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The Relationships of the Arctostylopidae (Mammalia) New Data and Interpretation
THE RELATIONSHIPS OF THE ARCTOSTYLOPIDAE (MAMMALIA) NEW DATA AND INTERPRETATION RICHARD L. CIFELLI,' CHARLES R. SCHAFF,- AND MALCOLM C. McKENNA CONTENTS Abstract. The dental morpholog steini, hitherto known onl) from pari Abstract cheek- tooth series is desi rilx-d on the ba Introduction collected specimen including .i near!) Acknowledgments per and lower dentition \U arctoMylopid • Abbreviations from North America principally from th Paleontology 5 Systematic Basin, Wyoming, are apparentl) referable l Order new 5 Arctostylopida, gle species, which therefore ranges from the lati 5 Family Arctostylopidae luiiian through the ( larklorkian Other an I 6 Matthew, 1915 to the \si.m Arctostylops genera are restricted I'.ileogi A. steini Matthew, 1915 6 A previously described 5pe< ies "l Matthew and Granger, Palaeostijlops sty/ops is placed in a new genus Gashal 1 1 1925 Arctostylopidae and its constituent subordii P. iturus Matthew and Granger, are diagnosed, and a h\ pothesis "I relationshi| 1925 1 5 in the family is presented B) comparison witl 15 new l>\ / Gashatostylops genus ungulate morphohpe as represented et .. 15 G. macrodon (Matthew al., 1929) latum, Asiostylops spumes is hypothesized 20 and 1976 ... Sinostylops Tang Yan, most primitive member ol the family; Both 1976 ... 20 S. promissus Tang and Yan, notios and B. progressus retain man) primitivi Bothriostylops Zheng and Huang, tures but clearK hear some ol the spec lalizatkx 22 other 1986 in Palaeostijlops, Arctostylops, and and 1986 ... North \mt B. notios Zheng Huang, genera. Of these derived taxa, and 1976) sister taxou to the n B. progressus (Tang Yan, tostylops may be the 1978 22 are in distributioi Anatolostylops Zhai, genera, all of which Vsiatfc 23 A. -
Evolutionary and Functional Implications of Incisor Enamel Microstructure Diversity in Notoungulata (Placentalia, Mammalia)
Journal of Mammalian Evolution https://doi.org/10.1007/s10914-019-09462-z ORIGINAL PAPER Evolutionary and Functional Implications of Incisor Enamel Microstructure Diversity in Notoungulata (Placentalia, Mammalia) Andréa Filippo1 & Daniela C. Kalthoff2 & Guillaume Billet1 & Helder Gomes Rodrigues1,3,4 # The Author(s) 2019 Abstract Notoungulates are an extinct clade of South American mammals, comprising a large diversity of body sizes and skeletal morphologies, and including taxa with highly specialized dentitions. The evolutionary history of notoungulates is characterized by numerous dental convergences, such as continuous growth of both molars and incisors, which repeatedly occurred in late- diverging families to counter the effects of abrasion. The main goal of this study is to determine if the acquisition of high-crowned incisors in different notoungulate families was accompanied by significant and repeated changes in their enamel microstructure. More generally, it aims at identifying evolutionary patterns of incisor enamel microstructure in notoungulates. Fifty-eight samples of incisors encompassing 21 genera of notoungulates were sectioned to study the enamel microstructure using a scanning electron microscope. We showed that most Eocene taxa were characterized by an incisor schmelzmuster involving only radial enamel. Interestingly, derived schmelzmusters involving the presence of Hunter-Schreger bands (HSB) and of modified radial enamel occurred in all four late-diverging families, mostly in parallel with morphological specializations, such as crown height increase. Despite a high degree of homoplasy, some characters detected at different levels of enamel complexity (e.g., labial versus lingual sides, upper versus lower incisors) might also be useful for phylogenetic reconstructions. Comparisons with perissodactyls showed that notoungulates paralleled equids in some aspects related to abrasion resistance, in having evolved transverse to oblique HSB combined with modified radial enamel and high-crowned incisors. -
