Phylogenetic Systematics of the Primate Genus Aotus Based on Hyoid Morphology
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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. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. -
Genome Sequence of the Basal Haplorrhine Primate Tarsius Syrichta Reveals Unusual Insertions
ARTICLE Received 29 Oct 2015 | Accepted 17 Aug 2016 | Published 6 Oct 2016 DOI: 10.1038/ncomms12997 OPEN Genome sequence of the basal haplorrhine primate Tarsius syrichta reveals unusual insertions Ju¨rgen Schmitz1,2, Angela Noll1,2,3, Carsten A. Raabe1,4, Gennady Churakov1,5, Reinhard Voss6, Martin Kiefmann1, Timofey Rozhdestvensky1,7,Ju¨rgen Brosius1,4, Robert Baertsch8, Hiram Clawson8, Christian Roos3, Aleksey Zimin9, Patrick Minx10, Michael J. Montague10, Richard K. Wilson10 & Wesley C. Warren10 Tarsiers are phylogenetically located between the most basal strepsirrhines and the most derived anthropoid primates. While they share morphological features with both groups, they also possess uncommon primate characteristics, rendering their evolutionary history somewhat obscure. To investigate the molecular basis of such attributes, we present here a new genome assembly of the Philippine tarsier (Tarsius syrichta), and provide extended analyses of the genome and detailed history of transposable element insertion events. We describe the silencing of Alu monomers on the lineage leading to anthropoids, and recognize an unexpected abundance of long terminal repeat-derived and LINE1-mobilized transposed elements (Tarsius interspersed elements; TINEs). For the first time in mammals, we identify a complete mitochondrial genome insertion within the nuclear genome, then reveal tarsier-specific, positive gene selection and posit population size changes over time. The genomic resources and analyses presented here will aid efforts to more fully understand the ancient characteristics of primate genomes. 1 Institute of Experimental Pathology, University of Mu¨nster, 48149 Mu¨nster, Germany. 2 Mu¨nster Graduate School of Evolution, University of Mu¨nster, 48149 Mu¨nster, Germany. 3 Primate Genetics Laboratory, German Primate Center, Leibniz Institute for Primate Research, 37077 Go¨ttingen, Germany. -
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. -
Cenozoic Primates of Eastern Eurasia (Russia and Adjacent Areas) EVGENY N
ANTHROPOLOGICAL SCIENCE Vol. 113, 103–115, 2005 Cenozoic Primates of eastern Eurasia (Russia and adjacent areas) EVGENY N. MASCHENKO1* 1Paleontological Institute, Russian Academy of Sciences, Profsouyznaya Street 123, 117995 Moscow, Russia Received 19 May 2003; accepted 7 May 2004 Abstract In the Eocene, distribution of the order Primates in the northern part of eastern Eurasia was confined to Mongolia. A form of Omomyidae (Altanius orlovi) is represented. Northern Eurasian pri- mates attributed to later times cover the interval between the Late Miocene (Late Turolian) to the Mid- dle Pleistocene (Mindel–Riss). Primates are distributed in the western part of eastern Eurasia (Moldavia, Ukraine), Transcaucasus (Georgia, Iranian Azerbaijan) and Central Asia (Tadjikistan, Afghanistan, Transbaikalian, Mongolia). The total number of known primate taxa is not large: seven genera and eleven species in three families (Omomyidae, Hominidae, Cercopithecidae). The Neogene and Pleistocene representatives of the order Primates comprise either widely distributed Eurasian forms or endemic taxa. The distribution pattern of primates in the western and eastern part of eastern Eurasia can be interpreted in relation to links with African and East Asian faunal provinces. By the Late Pleistocene all non-human representatives of the order Primates in the northern part of eastern Eurasia became extinct. Key words: Eocene, late Cenozoic, eastern Eurasia, Cercopithecoidea, Hominoidea Introduction Paleontological Institute, Russian Academy of Sciences, Moscow, Russia; GIN, Geological Institute, Russian Acad- The early history of the order Primates from the eastern emy of Sciences, Moscow, Russia; GIN U, Geological Insti- part of Eurasia reflects the restructuring of the mammalian tute Siberian Branch, Russian Academy of Sciences, Ulan- faunas of Eurasia and North America that occurred at the Ude, Russia; ZIN, Zoological Institute, Russian Academy of Paleocene–Eocene boundary at about 57 Ma. -
Evolutionary History of Lorisiform Primates
