Oldest Known Euarchontan Tarsals and Affinities of Paleocene Purgatorius to Primates
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ECOLOGY and the EXT]NCTTON of the DINOSAURS Robert E. Sl
37 ECOLOGYAND THE EXT]NCTTONOF THE DINOSAURS Leigh Van Valen Robert E. Sl-oan Dept. of Biolory Dept. of Geologl and Geophysics University of Chicago University of Minnesota Chicago, Ill . 6063T l4inneapolis, Minn. 551+55 Received November 3, I9T, ABSTMCT: The first d.irect evidence of the process of d.inosaur extinction comes from a sequence of vertebrate faunas in Montana, spanning the Cretaceous-Pal-eocene boundary. Much of the-physical, environment can be reconstructed. The extinction here lasted. roughly 10" years and proceeded by ordinary community evol-ution. Botanical- evidence shows a decline in winter temperatures and a replacement of much of the original subtropicaf flora by a temperate fl-ora. This southward.- moving community l-acked dinosaurs (and. marsupials) and. replaced the subtropical terrestrial community, apparently by d.iffuse competition. Mammalswere conunon but subord.inate in energll flov in the subtropical community; the temperate communi- ty included early members of the large Paleocene placental radiation. About seven d.inosaur species persisted d.uring the infiltratlon, but they gradually became rarer and then disappeared". The process implies that dinosaur extinction occurred. somewhat later in the tropics than in Montana. Some slight evidence supports this. The contemporaneous major extinction in the sea was also gradual and perhaps as long. ft is also erplicable by diffuse competition in an increasingly rigorous environment. *lcli Di-nosaurs were spectacul-ar animal-s. Althougfu some were probably feathered q.nd gave rise to bird.s (Ostrom, 1971+), dinosaurs as d.inosaurs had the misfortune to become extinct. Until recently (t) ttrere has been effectively no actual evi- d"enceon the cause of this extinction, and speculation has been unbounded. -
Diagnosis and Differentiation of the Order Primates
YEARBOOK OF PHYSICAL ANTHROPOLOGY 30:75-105 (1987) Diagnosis and Differentiation of the Order Primates FREDERICK S. SZALAY, ALFRED L. ROSENBERGER, AND MARIAN DAGOSTO Department of Anthropolog* Hunter College, City University of New York, New York, New York 10021 (F.S.S.); University of Illinois, Urbanq Illinois 61801 (A.L. R.1; School of Medicine, Johns Hopkins University/ Baltimore, h4D 21218 (M.B.) KEY WORDS Semiorders Paromomyiformes and Euprimates, Suborders Strepsirhini and Haplorhini, Semisuborder Anthropoidea, Cranioskeletal morphology, Adapidae, Omomyidae, Grades vs. monophyletic (paraphyletic or holophyletic) taxa ABSTRACT We contrast our approach to a phylogenetic diagnosis of the order Primates, and its various supraspecific taxa, with definitional proce- dures. The order, which we divide into the semiorders Paromomyiformes and Euprimates, is clearly diagnosable on the basis of well-corroborated informa- tion from the fossil record. Lists of derived features which we hypothesize to have been fixed in the first representative species of the Primates, Eupri- mates, Strepsirhini, Haplorhini, and Anthropoidea, are presented. Our clas- sification of the order includes both holophyletic and paraphyletic groups, depending on the nature of the available evidence. We discuss in detail the problematic evidence of the basicranium in Paleo- gene primates and present new evidence for the resolution of previously controversial interpretations. We renew and expand our emphasis on postcra- nial analysis of fossil and living primates to show the importance of under- standing their evolutionary morphology and subsequent to this their use for understanding taxon phylogeny. We reject the much advocated %ladograms first, phylogeny next, and scenario third” approach which maintains that biologically founded character analysis, i.e., functional-adaptive analysis and paleontology, is irrelevant to genealogy hypotheses. -
Mammalia, Plesiadapiformes) As Reflected on Selected Parts of the Postcranium
