Notoungulata, Mammalia)
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Zeitschrift Für Säugetierkunde)
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Mammalian Biology (früher Zeitschrift für Säugetierkunde) Jahr/Year: 1964 Band/Volume: 29 Autor(en)/Author(s): Thenius Erich Artikel/Article: Herkunft und Entwicklung der südamerikanischen Säugetierfauna 267-284 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/ Herkunft und Entwicklung der südamerikanischen Säugetierfauna ^ Von Erich Thenius Eingang des Ms. 30. 7. J964 Einleitung Die rezente südamerikanische Säugetierfauna hat durch ihre charakteristische Zusam- mensetzung seit jeher die Tiergeographen interessiert, ist doch die neotropische Region eines der kennzeichnendsten Faunengebiete überhaupt. Um die Zusammensetzung der Fauna verstehen zu können, ist die Kenntnis des geschichtlichen Werdens notwendig. Dieses Werden kann jedoch aus der gegenwärtigen Fauna bzw. der Verbreitung der einzelnen Arten allein nicht rekonstruiert werden. Dazu sind Fossilfunde erforderlich. Erst diese lassen, sofern sie stratigraphisch sicher eingestuft sind, durch ihr verschieden- zeitliches Auftreten Schlußfolgerungen über die wechselnde Zusammensetzung der Fauna im Laufe der Zeit zu. Sind überdies die stammesgeschichtlichen Zusammenhänge bekannt, so können — sofern die Fossilfunde dazu ausreichen — auch Aussagen über die Geschichte der einzelnen Faunengruppen gemacht werden. Aber erst in Verbin- dung mit der Kenntnis des paläogeographischen Werdeganges des Kontinentes kann schließlich die -
Chronostratigraphy of the Mammal-Bearing Paleocene of South America 51
Thierry SEMPERE biblioteca Y. Joirriiol ofSoiiih Ainorirari Euirli Sciriin~r.Hit. 111. No. 1, pp. 49-70, 1997 Pergamon Q 1‘197 PublisIlcd hy Elscvicr Scicncc Ltd All rights rescrvcd. Printed in Grcnt nrilsin PII: S0895-9811(97)00005-9 0895-9X 11/97 t I7.ol) t o.(x) -. ‘Inshute qfI Human Origins, 1288 9th Street, Berkeley, California 94710, USA ’Orstom, 13 rue Geoffroy l’Angevin, 75004 Paris, France 3Department of Geosciences, The University of Arizona, Tucson, Arizona 85721, USA Absfract - Land mammal faunas of Paleocene age in the southern Andean basin of Bolivia and NW Argentina are calibrated by regional sequence stratigraphy and rnagnetostratigraphy. The local fauna from Tiupampa in Bolivia is -59.0 Ma, and is thus early Late Paleocene in age. Taxa from the lower part of the Lumbrera Formation in NW Argentina (long regarded as Early Eocene) are between -58.0-55.5 Ma, and thus Late Paleocene in age. A reassessment of the ages of local faunas from lhe Rfo Chico Formation in the San Jorge basin, Patagonia, southern Argentina, shows that lhe local fauna from the Banco Negro Infeiior is -60.0 Ma, mak- ing this the most ancient Cenozoic mammal fauna in South,America. Critical reevaluation the ltaboraí fauna and associated or All geology in SE Brazil favors lhe interpretation that it accumulated during a sea-level lowsland between -$8.2-56.5 Ma. known South American Paleocene land inammal faunas are thus between 60.0 and 55.5 Ma (i.e. Late Paleocene) and are here assigned to the Riochican Land Maminal Age, with four subages (from oldest to youngest: Peligrian, Tiupampian, Ilaboraian, Riochican S.S.). -
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. -
Teeth Complexity, Hypsodonty and Body Mass in Santacrucian (Early Miocene) Notoungulates (Mammalia) Guillermo H
Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 106, 303–313, 2017 Teeth complexity, hypsodonty and body mass in Santacrucian (Early Miocene) notoungulates (Mammalia) Guillermo H. Cassini1,2,7, Santiago Herna´ndez Del Pino3,7, Nahuel A. Mun˜oz4,7, M. V. Walter G. Acosta5, Mercedes Ferna´ndez2,6,7, M. Susana Bargo4,8 and Sergio F. Vizcaı´no4,7 1 Divisio´n Mastozoologı´a, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Ciudad Auto´noma de Buenos Aires, Argentina. Email: [email protected] 2 Departamento de Ciencias Ba´sicas, Universidad Nacional de Luja´n, Luja´n, Buenos Aires, Argentina. Email: [email protected] 3 Paleontologı´a, Instituto de Nivologı´a, Glaciologı´a y Ciencias Ambientales, Centro Cientı´fico Tecnolo´gico – CONICET Mendoza, Mendoza, Argentina. Email: [email protected] 4 Divisio´n Paleontologı´a Vertebrados, Museo de La Plata, Unidades de Investigacio´n Anexo Museo, FCNyM-UNLP, 60 y 122, 1900 La Plata, Argentina. Email: [email protected]; [email protected]; [email protected] 5 Ca´tedra de Semiologı´a, Facultad de Ciencias Veterinarias, Universidad Nacional de La Plata, Calle 60 y 118 s/n, La Plata, Argentina. Email: [email protected] 6 Divisio´n Paleontologı´a de Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Ciudad Auto´noma de Buenos Aires, Argentina. 