Evolution: Reviewed Article Folia Primatol 1998;69(suppl 1):250–285 oooooooooooooooooooooooooooooooo Evolutionary History of Lorisiform Primates D. Tab Rasmussen, Kimberley A. Nekaris Department of Anthropology, Washington University, St. Louis, Mo., USA Key Words Lorisidae · Strepsirhini · Plesiopithecus · Mioeuoticus · Progalago · Galago · Vertebrate paleontology · Phylogeny · Primate adaptation Abstract We integrate information from the fossil record, morphology, behavior and mo- lecular studies to provide a current overview of lorisoid evolution. Several Eocene prosimians of the northern continents, including both omomyids and adapoids, have been suggested as possible lorisoid ancestors, but these cannot be substantiated as true strepsirhines. A small-bodied primate, Anchomomys, of the middle Eocene of Europe may be the best candidate among putative adapoids for status as a true strepsirhine. Recent finds of Eocene primates in Africa have revealed new prosimian taxa that are also viable contenders for strepsirhine status. Plesiopithecus teras is a Nycticebus- sized, nocturnal prosimian from the late Eocene, Fayum, Egypt, that shares cranial specializations with lorisoids, but it also retains primitive features (e.g. four premo- lars) and has unique specializations of the anterior teeth excluding it from direct lorisi- form ancestry. Another unnamed Fayum primate resembles modern cheirogaleids in dental structure and body size. Two genera from Oman, Omanodon and Shizarodon, also reveal a mix of similarities to both cheirogaleids and anchomomyin adapoids. Resolving the phylogenetic position of these Africa primates of the early Tertiary will surely require more and better fossils. By the early to middle Miocene, lorisoids were well established in East Africa, and the debate about whether these represent lorisines or galagines is reviewed. -
The Tempo of Trophic Evolution in Small-Bodied Primates 2 3 4 Running Title: Trophic Evolution in Small-Bodied Primates 5 6 7 Jeremiah E
bioRxiv preprint doi: https://doi.org/10.1101/2020.03.17.996207; this version posted March 20, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-ND 4.0 International license. 1 1 The tempo of trophic evolution in small-bodied primates 2 3 4 Running title: Trophic evolution in small-bodied primates 5 6 7 Jeremiah E. Scott 8 Department of Medical Anatomical Sciences 9 College of Osteopathic Medicine of the Pacific 10 Western University of Health Sciences 11 309 East Second Street 12 Pomona, California 91766 13 U.S.A. 14 [email protected] 15 16 17 Abstract 18 19 Objectives: As a primary trophic strategy, insectivory is uncommon and unevenly 20 distributed across extant primates. This pattern is partly a function of the challenges that 21 insectivory poses for large-bodied primates. In this study, I demonstrate that the uneven 22 distribution is also a consequence of variation in the rate of trophic evolution among small- 23 bodied lineages. 24 Methods: The sample consisted of 307 species classified by primary trophic strategy and 25 body size, creating an ordered three-state character: small-insectivorous, small-herbivorous, 26 and large-herbivorous. I tested for rate heterogeneity by partitioning major clades from the 27 rest of the primate tree and estimating separate rates of transition between herbivory and 28 insectivory for small-bodied lineages in each partition. 29 Results: Bayesian analysis of rate estimates indicates that a model with two rates of trophic 30 evolution provides the best fit to the data. -
New Eocene Primate from Myanmar Shares Dental Characters with African Eocene Crown Anthropoids
ARTICLE https://doi.org/10.1038/s41467-019-11295-6 OPEN New Eocene primate from Myanmar shares dental characters with African Eocene crown anthropoids Jean-Jacques Jaeger1, Olivier Chavasseau 1, Vincent Lazzari1, Aung Naing Soe2, Chit Sein 3, Anne Le Maître 1,4, Hla Shwe5 & Yaowalak Chaimanee1 Recent discoveries of older and phylogenetically more primitive basal anthropoids in China and Myanmar, the eosimiiforms, support the hypothesis that Asia was the place of origins of 1234567890():,; anthropoids, rather than Africa. Similar taxa of eosimiiforms have been discovered in the late middle Eocene of Myanmar and North Africa, reflecting a colonization event that occurred during the middle Eocene. However, these eosimiiforms were probably not the closest ancestors of the African crown anthropoids. Here we describe a new primate from the middle Eocene of Myanmar that documents a new clade of Asian anthropoids. It possesses several dental characters found only among the African crown anthropoids and their nearest rela- tives, indicating that several of these characters have appeared within Asian clades before being recorded in Africa. This reinforces the hypothesis that the African colonization of anthropoids was the result of several dispersal events, and that it involved more derived taxa than eosimiiforms. 