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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). -
The Oldest Platypus and Its Bearing on Divergence Timing of the Platypus and Echidna Clades
The oldest platypus and its bearing on divergence timing of the platypus and echidna clades Timothy Rowe*†, Thomas H. Rich‡§, Patricia Vickers-Rich§, Mark Springer¶, and Michael O. Woodburneʈ *Jackson School of Geosciences, University of Texas, C1100, Austin, TX 78712; ‡Museum Victoria, PO Box 666, Melbourne, Victoria 3001, Australia; §School of Geosciences, PO Box 28E, Monash University, Victoria 3800, Australia; ¶Department of Biology, University of California, Riverside, CA 92521; and ʈDepartment of Geology, Museum of Northern Arizona, Flagstaff, AZ 86001 Edited by David B. Wake, University of California, Berkeley, CA, and approved October 31, 2007 (received for review July 7, 2007) Monotremes have left a poor fossil record, and paleontology has broadly affect our understanding of early mammalian history, been virtually mute during two decades of discussion about with special implications for molecular clock estimates of basal molecular clock estimates of the timing of divergence between the divergence times. platypus and echidna clades. We describe evidence from high- Monotremata today comprises five species that form two resolution x-ray computed tomography indicating that Teinolo- distinct clades (16). The echidna clade includes one short-beaked phos, an Early Cretaceous fossil from Australia’s Flat Rocks locality species (Tachyglossus aculeatus; Australia and surrounding is- (121–112.5 Ma), lies within the crown clade Monotremata, as a lands) and three long-beaked species (Zaglossus bruijni, Z. basal platypus. Strict molecular clock estimates of the divergence bartoni, and Z. attenboroughi, all from New Guinea). The between platypus and echidnas range from 17 to 80 Ma, but platypus clade includes only Ornithorhynchus anatinus (Austra- Teinolophos suggests that the two monotreme clades were al- lia, Tasmania). -
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. -
Platypus Free Download
PLATYPUS FREE DOWNLOAD Joan Green Short | 24 pages | 01 Apr 1997 | Mondo Publishing | 9781572551954 | English | United States What is a platypus? Until the early 20th century Platypus hunted the platypus for its fur, but Platypus is now protected throughout Platypus range. Buy them: AmazonAmazon. Animals cats Platypus holidays shopping Smart Shopping. The platypus is a bottom-feeder that uses its beaver-like tail to steer and its webbed feet to propel itself Platypus the water while hunting for insects, shellfish, and worms. Instead, males have a hollow spur on each hind leg from which venom Platypus dispensed—but only sometimes. July Platypus The platypus is an excellent swimmer and spends much of its time in Platypus water foraging for food. Platypus Russell C. Journal of Physiology. The corneal surface and the adjacent surface of the lens is flat while the posterior surface of the lens is steeply curved, similar to Platypus eyes of other aquatic mammals Platypus as otters and sea-lions. Bibcode : Natur. ABC News. Eurylambda Tinodon Trishulotherium Yermakia. Species Profile and Threats Database. PlatypusOrnithorhynchus anatinusalso called duckbilla small amphibious Australian mammal noted for its odd combination of Platypus features and special adaptationsespecially the flat, almost comical Platypus that early observers thought was that of a Platypus sewn onto the body of a mammal. ZME Science. Conservation status. Test Your Vocabulary. The platypus is no longer found in the Platypus part of the Murray-Darling Basinpossibly due to the declining water Platypus brought Platypus by extensive land clearing and irrigation schemes. Retrieved 14 September The venom appears to have a different function from those Platypus by non-mammalian species; its effects are not life-threatening to humans, but nevertheless powerful enough to seriously impair the victim. -
How Many Kingdoms of Life? Eukaryotic Phylogeny and Philosophy of Systematics
