26 Animal Evolution and Diversity
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Early Sponge Evolution: a Review and Phylogenetic Framework
Available online at www.sciencedirect.com ScienceDirect Palaeoworld 27 (2018) 1–29 Review Early sponge evolution: A review and phylogenetic framework a,b,∗ a Joseph P. Botting , Lucy A. Muir a Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China b Department of Natural Sciences, Amgueddfa Cymru — National Museum Wales, Cathays Park, Cardiff CF10 3LP, UK Received 27 January 2017; received in revised form 12 May 2017; accepted 5 July 2017 Available online 13 July 2017 Abstract Sponges are one of the critical groups in understanding the early evolution of animals. Traditional views of these relationships are currently being challenged by molecular data, but the debate has so far made little use of recent palaeontological advances that provide an independent perspective on deep sponge evolution. This review summarises the available information, particularly where the fossil record reveals extinct character combinations that directly impinge on our understanding of high-level relationships and evolutionary origins. An evolutionary outline is proposed that includes the major early fossil groups, combining the fossil record with molecular phylogenetics. The key points are as follows. (1) Crown-group sponge classes are difficult to recognise in the fossil record, with the exception of demosponges, the origins of which are now becoming clear. (2) Hexactine spicules were present in the stem lineages of Hexactinellida, Demospongiae, Silicea and probably also Calcarea and Porifera; this spicule type is not diagnostic of hexactinellids in the fossil record. (3) Reticulosans form the stem lineage of Silicea, and probably also Porifera. (4) At least some early-branching groups possessed biminerallic spicules of silica (with axial filament) combined with an outer layer of calcite secreted within an organic sheath. -
The Cenozoic Era - Nýlífsöld 65 MY-Present Jarðsaga 2 Ólafur Ingólfsson Origin of the Term: the Tertiary Tertiary System
The Cenozoic Era - Nýlífsöld 65 MY-Present Jarðsaga 2 Ólafur Ingólfsson Origin of the Term: The Tertiary Tertiary System. [1760] Named by Giovanni Arduino Period as the uppermost part of his 65-1.8 MY three-fold subdivision of mountains in northern Italy. The Tertiary became a formal period and system when Lyell published his work describing further subdivisions of the Tertiary. The Tertiary Period is divided into five epochs (tímar): Paleocene (65-56 MY), Eocene (56-34 MY), Oligocene (34-24 MY), Miocene (24-5,3 MY), and Pliocene (5,3-1,8 MY). Confusing set of stratigraphic terms... More than 95% of the Cenozoic era belongs to the Tertiary period. During the 18th century the names Primary, Secondary, and Tertiary were given by Giovanni Arduino to successive rock strata, the Primary being the oldest, the Tertiary the more recent. In 1829 a fourth division, the Quaternary, was added by P. G. Desnoyers. These terms were later abandoned, the Primary becoming the Paleozoic Era, and the Secondary the Mesozoic. But Tertiary and Quaternary were retained for the two main stages of the Cenozoic. Attempts to replace the "Tertiary" with a more reasonable division of “Palaeogene” (early Tertiary) and “Neogene” (later Tertiary and Quaternary) have not been very successful. Stanley uses this division. The World at the K/T Boundary Paleocene plate tectonics During the Paleocene, the inland seas of the Cretaceous Period dry up, exposing large land areas in North America and Eurasia. Australia begins to separate from Antarctica, and Greenland splits from North America. A remnant Tethys Sea persists in the equatorial region. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 67, NUMBER 6 CAMBRIAN GEOLOGY AND PALEONTOLOGY IV No. 6.