1 Laboratory PALEVOPRIM, UMR CNRS 7262, University of Poitiers, 6 rue Michel Brunet Cedex 9, 86073 Poitiers, France. 2 University of Distance Education, Mandalay 05023, Myanmar. 3 Ministry of Education, Department of Higher Education, Naypyitaw 15011, Myanmar. 4 Department of Theoretical Biology, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria. 5 Department of Archaeology and National Museum, Mandalay Branch, Ministry of Religious Affairs and Culture, Mandalay 05011, Myanmar. -
Macroevolutionary Dynamics and Historical Biogeography of Primate Diversification Inferred from a Species Supermatrix
Macroevolutionary Dynamics and Historical Biogeography of Primate Diversification Inferred from a Species Supermatrix Mark S. Springer1*, Robert W. Meredith1,2, John Gatesy1, Christopher A. Emerling1, Jong Park1,3, Daniel L. Rabosky4,5, Tanja Stadler6, Cynthia Steiner7, Oliver A. Ryder7, Jan E. Janecˇka8, Colleen A. Fisher8, William J. Murphy8* 1 Department of Biology, University of California Riverside, Riverside, California, United States of America, 2 Department of Biology and Molecular Biology, Montclair State University, Montclair, New Jersey, United States of America, 3 Department of Biology, University of Washington, Seattle, Washington, United States of America, 4 Department of Integrative Biology, University of California, Berkeley, California, United States of America, 5 Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, Michigan, United States of America, 6 Institut fu¨r Integrative Biologie, Eidgeno¨ssiche Technische Hochschule Zurich, Zurich, Switzerland, 7 San Diego Zoo Institute for Conservation Research, San Diego Zoo Global, San Diego, California, United States of America, 8 Department of Veterinary Integrative Biosciences, Texas A&M University, College Station, Texas, United States of America Abstract Phylogenetic relationships, divergence times, and patterns of biogeographic descent among primate species are both complex and contentious. Here, we generate a robust molecular phylogeny for 70 primate genera and 367 primate species based on a concatenation of 69 nuclear gene segments and ten mitochondrial gene sequences, most of which were extracted from GenBank. Relaxed clock analyses of divergence times with 14 fossil-calibrated nodes suggest that living Primates last shared a common ancestor 71–63 Ma, and that divergences within both Strepsirrhini and Haplorhini are entirely post-Cretaceous. -
A New Omomyid Primate from the Earliest Eocene of Southern England: First Phase of Microchoerine Evolution
A new omomyid primate from the earliest Eocene of southern England: First phase of microchoerine evolution JERRY J. HOOKER Hooker, J.J. 2012. A new omomyid primate from the earliest Eocene of southern England: First phase of microchoerine evolution. Acta Palaeontologica Polonica 57 (3): 449–462. A second species of the microchoerine omomyid genus Melaneremia, M. schrevei sp. nov. is described. It has been col− lected from the upper shelly clay unit of the Woolwich Formation, earliest Ypresian, Eocene, of Croydon, Greater Lon− don, UK. Phylogenetic analysis shows M. schrevei to be the most primitive member of the main clade of the Microchoerinae and demonstrates the initial dental evolution that separated this European subfamily from other omomyids. Calibration of the Woolwich upper shelly clay unit to the later part of the Paleocene–Eocene Thermal Maxi− mum shows that speciation leading to the Microchoerinae took place within 170 ky of the beginning of the Eocene. Tenta− tive identification of M. schrevei in the Conglomérat de Meudon of the Paris Basin suggests close time correlation with the upper part of the Woolwich Formation. Key words: Mammalia, Primates, Melaneremia, evolution, phylogeny, Paleocene–Eocene Thermal Maximum. Jerry J. Hooker [[email protected]]. Department of Palaeontology, Natural History Museum, Cromwell Road, Lon− don, SW7 5BD, UK. Received 4 March 2011, accepted 25 July 2011, available on line 5 September 2012. Introduction Other abbreviations.—PETM, Paleocene–Eocene Thermal Maximum; RHTS, Red Hot Truck Stop. In 1998 at Park Hill, Croydon, Greater London, a section in the Woolwich Formation of earliest Eocene age, originally ex− posed in 1882 during excavation of a railway cutting, was re− Systematic palaeontology exposed when the cutting was widened for the Croydon Tram− link (Hooker et al. -