SHAPE MEETS FUNCTION: STRUCTURAL MODELS IN PRIMATOLOGY Edited by Emiliano Bruner Proceedings of the 20th Congress of the International Primatological Society Torino, Italy, 22-28 August 2004 MORPHOLOGY AND MORPHOMETRICS JASs Journal of Anthropological Sciences Vol. 82 (2004), pp. 103-118 Locomotor adaptations of Plesiadapis tricuspidens and Plesiadapis n. sp. (Mammalia, Plesiadapiformes) as reflected on selected parts of the postcranium Dionisios Youlatos1, Marc Godinot2 1) Aristotle University of Thessaloniki, School of Biology, Department of Zoology, GR-54124 Thessaloniki, Greece. email [email protected] 2) Ecole Pratique des Hautes Etudes, UMR 5143, Case Courrier 38, Museum National d’Histoire Naturelle, Institut de Paleontologie, 8 rue Buffon, F-75005 Paris, France Summary – Plesiadapis is one of the best-known Plesiadapiformes, a group of Archontan mammals from the Late Paleocene-Early Eocene of Europe and North America that are at the core of debates con- cerning primate origins. So far, the reconstruction of its locomotor behavior has varied from terrestrial bounding to semi-arboreal scansoriality and squirrel-like arboreal walking, bounding and claw climbing. In order to elucidate substrate preferences and positional behavior of this extinct archontan, the present study investigates quantitatively selected postcranial characters of the ulna, radius, femur, and ungual pha- langes of P. tricuspidens and P. n .sp. from three sites (Cernay-les-Reims, Berru, Le Quesnoy) in the Paris Basin, France. These species of Plesiadapis was compared to squirrels of different locomotor habits in terms of selected functional indices that were further explored through a Principal Components Analysis (PCA), and a Discriminant Functions Analysis (DFA). The indices treated the relative olecranon height, form of ulnar shaft, shape and depth of radial head, shape of femoral distal end, shape of femoral trochlea, and dis- tal wedging of ungual phalanx, and placed Plesiadapis well within arboreal quadrupedal, clambering, and claw climbing squirrels. -
SMC 136 Gazin 1958 1 1-112.Pdf
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 136, NUMBER 1 Cftarlesi 3B, anb JKarp "^aux OTalcott 3^es(earcf) Jf unb A REVIEW OF THE MIDDLE AND UPPER EOCENE PRIMATES OF NORTH AMERICA (With 14 Plates) By C. LEWIS GAZIN Curator, Division of Vertebrate Paleontology United States National Museum Smithsonian Institution (Publication 4340) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JULY 7, 1958 THE LORD BALTIMORE PRESS, INC. BALTIMORE, MD., U. S. A. CONTENTS Page Introduction i Acknowledgments 2 History of investigation 4 Geographic and geologic occurrence 14 Environment I7 Revision of certain lower Eocene primates and description of three new upper Wasatchian genera 24 Classification of middle and upper Eocene forms 30 Systematic revision of middle and upper Eocene primates 31 Notharctidae 31 Comparison of the skulls of Notharctus and Smilodectcs z:^ Omomyidae 47 Anaptomorphidae 7Z Apatemyidae 86 Summary of relationships of North American fossil primates 91 Discussion of platyrrhine relationships 98 References 100 Explanation of plates 108 ILLUSTRATIONS Plates (All plates follow page 112) 1. Notharctus and Smilodectes from the Bridger middle Eocene. 2. Notharctus and Smilodectes from the Bridger middle Eocene. 3. Notharctus and Smilodectcs from the Bridger middle Eocene. 4. Notharctus and Hemiacodon from the Bridger middle Eocene. 5. Notharctus and Smilodectcs from the Bridger middle Eocene. 6. Omomys from the middle and lower Eocene. 7. Omomys from the middle and lower Eocene. 8. Hemiacodon from the Bridger middle Eocene. 9. Washakius from the Bridger middle Eocene. 10. Anaptomorphus and Uintanius from the Bridger middle Eocene. 11. Trogolemur, Uintasorex, and Apatcmys from the Bridger middle Eocene. 12. Apatemys from the Bridger middle Eocene. -
New Fossil Discovery Illuminates the Lives of the Earliest Primates 24 February 2021
New fossil discovery illuminates the lives of the earliest primates 24 February 2021 Royal Society Open Science. "This discovery is exciting because it represents the oldest dated occurrence of archaic primates in the fossil record," Chester said. "It adds to our understanding of how the earliest primates separated themselves from their competitors following the demise of the dinosaurs." Chester and Gregory Wilson Mantilla, Burke Museum Curator of Vertebrate Paleontology and University of Washington biology professor, were co-leads on this study, where the team analyzed fossilized teeth found in the Hell Creek area of northeastern Montana. The fossils, now part of the collections at the University of California Museum of Paleontology, Berkeley, are estimated to be 65.9 Shortly after the extinction of the dinosaurs, the earliest million years old, about 105,000 to 139,000 years known archaic primates, such as the newly described after the mass extinction event. species Purgatorius mckeeveri shown in the foreground, quickly set themselves apart from their competition -- like Based on the age of the fossils, the team estimates the archaic ungulate mammal on the forest floor -- by that the ancestor of all primates (the group specializing in an omnivorous diet including fruit found including plesiadapiforms and today's primates up in the trees. Credit: Andrey Atuchin such as lemurs, monkeys, and apes) likely emerged by the Late Cretaceous—and lived alongside large dinosaurs. Stephen Chester, an assistant professor of anthropology and paleontologist at the Graduate Center, CUNY and Brooklyn College, was part of a team of 10 researchers from across the United States who analyzed several fossils of Purgatorius, the oldest genus in a group of the earliest-known primates called plesiadapiforms. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Geology and Vertebrate Paleontology of Western and Southern North America