Annualreportofdi72fiel.Pdf
mmmmm , THE UNIVERSITY OF ILLINOIS LIBRARY SOT CENTRAL CIRCULATION BOOKSTACKS The person charging this material is re- sponsible for its renewal or its return to the library from which it was borrowed on or before the Latest Date stamped below. The Minimum Fee for each Lost Book is $50.00. Theft/ mutilation, and underlining of books are reasons for disciplinary action and may result in dismissal from the University. TO RENEW CALL TELEPHONE CENTER, 333-8400 UNIVERSITY OF ILLINOIS LIBRARY AT URBANA-CHAMPAIGN MAR 9 1991 When renewing by phone, write new due date below previous due date. L162 Field Museum of Natural History Reports, Vol. VII, Plate XXI ERNEST R. GRAHAM Trustee of the Museum and member of the Building Committee Field Museum of Natural History Founded by Marshall Field, 1893 Publication 248 Report Series Vol. VII, No. 2 ANNUAL REPORT OF THE DIRECTOR TO THE BOARD OF TRUSTEES FOR THE YEAR 1927 nf -"^ THE imm JUL 3 1323 Of 'LUNOIS UNlVWSltY Chicago, U. S. A. January, 1928 OF THE tiW^ViiuSHY Of ILimOlS PRINTED IN THE UNITED STATES OF AMERICA BY FIELD MUSEUM PRESS ^ i V BEQUESTS Bequests to Field Museum of Natural History may be made in securities, money, books or collections. They may, if desired, take the form of a memorial to the memory of a person or cause, to be named by the giver. For those desirous of making bequests to the Museum, the following form is suggested: FORM OF BEQUEST I do hereby give and bequeath to Field Museum of Natural History of the City of Chicago, State of Illinois, Cash contributions made within the taxable year to Field Museum of Natural History to an amount not in excess of 15 per cent of the taxpayer's net income are allowable as deduc- tions in computing net income under Article 251 of Regula- tion 69 relating to the income tax under the Revenue Act of 1926. -
American Museum Novitates
AMERICAN MUSEUM NOVITATES Number 3737, 64 pp. February 29, 2012 New leontiniid Notoungulata (Mammalia) from Chile and Argentina: comparative anatomy, character analysis, and phylogenetic hypotheses BRUCE J. SHOCKEY,1 JOHN J. FLYNN,2 DARIN A. CROFT,3 PHILLIP GANS,4 ANDRÉ R. WYSS5 ABSTRACT Herein we describe and name two new species of leontiniid notoungulates, one being the first known from Chile, the other from the Deseadan South American Land Mammal Age (SALMA) of Patagonia, Argentina. The Chilean leontiniid is from the lower horizons of the Cura-Mallín Formation (Tcm1) at Laguna del Laja in the Andean Main Range of central Chile. This new species, Colpodon antucoensis, is distinguishable from Patagonian species of Colpodon by way of its smaller I2; larger I3 and P1; sharper, V-shaped snout; and squarer upper premo- lars. The holotype came from a horizon that is constrained below and above by 40Ar/39Ar ages of 19.53 ± 0.60 and 19.25 ± 1.22, respectively, suggesting an age of roughly 19.5 Ma, or a little older (~19.8 Ma) when corrected for a revised age of the Fish Canyon Tuff standard. Either age is slightly younger than ages reported for the Colhuehuapian SALMA fauna at the Gran Bar- ranca. Taxa from the locality of the holotype of C. antucoensis are few, but they (e.g., the mylo- dontid sloth, Nematherium, and a lagostomine chinchillid) also suggest a post-Colhuehuapian 1Department of Biology, Manhattan College, New York, NY 10463; and Division of Paleontology, American Museum of Natural History. 2Division of Paleontology, and Richard Gilder Graduate School, American Museum of Natural History. -
