Evidence for a Convergent Slowdown in Primate Molecular Rates and Its Implications for the Timing of Early Primate Evolution
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Molecular Clock: Insights and Pitfalls
Molecular clock: insights and pitfalls • An historical presentation of the molecular clock. • Birth of the molecular clock • Neutral Theory of evolution • The Nearly Neutral Theory of Evolution • The molecular clock is a « sloppy » clock. • A variable « tick rate » • Different rates for different groups • Calibrating a molecular phylogenetic tree • Dating Methods --- Introductory seminar on the use of molecular tools in natural history collections - 6-7 November 2007, RMCA --- A historical presentation of the molecular clock -1951-1955: Sanger sequenced the first protein, the insulin. Give the potential for using molecular sequences to construct phylogeny -1962: Zuckerkandl and Pauling: AA differences between the hemoglobin of different species is correlated with the time passed since they diverged. Divergence time (T) dAB / 2 A B Rate = (dAB / 2) / T C D --- Introductory seminar on the use of molecular tools in natural history collections - 6-7 November 2007, RMCA --- A historical presentation of the molecular clock Fixed or lost by chance Kimura, 1968 Eliminated by selection Fixed by selection Selection theory more in agreement with the rate of morphological evolution (Modified from Bromham and Penny, 2003) --- Introductory seminar on the use of molecular tools in natural history collections - 6-7 November 2007, RMCA --- The Neutral Theory of molecular evolution Eliminated by selection Fixed by selection Kimura, 1968 Fixed or lost by chance GENETIC DRIFT ν ν Molecular rate of evolution = Mutation rate 2N e * 1/2N e = (Modified from -
U-Pb Geochronology and the Calibration of Metazoan Evolution: Progress and Promise
Eleventh Annual V. M. Goldschmidt Conference (2001) 3867.pdf U-PB GEOCHRONOLOGY AND THE CALIBRATION OF METAZOAN EVOLUTION: PROGRESS AND PROMISE. S. A. Bowring, M. W. Martin, and J. P. Grotzinger. Intensive efforts by paleontologists, evolutionary and developmental biologists, and geologists are leading to a much better understanding of the first appearance and subsequent explosive diversification of animals. The recognition of thin zircon-bearing air-fall ash beds interlayered with fossil-bearing rocks has allowed the establishment of a high-precision temporal framework for animal evolution. Refined laboratory techniques permit analytical uncertainties that translate to age uncertainties of less than 1 Ma and the potential for global correlations at even higher resolution (100-300 ka) when combined with integrated paleontological, chemostratigraphic, and geological data. This framework, will allow evaluation of models that invoke both intrinsic and extrinsic triggers for Metazoan evolution and the Cambrian radiation. In particular, many have pointed out that the first appearance of metazoan fossils follows a period characterized by dramatic climate fluctuations and large fluctuations in the sequestration of carbon. The oldest dated Metazoan fossils (Ediacarans) are younger than ca. 575 Ma and appear to just post-date the youngest Neoproterozoic glacial deposits ca. 580 Ma. The Doushantuo phosphatic rocks of south China preserve spectacular animal fossils but have not been precisely dated. Geochronological data from Neoproterozoic to Cambrian rocks in North America, Namibia, Great Britain, Siberia, and Oman indicate that Ediacaran fossils range from at least 575 Ma (Newfoundland) to <543 Ma (Namibia). Shelly fossils (Cloudina and Namacalathus) are > 548 to ca. 542 Ma. Complex trace-fossils occur at least as far back as 555 Ma (White Sea, Russia). -
An Overview of the Independent Histories of the Human Y Chromosome and the Human Mitochondrial Chromosome
