Creativity, Origins, and Ancestors What Frog Evolution Can Teach Us
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Alfred Romer – Wikipedia
Alfred Romer – Wikipedia https://de.wikipedia.org/wiki/Alfred_Romer aus Wikipedia, der freien Enzyklopädie Alfred Sherwood Romer (* 28. Dezember 1894 in White Plains, New York; † 5. November 1973) war ein US-amerikanischer Paläontologe. Sein Fachgebiet war die Evolution der Wirbeltiere. Inhaltsverzeichnis 1 Leben 2 Romer-Lücke 3 Auszeichnungen und Ehrungen 4 Schriften 5 Weblinks 6 Einzelnachweise Leben Alfred Sherwood Romer wurde in White Plains, New York geboren, wo er seinen High-School-Abschluss machte. Danach arbeitete er ein Jahr lang als Angestellter bei der Eisenbahn und entschloss sich dann doch für den Besuch eines College. Mit Hilfe eines Stipendiums vom Amherst College konnte er dort Geschichte und deutsche Literatur studieren. Durch häufige Besuche des American Museum of Natural History entdeckte er seine Begeisterung für naturkundliche Fossilien. Bei Ausbruch des Ersten Weltkriegs meldete er sich als Freiwilliger zum Kriegsdienst und wurde sofort in Frankreich eingesetzt. 1919 kam er zurück nach New York und nahm das Studium der Biologie an der Columbia University auf, das er bereits zwei Jahre später mit der Promotion abschloss. Danach war er als wissenschaftliche Hilfskraft an der Bellevue Medical School der New York University beschäftigt und lehrte insbesondere Histologie, Embryologie und Allgemeine Anatomie. 1923 erhielt er einen Ruf von der Universität Chicago, wo er seine spätere Ehefrau Ruth kennenlernte, mit der er drei Kinder hatte. In Chicago fand er Bedingungen vor, die es ihm ermöglichten, sein Hauptinteresse zu intensivieren - die Paläontologie. So entstanden in den Jahren von 1925 bis 1935 37 Fachartikel, die sich mit diesem Thema befassten. 1934 wurde er zum Professor für Biologie an der Harvard University ernannt. -
Tadpole Consumption Is a Direct Threat to the Endangered Purple Frog, Nasikabatrachus Sahyadrensis
SALAMANDRA 51(3) 252–258 30 October 2015 CorrespondenceISSN 0036–3375 Correspondence Tadpole consumption is a direct threat to the endangered purple frog, Nasikabatrachus sahyadrensis Ashish Thomas & S. D. Biju Systematics Lab, Department of Environmental Studies, University of Delhi, Delhi 110 007, India Corresponding author: S. D. Biju, e-mail: [email protected] Manuscript received: 5 July 2014 Accepted: 30 December 2014 by Alexander Kupfer Amphibians across the world are suffering alarming popu- Southeast Asia have witnessed drastic population declines lation declines with nearly one third of the ca 7,300 species caused by overexploitation over the last couple of decades being threatened worldwide (Stuart et al. 2008, Wake & (Warkentin et al. 2008). Often, natural populations are Vredenburg 2008, IUCN 2014). Major factors attributed harvested without regard of the consequences or implica- to the decline include habitat destruction (Houlahan et tions of this practice on the dynamics or sustainability of al. 2000, Sodhi et al. 2008), chemical pollution (Ber ger the exploited populations (Getz & Haight 1989). When 1998), climate change (Adams 1999, Carpenter & Tur- the extent of exploitation is greater than the sustaining ca- ner 2000), diseases (McCallum 2007, Cushman 2006), pacity or turnover rate of a species, there is every possi- and invasive species (Boone & Bridges 2003). The West- bility that the species may become locally extinct, which ern Ghats of India, a global hotspot for amphibian diver- would subsequently have drastic ecological implications sity and endemism (Biju 2001, Biju & Bossuyt 2003), has in the particular region (Duffy 2002, Wright et al. 2006, more than 40% of its amphibian fauna threatened with ex- Carpenter et al. -
New Permian Fauna from Tropical Gondwana