A Evolução Dos Metatheria: Sistemática, Paleobiogeografia, Paleoecologia E Implicações Paleoambientais
UNIVERSIDADE FEDERAL DE PERNAMBUCO CENTRO DE TECNOLOGIA E GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS ESPECIALIZAÇÃO EM GEOLOGIA SEDIMENTAR E AMBIENTAL LEONARDO DE MELO CARNEIRO A EVOLUÇÃO DOS METATHERIA: SISTEMÁTICA, PALEOBIOGEOGRAFIA, PALEOECOLOGIA E IMPLICAÇÕES PALEOAMBIENTAIS RECIFE 2017 LEONARDO DE MELO CARNEIRO A EVOLUÇÃO DOS METATHERIA: SISTEMÁTICA, PALEOBIOGEOGRAFIA, PALEOECOLOGIA E IMPLICAÇÕES PALEOAMBIENTAIS Dissertação de Mestrado apresentado à coordenação do Programa de Pós-graduação em Geociências, da Universidade Federal de Pernambuco, como parte dos requisitos à obtenção do grau de Mestre em Geociências Orientador: Prof. Dr. Édison Vicente Oliveira RECIFE 2017 Catalogação na fonte Bibliotecária: Rosineide Mesquita Gonçalves Luz / CRB4-1361 (BCTG) C289e Carneiro, Leonardo de Melo. A evolução dos Metatheria: sistemática, paleobiogeografia, paleoecologia e implicações paleoambientais / Leonardo de Melo Carn eiro . – Recife: 2017. 243f., il., figs., gráfs., tabs. Orientador: Prof. Dr. Édison Vicente Oliveira. Dissertação (Mestrado) – Universidade Federal de Pernambuco. CTG. Programa de Pós-Graduação em Geociências, 2017. Inclui Referências. 1. Geociêcias. 2. Metatheria . 3. Paleobiogeografia. 4. Paleoecologia. 5. Sistemática. I. Édison Vicente Oliveira (Orientador). II. Título. 551 CDD (22.ed) UFPE/BCTG-2017/119 LEONARDO DE MELO CARNEIRO A EVOLUÇÃO DOS METATHERIA: SISTEMÁTICA, PALEOBIOGEOGRAFIA, PALEOECOLOGIA E IMPLICAÇÕES PALEOAMBIENTAIS Dissertação de Mestrado apresentado à coordenação do Programa de Pós-graduação -
Maquetación 1
ISSN 2469-0228 www.peapaleontologica.org.ar THE METATHERIA FROM THE RÍO SANTA CRUZ (SANTA CRUZ FORMATION, EARLY – MIDDLE MIOCENE, ARGENTINA): HISTORY AND NEW RECORDS LAURA CHORNOGUBSKY 1,2 MARÍA A. ABELLO 1,3 GERMÁN D. BARMAK 2 1Comisión Nacional de Investigaciones Científicas y Técnicas (CONICET). 2Sección Paleontología Vertebrados, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”. Av. Ángel Gallardo 470, C1405DRJ Ciudad Autónoma de Buenos Aires, Argentina. 3División Paleontología Vertebrados, Unidades de Investigación Anexo Museo, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata. Av. 122 y 60, B1904 La Plata, Argentina. Recibido: 22 de marzo 2019 - Aceptado: 4 de octubre 2019 Para citar este artículo: Laura Chornogubsky, María A. Abello, and Germán D. Barmak (2019). The Metathe - ria from the Río Santa Cruz (Santa Cruz Formation, Early–Middle Miocene, Argentina): History and new records . Publicación Electrónica de la Asociación Paleontológica Ar gentina 19 (2): 62–84. Link a este artículo: http://dx.doi.org/ 10.5710/PEAPA.04.10.2019.287 DESPLAZARSE HACIA ABAJO PARA ACCEDER AL ARTÍCULO Asociación Paleontológica Argentina Maipú 645 1º piso, C1006ACG, Buenos Aires República Argentina Tel/Fax (54-11) 4326-7563 Otros artículos en Publicación Electrónica de la APA 19(2): Web: www.apaleontologica.org.ar J.I. Cuitiño et al. M. Fernández, N.A. Muñoz R.F. Kay, J.M.G. Perry STRATIGRAPHY AND DEPOSITIONAL NOTOUNGULATA AND ASTRAPOTHERIA NEW PRIMATES FROM THE RÍO SANTA ENVIRONMENTS OF THE SANTA CRUZ (MAMMALIA, MERIDIUNGULATA) OF THE CRUZ AND RÍO BOTE (EARLY–MIDDLE FORMATION (EARLY–MIDDLE MIOCENE) SANTA CRUZ FORMATION (EARLY–MIDDLE MIOCENE), SANTA CRUZ PROVINCE, ALONG THE RÍO SANTA CRUZ, MIOCENE) ALONG THE RÍO SANTA CRUZ, ARGENTINA SOUTHERN PATAGONIA, ARGENTINA ARGENTINE PATAGONIA Año 2019 - 19(2): 62–84 ARTÍCULO ISSN 2469-0228 THE METATHERIA FROM THE RÍO SANTA CRUZ (SANTA CRUZ FORMATION, EARLY–MIDDLE MIOCENE, ARGENTINA): HISTORY AND NEW RECORDS LAURA CHORNOGUBSKY 1,2 , MARÍA A. -