OF WESTERN AND SOUTHERN NORTH AMERICA OF WESTERN AND SOUTHERN NORTH PALEONTOLOGY GEOLOGY AND VERTEBRATE Geology and Vertebrate Paleontology of Western and Southern North America Edited By Xiaoming Wang and Lawrence G. Barnes Contributions in Honor of David P. Whistler WANG | BARNES 900 Exposition Boulevard Los Angeles, California 90007 Natural History Museum of Los Angeles County Science Series 41 May 28, 2008 Paleocene primates from the Goler Formation of the Mojave Desert in California Donald L. Lofgren,1 James G. Honey,2 Malcolm C. McKenna,2,{,2 Robert L. Zondervan,3 and Erin E. Smith3 ABSTRACT. Recent collecting efforts in the Goler Formation in California’s Mojave Desert have yielded new records of turtles, rays, lizards, crocodilians, and mammals, including the primates Paromomys depressidens Gidley, 1923; Ignacius frugivorus Matthew and Granger, 1921; Plesiadapis cf. P. anceps; and Plesiadapis cf. P. churchilli. The species of Plesiadapis Gervais, 1877, indicate that Member 4b of the Goler Formation is Tiffanian. In correlation with Tiffanian (Ti) lineage zones, Plesiadapis cf. P. anceps indicates that the Laudate Discovery Site and Edentulous Jaw Site are Ti2–Ti3 and Plesiadapis cf. P. churchilli indicates that Primate Gulch is Ti4. The presence of Paromomys Gidley, 1923, at the Laudate Discovery Site suggests that the Goler Formation occurrence is the youngest known for the genus. Fossils from Member 3 and the lower part of Member 4 indicate a possible marine influence as Goler Formation sediments accumulated. On the basis of these specimens and a previously documented occurrence of marine invertebrates in Member 4d, the Goler Basin probably was in close proximity to the ocean throughout much of its existence. -
Sectional Geometry in a Simulated Fine Branch Niche
JOURNAL OF MORPHOLOGY 276:759–765 (2015) Mouse Hallucal Metatarsal Cross-Sectional Geometry in a Simulated Fine Branch Niche Craig D. Byron,1* Anthony Herrel,2,3 Elin Pauwels,4 Amelie De Muynck,4 and Biren A. Patel5,6 1Department of Biology, Mercer University, Macon, Georgia 2Departement d’Ecologie et de Gestion de la Biodiversite, CNRS/MNHN, Paris, France 3Department of Vertebrate Evolutionary Morphology, Ghent University, Gent, Belgium 4Department of Physics and Astronomy, Ghent University, UGCT, Ghent, Belgium 5Department of Cell and Neurobiology, Keck School of Medicine, University of Southern California, Los Angeles, California 6Human and Evolutionary Biology Section, Department of Biological Sciences, University of Southern California, Los Angeles, California ABSTRACT Mice raised in experimental habitats con- arboreal substrates (Le Gros Clark, 1959; Cart- taining an artificial network of narrow “arboreal” sup- mill, 1972; Szalay and Drawhorn, 1980; Sussman, ports frequently use hallucal grasps during locomotion. 1991; Schmitt and Lemelin, 2002; Bloch et al., Therefore, mice in these experiments can be used to 2007; Sargis et al., 2007). There are also examples model a rudimentary form of arboreal locomotion in an of rodent (Orkin and Pontzer, 2011), carnivoran animal without other morphological specializations for using a fine branch niche. This model would prove use- (Fabre et al., 2013), marsupial (Lemelin and ful to better understand the origins of arboreal behav- Schmitt, 2007; Shapiro et al., 2014), and nonmam- iors in mammals like primates. In this study, we malian vertebrates including frogs, lizards, and examined if locomotion on these substrates influences birds (Herrel et al., 2013; Sustaita et al., 2013) the mid-diaphyseal cross-sectional geometry of mouse that are effective in this niche without primate- metatarsals. -
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. -
Resolving the Relationships of Paleocene Placental Mammals