ARTICLE Received 18 Jun 2015 | Accepted 18 Sep 2015 | Published 5 Nov 2015 DOI: 10.1038/ncomms9676 OPEN New Permian fauna from tropical Gondwana Juan C. Cisneros1,2, Claudia Marsicano3, Kenneth D. Angielczyk4, Roger M. H. Smith5,6, Martha Richter7, Jo¨rg Fro¨bisch8,9, Christian F. Kammerer8 & Rudyard W. Sadleir4,10 Terrestrial vertebrates are first known to colonize high-latitude regions during the middle Permian (Guadalupian) about 270 million years ago, following the Pennsylvanian Gondwanan continental glaciation. However, despite over 150 years of study in these areas, the bio- geographic origins of these rich communities of land-dwelling vertebrates remain obscure. Here we report on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana that sheds new light on patterns of tetrapod distribution. Northeastern Brazil hosted an extensive lacustrine system inhabited by a unique community of temnospondyl amphibians and reptiles that considerably expand the known temporal and geographic ranges of key subgroups. Our findings demonstrate that tetrapod groups common in later Permian and Triassic temperate communities were already present in tropical Gondwana by the early Permian (Cisuralian). This new fauna constitutes a new biogeographic province with North American affinities and clearly demonstrates that tetrapod dispersal into Gondwana was already underway at the beginning of the Permian. 1 Centro de Cieˆncias da Natureza, Universidade Federal do Piauı´, 64049-550 Teresina, Brazil. 2 Programa de Po´s-Graduac¸a˜o em Geocieˆncias, Departamento de Geologia, Universidade Federal de Pernambuco, 50740-533 Recife, Brazil. 3 Departamento de Cs. Geologicas, FCEN, Universidad de Buenos Aires, IDEAN- CONICET, C1428EHA Ciudad Auto´noma de Buenos Aires, Argentina. -
What Do Tadpoles Really Eat? Assessing the Trophic Status of an Understudied and Imperiled Group of Consumers in Freshwater Habitats
Freshwater Biology (2007) 52, 386–395 doi:10.1111/j.1365-2427.2006.01694.x OPINION What do tadpoles really eat? Assessing the trophic status of an understudied and imperiled group of consumers in freshwater habitats RONALD ALTIG,* MATT R. WHILES† AND CINDY L. TAYLOR‡ *Department of Biological Sciences, Mississippi State University, Mississippi State, MS, U.S.A. †Department of Zoology and Center for Ecology, Southern Illinois University, Carbondale, IL, U.S.A. ‡Department of Biology, Austin Peay State University, Clarksville, TN, U.S.A. SUMMARY 1. Understanding the trophic status of consumers in freshwater habitats is central to understanding their ecological roles and significance. Tadpoles are a diverse and abundant component of many freshwater habitats, yet we know relatively little about their feeding ecology and true trophic status compared with many other consumer groups. While many tadpole species are labelled herbivores or detritivores, there is surprisingly little evidence to support these trophic assignments. 2. Here we discuss shortcomings in our knowledge of the feeding ecology and trophic status of tadpoles and provide suggestions and examples of how we can more accurately quantify their trophic status and ecological significance. 3. Given the catastrophic amphibian declines that are ongoing in many regions of the planet, there is a sense of urgency regarding this information. Understanding the varied ecological roles of tadpoles will allow for more effective conservation of remaining populations, benefit captive breeding programmes, and allow for more accurate predic- tions of the ecological consequences of their losses. Keywords: amphibian, assimilation, diet, feeding behaviour, omnivory Amphibians are disappearing from the planet at an of the functional roles and trophic status of general- alarming rate (Stuart et al., 2004; Lips et al., 2005). -
BOA2.1 Caecilian Biology and Natural History.Key
