADOS MESOZOICOS DE LA LOCALIDAD DE GALVE (TERUEL)>> [ESTUDIOS GEOL., 58 (2002), 189-193] B. Sánchez Hernández * Una vez analizados los Comentarios a mi artículo lizó en el año 1958, difícilmente pudo llevarse a realizados por Canudo, Ruiz-Omeñaca, Barco, cabo el trabajo de campo, selección del área correc Cuenca-Bescós y Royo, sorprende el exceso de celo ta de prospección, estudio del material hallado y para descalificar un artículo que nunca pretendió excavación de la zona atendiendo a los resultados otra cosa -como se especifica claramente en su de las etapas anteriores señaladas, estudio del mate introducción- que ser una actualización temporal rial hallado, redacción del artículo y publicación de de la «Lista faunística de los vertebrados de Galve éste en ese mismo año. Parece razonable que todo (Teruel)>> realizada por los investigadores Buscalio ese trabajo le llevara un poco más de tiempo, posi ni y Sanz (1987). En esta publicación se pretende blemente años. Cabe señalar que algunos de estos clarificar algunas afirmaciones contenidas en dichos mismos autores aceptaban fechas aún anteriores Comentarios. para esa actividad, como se puede comprobar en la Guía del Parque Paleontológico de Galve (Teruel), cuyos autores son J. 1. Canudo, G. Cuenca Bescós y Fecha de inicio del estudio de los yacimientos de J. 1. Ruiz Omeñaca (1996), en donde señalan «Este Galve yacimiento (el de Las Zabacheras) lo encontró José María (se refieren a D. José M.ª Herrero, antiguo Canudo et al. afirman que es incorrecta mi afir propietario de la colección Herrero donada al mación del comienzo de los estudios sobre los Museo de Galve) a la orilla de la carretera de depósitos de Galve a principios del siglo xx, así entrada al pueblo, construida sobre el año 1934, y como la fecha de 1950 para el comienzo de las cuyo trazado cortó el yacimiento y cuantos materia excavaciones. -
La Cantalera: an Exceptional Window Onto the Vertebrate Biodiversity of the Hauterivian-Barremian Transition in the Iberian Peninsula
ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 36 (2) 2010: 205-224 doi:10.5209/rev_JIGE.2010.v36.n2.8 La Cantalera: an exceptional window onto the vertebrate biodiversity of the Hauterivian-Barremian transition in the Iberian Peninsula La Cantalera: una excepcional ventana a la biodiversidad del tránsito Hauteriviense- Barremiense en la Península Ibérica J.I. Canudo1, J.M. Gasca1, M. Aurell2, A. Badiola1, H.-A. Blain3, P. Cruzado-Caballero1, D. Gómez- Fernández1, M. Moreno-Azanza1, J. Parrilla1, R. Rabal-Garcés1, J. I. Ruiz-Omeñaca1,4 1Grupo Aragosaurus (http://www.aragosaurus.com). Universidad de Zaragoza. 50009 Zaragoza, Spain. [email protected], [email protected], [email protected], [email protected], [email protected], [email protected], [email protected] 2Estratigrafía. Universidad de Zaragoza. 50009 Zaragoza. Spain. [email protected] 3Institut Català de Paleoecologia Humana y Evolució Social (Unitat asociada al CSIC). Universitat Rovira i Virgili. 43005 Tarragona. Spain. [email protected] 4Museo del Jurásico de Asturias (MUJA). 33328 Colunga. Asturias. Spain. [email protected] Received: 15/11/09 / Accepted: 30/06/10 Abstract La Cantalera is an accumulation site for fossil vertebrates consisting mainly of teeth and isolated postcranial remains. It has the greatest vertebrate biodiversity of any site from the Hauterivian-Barremian transition in the Iberian Peninsula. Up to now, 31 vertebrate taxa have been recognized: an osteichthyan (Teleostei indet.), two amphibians (Albanerpetonidae indet. and Discoglos- sidae indet.), a chelonian (Pleurosternidae? indet.), a lizard (Paramacellodidae? indet.), four crocodylomorphs (cf. Theriosuchus sp., Bernissartiidae indet., Goniopholididae indet., cf. -
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. -
Teruel, Spain)