A Palaeontological Model for Determining the Limits of Early Hominid Taxonomic Variability
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Wits Institutional Repository on DSPACE Palaeont. afr., 28, 71-77 (1991) A PALAEONTOLOGICAL MODEL FOR DETERMINING THE LIMITS OF EARLY HOMINID TAXONOMIC VARIABILITY by Bernard Wood Hominid Palaeontology Research Group, Department ofHuman Anatomy and Cell Biology, University of Liverpool, PO Box 147, LNERPOOL L69 3BX, United Kingdom ABSTRACT This paper has examined the utility and implications of using Australopithecus boisei as a model for assessing the limits of intraspecific variation in early hominid species. When compared to variation in a sample of lowland gorilla, the coefficient of variation values of the 25 cranial and mandibular, and 44 dental measurements taken on the A. boisei hypodigm were not excessive; the main difference between the two samples was the higher levels of canine variability within gorilla. Levels of variability in A. boisei were compared with those in the hypodigms of A. robustus and A. africanus. In neither case did comparisons demonstrate that those hypodigms were excessively variable. This suggests that if more than one taxon is present within these collections, then any differential diagnosis needs to be based on excessive variation in shape and not size. INTRODUCTION that the 'degree' and the 'pattern' of variation should be The problem of deciding the point at which phenotypic given separate consideration (Wood, Li and Willoughby variation exceeds that which can be tolerated within a 1991). The same study used an 'outgroup' approach, and single species is one that is widely recognised in both investigated the pattern of variation in modem humans palaeontology in general (Mayr, Linsley and Usinger and the African higher primates. -
The Primate Cranial Base: Ontogeny, Function, and Integration
YEARBOOK OF PHYSICAL ANTHROPOLOGY 43:117–169 (2000) The Primate Cranial Base: Ontogeny, Function, and Integration DANIEL E. LIEBERMAN,1 CALLUM F. ROSS,2 AND MATTHEW J. RAVOSA3 1Department of Anthropology, George Washington University, Washington, DC 20052, and Human Origins Program, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560 2Department of Anatomical Sciences, Health Sciences Center, SUNY at Stony Brook, Stony Brook, NY 11794-8081 3Department of Cell and Molecular Biology, Northwestern University Medical School, Chicago, Illinois 60611-3008, and Mammals Division, Department of Zoology, Field Museum of Natural History, Chicago, Illinois 60605-2496 KEY WORDS cranial base; basicranium; chondrocranium; pri- mates; humans ABSTRACT Understanding the complexities of cranial base develop- ment, function, and architecture is important for testing hypotheses about many aspects of craniofacial variation and evolution. We summarize key aspects of cranial base growth and development in primates that are useful for formulating and testing hypotheses about the roles of the chondrocranium and basicranium in cranial growth, integration, and function in primate and human evolution. We review interspecific, experimental, and ontogenetic evidence for interactions between the cranial base and brain, and between the cranial base and the face. These interactions indicate that the cranial base plays a key role in craniofacial growth, helping to integrate, spatially and functionally, different patterns of growth in various adjoining regions of the skull such as components of the brain, the eyes, the nasal cavity, the oral cavity, and the pharynx. Brain size relative to cranial base length appears to be the dominant influence on many aspects of basicranial variation, espe- cially the angle of the cranial base in the midsagittal plane, but other factors such as facial size, facial orientation, and posture may also be important.