Large Archaeohyracids (Typotheria, Notoungulata) from Central Chile and Patagonia, Including a Revision of Archaeotypotherium
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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. -
Paleogene Pseudoglyptodont Xenarthrans from Central Chile and Argentine Patagonia
PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, NY 10024 Number 3536, 18 pp., 4 figures October 19, 2006 Paleogene Pseudoglyptodont Xenarthrans from Central Chile and Argentine Patagonia 1 2 3 MALCOLM C. MCKENNA, ANDRE´ R. WYSS, AND JOHN J. FLYNN ABSTRACT Herein we describe a new, large-bodied species of Pseudoglyptodon, a close sloth ally, from volcaniclastic deposits of the Abanico (5 Coya-Machalı´) Formation of the central Chilean Andean Main Range. This species, P. chilensis, is a rare element of the Tinguiririca Fauna, on which the recently formalized Tinguirirican South American Land Mammal ‘‘Age’’ is founded, being known from just two specimens. The holotype of P. chilensis, a partial skull and largely complete mandibles (preserving seemingly complete upper and lower dentitions), is by far the best-preserved specimen referable to Pseudoglyptodon known. As such, this material permits a more refined phylogenetic placement of this enigmatic xenarthran than has been possible previously, with Pseudoglyptodon representing the proximal outgroup to the clade including the most recent common ancestor of Choelepus and Bradypus, plus all its descendants (i.e., crown clade sloths). A fragmentary specimen from Argentina is removed from Glyptatelus and referred to Pseudoglyptodon. Although this specimen is distinct from P. chilensis and other previously recognized species of Pseudoglyptodon, it offers too meager a basis for formally establishing a new name. Finally, phylogenetic definitions of the names Phyllophaga and Tardigrada are proposed. Historically these terms have been used largely interchangeably, but here we advocate linking the latter to the crown clade. 1 Division of Paleontology, American Museum of Natural History ([email protected]). -
Late Oligocene) of Argentina
J. Paleont., 81(6), 2007, pp. 1301–1307 Copyright ᭧ 2007, The Paleontological Society 0022-3360/07/0081-1301$03.00 A POORLY KNOWN RODENTLIKE MAMMAL (PACHYRUKHINAE, HEGETOTHERIIDAE, NOTOUNGULATA) FROM THE DESEADAN (LATE OLIGOCENE) OF ARGENTINA. PALEOECOLOGY, BIOGEOGRAPHY, AND RADIATION OF THE RODENTLIKE UNGULATES IN SOUTH AMERICA MARCELO A. REGUERO,1 MARI´A TERESA DOZO,2 AND ESPERANZA CERDEN˜ O3 1Divisio´n Paleontologı´a de Vertebrados, Museo de La Plata, B1900FWA La Plata, Argentina, Ͻ[email protected]Ͼ, 2Laboratorio de Paleontologı´a, Centro Nacional Patagonico, Consejo Nacional de Investigaciones Cientificas y Te´cnicas, 9120 Puerto Madryn, Chubut, Argentina, Ͻ[email protected]Ͼ, and 3Departamento de Geologı´a y Paleontologı´a, Instituto Argentino de Nivologı´a, Glaciologı´a, y Ciencias Ambientales, Centro Regional de Investigaciones Cientı´ficas y Te´cnicas, Consejo Nacional de Investigaciones Cientı´ficas y Te´cnicas, Avda. Ruiz Leal s/n, 5500 Mendoza, Argentina, Ͻ[email protected]Ͼ ABSTRACT—The cranial anatomy of the Deseadan species Medistylus dorsatus (Ameghino, 1903) is described based on new and complete material from Cabeza Blanca (Chubut, Argentina). Medistylus is the largest of the Pachyrukhinae and the specimen described here is probably the best-preserved pachyrukhine skull known in the Paleogene of South America. Previously, the validity of the species and its phylogenetic affinities with Interatheriidae (Notoungulata, Typotheria) were ambiguous and not conclusive. The syntypes, now reported lost, were isolated teeth poorly described by Ameghino in 1903. This almost complete skull with teeth provides more diagnostic features in order to complete the knowledge of genus. Details about cranial and dental morphology allow the reassessment of Medistylus dorsatus and its inclusion within the subfamily Pachyrukhinae (Hegetotheriidae, Notoungulata). -