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/232388110 A systematic reassessment of Early Cretaceous multituberculates from Galve (Teruel, Spain) Article in Cretaceous Research · February 2011 DOI: 10.1016/j.cretres.2010.10.003 CITATIONS READS 12 34 3 authors: Ainara Badiola José Ignacio Canudo Universidad del País Vasco / Euskal Herriko… University of Zaragoza 15 PUBLICATIONS 109 CITATIONS 430 PUBLICATIONS 3,138 CITATIONS SEE PROFILE SEE PROFILE Gloria Cuenca-Bescós University of Zaragoza 300 PUBLICATIONS 4,166 CITATIONS SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: José Ignacio Canudo letting you access and read them immediately. Retrieved on: 29 July 2016 Author's personal copy Cretaceous Research 32 (2011) 45e57 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A systematic reassessment of Early Cretaceous multituberculates from Galve (Teruel, Spain) Ainara Badiola*, José Ignacio Canudo, Gloria Cuenca-Bescós Grupo Aragosaurus-IUCA,1 Paleontología, Facultad de Ciencias, Universidad de Zaragoza, Pedro Cerbuna 12, E-50009 Zaragoza, Spain article info abstract Article history: This paper includes a systematic reassessment of the Early Cretaceous (late Hauterivianeearly Barre- Received 19 April 2010 mian) multituberculate fossils of Galve (Teruel, Spain), previously studied by Crusafont-Pairó and Adr- Accepted in revised form 1 October 2010 over, and Crusafont-Pairó and Gibert in 1966 and 1976, respectively, as well the study of other Available online 4 November 2010 unpublished specimens found in the revised collection of Institut Català de Paleontologia (ICP). We here include for the first time the emended descriptions and comparisons as well as the SEM photographs of Keywords: all the specimens found in the collection and update the biostratigraphic data that they have provided. -
The Earliest Mammal of the European Paleocene: the Multituberculate Hainina
J. Paleont., 74(4), 2000, pp. 701–711 Copyright ᭧ 2000, The Paleontological Society 0022-3360/00/0074-0701$03.00 THE EARLIEST MAMMAL OF THE EUROPEAN PALEOCENE: THE MULTITUBERCULATE HAININA P. PELA´ EZ-CAMPOMANES,1 N. LO´ PEZ-MARTI´NEZ,2 M.A. A´ LVAREZ-SIERRA,2 R. DAAMS3 1Department Paleobiologı´a,Museo Nacional de Ciencias Naturales, Gutie´rrez Abascal 2, 28006 Madrid, Spain, Ͻ[email protected]Ͼ, and 2Department-UEI Paleontologı´a, Facultad C. Geolo´gicas-Instit. Geologı´a Econo´mica,Universidad Complutense-CSIC, 28040 Madrid, Spain ABSTRACT—A new species of multituberculate mammal, Hainina pyrenaica n. sp. is described from Fontllonga-3 (Tremp Basin, Southern Pyrenees, Spain), correlated to the later part of chron C29r just above the K/T boundary. This taxon represents the earliest European Tertiary mammal recovered so far, and is related to other Hainina species from the European Paleocene. A revision of the species of Hainina allows recognition of a new species, H. vianeyae n. sp. from the Late Paleocene of Cernay (France). The genus is included in the family Kogaionidae Ra˜dulescu and Samson, 1996 from the Late Cretaceous of Romania on the basis of unique dental characters. The Kogaionidae had a peculiar masticatory system with a large, blade-like lower p4, similar to that of advanced Ptilodon- toidea, but occluding against two small upper premolars, interpreted as P4 and P5, instead of a large upper P4. The endemic European Kogaionidae derive from an Early Cretaceous group with five premolars, and evolved during the Late Cretaceous and Paleocene. The genus Hainina represents a European multituberculate family that survived the K/T boundary mass extinction event. -
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 -
ART. El Material Tipo De La
Ortiz-Jaureguizar, E. and Pascual, R. , 2011. The tectonic setting of the Caribbean region and the K/T turnover of the South American land-mammal fauna . Boletín Geológico y Minero, 122 (3): 333-344 ISSN: 0366-0176 The tectonic setting of the Caribbean region and the K/T turnover of the South American land-mammal fauna E. Ortiz-Jaureguizar (1) and R. Pascual (2) (1) LASBE (Laboratorio de Sistemática y Biología Evolutiva), Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s/n, B1900FWA La Plata, Argentina. [email protected] (2) División Paleontología Vertebrados, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s/n, B1900FWA La Plata, Argentina. [email protected] ABSTRACT