—MIDDLE CAMBRIAN SPONGIAE (With Plates 60 to 90) BY CHARLES D. WALCOTT (Publication 2580) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION 1920 Z$t Bovb Qgattimote (press BALTIMORE, MD., U. S. A. CAMBRIAN GEOLOGY AND PALEONTOLOGY IV No. 6.—MIDDLE CAMBRIAN SPONGIAE By CHARLES D. WALCOTT (With Plates 60 to 90) CONTENTS PAGE Introduction 263 Habitat = 265 Genera and species 265 Comparison with recent sponges 267 Comparison with Metis shale sponge fauna 267 Description of species 269 Sub-Class Silicispongiae 269 Order Monactinellida Zittel (Monaxonidae Sollas) 269 Sub-Order Halichondrina Vosmaer 269 Halichondrites Dawson 269 Halichondrites elissa, new species 270 Tuponia, new genus 271 Tuponia lineata, new species 272 Tuponia bellilineata, new species 274 Tuponia flexilis, new species 275 Tuponia flexilis var. intermedia, new variety 276 Takakkawia, new genus 277 Takakkawia lineata, new species 277 Wapkia, new genus 279 Wapkia grandis, new species 279 Hazelia, new genus 281 Hazelia palmata, new species 282 Hazelia conf erta, new species 283 Hazelia delicatula, new species 284 Hazelia ? grandis, new species 285. Hazelia mammillata, new species 286' Hazelia nodulifera, new species 287 Hazelia obscura, new species 287 Corralia, new genus 288 Corralia undulata, new species 288 Sentinelia, new genus 289 Sentinelia draco, new species 290 Smithsonian Miscellaneous Collections, Vol. 67, No. 6 261 262 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 6j Family Suberitidae 291 Choia, new genus 291 Choia carteri, new species 292 Choia ridleyi, new species 294 Choia utahensis, new species 295 Choia hindei (Dawson) 295 Hamptonia, new genus 296 Hamptonia bowerbanki, new species 297 Pirania, new genus 298 Pirania muricata, new species 298 Order Hexactinellida O. -
New Paleocene Skeletons and the Relationship of Plesiadapiforms to Crown-Clade Primates
New Paleocene skeletons and the relationship of plesiadapiforms to crown-clade primates Jonathan I. Bloch*†, Mary T. Silcox‡, Doug M. Boyer§, and Eric J. Sargis¶ʈ *Florida Museum of Natural History, University of Florida, P. O. Box 117800, Gainesville, FL 32611; ‡Department of Anthropology, University of Winnipeg, 515 Portage Avenue, Winnipeg, MB, Canada, R3B 2E9; §Department of Anatomical Science, Stony Brook University, Stony Brook, NY 11794-8081; ¶Department of Anthropology, Yale University, P. O. Box 208277, New Haven, CT 06520; and ʈDivision of Vertebrate Zoology, Peabody Museum of Natural History, Yale University, New Haven, CT 06520 Communicated by Alan Walker, Pennsylvania State University, University Park, PA, November 30, 2006 (received for review December 6, 2005) Plesiadapiforms are central to studies of the origin and evolution preserved cranium of a paromomyid (10) seemed to independently of primates and other euarchontan mammals (tree shrews and support a plesiadapiform–dermopteran link, leading to the wide- flying lemurs). We report results from a comprehensive cladistic spread acceptance of this phylogenetic hypothesis. The evidence analysis using cranial, postcranial, and dental evidence including supporting this interpretation has been questioned (7, 9, 13, 15, 16, data from recently discovered Paleocene plesiadapiform skeletons 19, 20), but no previous study has evaluated the plesiadapiform– (Ignacius clarkforkensis sp. nov.; Dryomomys szalayi, gen. et sp. dermopteran link by using cranial, postcranial, and dental evidence, -
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. -
RELATED PHENOTYPIC VARIATION? a CASE STUDY from the BURGESS SHALE by TIMOTHY P