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). -
Xxvi Jornadas...Qxd
AMEGHINIANA Revista de la Asociación Paleontológica Argentina RESÚMENES TOMO 46 Número 4 BUENOS AIRES REPÚBLICA ARGENTINA 2009 Se deja constancia que el presente suplemento se halla desprovisto de validez para propósitos nomenclaturales Disclaimer: this supplement is not deemed to be valid for nomenclatural purposes El Comité Editor de la Asociación Paleontológica Argentina deja constancia que solamente se incluyen en este Suplemento los resúmenes enviados por los organizadores de las diferentes reuniones. AMEGHINIANA 46 (4) Suplemento, 2009-RESÚMENES XXIV JORNADAS ARGENTINAS DE PALEONTOLOGÍA DE VERTEBRADOS RESÚMENES 4 al 7 de mayo de 2009 Museo de Historia Natural de San Rafael (MHNSR), San Rafael, Mendoza COMISIÓN ORGANIZADORA Presidente Marcelo S. de la Fuente (MHNSR) Secretarias Analía Forasiepi (MHNSR) Juliana Sterli (MHNSR) Vocales Miriam Ayala (MHNSR) René Biglione (DGE-Mendoza) Sergio Dieguez (CNEA) Gladys García (Universidad Champagnat) Miguel Giardina (MHNSR) Adolfo Gil (MHNSR) Gustavo Neme (MHNSR) Clara Otaola (MHNSR) Nuria Sugrañes (MHNSR) Financiado por ANPCyT, CONICET y Fondo Provincial de la Cultura de la Pcia. de Mendoza. Auspiciado por Asociación Paleontológica Argentina, Museo de Historia Natural de San Rafael y Municipalidad de San Rafael (Mendoza). AMEGHINIANA 46 (4) Sumplemento, 2009-RESÚMENES 4R CONFERENCIAS Origen de la ictiofauna marina y continental de América del Sur Austral A.L. CIONE1 La ictiofauna neotropical continental es la más rica en especies del mundo. Su mayor riqueza se localiza en las áreas intertropi- cales, un paralelo de lo que sucede con otros organismos. Se calcula que pueden existir 8.000 especies de peces continentales, un cuarto de la totalidad de los conocidos en todo el mundo en ambiente marino o continental. -
Evidence from Ecological Diversity Analysis (EDA)
Palaeontologia Electronica palaeo-electronica.org What are the best modern analogs for ancient South American mammal communities? Evidence from ecological diversity analysis (EDA) Angeline M. Catena and Darin A. Croft ABSTRACT Ecological diversity analysis (EDA) is a technique that uses ecological attributes of mammals to reconstruct the community structure and habitat of a fossil locality. EDAs of South American paleofaunas have generally relied on modern comparative datasets from that continent, but modern faunas from other continents may be more appropriate models considering the high-level taxonomic differences that exist between modern and fossil South American mammal communities. To test this hypoth- esis, we selected five, well-sampled fossil localities for which independent paleoenvi- ronmental data (e.g., paleosols, ichnofossils) have been published: four from South America (La Venta, Colombia; Quebrada Honda, Bolivia; Santa Cruz, Argentina; Tin- guiririca, Chile) and one from Europe (Rümikon, Switzerland). We coded the extinct species from these sites, as well as ca. 2,450 modern mammal species, for three eco- logical attributes: diet (eight categories), locomotor habit (six categories), and body mass (six categories). Percentages of species in each attribute category were used to compare the five paleofaunas to 179 modern faunas from six continents using corre- spondence analysis, hierarchical clustering, similarity percentage, and classification trees. The four South American paleofaunas were found to be most similar to Afrotrop- ical, Indo-Malayan, and Palearctic modern faunas and, similarly, the European paleo- fauna most resembled faunas from a biome not currently present in the Palearctic. Our study highlights important differences in community structure between ancient and modern South American mammal faunas and suggests that modern mammalian com- munities from other continents are better analogues for ancient South American com- munities than modern South American faunas. -