According to the fossil record, a biotic interchange of land vertebrates ( e.g. booid snakes, dinosaurs and mammals) occurred between the Americas during the Late Cretaceous-Early Palaeocene. The arrival of North American immigrants (particularly marsupials and placentals) during the latest Cretaceous-earliest Palaeocene had a profound influence on the composition of the South American mammal commu - nities. During the Late Cretaceous these communities were dominated by native groups of Pangeic lineages, which represented more than 95% of the known genera, but during the Early Palaeocene 70% of South American mammals were derived from North American immi - grants that had arrived during the Late Cretaceous-earliest Palaeocene, and by the Late Palaeocene all the South American mammals (with the possible exception of the xenarthrans) were descendants of these North American immigrants. In spite of the fact that no geological evidence is currently available to support the existence of a continuous land connection between the Americas during the Late Cretaceous- early Palaeocene, the fossil record is substantial enough to point to a temporary inter-American connection that permitted the beginning of a land-mammal exchange by the end of the Cretaceous. -
Paleocene Mammalian Biostratigraphy of the Carbon Basin, Southeastern Wyoming, and Age Constraints on Local Phases of Tectonism
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 5-1998 Paleocene Mammalian Biostratigraphy of the Carbon Basin, Southeastern Wyoming, and Age Constraints on Local Phases of Tectonism Ross Secord University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Secord, Ross, "Paleocene Mammalian Biostratigraphy of the Carbon Basin, Southeastern Wyoming, and Age Constraints on Local Phases of Tectonism" (1998). Papers in the Earth and Atmospheric Sciences. 170. https://digitalcommons.unl.edu/geosciencefacpub/170 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Paleocene mammalian biostratigraphy of the Carbon Bash, southeastern woming, and age constraints on local phases of tectonism Ross Secord Department of Geology and Geophysics, The University of Wyoming, Laramie, Wyoming 82071-3006, U.S.A. ABSTRACT Mammalian fossils from two principal collecting areas in the lower Hanna Formation of the Carbon Basin comprise three faunas, the Grayson Ridge, Halfway Hill, and Sand Creek faunas. The Grayson Ridge and Halfway Hill faunas are diverse, consisting cumulatively of 29 mammalian species, at least two of which are new. The faunas are approximately equivalent in age and are either latest lbrrejonian or earliest Tiffanian, or possibly sample both NALMAs. In any event, the faunas are very close in age to the lbrrejonian-Tiffanian boundary. -
New Multituberculate Teeth from the Early Cretaceous of Morocco
New multituberculate teeth from the Early Cretaceous of Morocco GERHARD HAHN and RENATE HAHN Hahn, G. and Hahn, R. 2003. New multituberculate teeth from the Early Cretaceous of Morocco. Acta Palaeontologica Polonica 48 (3): 349–356. Three new multituberculate teeth are described from the Early Cretaceous of Morocco. Denisodon moroccensis gen. et sp. nov. is established for a second lower molar which differs from that of Hahnodon taqueti, from the same locality, by a preserved posterior buccal cusp, a smaller posterior lingual cusp and the less indented lingual wall of the crown. The sec− ond tooth is a posterior upper premolar. It is represented by the posterior portion of its crown on which is present only one row of cusps, similar to the conditions in Kielanodon, Eobaatar, Bolodon, and the Pinheirodontidae. The third tooth is a lower incisor, similar to that in Kuehneodon. Both teeth are grouped as „Hahnodontidae, gen. et sp. indet.” Paulchof− fatioidea new superfamily is established for the Paulchoffatiidae, Hahnodontidae, and Pinheirodontidae. It is character− ized by the following autapomorphies: premolarisation of I2−C, presence of a third row of cusps on the posterior upper premolars and the basin−like structure of the m2. Hahnodontidae and Hahnodon are redefined. Key words: Mammalia, Multituberculata, Paulchoffatioidea, Denisodon, Early Cretaceous, Morocco. Gerhard Hahn and Renate Hahn [[email protected]], Berliner Strasse 31, D−35282 Rauschenberg; Germany. Introduction Anoual fauna stands in stark contrast to their abundance in penecontemporaneous Laurasian faunas. Usually, remains Remains of multituberculates are very rare fossils in the of multituberculates are, as rodents today, abundant in the Gondwana area. -