How many kingdoms of life? Eukaryotic phylogeny and philosophy of systematics Łukasz Lamża Copernicus Center for Interdisciplinary Studies, Jagiellonian University Abstract According to contemporary understanding of the universal tree of life, the traditionally recognized kingdoms of eukaryotic organisms— Protista, Fungi, Animalia and Plantae—are irregularly interspersed in a vast phylogenetic tree. There are numerous groups that in any Linnaean classification advised by phylogenetic relationships (i.e. a Hennigian system) would form sister groups to those kingdoms, therefore requiring us to admit them the same rank. In practice, this would lead to the creation of ca. 25-30 new kingdoms that would now be listed among animals and plants as “major types of life”. This poses problems of an aesthetic and educational nature. There are, broadly speaking, two ways to deal with that issue: a) ignore the aesthetic and educational arguments and propose classification sys- tems that are fully consistent with the Hennigian principles of phylo- genetic classification, i.e. are only composed of monophyletic taxa; CC-BY-NC-ND 4.0 b) ignore Hennigian principles and bunch small, relatively uncharac- • teristic groups into paraphyletic taxa, creating systems that are more 227 – convenient. In the paper, I present the debate and analyze the pros 203 and cons of both options, briefly commenting on the deeper, third resolution, which would be to abandon classification systems entirely. Philosophical Problems in Science (Zagadnienia FilozoficzneNo w Nauce) 66 (2019), pp. 204 Łukasz Lamża Recent advances in eukaryotic classification and phylogeny are com- mented in the light of the philosophical question of the purpose and design principles of biological classification systems. -
Mammalian Fauna of the Late Jurassic Guimarota Ecosystem
Asociación Paleontológica Argentina. Publicación Especial 7 ISSN 0328-347X VII International Symposium on Mesozoic Terrestrial Ecosystems: 123-126. Buenos Aires, 30-6-2001 MaMMalian fauna of the Late Jurassic Guimarota ecoSyStem Thomas MARTIN1 Abstract. The Late Jurassic (Kirnmeridgian) Guimarota loca lit y near Leiria in west-central Portugal has yielded more than 800 mammalian dentaries and partial skulls representing the largest sample of Late Jurassic mammals in the world. However, despite the enormous number of specimens collected, the mam- malian fauna appears somewhat depauperate. So far, only Multituberculata (several genera of Paulchoffatiidae; 28% of total number), Docodonta (Halda nadan exspectaius Kühne and Krusat; 24%), and Holotheria (48%) represented by Paurodontidae (Henkelatherium guimaratae Krebs and Drescheratherium acutum Krebs) and Dryolestidae (Dryalestes leiriensis Martín, Krebsoiherium Iusiianicum Martin, and Guimaroiodus inflatus Martin) have been detected. "Triconodonta" and Syrnmetrodonta, which are well represented at other Late Jurassic localities (e.g., Morrison Forrnation), are missing. To recover the rare mammalian taxa of the Guimarota ecosystem, a project was initiated to study the nearly 7000 isolated mammalian teeth that had been obtained by screenwashing. With a single exception, the same taxa are represented. Among the thousands of isolated teeth, however, 25 lower and 23 upper premolars and mo- lars of a tiny primitive Zatheria have been found, of which the lower molars closely resemble the "Porto Pinheiro molar". After sorting the isolated teeth, the mammalian fauna of the Guimarota ecosystem prob- ably is completely recorded. Apparently, the coastal swamp in the Lusitanian graben where the lignite formed represented a stressed environment not appropriate for some marnmalian groups. -
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 -
Jaw Roll and Jaw Yaw in Early Mammals
Matters arising Reply to: Jaw roll and jaw yaw in early mammals https://doi.org/10.1038/s41586-020-2364-z Bhart-Anjan S. Bhullar1,2,6 ✉, Armita R. Manafzadeh3,6, Juri A. Miyamae1,2, Eva A. Hoffman4, Elizabeth L. Brainerd3, Catherine Musinsky5 & Alfred W. Crompton5 Published online: 17 June 2020 Check for updates REPLYING TO D. M. Grossnickle Nature (2020) In the accompanying Comment1, Grossnickle disputes our conclusion2 identification1,11 of the ancestral cladotherian talonid surface with the that roll-dominated processing is ancestral for therian mammals on the therian hypoflexid alone. It is true that the primitive talonid favoured basis of the following assertions: that the surface of the therian