7 CONICET. Consejo Nacional de Investigaciones Cientı´ficas y Te´cnicas. 8 CIC. Comisio´n de Investigaciones Cientı´ficas de la provincia de Buenos Aires. ABSTRACT: Notoungulates, native South American fossil mammals, have been recently objective of several palaeoecological studies. -
Revised Stratigraphy of Neogene Strata in the Cocinetas Basin, La Guajira, Colombia
Swiss J Palaeontol (2015) 134:5–43 DOI 10.1007/s13358-015-0071-4 Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia F. Moreno • A. J. W. Hendy • L. Quiroz • N. Hoyos • D. S. Jones • V. Zapata • S. Zapata • G. A. Ballen • E. Cadena • A. L. Ca´rdenas • J. D. Carrillo-Bricen˜o • J. D. Carrillo • D. Delgado-Sierra • J. Escobar • J. I. Martı´nez • C. Martı´nez • C. Montes • J. Moreno • N. Pe´rez • R. Sa´nchez • C. Sua´rez • M. C. Vallejo-Pareja • C. Jaramillo Received: 25 September 2014 / Accepted: 2 February 2015 / Published online: 4 April 2015 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2015 Abstract The Cocinetas Basin of Colombia provides a made exhaustive paleontological collections, and per- valuable window into the geological and paleontological formed 87Sr/86Sr geochronology to document the transition history of northern South America during the Neogene. from the fully marine environment of the Jimol Formation Two major findings provide new insights into the Neogene (ca. 17.9–16.7 Ma) to the fluvio-deltaic environment of the history of this Cocinetas Basin: (1) a formal re-description Castilletes (ca. 16.7–14.2 Ma) and Ware (ca. 3.5–2.8 Ma) of the Jimol and Castilletes formations, including a revised formations. We also describe evidence for short-term pe- contact; and (2) the description of a new lithostratigraphic riodic changes in depositional environments in the Jimol unit, the Ware Formation (Late Pliocene). We conducted and Castilletes formations. The marine invertebrate fauna extensive fieldwork to develop a basin-scale stratigraphy, of the Jimol and Castilletes formations are among the richest yet recorded from Colombia during the Neogene. -
PROGRAMME ABSTRACTS AGM Papers
The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important. -
Mammalia, Notoungulata), from the Eocene of Patagonia, Argentina
Palaeontologia Electronica palaeo-electronica.org An exceptionally well-preserved skeleton of Thomashuxleya externa (Mammalia, Notoungulata), from the Eocene of Patagonia, Argentina Juan D. Carrillo and Robert J. Asher ABSTRACT We describe one of the oldest notoungulate skeletons with associated cranioden- tal and postcranial elements: Thomashuxleya externa (Isotemnidae) from Cañadón Vaca in Patagonia, Argentina (Vacan subage of the Casamayoran SALMA, middle Eocene). We provide body mass estimates given by different elements of the skeleton, describe the bone histology, and study its phylogenetic position. We note differences in the scapulae, humerii, ulnae, and radii of the new specimen in comparison with other specimens previously referred to this taxon. We estimate a body mass of 84 ± 24.2 kg, showing that notoungulates had acquired a large body mass by the middle Eocene. Bone histology shows that the new specimen was skeletally mature. The new material supports the placement of Thomashuxleya as an early, divergent member of Toxodon- tia. Among placentals, our phylogenetic analysis of a combined DNA, collagen, and morphology matrix favor only a limited number of possible phylogenetic relationships, but cannot yet arbitrate between potential affinities with Afrotheria or Laurasiatheria. With no constraint, maximum parsimony supports Thomashuxleya and Carodnia with Afrotheria. With Notoungulata and Litopterna constrained as monophyletic (including Macrauchenia and Toxodon known for collagens), these clades are reconstructed on the stem -
