The Origin of Lissamphibia
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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. -
Limb Ossification in the Paleozoic Branchiosaurid Apateon (Temnospondyli) and the Early Evolution of Preaxial Dominance in Tetrapod Limb Development
EVOLUTION & DEVELOPMENT 9:1, 69 –75 (2007) Limb ossification in the Paleozoic branchiosaurid Apateon (Temnospondyli) and the early evolution of preaxial dominance in tetrapod limb development Nadia B. Fro¨bisch,a,Ã Robert L. Carroll,a and Rainer R. Schochb aRedpath Museum, McGill University, 859 Sherbrooke Street West, Montreal H3A 2K6, Canada bStaatliches Museum fu¨r Naturkunde Stuttgart, Rosenstein 1, 70191 Stuttgart, Germany ÃAuthor for correspondence (email: [email protected]) SUMMARY Despite the wide range of shapes and sizes that divergent evolution of these two pathways and its causes are accompany a vast variety of functions, the development of still not understood. Based on an extensive ontogenetic series tetrapod limbs follows a conservative pattern of de novo we investigated the pattern of limb development of the 300 Ma condensation, branching, and segmentation. Development of old branchiosaurid amphibian Apateon. This revealed a the zeugopodium and digital arch typically occurs in a posterior preaxial dominance in limb development that was previously to anterior sequence, referred to as postaxial dominance, with believed to be unique and derived for modern salamanders. a digital sequence of 4–3–5–2–1. The only exception to this The Branchiosauridae are favored as close relatives of pattern in all of living Tetrapoda can be found in salamanders, extant salamanders in most phylogenetic hypotheses of the which display a preaxial dominance in limb development, a de highly controversial origins and relationships of extant novo condensation of a basale commune (distal carpal/tarsal amphibians. The findings provide new insights into the 112) and a precoccial development of digits I and II. -
AMS112 1978-1979 Lowres Web
--~--------~--------------------------------------------~~~~----------~-------------- - ~------------------------------ COVER: Paul Webber, technical officer in the Herpetology department searchers for reptiles and amphibians on a field trip for the Colo River Survey. Photo: John Fields!The Australian Museum. REPORT of THE AUSTRALIAN MUSEUM TRUST for the YEAR ENDED 30 JUNE , 1979 ST GOVERNMENT PRINTER, NEW SOUTH WALES-1980 D. WE ' G 70708K-1 CONTENTS Page Page Acknowledgements 4 Department of Palaeontology 36 The Australian Museum Trust 5 Department of Terrestrial Invertebrate Ecology 38 Lizard Island Research Station 5 Department of Vertebrate Ecology 38 Research Associates 6 Camden Haven Wildlife Refuge Study 39 Associates 6 Functional Anatomy Unit.. 40 National Photographic Index of Australian Director's Research Laboratory 40 Wildlife . 7 Materials Conservation Section 41 The Australian Museum Society 7 Education Section .. 47 Letter to the Premier 9 Exhibitions Department 52 Library 54 SCIENTIFIC DEPARTMENTS Photographic and Visual Aid Section 54 Department of Anthropology 13 PublicityJ Pu bl ications 55 Department of Arachnology 18 National Photographic Index of Australian Colo River Survey .. 19 Wildlife . 57 Lizard Island Research Station 59 Department of Entomology 20 The Australian Museum Society 61 Department of Herpetology 23 Appendix 1- Staff .. 62 Department of Ichthyology 24 Appendix 2-Donations 65 Department of Malacology 25 Appendix 3-Acknowledgements of Co- Department of Mammalogy 27 operation. 67 Department of Marine -
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 -
Cape Range National Park
Cape Range National Park Management Plan No 65 2010 R N V E M E O N G T E O H F T W A E I S L T A E R R N A U S T CAPE RANGE NATIONAL PARK Management Plan 2010 Department of Environment and Conservation Conservation Commission of Western Australia VISION By 2020, the park and the Ningaloo Marine Park will be formally recognised amongst the world’s most valuable conservation and nature based tourism icons. The conservation values of the park will be in better condition than at present. This will have been achieved by reducing stress on ecosystems to promote their natural resilience, and facilitating sustainable visitor use. In particular, those values that are not found or are uncommon elsewhere will have been conserved, and their special conservation significance will be recognised by the local community and visitors. The park will continue to support a wide range of nature-based recreational activities with a focus on preserving the remote and natural character of the region. Visitors will continue to enjoy the park, either as day visitors from Exmouth or by camping in the park itself at one of the high quality camping areas. The local community will identify with the park and the adjacent Ningaloo Marine Park, and recognise that its values are of international significance. An increasing number of community members will support and want to be involved in its ongoing management. The Indigenous heritage of the park will be preserved by the ongoing involvement of the traditional custodians, who will have a critical and active role in jointly managing the cultural and conservation values of the park. -