The Proceedings of the International Conference on Creationism Volume 8 Print Reference: Pages 133-151 Article 7 2018 An Overview of the Independent Histories of the Human Y Chromosome and the Human Mitochondrial chromosome Robert W. Carter Stephen Lee University of Idaho John C. Sanford Cornell University, Cornell University College of Agriculture and Life Sciences School of Integrative Plant Science,Follow this Plant and Biology additional Section 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 Carter, R.W., S.S. Lee, and J.C. Sanford. An overview of the independent histories of the human Y- chromosome and the human mitochondrial chromosome. 2018. In Proceedings of the Eighth International Conference on Creationism, ed. J.H. Whitmore, pp. 133–151. Pittsburgh, Pennsylvania: Creation Science Fellowship. Carter, R.W., S.S. Lee, and J.C. Sanford. An overview of the independent histories of the human Y-chromosome and the human mitochondrial chromosome. 2018. In Proceedings of the Eighth International Conference on Creationism, ed. J.H. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Molecular Clocks Fossil Evidence Is Sparse and Imprecise Rose Hoberman (Or Nonexistent)
The Holy Grail Molecular Clocks Fossil evidence is sparse and imprecise Rose Hoberman (or nonexistent) Predict divergence times by comparing molecular data Rate Constancy? •Given 110 MYA – a phylogenetic tree – branch lengths (rt) – a time estimate for one (or more) node C D R M H • Can we date other nodes in the tree? • Yes... if the rate of molecular change is constant across all branches Page & Holmes p240 Protein Variability Evidence for Rate Constancy in Hemoglobin • Protein structures & functions differ – Proportion of neutral sites differ • Rate constancy does not hold across different protein types Large carniverous marsupial • However... – Each protein does appear to have a characteristic rate of evolution Page and Holmes p229 1 The Outline Molecular Clock • Methods for estimating time under a molecular Hypothesis clock – Estimating genetic distance • Amount of genetic difference between – Determining and using calibration points sequences is a function of time since – Sources of error separation. • Rate heterogeneity – reasons for variation • Rate of molecular change is constant – how its taken into account when estimating times (enough) to predict times of divergence • Reliability of time estimates • Estimating gene duplication times Measuring Evolutionary time with a Estimating Genetic Differences molecular clock 1. Estimate genetic distance If all nt equally likely, observed difference d = number amino acid replacements would plateau at 0.75 2. Use paleontological data to determine date of common ancestor Simply counting -
Aspen Ecology in Rocky Mountain National Park: Age Distribution, Genetics, and the Effects of Elk Herbivory
Aspen Ecology in Rocky Mountain National Park: Age Distribution, Genetics, and the Effects of Elk Herbivory By Linda C. Zeigenfuss, Dan Binkley, Gerald A. Tuskan, William H. Romme, Tongming Yin, Stephen DiFazio, and Francis J. Singer Open-File Report 2008–1337 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Zeigenfuss, L.C., Binkley, D., Tuskan, G.A., Romme, W.H., Yin, T., DiFazio, S., and Singer, F.J. 2008, Aspen Ecology in Rocky Mountain National Park: Age distribution, genetics, and the effects of elk herbivory: U.S. Geological Survey Open-File Report 2008–1337, 52 p. Available online only Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Cover photo courtesy of Carolyn Widman ii Contents Executive Summary............................................................................................................................................................1 -
MOLECULAR CLOCKS Definition Introduction
MOLECULAR CLOCKS 583 Kishino, H., Thorne, J. L., and Bruno, W. J., 2001. Performance of Thorne, J. L., Kishino, H., and Painter, I. S., 1998. Estimating the a divergence time estimation method under a probabilistic model rate of evolution of the rate of molecular evolution. Molecular of rate evolution. Molecular Biology and Evolution, 18,352–361. Biology and Evolution, 15, 1647–1657. Kodandaramaiah, U., 2011. Tectonic calibrations in molecular dat- Warnock, R. C. M., Yang, Z., Donoghue, P. C. J., 2012. Exploring ing. Current Zoology, 57,116–124. uncertainty in the calibration of the molecular clock. Biology Marshall, C. R., 1997. Confidence intervals on stratigraphic ranges Letters, 8, 156–159. with nonrandom distributions of fossil horizons. Paleobiology, Wilkinson, R. D., Steiper, M. E., Soligo, C., Martin, R. D., Yang, Z., 23, 165–173. and Tavaré, S., 2011. Dating primate