Apa 1068.Qxd
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 41 (3): 475-484. Buenos Aires, 30-09-2004 ISSN 0002-7014 A new South American mioclaenid (Mammalia: Ungulatomorpha) from the Tertiary of Patagonia, Argentina Javier N. GELFO1 Resumen. UN NUEVO MIOCLAENIDO SUDAMERICANO (MAMMALIA: UNGULATOMORPHA) DEL TERCIARIO DE PATAGONIA, ARGENTINA. Se describe un nuevo “condilartro” Mioclaenidae, proveniente de la Edad Mamífero Casamayorense, Subedad Barranquense, de Paso de Indios, Provincia del Chubut. El nuevo ta- xón Pascualodus patagoniensis gen. et sp. nov., representado por un molar superior izquierdo, es compara- do con otros Mioclaenidae, con los Didolodontidae y los más primitivos Litopterna. Una hipótesis filoge- nética provisoria es expresada a través de un cladograma de consenso estricto y uno de compromiso de mayoría. Si bien el análisis confirma la agrupación de los taxa sudamericanos en un grupo monofilético, existen numerosos puntos sin resolver. Pascualodus patagoniensis se ubica como un taxón terminal, en una politomía que reúne por un lado a los Mioclaenidae sudamericanos y por el otro, a los Didolodontidae y Litopterna. Por otra parte la consideración de caracteres dentales superiores de Escribania chubutensis, pre- viamente el único Mioclaenidae patagónico conocido, modifica sus relaciones filogenéticas vinculándolo al Didolodontidae Didolodus sp. La asignación de Pascualodus patagoniensis a los Mioclaenidae constituye el registro más moderno y el más austral de la familia. Abstract. A new Mioclaenidae “condylarth” of the Casamayoran Land Mammal Age, Barrancan subage, from Paso de Indios, Chubut Province is described. The new taxon Pascualodus patagoniensis gen. et sp. nov., represented by a left upper first molar, is compared with other Mioclaenidae; the Didolodontidae and some primitive litopterns. -
Diversidad Con Alas
VI Congreso Latinoamericano de Paleontología de Vertebrados Diversidad con alas Villa de Leyva, Boyacá, Colombia Agosto 20 al 25 de 2018 PRESENCIA DE GRANASTRAPOTHERIUM EN EL MIOCENO DE TUMBES (NOROESTE DEL PERÚ): PRIMER REGISTRO DE ASTRAPOTERIO EN LA COSTA PERUANA Jean-Noël Martinez/ Instituto de Paleontología, Universidad Nacional de Piura / [email protected]/ Perú Darin Croft /Department of Anatomy, Case Western Reserve University, School of Medicine/ [email protected]/ USA El orden Astrapotheria reúne mamíferos ungulados de Sudamérica y Antártida cuyo registro se extiende cronológicamente desde el Paleoceno superior hasta el Mioceno medio. Los miembros más característicos de este orden, los Astrapotheriidae, conocidos desde el Eoceno, eran animales de gran tamaño con curiosos rasgos anatómicos que evocan los hipopótamos por la morfología de sus caninos sobresalientes y los tapires por la ubicación de sus fosas nasales, sugiriendo la presencia de una proboscis. Bien conocidos a través del continente sudamericano, su registro es muy escaso en el Perú, siendo mencionados en una localidad de la región amazónica y atribuidos a los géneros Xenastrapotherium y Granastrapotherium. La presencia conjunta de estos dos géneros en la denominada fauna local de Fitzcarrald evoca la asociación Xenastrapotherium kraglievichi - Granastrapotherium snorki del Mioceno medio de La Venta (Colombia) y marca el final de la historia evolutiva del orden Astrapotheria. Dos otros sitios ubicados a la frontera Perú- Brasil constituyen los registros geográficamente más cercanos a la fauna local de Fitzcarrald. El presente trabajo reporta el hallazgo de los maxilares de un astrapoterio en la región de Tumbes (extremo noroeste del Perú). El fósil arrancado por erosión natural a sus estratos de origen pudo ser fácilmente contextualizado. -
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]). -
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.