(Mammalia, Notoungulata) with Emphases in Basicranial and Auditory Region
RESEARCH ARTICLE Cranial Morphology of the Late Oligocene Patagonian Notohippid Rhynchippus equinus Ameghino, 1897 (Mammalia, Notoungulata) with Emphases in Basicranial and Auditory Region Gastón Martínez1,2*, María Teresa Dozo1, Javier N. Gelfo3,4, Hernán Marani5 1 Instituto Patagónico de Geología y Paleontología, Centro Nacional Patagónico, CONICET, Puerto Madryn, Chubut, Argentina, 2 Facultad de Ciencias Exactas Físicas y Naturales, Universidad Nacional de Córdoba, Córdoba, Argentina, 3 División Paleontología Vertebrados, Museo de la Plata, CONICET, La Plata, Buenos a11111 Aires, Argentina, 4 Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Buenos Aires, Argentina, 5 Facultad de Ciencias Naturales, Universidad Nacional de la Patagonia San Juan Bosco, Puerto Madryn, Chubut, Argentina * [email protected] OPEN ACCESS Abstract Citation: Martínez G, Dozo MT, Gelfo JN, Marani H “Notohippidae” is a probably paraphyletic family of medium sized notoungulates with com- (2016) Cranial Morphology of the Late Oligocene Patagonian Notohippid Rhynchippus equinus plete dentition and early tendency to hypsodonty. They have been recorded from early Ameghino, 1897 (Mammalia, Notoungulata) with Eocene to early Miocene, being particularly diverse by the late Oligocene. Although Emphases in Basicranial and Auditory Region. PLoS Rhynchippus equinus Ameghino is one of the most frequent notohippids in the fossil record, ONE 11(5): e0156558. doi:10.1371/journal. pone.0156558 there are scarce data about cranial -
Anatomía Y Sistemática De Los Toxodontidae (Notoungulata) De La Formación Santa Cruz, Mioceno Temprano, Argentina
Carrera del Doctorado en Ciencias Naturales Anatomía y Sistemática de los Toxodontidae (Notoungulata) de la Formación Santa Cruz, Mioceno Temprano, Argentina. Tesis doctoral por: Lic. Santiago Hernández Del Pino Dra. Ma. Esperanza Cerdeño Serrano Dr. Sergio F. Vizcaíno Directora Director TOMO II La Plata – Argentina 2018 Anatomía y Sistemática de los Toxodóntidos de Santa Cruz Capitulo V. Cuantificación del morfoespacio teórico En este capítulo se presentan los resultados obtenidos de los análisis de cuantificación del morfoespacio teórico de los Nesodontinae de la Formación Santa Cruz. El primer subcapitulo (V. 1) corresponde a un análisis exploratorio realizado a partir de medidas lineales del cráneo y la mandíbula de 110 ejemplares de nesodontinos El segundo subcapítulo corresponde al análisis realizados a partir de landmarks 3D para el cráneo de Nesodontinae (V. 2. 1) y para las especies integrantes de la subfamilia, Nesodon imbricatus (V. 2.2) y Adinotherium ovinum (V. 2.3). Cada uno de estos apartados cuenta con dos secciones; la primera, con los resultados obtenidos para los análisis sin aplicar retrodeformación, y la segunda, correspondiente a los resultados del análisis de los datos retrodeformados. Para los Nesodontinae, además, se incluye el análisis del morfoespacio para la mandíbula, que no se desarrolla en cada especie debido a que la muestra es demasiado pequeña y solo cuenta con un ejemplar de Adinotherium ovinum. También, se presenta una regresión con los resultados del ACP contra el logaritmo del tamaño del centroide para evaluar el rol del tamaño como estructurador de la variación en la forma (V. 3), un análisis de parsimonia (V. 4) para todos los ejemplares contemplados en los análisis realizados en este capítulo y una discusión de los resultados obtenidos (V. -