divergences through an Müller, J., and Reisz, R. R., 2005. Four well-constrained calibration integrated analysis of palaeontological and molecular data. Sys- points from the vertebrate fossil record for molecular clock esti- tematic Biology, 60,16–31. mates. Bioessays, 27, 1069–1075. Yang, Z., and Rannala, B., 2006. Bayesian estimation of species Parham, J. F., Donoghue, P. C. J., Bell, C. J., et al., 2012. Best practices divergence times under a molecular clock using multiple fossil for justifying fossil calibrations. Systematic Biology, 61,346–359. calibrations with soft bounds. Molecular Biology and Evolution, Peters, S. E., 2005. Geologic constraints on the macroevolutionary 23, 212–226. history of marine animals. Proceedings of the National Academy Zuckerkandl, E., and Pauling, L., 1962. Molecular disease, evolution of Sciences, 102, 12326–12331. -
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. -
Pseudotsuga Menziesii)
120 - PART 1. CONSENSUS DOCUMENTS ON BIOLOGY OF TREES Section 4. Douglas-Fir (Pseudotsuga menziesii) 1. Taxonomy Pseudotsuga menziesii (Mirbel) Franco is generally called Douglas-fir (so spelled to maintain its distinction from true firs, the genus Abies). Pseudotsuga Carrière is in the kingdom Plantae, division Pinophyta (traditionally Coniferophyta), class Pinopsida, order Pinales (conifers), and family Pinaceae. The genus Pseudotsuga is most closely related to Larix (larches), as indicated in particular by cone morphology and nuclear, mitochondrial and chloroplast DNA phylogenies (Silen 1978; Wang et al. 2000); both genera also have non-saccate pollen (Owens et al. 1981, 1994). Based on a molecular clock analysis, Larix and Pseudotsuga are estimated to have diverged more than 65 million years ago in the Late Cretaceous to Paleocene (Wang et al. 2000). The earliest known fossil of Pseudotsuga dates from 32 Mya in the Early Oligocene (Schorn and Thompson 1998). Pseudostuga is generally considered to comprise two species native to North America, the widespread Pseudostuga menziesii and the southwestern California endemic P. macrocarpa (Vasey) Mayr (bigcone Douglas-fir), and in eastern Asia comprises three or fewer endemic species in China (Fu et al. 1999) and another in Japan. The taxonomy within the genus is not yet settled, and more species have been described (Farjon 1990). All reported taxa except P. menziesii have a karyotype of 2n = 24, the usual diploid number of chromosomes in Pinaceae, whereas the P. menziesii karyotype is unique with 2n = 26. The two North American species are vegetatively rather similar, but differ markedly in the size of their seeds and seed cones, the latter 4-10 cm long for P. -
Fossil Primates
AccessScience from McGraw-Hill Education Page 1 of 16 www.accessscience.com Fossil primates Contributed by: Eric Delson Publication year: 2014 Extinct members of the order of mammals to which humans belong. All current classifications divide the living primates into two major groups (suborders): the Strepsirhini or “lower” primates (lemurs, lorises, and bushbabies) and the Haplorhini or “higher” primates [tarsiers and anthropoids (New and Old World monkeys, greater and lesser apes, and humans)]. Some fossil groups (omomyiforms and adapiforms) can be placed with or near these two extant groupings; however, there is contention whether the Plesiadapiformes represent the earliest relatives of primates and are best placed within the order (as here) or outside it. See also: FOSSIL; MAMMALIA; PHYLOGENY; PHYSICAL ANTHROPOLOGY; PRIMATES. Vast evidence suggests that the order Primates is a monophyletic group, that is, the primates have a common genetic origin. Although several peculiarities of the primate bauplan (body plan) appear to be inherited from an inferred common ancestor, it seems that the order as a whole is characterized by showing a variety of parallel adaptations in different groups to a predominantly arboreal lifestyle, including anatomical and behavioral complexes related to improved grasping and manipulative capacities, a variety of locomotor styles, and enlargement of the higher centers of the brain. Among the extant primates, the lower primates more closely resemble forms that evolved relatively early in the history of the order, whereas the higher primates represent a group that evolved more recently (Fig. 1). A classification of the primates, as accepted here, appears above. Early primates The earliest primates are placed in their own semiorder, Plesiadapiformes (as contrasted with the semiorder Euprimates for all living forms), because they have no direct evolutionary links with, and bear few adaptive resemblances to, any group of living primates. -
