Toxodontia of Salla, Bolivia (Late Oligocene) : Taxonomy, Systematics
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Mioceno Tardío) De Entre Ríos, Argentina
Rev. bras. paleontol. 18(3):521-546, Setembro/Dezembro 2015 © 2015 by the Sociedade Brasileira de Paleontologia doi: 10.4072/rbp.2015.3.14 ACTUALIZACIÓN SISTEMÁTICA Y FILOGENIA DE LOS PROTEROTHERIIDAE (MAMMALIA, LITOPTERNA) DEL “MESOPOTAMIENSE” (MIOCENO TARDÍO) DE ENTRE RÍOS, ARGENTINA GABRIELA INÉS SCHMIDT Laboratorio de Paleontología de Vertebrados, Centro de Investigaciones Científi cas y Transferencia de Tecnología a la Producción (CICYTTP-CONICET), Materi y España (E3105BWA), Diamante, Entre Ríos, Argentina. [email protected] ABSTRACT – SYSTEMATIC UPDATE AND PHYLOGENY OF THE PROTEROTHERIIDAE (MAMMALIA, LITOPTERNA) FROM THE “MESOPOTAMIENSE” (LATE MIOCENE) OF ENTRE RÍOS PROVINCE, ARGENTINA. A systematic update of the species of Proterotheriidae (Litopterna) from the “Mesopotamiense” of Entre Ríos Province (Argentina) is performed, and their phylogenetic relationships with other members of the family are tested. Brachytherium cuspidatum Ameghino is validated (considered nomen dubium hitherto) and a sexual dimorphism is proposed for this species. This idea is based on metric, but not morphological, differences among the specimens included in it, which is supported by a discriminant analysis. Neobrachytherium ameghinoi Soria and Proterotherium cervioides Ameghino are also valid, and Epitherium? eversus (Ameghino) is assigned to the genus Diadiaphorus. Detailed descriptions of the specimens are presented for each taxon, and their diagnosis are revised. Key words: Proterotheriidae, Ituzaingó Formation, Entre Ríos Province, systematics, phylogeny. RESUMO – Uma atualização sistemática, das espécies de Proterotheriidae (Litopterna) presentes no “Mesopotamiense” da Província de Entre Ríos, Argentina, é realizada, bem como são testadas as suas relações fi logenéticas com outros integrantes da família. Brachytherium cuspidatum (previamente considerada nomen dubium) é revalidada, e um dimorfi smo sexual é proposto para esta espécie. -
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.). -
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. -
A Dated Phylogeny of Marsupials Using a Molecular Supermatrix and Multiple Fossil Constraints
Journal of Mammalogy, 89(1):175–189, 2008 A DATED PHYLOGENY OF MARSUPIALS USING A MOLECULAR SUPERMATRIX AND MULTIPLE FOSSIL CONSTRAINTS ROBIN M. D. BECK* School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales 2052, Australia Downloaded from https://academic.oup.com/jmammal/article/89/1/175/1020874 by guest on 25 September 2021 Phylogenetic relationships within marsupials were investigated based on a 20.1-kilobase molecular supermatrix comprising 7 nuclear and 15 mitochondrial genes analyzed using both maximum likelihood and Bayesian approaches and 3 different partitioning strategies. The study revealed that base composition bias in the 3rd codon positions of mitochondrial genes misled even the partitioned maximum-likelihood analyses, whereas Bayesian analyses were less affected. After correcting for base composition bias, monophyly of the currently recognized marsupial orders, of Australidelphia, and of a clade comprising Dasyuromorphia, Notoryctes,and Peramelemorphia, were supported strongly by both Bayesian posterior probabilities and maximum-likelihood bootstrap values. Monophyly of the Australasian marsupials, of Notoryctes þ Dasyuromorphia, and of Caenolestes þ Australidelphia were less well supported. Within Diprotodontia, Burramyidae þ Phalangeridae received relatively strong support. Divergence dates calculated using a Bayesian relaxed molecular clock and multiple age constraints suggested at least 3 independent dispersals of marsupials from North to South America during the Late Cretaceous or early Paleocene. Within the Australasian clade, the macropodine radiation, the divergence of phascogaline and dasyurine dasyurids, and the divergence of perameline and peroryctine peramelemorphians all coincided with periods of significant environmental change during the Miocene. An analysis of ‘‘unrepresented basal branch lengths’’ suggests that the fossil record is particularly poor for didelphids and most groups within the Australasian radiation. -
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. -