Caudal Cranium of Thylacosmilus Atrox (Mammalia, Metatheria, Sparassodonta), a South American Predaceous Sabertooth
CAUDAL CRANIUM OF THYLACOSMILUS ATROX (MAMMALIA, METATHERIA, SPARASSODONTA), A SOUTH AMERICAN PREDACEOUS SABERTOOTH ANALÍA M. FORASIEPI, ROSS D. E. MACPHEE, AND SANTIAGO HERNANDEZ DEL PINO BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY CAUDAL CRANIUM OF THYLACOSMILUS ATROX (MAMMALIA, METATHERIA, SPARASSODONTA), A SOUTH AMERICAN PREDACEOUS SABERTOOTH ANALÍA M. FORASIEPI IANIGLA, CCT-CONICET, Mendoza, Argentina ROSS D.E. MacPHEE Department of Mammalogy, American Museum of Natural History, New York SANTIAGO HERNÁNDEZ DEL PINO IANIGLA, CCT-CONICET, Mendoza, Argentina BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY Number 433, 64 pp., 27 figures, 1 table Issued June 14, 2019 Copyright © American Museum of Natural History 2019 ISSN 0003-0090 CONTENTS Abstract.............................................................................3 Introduction.........................................................................3 Materials and Methods................................................................7 Specimens . 7 CT Scanning and Bone Histology....................................................8 Institutional and Other Abbreviations ...............................................12 Comparative Osteology of the Caudal Cranium of Thylacosmilus and Other Sparassodonts . .12 Tympanic Floor and Basicranial Composition in Thylacosmilus . 12 Tympanic Floor Composition in the Comparative Set .................................19 Petrosal Morphology..............................................................26 Tympanic Roof Composition -
Un Nuevo Trachytheriinae (Mammalia,†Notoungulata) Del
Un nuevo Trachytheriinae (Mammalia, †Notoungulata) del Deseadense (Oligoceno tardío) de Patagonia, Argentina: implicancias en la filogenia, biogeografía y bioestratigrafía de los Mesotheriidae Marcelo A. Reguero Departamento Científico Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900, La Plata, Argentina [email protected] Paula V. Castro Subsecretaría de Cultura, Ministerio de Gobierno, Trabajo y Justicia, Roberto Jones 572, 9103 Rawson, Argentina [email protected] RESUMEN Una mandíbula incompleta de un Trachytheriinae de Edad deseadense recolectada por Carlos Ameghino en Cabeza Blanca, Provincia de Chubut, Argentina, es asignada a Anatrachytherus soria gen et sp. nov. Florentino Ameghino la ilustró, refiriéndola a Trachytherus spegazzinianus Ameghino, un taxón característico de la Edad deseadense (Oligoceno tardío) de Argentina y Bolivia. Algunas características de A. soriai, e.g., cuerpo mandibular más corto, i1-2 poco procumbentes, fórmula dentaria más completa, corto diastema entre i2 y canino y m3 más corto que el m2, sugieren que se trata de un taxón más primitivo que T. spegazzinianus. El análisis filogenético sobre la base de 39 caracteres craneanos y dentarios sustenta la monofilia de esta especie, con una sola sinapomorfía, y una relación próxima de grupo hermano con Trachytherus. El análisis de parsimonia también sugiere que Mesotheriidae es el clado que contiene el ancestro común más reciente con Trachytherus? mendocensis, Anatrachytherus y Trachytherus y todos sus descendien- tes incluyendo a Mesotheriinae. La ausencia de mesotéridos en las SALMAs ('South American Land Mammal Age') Colhuehuapense y Santacrucense en Patagonia y las relaciones estratigráficas y filogenéticas de los Mesotheriinae, sugieren que el Altiplano chileno y boliviano habría actuado biogeográficamente como centro de origen y dispersión de los Mesotheriinae (clado hipselodonte). -
Rodentia, Caviomorpha) in Chubut Province, Patagonia (Argentina)