Biol. Rev. (2015), pp. 000–000. 1 doi: 10.1111/brv.12242 Resolving the relationships of Paleocene placental mammals Thomas J. D. Halliday1,2,∗, Paul Upchurch1 and Anjali Goswami1,2 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, U.K. 2Department of Genetics, Evolution and Environment, University College London, Gower Street, London WC1E 6BT, U.K. ABSTRACT The ‘Age of Mammals’ began in the Paleocene epoch, the 10 million year interval immediately following the Cretaceous–Palaeogene mass extinction. The apparently rapid shift in mammalian ecomorphs from small, largely insectivorous forms to many small-to-large-bodied, diverse taxa has driven a hypothesis that the end-Cretaceous heralded an adaptive radiation in placental mammal evolution. However, the affinities of most Paleocene mammals have remained unresolved, despite significant advances in understanding the relationships of the extant orders, hindering efforts to reconstruct robustly the origin and early evolution of placental mammals. Here we present the largest cladistic analysis of Paleocene placentals to date, from a data matrix including 177 taxa (130 of which are Palaeogene) and 680 morphological characters. We improve the resolution of the relationships of several enigmatic Paleocene clades, including families of ‘condylarths’. Protungulatum is resolved as a stem eutherian, meaning that no crown-placental mammal unambiguously pre-dates the Cretaceous–Palaeogene boundary. Our results support an Atlantogenata–Boreoeutheria split at the root of crown Placentalia, the presence of phenacodontids as closest relatives of Perissodactyla, the validity of Euungulata, and the placement of Arctocyonidae close to Carnivora. Periptychidae and Pantodonta are resolved as sister taxa, Leptictida and Cimolestidae are found to be stem eutherians, and Hyopsodontidae is highly polyphyletic. -
Late Paleocene) of the Eastern Crazy Mountain Basin, Montana
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 26, NO. 9, p. 157-196 December 3 1, 1983 MAMMALIAN FAUNA FROM DOUGLASS QUARRY, EARLIEST TIFFANIAN (LATE PALEOCENE) OF THE EASTERN CRAZY MOUNTAIN BASIN, MONTANA BY DAVID W. KRAUSE AND PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director Gerald R. Smith, Editor This series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan, 48 109. VOLS. 11-XXVI. Parts of volumes may be obtained if available. Price lists available upon inquiry. MAMMALIAN FAUNA FROM DOUGLASS QUARRY, EARLIEST TIFFANIAN (LATE PALEOCENE) OF THE EASTERN CRAZY MOUNTAIN BASIN, MONTANA BY David W. ~rause'and Philip D. ~in~erich' Abstract.-Douglass Quarry is the fourth major locality to yield fossil mammals in the eastern Crazy Mountain Basin of south-central Montana. It is stratigraphically intermediate between Gidley and Silberling quarries below, which are late Torrejonian (middle Paleocene) in age, and Scarritt Quarry above, which is early Tiffanian (late Paleocene) in age. The stratigraphic position of Douglass Quarry and the presence of primitive species of Plesiadapis, Nannodectes, Phenacodus, and Ectocion (genera first appearing at the Torrejonian-Tiffanian boundary) combine to indicate an earliest Tiffanian age. -
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WHAT S A HUMAN? Mammals ’ Humans are mammals. Humans are unique. We grow crops, breed domestic animals and trade across Like all mammals, humans continents. We talk and write with complex languages. We have the ability to reason, have hair and human and we explore and try to understand the workings of the world. Art, music and babies drink their mother’s literature celebrate what we see and hear. Complex tools enable us to construct milk. It contains all the goodness that a growing buildings and create complicated machines, and we can even explore outer space. human baby needs. No other animal achieves all these things, but, like all animals, our evolutionary story has much simpler beginnings. In this book we explore the journey our ancestors took and the changes we went through to become humans. Primates Humans are primates. This is a subgroup of mammals that includes lemurs and lorises on the one hand and tarsiers, monkeys and apes (including humans) on the other. Haplorhines So wher s fit in? e exactly do human Humans are haplorhines, meaning ‘simple noses’, a group which includes monkeys and apes. One difference between monkeys Hominids and apes is very obvious: most Humans are also included with the monkeys have tails but apes hominids, or great apes. This is a do not, which, if you look in the Hominins subgroup of the apes that includes mirror, makes us an ape. And, just when you orangutans, gorillas, chimpanzees, thought scientists had bonobos and us, but not the gibbons. invented enough words to describe humans, there’s another one.