talonid shearing, whereas the therian basin allowed grinding. However, it has basin (Fig. 1a–i) is not homologous to the ancestral cladotherian talo- previously been observed that mediolateral motion from jaw roll would nid heel; that the inflected angle in marsupials suggests secondarily have increased the efficiency of both kinds of processing4, which exist increased jaw roll; that the rotational grinding stroke as we describe as points on a continuum rather than a dichotomy. it might be a passive movement; that the cladotherian angular pro- With regard to the so-called inflection of the marsupial angle, this cess (Fig. 1j–s) increases mechanical advantage for yaw instead of for phenomenon has previously been found12 to be little more than an roll; and that the angular process of yaw-processing mammals has elaboration of a ventral bony lamina known as the pterygoid shelf in expanded instead of vanished. stem therians. -
Brief Report Vol
Brief report Vol. 46, No. 1, pp. 113-1 18, Warszawa 2001 Monotreme nature of the Australian Early Cretaceous mammal Teinolophos THOMAS H. RICH, PATRICIA VICKERS-RICH, PETER TRUSLER, TIMOTHY F. FLANNERY, RICHARD CIFELLI, ANDREW CONSTANTINE, LESLEY KOOL, and NICHOLAS VAN KLAVEREN The morphology of the single preserved molar of the holotype of the Australian Early Creta- ceous (Aptian) mammal Teinolophos trusleri shows that it is a monotreme and probably a steropodontid, rather than a 'eupantothere' as originally proposed. The structure of the rear of the jaw of T. trusleri supports the molecular evidence that previously formed the sole basis for recognising the Steropodontidae as a distinct family. When the holotype of Teinolophos trusleri was first described from the Early Cretaceous (Aptian) Strzelecki Group of southern Victoria, Australia (Rich et al. 1999), it was regarded as a member of the Order Eupantotheria Kermack & Mussett, 1958 (= Legion Cladotheria McKenna, 1975 - Infralegion Tribosphenida McKenna, 1975) of uncertain family. This interpretation was based in large part on the inferred structure of the penultimate lower molar, the only tooth preserved on the se- verely crushed holotype. The crown of that tooth was largely obscured by a hard matrix. As a conse- quence of that, a critical misidentification of the cusp in the posterolingual region of the tooth as the metaconid rather than the hypoconulid was made. It was this erroneous interpretation and the conse- quent corollaries that the trigonid was anteroposteriorlyexpanded and the talonid unbasined that led Rich et al. (1999) to intepret the specimen as a 'eupantothere'. In September 1999, Mr. Charles Schaff of Harvard University successfully cleared the obscuring matrix from crown of the tooth (Fig. -
The Miocene Mammal Necrolestes Demonstrates the Survival of a Mesozoic Nontherian Lineage Into the Late Cenozoic of South America
The Miocene mammal Necrolestes demonstrates the survival of a Mesozoic nontherian lineage into the late Cenozoic of South America Guillermo W. Rougiera,b,1, John R. Wibleb, Robin M. D. Beckc, and Sebastian Apesteguíad,e aDepartment of Anatomical Sciences and Neurobiology, University of Louisville, Louisville, KY 40202; bSection of Mammals, Carnegie Museum of Natural History, Pittsburgh, PA 15206; cSchool of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, Australia; dCEBBAD–Fundación de Historia Natural ‘Félix de Azara’, Universidad Maimónides, 1405 Buenos Aires, Argentina; and eConsejo Nacional de Investigaciones Científicas y Técnicas de Argentina, C1033AAJ Buenos Aires, Argentina Edited by Richard L. Cifelli, University of Oklahoma, Norman, OK, and accepted by the Editorial Board October 18, 2012 (received for review July 27, 2012) The early Miocene mammal Necrolestes patagonensis from Pata- not referable to either Metatheria or Eutheria, but did not discuss gonia, Argentina, was described in 1891 as the only known extinct the evidence for this interpretation, nor did they identify the placental “insectivore” from South America (SA). Since then, and specific therian lineages they considered to be potential relatives despite the discovery of additional well-preserved material, the of Necrolestes. Starting in 2007, we oversaw additional prepara- systematic status of Necrolestes has remained in flux, with earlier tion of Necrolestes specimens that comprise the best-preserved studies leaning toward placental affinities and more recent ones material currently available, including skulls, jaws, and some iso- endorsing either therian or specifically metatherian relationships. We lated postcranial bones; as a result, many phylogenetically signif- have further prepared the best-preserved specimens of Necrolestes icant features have been revealed for the first time. -