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. -
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha)
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) by Richard Kissel A thesis submitted in conformity with the requirements for the degree of doctor of philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto © Copyright by Richard Kissel 2010 Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) Richard Kissel Doctor of Philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto 2010 Abstract Based on dental, cranial, and postcranial anatomy, members of the Permo-Carboniferous clade Diadectidae are generally regarded as the earliest tetrapods capable of processing high-fiber plant material; presented here is a review of diadectid morphology, phylogeny, taxonomy, and paleozoogeography. Phylogenetic analyses support the monophyly of Diadectidae within Diadectomorpha, the sister-group to Amniota, with Limnoscelis as the sister-taxon to Tseajaia + Diadectidae. Analysis of diadectid interrelationships of all known taxa for which adequate specimens and information are known—the first of its kind conducted—positions Ambedus pusillus as the sister-taxon to all other forms, with Diadectes sanmiguelensis, Orobates pabsti, Desmatodon hesperis, Diadectes absitus, and (Diadectes sideropelicus + Diadectes tenuitectes + Diasparactus zenos) representing progressively more derived taxa in a series of nested clades. In light of these results, it is recommended herein that the species Diadectes sanmiguelensis be referred to the new genus -
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 -
<Article-Title>Your Inner Fish
ELIZABETHCOWLES, DEPARTMENT EDITOR We are happy to welcomeABM new Book ReviewsEditor, ElizabethCowles. ANIMAL EVOLUTION describeshis evolutionfrom "wetbehind the ears"novice to world famous,verte- R brate variousfield YourInner Fish: A Into the 3.5- paleontologist.Noting Journey he shares lessons Billion-Year of the Human experiences, important History Body. he has learned the He details Neil Shubin. 2008. Pantheon Books. along way. By from the to find- 240 Hardcover. everystep, planning trip (ISBN0375424474). pp. fossils to the $24.00. ing requiredpost-expedi- tion lab work. Of course, Shubin'smost In April2006, an above-the-foldstory impressive,logistically difficult expedition B on the front page of TheNew YorkTimes to date involvedfinding, unearthing, and introducedthe world to the fossilTiktaalik. extractingTiktaalik and thatreceives early, Composed of featuresthat are part fish prominenttreatment. Downloaded from http://online.ucpress.edu/abt/article-pdf/70/5/308/54744/30163281.pdf by guest on 29 September 2021 and Tiktaalikwas held part amphibian, But the real of this book is as an link"in ter- triumph up important"missing the ease with which Shubin the restrialvertebrate evolution. The fossiland plucks same in different its Dr. Neil were thus string many ways-name- discoverer, Shubin, that whatever thrust into the currentdebate ly, through organ system headlong or scientific lens it is on the of evolutionin the biol- analyzed viewed, teaching clearthat within fish areantecedents to all classroom.Shubin has on ogy capitalized limbed vertebrates.In discrete the fame the of chapters, accompanying discovery the evolution of terres- Tiktaalikto his firstbook YourInner Shubin explores pen trial ears,teeth, limbs, and chemore- Fish: A Journey Into the 3.5-Billion-Year eyes, ceptors from structureswithin fish (and History of the HumanBody. -
The Braincase of Eocaecilia Micropodia (Lissamphibia, Gymnophiona) and the Origin of Caecilians
The Braincase of Eocaecilia micropodia (Lissamphibia, Gymnophiona) and the Origin of Caecilians Hillary C. Maddin1,2*, Farish A. Jenkins, Jr.1, Jason S. Anderson2 1 Department of Organismic and Evolutionary Biology and Museum of Comparative Zoology, Harvard University, Cambridge, Massachusetts, United States of America, 2 Department of Comparative Biology and Experimental Medicine, University of Calgary, Calgary, Alberta, Canada Abstract The scant fossil record of caecilians has obscured the origin and evolution of this lissamphibian group. Eocaecilia micropodia from the Lower Jurassic of North America remains the only stem-group caecilian with an almost complete skull preserved. However, this taxon has been controversial, engendering re-evaluation of traits considered to be plesiomorphic for extant caecilians. Both the validity