New Tribosphenic Mammals from the Mussentuchit Local Fauna (Cedar Mountain Formation, Cenomanian), Utah, Usa
NEW TRIBOSPHENIC MAMMALS FROM THE MUSSENTUCHIT LOCAL FAUNA (CEDAR MOUNTAIN FORMATION, CENOMANIAN), UTAH, USA RICHARD L. CIFELLI, JOSHUA E. COHEN, and BRIAN M. DAVIS Cifelli, R.L., Cohen, J.E., and Davis, B.M. 2016. New tribosphenic mammals from the Mussentuchit Local Fauna (Cedar Mountain Formation, Cenomanian), Utah, USA. Palaeontologia Polonica 67, 67–81. LSID urn:lsid:zoobank.org:pub:C7A0F8DD-F04A- 467C-8E45-3BFABDEEC6F5 Herein we describe two new tribosphenic mammals from the Cedar Mountain Formation of Emery County, Utah, USA. The fossils occur in a narrow stratigraphic interval near the top of the unit (Mussentuchit Member) and date to approximately the Early–Late Cretaceous boundary (early Cenomanian, ~97 Mya). The specimens were recovered from screen-wash- ing bulk rock samples. Both taxa are based on isolated teeth; from the limited morphology represented, both lack obvious specializations of the two major therian groups, Metatheria and Eutheria, and for present purposes they are regarded as basal tribosphenidans. Dakotadens pertritus sp. n. is the more abundant of the two and is closely related to a previously known species from the overlying (upper Cenomanian) Naturita Formation. Culicolestes kielanae gen. et sp. n. is notable in its large size (similar to Pariadens mckennai from the same fauna) relative to most other pre-Campanian tribosphenidans. The mammals of the Mussentuchit Local Fauna, now fully described on the basis of available fossils, represent one of the most diverse assemblages known from the Mesozoic, including some 22 taxa. Tribosphenidans, however, are neither abundant nor diverse, and include only six recognized species; most Late Cretaceous assemblages of North America include twice as many. -
Mammalia, Multituberculata) from Near Calgary, Southwestern Alberta, Canada
Canadian Journal of Earth Sciences First mammal from the Willow Creek Formation: a new, early Paleocene ptilodontid (Mammalia, Multituberculata) from near Calgary, southwestern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2020-0151.R2 Manuscript Type: Article Date Submitted by the 26-Jan-2021 Author: Complete List of Authors: Scott, Craig S.; Royal Tyrrell Museum of Palaeontology, Preservation and Research Keyword: Multituberculate,Draft Paleocene, Puercan, Alberta, Willow Creek Formation Is the invited manuscript for consideration in a Special Not applicable (regular submission) Issue? : © The Author(s) or their Institution(s) Page 1 of 58 Canadian Journal of Earth Sciences 1 First mammal from the Willow Creek Formation: a new, early Paleocene ptilodontid 2 (Mammalia, Multituberculata) from near Calgary, southwestern Alberta, Canada 3 4 Craig S. Scott 5 6 Royal Tyrrell Museum of Palaeontology, P. O. Box 7500, Drumheller, Alberta, T0J 0Y0, 7 CANADA 8 Ph: 403-820-6219 9 Fax: 403-823-7131 10 [email protected] 11 Draft 12 13 14 15 16 17 18 19 20 21 22 23 1 © The Author(s) or their Institution(s) Classification: Protected A Canadian Journal of Earth Sciences Page 2 of 58 24 First mammal from the Willow Creek Formation: a new, early Paleocene ptilodontid 25 (Mammalia, Multituberculata) from near Calgary, southwestern Alberta, Canada 26 27 Craig S. Scott 28 29 Abstract: 30 Although multituberculates are among the best-represented mammals of the Late Cretaceous and 31 early Paleogene in North America, their evolution during the first several tens to hundreds of 32 thousands of years following the Cretaceous-Paleogene (K-Pg) impact event is largely obscure.