[Palaeontology, 2017, pp. 1–11] DO BRACHIOPODS SHOW SUBSTRATE-RELATED PHENOTYPIC VARIATION? A CASE STUDY FROM THE BURGESS SHALE by TIMOTHY P. TOPPER1 ,LUKEC.STROTZ2, CHRISTIAN B. SKOVSTED3 and LARS E. HOLMER4 1Palaeoecosystems Group, Department of Earth Sciences, Durham University, Durham, DH1 3LE, UK; [email protected] 2Biodiversity Institute & Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS 66045, USA; [email protected] 3Department of Palaeobiology, Swedish Museum of Natural History, PO Box 50007, SE-104 05, Stockholm, Sweden; [email protected] 4Department of Earth Sciences, Palaeobiology, Uppsala University, Villav€agen 16, SE - 752 36, Uppsala, Sweden; [email protected] Typescript received 18 November 2016; accepted in revised form 18 January 2017 Abstract: As sessile, benthic filter feeders, brachiopods ANOVA, we determine that there is some variation in shape share an intimate relationship with their chosen substrate. related to substrate. Canonical variate analyses, for ventral Individuals of Micromitra burgessensis in the Burgess Shale valves and dorsal valves, indicate that specimens attached to Formation are preserved in life position, attached to a range the same substrate are recognizable in shape from specimens of hard substrates, including skeletal debris, conspecific bra- attached to other substrate types. The strength of differentia- chiopods, sponges and enigmatic tubes. Here we investigate tion however, is not robust and combined with our discrimi- the phenotypic variability of M. burgessensis associated with nate analysis of separate populations suggests that there is differing substrate attachments. We apply geometric mor- the potential for substrates to exercise only weak control phometrics to test for variation by plotting landmarks on over the morphology of Brachiopoda. -
From the Lower Ordovician of the Central Anti-Atlas (Morocco)
Journal of Paleontology, 91(4), 2017, p. 685–714 Copyright © 2017, The Paleontological Society 0022-3360/17/0088-0906 doi: 10.1017/jpa.2017.6 Morphological disparity and systematic revision of the eocrinoid genus Rhopalocystis (Echinodermata, Blastozoa) from the Lower Ordovician of the central Anti-Atlas (Morocco) Ninon Allaire,1,2 Bertrand Lefebvre,2 Elise Nardin,3 Emmanuel L.O. Martin,2 Romain Vaucher,2 and Gilles Escarguel4 1Université de Lille, CNRS, UMR 8198 Evo-Eco-Paleo, F-59000 Lille, France 〈[email protected]〉 2Université Claude Bernard Lyon 1, ENS de Lyon, CNRS, UMR 5276 LGL-TPE, F-69622 Villeurbanne, France 〈[email protected]〉, 〈[email protected]〉, 〈[email protected]〉 3Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, CNRS/UPS/IRD, 14 avenue Edouard Belin, 31400 Toulouse, France 〈[email protected]〉 4Université Claude Bernard Lyon 1, CNRS, ENTPE, UMR 5023 LEHNA, F-69622 Villeurbanne, France 〈[email protected]〉 Abstract.—The genus Rhopalocystis (Eocrinoidea, Blastozoa) is characterized by both a short stratigraphic range (Fezouata Shale, middle Tremadocian to middle Floian, Lower Ordovician) and a reduced geographic extension (Agdz-Zagora area, central Anti-Atlas, Morocco). Since the original description of its type species (R. destombesi Ubaghs, 1963), three successive revisions of the genus Rhopalocystis have led to the erection of nine additional species. The morphological disparity within this genus is here critically reassessed on the basis of both historical material and new recently collected samples. The detailed examination of all specimens, coupled with morphometric and cladistic analyses, points toward a relatively strong support for five morphotypes. -
An Anachronistic Clarkforkian Mammal Fauna from the Paleocene Fort Union Formation (Great Divide Basin, Wyoming, USA)
Geologica Acta, Vol.7, Nos 1-2, March-June 2009, 113-124 DOI: 10.1344/105.000000274 Available online at www.geologica-acta.com An anachronistic Clarkforkian mammal fauna from the Paleocene Fort Union Formation (Great Divide Basin, Wyoming, USA) 1 2 ROBERT L. ANEMONE and WENDY DIRKS 1 Department of Anthropology. Western Michigan University Kalamazoo, MI 49008-5306, USA. E-mail: [email protected] 2 Oral Biology, School of Dental Sciences. Newcastle University Framlington Place. Newcastle-upon-Tyne, NE2 4BW, United Kingdom. E-mail: [email protected] ABSTRACT The Clarkforkian (latest Paleocene) North American Land Mammal Age (NALMA) remains a relatively poorly sampled biostratigraphic