A Survey of Cenozoic Mammal Baramins
The Proceedings of the International Conference on Creationism Volume 8 Print Reference: Pages 217-221 Article 43 2018 A Survey of Cenozoic Mammal Baramins C Thompson Core Academy of Science Todd Charles Wood Core Academy of Science Follow this and additional works at: https://digitalcommons.cedarville.edu/icc_proceedings DigitalCommons@Cedarville provides a publication platform for fully open access journals, which means that all articles are available on the Internet to all users immediately upon publication. However, the opinions and sentiments expressed by the authors of articles published in our journals do not necessarily indicate the endorsement or reflect the views of DigitalCommons@Cedarville, the Centennial Library, or Cedarville University and its employees. The authors are solely responsible for the content of their work. Please address questions to [email protected]. Browse the contents of this volume of The Proceedings of the International Conference on Creationism. Recommended Citation Thompson, C., and T.C. Wood. 2018. A survey of Cenozic mammal baramins. In Proceedings of the Eighth International Conference on Creationism, ed. J.H. Whitmore, pp. 217–221. Pittsburgh, Pennsylvania: Creation Science Fellowship. Thompson, C., and T.C. Wood. 2018. A survey of Cenozoic mammal baramins. In Proceedings of the Eighth International Conference on Creationism, ed. J.H. Whitmore, pp. 217–221, A1-A83 (appendix). Pittsburgh, Pennsylvania: Creation Science Fellowship. A SURVEY OF CENOZOIC MAMMAL BARAMINS C. Thompson, Core Academy of Science, P.O. Box 1076, Dayton, TN 37321, [email protected] Todd Charles Wood, Core Academy of Science, P.O. Box 1076, Dayton, TN 37321, [email protected] ABSTRACT To expand the sample of statistical baraminology studies, we identified 80 datasets sampled from 29 mammalian orders, from which we performed 82 separate analyses. -
Libro De Resúmenes
33.as JORNADAS ARGENTINAS DE PALEONTOLOGÍA DE VERTEBRADOS LIBRO DE RESÚMENES 29 al 31 de mayo de 2019 Centro Cultural Córdoba Av. Poeta Lugones 401 Córdoba, Argentina Instituciones Organizadoras Avalan COMISIÓN ORGANIZADORA Adan Tauber1-3 Augusto Haro1,2 Claudia Tambussi4 Emilia Sferco4 Federico Javier Degrange4 Gastón Martínez2 Gastón Nieto2 H. Santiago Druetta4 Ivana Tapia4 Jeremías R. A. Taborda4 Colaboradores: 3 3 Jerónimo Krapovickas Cristina Martínez Juan José López3 Miguel Pizarro1 Lila Echenique3 Natalia Imbarratta3 Lorena Adduci3 Virginia Llanos3 Manuela Demmel4 Maximiliano Fabianelli1,2 Paola Arias3 Santiago Centorbi1 1Facultad de Ciencias Exactas, Físicas y Naturales (UNC) 2Museo de Paleontología de la FCEFyN (UNC) 3Museo de Ciencias Naturales Dr. Arturo U. Illia (Agencia Córdoba Cultura) 4Centro de Investigaciones en Ciencias de la Tierra (UNC, CONICET) COMITÉ CIENTÍFICO López Arbarello, Adriana (Ludwig-Maximilians-University of Munich) Arnal, Michelle (Museo de La Plata) Bonini, Ricardo (Museo de La Plata) Candela, Adriana (Museo de La Plata) Carballido, José Luis (Museo Egidio Feruglio) Desojo, Julia (Museo de La Plata) Cassini, Guillermo (Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”) Ezcurra, Martín (Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”) Fernícola, Juan Carlos (Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”) González Ruiz, Laureano (Centro De InvestigacionEsquelde Montaña y Estepa Patagonica) Ibiricu, Lucio (Instituto Patagónico de Geología y Paleontología) Isasi, Marcelo (Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”) Krapovickas, Verónica (Instituto de Estudios Andinos "Fon Pablo Groeber") Nicoli, Laura (Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”) Pérez, María Encarnación (Museo Egidio Feruglio) Zamorano, Martín (Museo de La Plata) ÍNDICE CRONOGRAMA EXTENDIDO 11 Acuña Suarez, G.E., K.V. Chichkoyan, P.S. -