of the placement of E. micropodia as a stem caecilian and estimates of the plesiomorphic condition of extant caecilians have been questioned. In order to address these issues, the braincase of E. micropodia was examined via micro-computed tomography. The braincase is considered to be a more reliable phylogenetic indicator than peripheral regions of the skull. These data reveal significant new information, including the possession of an ossified nasal septum, ossified anterior wall of the sphenethmoid, long anterolateral processes on the sphenethmoid, and paired olfactory nerve foramina, which are known only to occur in extant caecilians; the latter are possibly related to the evolution of the tentacle, a caecilian autapomorphy. A phylogenetic analysis that included 64 non-amniote taxa and 308 characters represents the first extensive test of the phylogenetic affinities of E. micropodia. The results place E. micropodia securely on the stem of extant caecilians, representing a clade within Temnospondyli that is the sister taxon to batrachians plus Gerobatrachus. -
Permian Tetrapods from the Sahara Show Climate-Controlled Endemism in Pangaea
letters to nature 6. Wysession, M. et al. The Core-Mantle Boundary Region 273–298 (American Geophysical Union, faunas that dominated tropical-to-temperate zones to the north Washington, DC, 1998). 13–15 7. Sidorin, I., Gurnis, M., Helmberger, D. V.& Ding, X. Interpreting D 00 seismic structure using synthetic and south . Our results show that long-standing theories of waveforms computed from dynamic models. Earth Planet. Sci. Lett. 163, 31–41 (1998). Late Permian faunal homogeneity are probably oversimplified as 8. Boehler, R. High-pressure experiments and the phase diagram of lower mantle and core constituents. the result of uneven latitudinal sampling. Rev. Geophys. 38, 221–245 (2000). For over 150 yr, palaeontologists have understood end-Palaeozoic 9. Alfe`, D., Gillan, M. J. & Price, G. D. Composition and temperature of the Earth’s core constrained by combining ab initio calculations and seismic data. Earth Planet. Sci. Lett. 195, 91–98 (2002). terrestrial ecosystems largely on the basis of Middle and Late 10. Thomas, C., Kendall, J. & Lowman, J. Lower-mantle seismic discontinuities and the thermal Permian tetrapod faunas from southern Africa. The fauna of these morphology of subducted slabs. Earth Planet. Sci. Lett. 225, 105–113 (2004). rich beds, particularly South Africa’s Karoo Basin, has provided 11. Thomas, C., Garnero, E. J. & Lay, T. High-resolution imaging of lowermost mantle structure under the fundamental insights into the origin of modern terrestrial trophic Cocos plate. J. Geophys. Res. 109, B08307 (2004). 16 12. Mu¨ller, G. The reflectivity method: A tutorial. Z. Geophys. 58, 153–174 (1985). structure and the successive adaptations that set the stage for the 13 13. -
Origin and Phylogenetic Relationships of Living Amphibians
Points of View Syst. Biol. 51(2):364–369, 2002 Tetrapod Phylogeny, Amphibian Origins, and the Denition of the Name Tetrapoda MICHEL LAURIN Equip´ e “Formations squelettiques” UMR CNRS 8570, Case 7077, Universite´ Paris 7, 75005 Paris, France; E-mail: [email protected] The most detailed, computer-generated Ahlberg and Milner, 1994) or did not include phylogeny of early amphibians has been amphibians (Gauthier et al., 1988), thus published recently (Anderson, 2001). The precluding identication of the dichotomy study was based on an analysis of 182 os- between amphibians and reptiliomorphs teological characters and 49 taxa, including (the clade that includes amniotes and the 41 “lepospondyls,” 7 other Paleozoic taxa extinct taxa that are more closely related representing other major groups (seymouri- to amniotes than to lissamphibians). The amorphs, embolomeres, temnospondyls, latest phylogeny (Anderson, 2001) suggests Downloaded By: [University of Tennessee] At: 00:39 18 January 2008 etc.), and a single lissamphibian (the oldest that despite initial skepticism (Coates et al., known apodan, the Jurassic taxon Eocae- 2000), the new pattern of stegocephalian cilia). The publication of this phylogeny is relationships appears to be well supported welcome, but several points raised in that and relatively stable, at least as it pertains to paper deserve to be discussed further. Espe- the relationships between major taxa such cially problematic are the views Anderson as Temnospondyli, Embolomeri, Seymouri- expressed about the polyphyletic origin of amorpha, Amniota, and the paraphyletic extant amphibians and about the application group informally called lepospondyls of phylogenetic nomenclature. (Figs. 1a, 1b). TETRAPOD PHYLOGENY Anderson (2001) found that the lep- Origin of Extant Amphibians ospondyls are more closely related to This brings us to the more difcult ques- amniotes than to seymouriamorphs and em- tion of amphibian origins.