interval at the close of the Paleocene epoch that is best known from the Bighorn Basin of northwestern Wyoming. A period of global warming between the cooler early and middle Paleocene and the extreme warming of the early Eocene, the Clarkforkian witnessed significant floral and faunal turnover with important ramifications for the development of Cenozoic biotas. The combination of warming global climates with mammalian turnover (including likely intercontinental dispersals) marks the Clarkforkian and the succeeding Wasatchian (Earliest Eocene) NALMAs as periods of intense interest to paleobiologists and other earth scientists concerned with aspects of biostratigraphy and with the biotic effects of climate change in the past. In this paper we describe a new Clarkforkian mammalian fauna from the Great Divide Basin of southwestern Wyoming with some surprising faunal elements that differ from the typical suite of taxic associations found in Clarkforkian assemblages of the Bighorn Basin. Several different scenarios are explored to explain this “anachronistic” assem- blage of mammals from southern Wyoming in relation to the typical patterns found in northern Wyoming, includ- ing the concepts of basin-margin faunas, latitudinal and climatic gradients, and a chronologically transitional fau- na. -
Ordovician Stratigraphy and Benthic Community Replacements in the Eastern Anti-Atlas, Morocco J
Ordovician stratigraphy and benthic community replacements in the eastern Anti-Atlas, Morocco J. Javier Alvaro, Mohammed Benharref, Jacques Destombes, Juan Carlos Gutiérrez-Marco, Aaron Hunter, Bertrand Lefebvre, Peter van Roy, Samuel Zamora To cite this version: J. Javier Alvaro, Mohammed Benharref, Jacques Destombes, Juan Carlos Gutiérrez-Marco, Aaron Hunter, et al.. Ordovician stratigraphy and benthic community replacements in the eastern Anti- Atlas, Morocco. The Great Ordovician Biodiversification Event: Insights from the Tafilalt Biota, Morocco, 485, The Geological Society of London, pp.SP485.20, In press, Geological Society, London, Special Publication, 10.1144/SP485.20. hal-02405970 HAL Id: hal-02405970 https://hal.archives-ouvertes.fr/hal-02405970 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The Geological Society Special Publications Ordovician stratigraphy and benthic community replacements in the eastern Anti-Atlas, Morocco --Manuscript Draft-- Manuscript Number: GSLSpecPub2019-17R1 Article Type: Research article Full Title: Ordovician stratigraphy and benthic community replacements in the eastern Anti-Atlas, Morocco Short Title: Ordovician stratigraphy of the Anti-Atlas Corresponding Author: Javier Alvaro Instituto de Geociencias SPAIN Corresponding Author E-Mail: [email protected] Other Authors: MOHAMMED BENHARREF JACQUES DESTOMBES JUAN CARLOS GUTIÉRREZ-MARCO AARON W. -
Foraging Behaviour of the Slender Loris (Loris Lydekkerianus Lydekkerianus): Implications for Theories of Primate Origins
Journal of Human Evolution 49 (2005) 289e300 Foraging behaviour of the slender loris (Loris lydekkerianus lydekkerianus): implications for theories of primate origins K.A.I. Nekaris* Department of Anthropology, Washington University, Campus Box 1114, One Brookings Drive, St. Louis, MO 63110, USA Received 3 May 2004; accepted 18 April 2005 Abstract Members of the Order Primates are characterised by a wide overlap of visual fields or optic convergence. It has been proposed that exploitation of either insects or angiosperm products in the terminal branches of trees, and the corresponding complex, three-dimensional environment associated with these foraging strategies, account for visual convergence. Although slender lorises (Loris sp.) are the most visually convergent of all the primates, very little is known about their feeding ecology. This study, carried out over 10 ½ months in South India, examines the feeding behaviour of L. lydekkerianus lydekkerianus in relation to hypotheses regarding