Mammalia, Theria) Un Primitivo Mamífero Del Cretacico Inferior De La Cuenca Neuquina Rougier, Guillermo Walter 1993
Tesis de Posgrado Vincelestes neuquenianus bonaparte (mammalia, theria) un primitivo mamífero del cretacico inferior de la cuenca neuquina Rougier, Guillermo Walter 1993 Tesis presentada para obtener el grado de Doctor en Ciencias Biológicas de la Universidad de Buenos Aires Este documento forma parte de la colección de tesis doctorales y de maestría de la Biblioteca Central Dr. Luis Federico Leloir, disponible en digital.bl.fcen.uba.ar. Su utilización debe ser acompañada por la cita bibliográfica con reconocimiento de la fuente. This document is part of the doctoral theses collection of the Central Library Dr. Luis Federico Leloir, available in digital.bl.fcen.uba.ar. It should be used accompanied by the corresponding citation acknowledging the source. Cita tipo APA: Rougier, Guillermo Walter. (1993). Vincelestes neuquenianus bonaparte (mammalia, theria) un primitivo mamífero del cretacico inferior de la cuenca neuquina. Facultad de Ciencias Exactas y Naturales. Universidad de Buenos Aires. http://digital.bl.fcen.uba.ar/Download/Tesis/Tesis_2605_Rougier.pdf Cita tipo Chicago: Rougier, Guillermo Walter. "Vincelestes neuquenianus bonaparte (mammalia, theria) un primitivo mamífero del cretacico inferior de la cuenca neuquina". Tesis de Doctor. Facultad de Ciencias Exactas y Naturales. Universidad de Buenos Aires. 1993. http://digital.bl.fcen.uba.ar/Download/Tesis/Tesis_2605_Rougier.pdf Dirección: Biblioteca Central Dr. Luis F. Leloir, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires. Contacto: [email protected] Intendente Güiraldes 2160 - C1428EGA - Tel. (++54 +11) 4789-9293 UNIVERSIDAD NACIONAL DE BUENOS AIRES FACULTAD DE CIENCIAS EXACTAS Y NATURALES VINCELESTES NEUQUENIANUS BONAPARTE (MAMMAIJA, THERIA) UN PRIMITIVO MAMIFERO DEL CRETACICO INFERIOR DE LA CUENCA NEUQUINA. -
Molecules, Morphology, and Ecology Indicate a Recent, Amphibious Ancestry for Echidnas
Molecules, morphology, and ecology indicate a recent, amphibious ancestry for echidnas Matthew J. Phillipsa,1, Thomas H. Bennetta, and Michael S. Y. Leeb,c aCentre for Macroevolution and Macroecology, Research School of Biology, Australian National University, Canberra, ACT 0200, Australia; bSchool of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia; and cEarth Sciences Section, South Australian Museum, Adelaide, SA 5000, Australia Edited by David B. Wake, University of California, Berkeley, CA, and approved August 14, 2009 (received for review April 28, 2009) The semiaquatic platypus and terrestrial echidnas (spiny anteaters) Fossil echidnas do not appear until the mid-Miocene (Ϸ13 are the only living egg-laying mammals (monotremes). The fossil Ma) (13), despite excellent late Oligocene–Early Miocene mam- record has provided few clues as to their origins and the evolution mal fossil records in both northern and southern Australia. This of their ecological specializations; however, recent reassignment absence has tentatively been attributed in part to echidnas of the Early Cretaceous Teinolophos and Steropodon to the platy- lacking teeth (14), which are the most common fossil remains pus lineage implies that platypuses and echidnas diverged >112.5 from mammals. Alternatively, if the molecular dating studies million years ago, reinforcing the notion of monotremes as living that estimate the divergence of echidnas from platypuses at fossils. This placement is based primarily on characters related to 17–35 Ma (15–22) are correct, then characters that clearly ally a single feature, the enlarged mandibular canal, which supplies fossil taxa with echidnas would not be expected to have evolved blood vessels and dense electrosensory receptors to the platypus until even more recently.