Decoupling the Spread of Grasslands from the Evolution of Grazer-Type Herbivores in South America
ARTICLE Received 3 Jul 2012 | Accepted 17 Jan 2013 | Published 12 Feb 2013 DOI: 10.1038/ncomms2508 Decoupling the spread of grasslands from the evolution of grazer-type herbivores in South America Caroline A.E. Stro¨mberg1, Regan E. Dunn1, Richard H. Madden2, Matthew J. Kohn3 & Alfredo A. Carlini4 The evolution of high-crowned cheek teeth (hypsodonty) in herbivorous mammals during the late Cenozoic is classically regarded as an adaptive response to the near-global spread of grass-dominated habitats. Precocious hypsodonty in middle Eocene (B38 million years (Myr) ago) faunas from Patagonia, South America, is therefore thought to signal Earth’s first grasslands, 20 million years earlier than elsewhere. Here, using a high-resolution, 43–18 million-year record of plant silica (phytoliths) from Patagonia, we show that although open-habitat grasses existed in southern South America since the middle Eocene (B40 Myr ago), they were minor floral components in overall forested habitats between 40 and 18 Myr ago. Thus, distinctly different, continent-specific environmental conditions (arid grasslands versus ash-laden forests) triggered convergent cheek–tooth evolution in Cenozoic herbivores. Hypsodonty evolution is an important example where the present is an insufficient key to the past, and contextual information from fossils is vital for understanding processes of adaptation. 1 Department of Biology and Burke Museum of Natural History and Culture, University of Washington, Seattle, Washington 98195, USA. 2 Department of Organismal Biology and Anatomy, University of Chicago, Chicago, Illinois 60637, USA. 3 Department of Geosciences, Boise State University, Boise, Idaho 83725, USA. 4 Departamento de Paleontologı´a de Vertebrados, Universidad Nacional de La Plata, La Plata B1900FWA, Argentina (CONICET). -
Revised Geochronology of the Casamayoran South American Land Mammal Age: Climatic and Biotic Implications
Revised geochronology of the Casamayoran South American Land Mammal Age: Climatic and biotic implications Richard F. Kay*†, Richard H. Madden*, M. Guiomar Vucetich‡, Alfredo A. Carlini‡, Mario M. Mazzoni‡§, Guillermo H. Re¶, Matthew Heizlerʈ, and Hamish Sandeman** *Department of Biological Anthropology and Anatomy, Duke University, Durham, NC 27710; ‡Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Argentina; ¶Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires, Argentina; ʈDepartment of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology, Socorro, NM 87801; and **Department of Geological Sciences, Queen’s University, Kingston, ON, Canada K7L 3N6 Edited by David L. Dilcher, University of Florida, Gainesville, FL, and approved July 21, 1999 (received for review April 20, 1999) Isotopic age determinations (40Ar͞39Ar) and associated magnetic Methods and Results polarity stratigraphy for Casamayoran age fauna at Gran Barranca A stratigraphic interval (75 m) of the Gran Barranca, encompassing (Chubut, Argentina) indicate that the Barrancan ‘‘subage’’ of the the Gran Barranca and Puesto Almendra members and including Casamayoran South American Land Mammal ‘‘Age’’ is late Eocene, 18 the Barrancan, Mustersan, and Astraponote´en plus Supe´rieur to 20 million years younger than hitherto supposed. Correlations of faunas, was sampled for radiometric age determination and mag- the radioisotopically dated magnetic polarity stratigraphy at Gran netic polarity stratigraphy. Three 40Ar͞39Ar dates were obtained Barranca with the Cenozoic geomagnetic polarity time scale indicate from a sample of dark glass-rich pyroclastic tuff, MZ-7 level that Barrancan faunal levels at the Gran Barranca date to within the [stratigraphic levels in the measured composite section of the magnetochronologic interval from 35.34 to 36.62 megannums (Ma) or Sarmiento Formation at the west end of Gran Barranca are staked, 35.69 to 37.60 Ma. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Mammalian Biology 76 (2011) 101–108 Contents lists available at ScienceDirect Mammalian Biology journal homepage: www.elsevier.de/mambio Original Investigation Afrotherian affinities for endemic South American “ungulates” Federico L. Agnolin a,b, Nicolás R. Chimento c,∗ a Laboratorio de Anatomía Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Av. Ángel Gallardo 470 (C1405BDB), Buenos Aires, Argentina b Fundación de Historia Natural “Félix de Azara”, Departamento de Ciencias Naturales y Antropología, CEBBAD – Universidad Maimónides, Valentín Virasoro 732 (C1405BDB), Buenos Aires, Argentina c División Paleontología de Vertebrados, Museo de La Plata, Paseo del Bosque s/n (B1900FWA), La Plata, Buenos Aires, Argentina article info abstract Article history: The phylogenetic relationships of endemic South American ungulates are a highly debated topic. Among Received 25 November 2010 them, the most well-known clades are the Notoungulata and the Astrapotheria. Three unambiguous Accepted 3 December 2010 hard-tissue features characteristic of afrotherian mammals potentially indicate a relationship with the two South American clades: delayed cheek-tooth replacement, more than 19 thoracolumbar vertebrae, Keywords: and the presence of a well defined astragalar cotylar fossa. -
Structural Variation of the Masseter Muscle in Typothe- Ria (Mammalia, Notoungulata) Luis Marcelo SOSA1 and Daniel Alfredo GARCÍA LÓPEZ2
Serie Correlación Geológica - 34 (1): 53 - 70 Tucumán, 2018 - ISSN 1514-4186 - ISSN on-line 1666-9479 Structural variation of the masseter muscle in Typothe- ria (Mammalia, Notoungulata) Luis Marcelo SOSA1 and Daniel Alfredo GARCÍA LÓPEZ2 Resumen: VARIACIÓN ESTRUCTURAL DEL MÚSCULO MASETERO EN TYPOTHERIA (MAMMALIA, NOTOUNGULATA). La gran diversidad morfológica del orden Notoungulata se expresa en rasgos notorios, como el tamaño corporal, incluyéndose aquí desde animales del porte de un pequeño roedor (e.g., Punapithecus) hasta formas de más de una tonelada (e.g., Trigodon). Se conocen ade- más, diferentes casos de convergencia con otros placentarios, reconociéndose formas rodentiformes y otras similares a lagomorfos, perisodáctilos y artiodáctilos. Esta notable diversidad se expresa también en rasgos específicos, como la región auditiva y el aparato masticatorio. En este trabajo se presenta un análisis sobre la evolución estructural de la zona de origen del músculo masetero enfocada en el subor- den Typotheria. Se seleccionó una muestra de 12 representantes de ese grupo más dos representan- tes de notoungulados tempranamente divergentes (Henricosborniidae y Notostylopidae). La muestra abarca un lapso de más de 43 Ma (Eoceno–Pleistoceno). Se establecieron tres condiciones principales relacionadas con el origen del masetero que muestran cierto ordenamiento temporal y filogenético. La Condición 0 (e.g., Colbertia, Oldfieldthomasia) se caracteriza por el origen puntual y restringido del masetero superficial y por una zona limitada para el masetero profundo, encontrándose exclusivamen- te en formas eocenas y siendo comparable al plan generalizado presente en ciertos marsupiales (e.g., Didelphis). La Condición 1 (e.g., Notopithecus, Protypotherium) presenta un masetero profundo de desarrollo limitado y un masetero superficial asociado a un proceso descendente conspicuo, mostrando simili- tudes con Lagomorpha (e.g., Oryctolagus).