The Biology of Amphibians @ Agnes Scott College Mark Mandica Executive Director The Amphibian Foundation [email protected] 678 379 TOAD (8623) 2.1: Introduction to Caecilians Microcaecilia dermatophaga Synapomorphies of Lissamphibia There are more than 20 synapomorphies (shared characters) uniting the group Lissamphibia Synapomorphies of Lissamphibia Integumen is Glandular Synapomorphies of Lissamphibia Glandular Skin, with 2 main types of glands. Mucous Glands Aid in cutaneous respiration, reproduction, thermoregulation and defense. Granular Glands Secrete toxic and/or noxious compounds and aid in defense Synapomorphies of Lissamphibia Pedicellate Teeth crown (dentine, with enamel covering) gum line suture (fibrous connective tissue, where tooth can break off) basal element (dentine) Synapomorphies of Lissamphibia Sacral Vertebrae Sacral Vertebrae Connects pelvic girdle to The spine. Amphibians have no more than one sacral vertebrae (caecilians have none) Synapomorphies of Lissamphibia Amphicoelus Vertebrae Synapomorphies of Lissamphibia Opercular apparatus Unique to amphibians and Operculum part of the sound conducting mechanism Synapomorphies of Lissamphibia Fat Bodies Surrounding Gonads Fat Bodies Insulate gonads Evolution of Amphibians † † † † Actinopterygian Coelacanth, Tetrapodomorpha †Amniota *Gerobatrachus (Ray-fin Fishes) Lungfish (stem-tetrapods) (Reptiles, Mammals)Lepospondyls † (’frogomander’) Eocaecilia GymnophionaKaraurus Caudata Triadobatrachus Anura (including Apoda Urodela Prosalirus †) Salientia Batrachia Lissamphibia -
A New Species of the Genus Nasikabatrachus (Anura, Nasikabatrachidae) from the Eastern Slopes of the Western Ghats, India
Alytes, 2017, 34 (1¢4): 1¢19. A new species of the genus Nasikabatrachus (Anura, Nasikabatrachidae) from the eastern slopes of the Western Ghats, India S. Jegath Janani1,2, Karthikeyan Vasudevan1, Elizabeth Prendini3, Sushil Kumar Dutta4, Ramesh K. Aggarwal1* 1Centre for Cellular and Molecular Biology (CSIR-CCMB), Uppal Road, Tarnaka, Hyderabad, 500007, India. <[email protected]>, <[email protected]>. 2Current Address: 222A, 5th street, Annamalayar Colony, Sivakasi, 626123, India.<[email protected]>. 3Division of Vertebrate Zoology, Department of Herpetology, American Museum of Natural History, Central Park West at 79th Street, New York NY 10024-5192, USA. <[email protected]>. 4Nature Environment and Wildlife Society (NEWS), Nature House, Gaudasahi, Angul, Odisha. <[email protected]>. * Corresponding Author. We describe a new species of the endemic frog genus Nasikabatrachus,from the eastern slopes of the Western Ghats, in India. The new species is morphologically, acoustically and genetically distinct from N. sahyadrensis. Computed tomography scans of both species revealed diagnostic osteological differences, particularly in the vertebral column. Male advertisement call analysis also showed the two species to be distinct. A phenological difference in breeding season exists between the new species (which breeds during the northeast monsoon season; October to December), and its sister species (which breeds during the southwest monsoon; May to August). The new species shows 6 % genetic divergence (K2P) at mitochondrial 16S rRNA (1330 bp) partial gene from its congener, indicating clear differentiation within Nasikabatra- chus. Speciation within this fossorial lineage is hypothesized to have been caused by phenological shift in breeding during different monsoon seasons—the northeast monsoon in the new species versus southwest monsoon in N. -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
August 2008 Issue 96
NEWSLETTER No. 96 THE FROG AND TADPOLE STUDY GROUP OF NSW INC The Year of the Frog Email [email protected] August 2008 PO Box 296 Rockdale NSW 2216 Website www.fats.org.au ABN 34 282 154 794 Pseudophryne covacevichae photo by Wendy Grimm Arrive at 6.30pm for a 7.00 pm start. AGM commences 7pm followed by our usual meeting Friday 1st August 2008 end of Jamieson St. (off Holker Street), Follow the signs to Building 22 Homebush Bay, Sydney Olympic Park Accessible by bus or train. Call us for details. Photo taken near Millaa Millaa on the Atherton tablelands The FATS Annual General Meeting commences on Friday at 7pm 1/8/08, for about 30 minutes and followed by our usual meeting. CONTENTS Main speakers 3 large glass tanks for sale, make us an offer, see p12 Mark Semeniuk p2-3 and Arthur White st MEETING FORMAT for 1 August 2008 Map of Arthur’s trip p4 Media clippings p4 6.30 pm Lots of White Lips, Gracilentas, Perons, Green Tree Frogs, Fallaxes and Rubellas need homes. Please bring your FATS Pharyngula p5 membership card, donation & amphibian licence to the meeting Bacteria could stop frog killer p6-7 and take home a lost froggy friend. Hiccups 7.00 pm Welcome and AGM have a purpose for tadpoles p8 7.30 pm Announcements. Cane toads on Oz p9 7.45 pm The main speaker is David Nelson :- “Bufo for breakfast. Greenwash, How Cane Toads affect native predators and their prey” bottled water and Coca Cola p10 9.00 pm Field trip reports and five favourite slides. -