Rev. Mus. Argentino Cienc. Nat., n.s. 19(2): 121-129, 2017 ISSN 1514-5158 (impresa) ISSN 1853-0400 (en línea) First record of Banderomys leanzai Kramarz, 2005 (Rodentia, Caviomorpha) in Chubut Province, Patagonia (Argentina) Felipe BUSKER1,5, María E. PÉREZ2,5, Javier M. KRAUSE3,5 & María G. VUCETICH4,5 1Instituto Patagónico de Geología y Paleontología, Centro Nacional Patagónico (IPGP, CCT CONICET- CENPAT). Bvd. Brown 2915 (U9120ACD). Puerto Madryn, Chubut, Argentina. [email protected]. ar. 2Museo Paleontológico Egidio Feruglio (MEF). Av. Fontana 140, Trelew (U9100GYO), Chubut, Argentina. Researcher Associate Field Museum of Natural History (FMNH), Chicago, IL, USA. [email protected]. 3Museo Paleontológico Egidio Feruglio, Av. Fontana 140, Trelew, (U9100GYO), Chubut, Argentina. Departamento de Geología, Universidad Nacional de la Patagonia San Juan Bosco, Comodoro Rivadavia, Chubut, Argentina. [email protected]. 4División de Paleontología Vertebrados, Museo de La Plata, UNLP, Paseo del Bosque s/n, (B1900FWA) La Plata, Buenos Aires, Argentina. [email protected]. 5Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) Abstract: �������������������������������������Cephalomyidae was established in the �I������������������������������������������������������������ century, and was considered by different authors as a het- erogeneous group of hypsodont South American hystricognath rodents. Other authors corroborated this family as a natural group among caviomorphs and recognized some taxa recorded from the Deseadan–Colhuehuapian South American Land Mammals Ages (SALMAs). Among them, Banderomys leanzai (the only species of this ge- nus) was, until now, characteristic and exclusive of the locality of Cerro Bandera (early Miocene, Colhuehuapian?, Neuquén Province, Argentina). The aim of this work is to report the first record of B. leanzai outside the type locality; the new specimens come from the early Miocene of central Chubut Province (Patagonia, Argentina). -
IJOMS Vol 18-4 7.Indd
IJOMS Vol 18-3_4 IJOMS Vol 18-3_4 164 Int J Oral-Med Sci 18(3)( 4):164–171, 2020 Original Article Undulating Vertical Prism Decussation of Pyrotherium(Pyrotheria, Mammalia)Mo- lar Tomohiko Hirayama1, 2, 3 and Kunihiro Suzuki3 Department of 1Histology and 2Liberal Arts(Biology), Nihon University School of Dentistry at Matsudo, Matsudo, Chiba 271–8587, Japan 3Research Institute of Oral Science, Nihon University School of Dentistry at Matsudo, Matsudo, Chiba 271–8587, Japan Article History Abstract Received 9 August 2019 Most mammalian teeth are covered in enamel and its external tooth shape is deter- Accepted 25 September 2019 mined by the phylogenic background and the mode of mastication and occlusion. Char- acteristic microstructure also exists in the internal structure of enamel, and the charac- teristics of enamel prism and Hunter-Schreger bands(HSB)are well studied. Pyrotherium(Pyroteria)is an extinct Tertiary period mammal of South America, with unknown ecology and phylogeny. In previous study, we observed a dendritic streak with a thick, wavy trunk extending in the direction of the tooth axis. This is classified as a vertical HSB with some similarity to rhinoceros molar. We demonstrate a complex Keywords: structure of the vertical HSB of Pyrotherium molar by using three-dimensional imag- enamel prism, ing of prisms based on serial SEM images. And also, we report the shape of the enamel Hunter-Schreger bands, prisms of Pyrotherium molar is keyhole-shaped with a head and tail, which is a pre- Pyrotherium, dominantly found in humans and other animals, but in some parts it is similar to the 3D reconstruction ginkgo-shape found in proboscideans.