The Evolution of the Platyrrhine Talus: a Comparative Analysis of the Phenetic Affinities of the Miocene Platyrrhines with Their Modern Relatives
Journal of Human Evolution 111 (2017) 179e201 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol The evolution of the platyrrhine talus: A comparative analysis of the phenetic affinities of the Miocene platyrrhines with their modern relatives * Thomas A. Püschel a, , Justin T. Gladman b, c,Rene Bobe d, e, William I. Sellers a a School of Earth and Environmental Sciences, University of Manchester, M13 9PL, United Kingdom b Department of Anthropology, The Graduate Center, CUNY, New York, NY, USA c NYCEP, New York Consortium in Evolutionary Primatology, New York, NY, USA d Departamento de Antropología, Universidad de Chile, Santiago, Chile e Institute of Cognitive and Evolutionary Anthropology, School of Anthropology, University of Oxford, United Kingdom article info abstract Article history: Platyrrhines are a diverse group of primates that presently occupy a broad range of tropical-equatorial Received 8 August 2016 environments in the Americas. However, most of the fossil platyrrhine species of the early Miocene Accepted 26 July 2017 have been found at middle and high latitudes. Although the fossil record of New World monkeys has Available online 29 August 2017 improved considerably over the past several years, it is still difficult to trace the origin of major modern clades. One of the most commonly preserved anatomical structures of early platyrrhines is the talus. Keywords: This work provides an analysis of the phenetic affinities of extant platyrrhine tali and their Miocene New World monkeys counterparts through geometric morphometrics and a series of phylogenetic comparative analyses. Talar morphology fi Geometric morphometrics Geometric morphometrics was used to quantify talar shape af nities, while locomotor mode per- Locomotor mode percentages centages (LMPs) were used to test if talar shape is associated with locomotion. -
First North American Fossil Monkey and Early Miocene Tropical Biotic Interchange Jonathan I
LETTER doi:10.1038/nature17415 First North American fossil monkey and early Miocene tropical biotic interchange Jonathan I. Bloch1, Emily D. Woodruff1,2, Aaron R. Wood1,3, Aldo F. Rincon1,4, Arianna R. Harrington1,2,5, Gary S. Morgan6, David A. Foster4, Camilo Montes7, Carlos A. Jaramillo8, Nathan A. Jud1, Douglas S. Jones1 & Bruce J. MacFadden1 New World monkeys (platyrrhines) are a diverse part of modern Primates Linnaeus, 1758 tropical ecosystems in North and South America, yet their early Anthropoidea Mivart, 1864 evolutionary history in the tropics is largely unknown. Molecular Platyrrhini Geoffroy, 1812 divergence estimates suggest that primates arrived in tropical Cebidae Bonaparte, 1831 Central America, the southern-most extent of the North American Panamacebus transitus gen. et sp. nov. landmass, with several dispersals from South America starting with the emergence of the Isthmus of Panama 3–4 million years Etymology. Generic name combines ‘Panama’ with ‘Cebus’, root taxon ago (Ma)1. The complete absence of primate fossils from Central for Cebidae. Specific name ‘transit’ (Latin, crossing) refers to its implied America has, however, limited our understanding of their history early Miocene dispersal between South and North America. in the New World. Here we present the first description of a fossil Holotype. UF 280128, left upper first molar (M1; Fig. 2a, b). monkey recovered from the North American landmass, the oldest Referred material. Left upper second molar (M2; UF 281001; Fig. 2a, b), known crown platyrrhine, from a precisely dated 20.9-Ma layer in partial left lower first incisor (I1; UF 280130), right lower second the Las Cascadas Formation in the Panama Canal Basin, Panama.