visual predation of insects. Of 1238 feeding observations, 96% were of animal prey. Lorises showed an equal and overwhelming preference for terminal and middle branch feeding, using the undergrowth and trunk rarely. The type of prey caught on terminal branches (Lepidoptera, Odonata, Homoptera) differed significantly from those caught on middle branches (Hymenoptera, Coleoptera). A two-handed catch accompanied by bipedal postures was used almost exclusively on terminal branches where mobile prey was caught, whereas the more common capture technique of one-handed grab was used more often on sturdy middle branches to obtain slow moving prey. Although prey was detected with senses other than vision, vision was the key sense used upon the final strike. -
AMERICAN MUSEUM NOVITATES Published by Number 940 the AMERICAN MUSEUM of NATURAL HISTORY August 18, 1937 New York City
AMERICAN MUSEUM NOVITATES Published by Number 940 THE AMERICAN MUSEUM OF NATURAL HISTORY August 18, 1937 New York City ADDITIONS TO THE UPPER PALEOCENE FAUNA OF THE CRAZY MOUNTAIN FIELD By GEORGE GAYLORD SIMPSON In a previous paper (Simpson, 1936) an Upper Paleocene fauna from a high level in the Fort Union group east of the Crazy Mountains in cen- tral Montana was described. During the summer of 1936, Mr. Albert C. Silberling reopened the Scarritt Quarry, from which this fauna was derived, and made a second and still larger collection there for the Ameri- can Museum. The present paper records the new data derived from this addition to the collection. A specimen from a still higher level at a nearby locality is also described. This specimen was collected by Mr. Silberling personally and was presented to the Museum, while the Scar- ritt Quarry collection was incidental to Museum expeditions under my direction. The specimens have all been prepared by Albert C. Thomson, and the illustrations are by John C. Germann. The common forms in the Scarritt Quarry are now all represented by large suites of jaws and teeth, and most of the specimens found by the last collecting added little or nothing to knowledge of the fauna. There are still several rare forms on which our data are very inadequate, but the chances of obtaining better specimens of these by any reasonable amount of quarrying have become small. No further work in the quarry is planned for the near future, and this paper is essentially a final report on the fauna. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNTVERSITY OF MICHIGAN VOL.30, NO. 4, PP. 131-162 December 31,1998 CARPOLESTES SZMPSONZ, NEW SPECIES (MAMMALIA, PROPRIMATES) FROM THE LATE PALEOCENE OF THE CLARKS FORK BASIN, WYOMING JONATHAN I. BLOCH AND PHnIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page plus a table of contents will be sent to libraries on the Museum's mailing list. This will be sent to individuals on request. A list of the separate issues may also be obtained by request. Correspondence should be directed to the Publications Secretary, Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48 109- 1079. VOLS. 2-29 Parts of volumes may be obtained if available. Price lists are available upon inquiry. Text and illustrations 01998 by the Museum of Paleontology, University of Michigan CARPOLESTES SZMPSONZ, NEW SPECIES (MAMMALIA, PROPRIMATES) FROM THE LATE PALEOCENE OF THE CLARKS FORK BASIN, WYOMING BY JONATHAN I. BLOCH AND PHILIP D. GINGERICH Abstract - Carpolestes is a small North American late Paleocene mammal with distinctively specialized premolar teeth. P3 is polycuspate with a distinct anteroexternal extension, and P4 is high-crowned, bladelike, and multicuspate. Carpolestes is now known from at least 180 specimens representing four mor- phologically and stratigraphically distinct species. Fossils from freshwater lime- stones of the Clarks Fork Basin include complete dentitions of a new species, Carpolestes simpsoni, from Clarkforkian faunal zones Cf-2 and earliest Cf-3.