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. -
Early Tetrapod Relationships Revisited
Biol. Rev. (2003), 78, pp. 251–345. f Cambridge Philosophical Society 251 DOI: 10.1017/S1464793102006103 Printed in the United Kingdom Early tetrapod relationships revisited MARCELLO RUTA1*, MICHAEL I. COATES1 and DONALD L. J. QUICKE2 1 The Department of Organismal Biology and Anatomy, The University of Chicago, 1027 East 57th Street, Chicago, IL 60637-1508, USA ([email protected]; [email protected]) 2 Department of Biology, Imperial College at Silwood Park, Ascot, Berkshire SL57PY, UK and Department of Entomology, The Natural History Museum, Cromwell Road, London SW75BD, UK ([email protected]) (Received 29 November 2001; revised 28 August 2002; accepted 2 September 2002) ABSTRACT In an attempt to investigate differences between the most widely discussed hypotheses of early tetrapod relation- ships, we assembled a new data matrix including 90 taxa coded for 319 cranial and postcranial characters. We have incorporated, where possible, original observations of numerous taxa spread throughout the major tetrapod clades. A stem-based (total-group) definition of Tetrapoda is preferred over apomorphy- and node-based (crown-group) definitions. This definition is operational, since it is based on a formal character analysis. A PAUP* search using a recently implemented version of the parsimony ratchet method yields 64 shortest trees. Differ- ences between these trees concern: (1) the internal relationships of aı¨stopods, the three selected species of which form a trichotomy; (2) the internal relationships of embolomeres, with Archeria -
Phylogeny and Evolution of the Dissorophoid Temnospondyls
Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses. -
Proceedings of the Open University Geological Society
Proceedings of the Open University Geological Society Volume 4 2018 Including lecture articles from the AGM 2017, the Milton Keynes Symposium 2017, OUGS Members’ field trip reports, the Annual Report for 2017, and the 2017 Moyra Eldridge Photographic Competition winning and highly commended photographs Edited and designed by: Dr David M. Jones 41 Blackburn Way, Godalming, Surrey GU7 1JY e-mail: [email protected] The Open University Geological Society (OUGS) and its Proceedings Editor accept no responsibility for breach of copyright. Copyright for the work remains with the authors, but copyright for the published articles is that of the OUGS. ISSN 2058-5209 © Copyright reserved Proceedings of the OUGS 4 2018; published 2018; printed by Hobbs the Printers Ltd, Totton, Hampshire Evolution of life on land: how new Scottish fossils are re-writing our under- standing of this important transition Dr Tim Kearsey BGS Edinburgh Romer’s gap — a hole in our understanding t has long been understood that at some point in the evolution Meanwhile at a quarry called East Kirkton Quarry near Iof vertebrates there was a transition point where they moved Edinburgh in Scotland vertebrate fossils were discovered that are from mainly subsiding in water to living on land. However, until 10 million years younger than the Greenland fossils. These include recently there had been no fossil evidence that documented how Westlothiana, which is thought to be the first amniote (egg-layer) vertebrate life stepped from water to land. This significant hole in or possibly early reptile (Smithson and Rolfe 1990) and scientific knowledge of evolution is referred to as Romer’s gap Balanerpeton an extinct genus of temnospondyl amphibian.