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 -
New Insights Into the Anatomy of Extinct Paucituberculatan Marsupials
Swiss J Palaeontol DOI 10.1007/s13358-014-0063-9 An exceptionally well-preserved skeleton of Palaeothentes from the Early Miocene of Patagonia, Argentina: new insights into the anatomy of extinct paucituberculatan marsupials Analia M. Forasiepi • Marcelo R. Sa´nchez-Villagra • Thomas Schmelzle • Sandrine Ladeve`ze • Richard F. Kay Received: 8 September 2013 / Accepted: 13 February 2014 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2014 Abstract During the Cenozoic paucituberculatans were an anterior semicircular canal (SC) projecting slightly much more diverse taxonomically and ecomorphologically dorsally from the dorsal-most point of the posterior SC, and than the three extant genera of shrew-like marsupials. lateral and posterior SCs projecting laterally to the same Among paucituberculatans, palaeothentids were abundant level. On the basis of postcranial anatomy, previous studies during the Early Miocene, although most of the fossil have demonstrated that P. lemoinei was an agile cursorial remains consist of isolated teeth or fragmentary jaws. We form, an inference supported by study of the new post- describe a new and exceptional partial skeleton of Palaeo- cranial elements. thentes lemoinei (Palaeothentidae), collected from the Santa Cruz Formation (Santacrucian age, Early Miocene) Keywords Marsupialia Á Metatheria Á Cenozoic Á in Patagonia. Whereas the skull of P. lemoinei has more South America Á Skull Á Inner ear Á Postcranium plesiomorphic traits in the face, palate, and cranial vault than that of living paucituberculatans, the dental mor- Abbreviations phology is more derived. The osseous inner ear was examined using micro-CT scanning, revealing a cochlea Institutional abbreviations with 1.9 turns, the presence of a ‘‘second crus commune’’, FMNH Field Museum of Natural History, Chicago, USA IEEUACH Universidad Austral de Chile, A. -
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. -
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]). -
Cambios En La Riqueza Taxonómica Y En Las Tasas De Primera Y Última Aparición De Los Proterotheriidae (Mammalia, Litopterna) Durante El Cenozoico
Estudios Geológicos, 62 (1) enero-diciembre 2006, 155-166 ISSN: 0367-0449 Cambios en la riqueza taxonómica y en las tasas de primera y última aparición de los Proterotheriidae (Mammalia, Litopterna) durante el Cenozoico A. L. Villafañe1, E. Ortiz-Jaureguizar2, M. Bond3 RESUMEN Los Proterotheriidae han sido registrados desde el Paleoceno Superior hasta el Holoceno [«Edades- mamífero (= SALMAs) Itaboraiense-Lujanense]. Son mayoritariamente braquiodontes, cursoriales, de tamaño pequeño a mediano, que muestran una temprana tendencia hacia la monodactilia. Los objetivos del presente trabajo son: 1) analizar los cambios en la diversidad y las tasas de recambio de estos «ungulados» sudamericanos (tanto a nivel de especies como de géneros) a lo largo de todo su biocrón; y 2) vincular estos cambios con las principales variaciones en las condiciones climático-ambientales. Los resultados muestran que durante el lapso comprendido entre las SALMAs Itaboraiense-Lujanense, los Proterotheriidae sufren grandes cambios en la diversidad genérica y específica, con cuatro picos de diversidad (dos menores en las SALMAs Casamayorense y Laventense y dos mayores en las SALMAs Santacrucense y Huayqueriense). Estos picos están interrumpidos por dos hiatos en el registro fósil, en las SALMAs Divisaderense-Tinguiririquense y en la SALMA Mayoense, respectivamente). En líneas generales, los Proterotheriidae muestran durante su biocrón una elevada tasa de recambio tanto a nivel de géneros como de especies, razón por la cual esta familia puede ser considerada de gran valor bio- cronológico. Las fluctuaciones en la riqueza taxonómica y las tasas de recambio taxonómico guardan relación con los cambios climático-ambientales acaecidos durante el Cenozoico. Asimismo, la mayor diversidad se observa en aquellas SALMAs en las que hay una relación relativamente equilibrada entre bosques y pastizales, declinando marcadamente la diversidad a medida que los ambientes se tornan más abiertos y áridos. -
8. Primate Evolution
8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America.