The Remarkable Tuatara Finds Its Place
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Climatic Shifts Drove Major Contractions in Avian Latitudinal Distributions Throughout the Cenozoic
Climatic shifts drove major contractions in avian latitudinal distributions throughout the Cenozoic Erin E. Saupea,1,2, Alexander Farnsworthb, Daniel J. Luntb, Navjit Sagooc, Karen V. Phamd, and Daniel J. Fielde,1,2 aDepartment of Earth Sciences, University of Oxford, OX1 3AN Oxford, United Kingdom; bSchool of Geographical Sciences, University of Bristol, Clifton, BS8 1SS Bristol, United Kingdom; cDepartment of Meteorology, Stockholm University, 106 91 Stockholm, Sweden; dDivision of Geological and Planetary Sciences, Caltech, Pasadena, CA 91125; and eDepartment of Earth Sciences, University of Cambridge, CB2 3EQ Cambridge, United Kingdom Edited by Nils Chr. Stenseth, University of Oslo, Oslo, Norway, and approved May 7, 2019 (received for review March 8, 2019) Many higher level avian clades are restricted to Earth’s lower lati- order avian historical biogeography invariably recover strong evi- tudes, leading to historical biogeographic reconstructions favoring a dence for an origin of most modern diversity on southern land- Gondwanan origin of crown birds and numerous deep subclades. masses (2, 6, 11). However, several such “tropical-restricted” clades (TRCs) are repre- The crown bird fossil record has unique potential to reveal sented by stem-lineage fossils well outside the ranges of their clos- where different groups of birds were formerly distributed in deep est living relatives, often on northern continents. To assess the time. Fossil evidence, for example, has long indicated that total- drivers of these geographic disjunctions, we combined ecological group representatives of clades restricted to relatively narrow niche modeling, paleoclimate models, and the early Cenozoic fossil geographic regions today were formerly found in different parts of record to examine the influence of climatic change on avian geo- – graphic distributions over the last ∼56 million years. -
Mesozoic Marine Reptile Palaeobiogeography in Response to Drifting Plates
ÔØ ÅÒÙ×Ö ÔØ Mesozoic marine reptile palaeobiogeography in response to drifting plates N. Bardet, J. Falconnet, V. Fischer, A. Houssaye, S. Jouve, X. Pereda Suberbiola, A. P´erez-Garc´ıa, J.-C. Rage, P. Vincent PII: S1342-937X(14)00183-X DOI: doi: 10.1016/j.gr.2014.05.005 Reference: GR 1267 To appear in: Gondwana Research Received date: 19 November 2013 Revised date: 6 May 2014 Accepted date: 14 May 2014 Please cite this article as: Bardet, N., Falconnet, J., Fischer, V., Houssaye, A., Jouve, S., Pereda Suberbiola, X., P´erez-Garc´ıa, A., Rage, J.-C., Vincent, P., Mesozoic marine reptile palaeobiogeography in response to drifting plates, Gondwana Research (2014), doi: 10.1016/j.gr.2014.05.005 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Mesozoic marine reptile palaeobiogeography in response to drifting plates To Alfred Wegener (1880-1930) Bardet N.a*, Falconnet J. a, Fischer V.b, Houssaye A.c, Jouve S.d, Pereda Suberbiola X.e, Pérez-García A.f, Rage J.-C.a and Vincent P.a,g a Sorbonne Universités CR2P, CNRS-MNHN-UPMC, Département Histoire de la Terre, Muséum National d’Histoire Naturelle, CP 38, 57 rue Cuvier, -
A Small Lepidosauromorph Reptile from the Early Triassic of Poland
A SMALL LEPIDOSAUROMORPH REPTILE FROM THE EARLY TRIASSIC OF POLAND SUSAN E. EVANS and MAGDALENA BORSUK−BIAŁYNICKA Evans, S.E. and Borsuk−Białynicka, M. 2009. A small lepidosauromorph reptile from the Early Triassic of Poland. Palaeontologia Polonica 65, 179–202. The Early Triassic karst deposits of Czatkowice quarry near Kraków, southern Poland, has yielded a diversity of fish, amphibians and small reptiles. Two of these reptiles are lepido− sauromorphs, a group otherwise very poorly represented in the Triassic record. The smaller of them, Sophineta cracoviensis gen. et sp. n., is described here. In Sophineta the unspecial− ised vertebral column is associated with the fairly derived skull structure, including the tall facial process of the maxilla, reduced lacrimal, and pleurodonty, that all resemble those of early crown−group lepidosaurs rather then stem−taxa. Cladistic analysis places this new ge− nus as the sister group of Lepidosauria, displacing the relictual Middle Jurassic genus Marmoretta and bringing the origins of Lepidosauria closer to a realistic time frame. Key words: Reptilia, Lepidosauria, Triassic, phylogeny, Czatkowice, Poland. Susan E. Evans [[email protected]], Department of Cell and Developmental Biology, Uni− versity College London, Gower Street, London, WC1E 6BT, UK. Magdalena Borsuk−Białynicka [[email protected]], Institut Paleobiologii PAN, Twarda 51/55, PL−00−818 Warszawa, Poland. Received 8 March 2006, accepted 9 January 2007 180 SUSAN E. EVANS and MAGDALENA BORSUK−BIAŁYNICKA INTRODUCTION Amongst living reptiles, lepidosaurs (snakes, lizards, amphisbaenians, and tuatara) form the largest and most successful group with more than 7 000 widely distributed species. The two main lepidosaurian clades are Rhynchocephalia (the living Sphenodon and its extinct relatives) and Squamata (lizards, snakes and amphisbaenians). -
Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
Final Copy 2019 10 01 Herrera
This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Herrera Flores, Jorge Alfredo A Title: The macroevolution and macroecology of Mesozoic lepidosaurs General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. A copy of this may be found at https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode This license sets out your rights and the restrictions that apply to your access to the thesis so it is important you read this before proceeding. Take down policy Some pages of this thesis may have been removed for copyright restrictions prior to having it been deposited in Explore Bristol Research. However, if you have discovered material within the thesis that you consider to be unlawful e.g. breaches of copyright (either yours or that of a third party) or any other law, including but not limited to those relating to patent, trademark, confidentiality, data protection, obscenity, defamation, libel, then please contact [email protected] and include the following information in your message: •Your contact details •Bibliographic details for the item, including a URL •An outline nature of the complaint Your claim will be investigated and, where appropriate, the item in question will be removed from public view as soon as possible. This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Herrera Flores, Jorge Alfredo A Title: The macroevolution and macroecology of Mesozoic lepidosaurs General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. -
Clades™ Prehistoric Card Game a Clade Is a Section of the Evolutionary Family Tree—Basically Any Branch, Including All Its Sub-Branches
CLADES™ PREHISTORIC Card Game A clade is a section of the evolutionary family tree —basically any branch, including all its sub-branches. A clade is a family of organisms, or living things, that are all more closely related to each other than they are to any other organisms. In this game you match cards according to their clades. Contents: Deck of 83 Clades Prehistoric cards. Includes 27 cards of each color and 2 bonus cards. There are also 5 animal description cards not used in play. Object: Spot matching card triples to collect the biggest animal pile! Setup Deal 1 face-down card to each player as their personal card. For now, players keep these cards face-down and don’t look at them. Deal 12 face-down shared cards to the middle of the play area. If you’re learning or teaching the game: • Before dealing, set aside the bonus cards and the cards showing only one or two animals. Play with just the cards showing three animals. • Deal 7 shared cards instead of 12. CLADESPrehistoricRules2.indd 1 10/17/17 10:15 AM All players help flip the 12 shared cards face-up. Sort the cards into three Making Triples rows according to their clades: top for Mammalia (mammals), middle for Sauropsida (sauropsids, or reptiles and birds), and bottom for Arthropoda In Clades Prehistoric, any two cards can make a triple with exactly one other (arthropods, or “bugs”). When the table is ready, each player picks up their card in the deck. personal card and looks at it. -
Antimicrobial Peptides in Reptiles
Pharmaceuticals 2014, 7, 723-753; doi:10.3390/ph7060723 OPEN ACCESS pharmaceuticals ISSN 1424-8247 www.mdpi.com/journal/pharmaceuticals Review Antimicrobial Peptides in Reptiles Monique L. van Hoek National Center for Biodefense and Infectious Diseases, and School of Systems Biology, George Mason University, MS1H8, 10910 University Blvd, Manassas, VA 20110, USA; E-Mail: [email protected]; Tel.: +1-703-993-4273; Fax: +1-703-993-7019. Received: 6 March 2014; in revised form: 9 May 2014 / Accepted: 12 May 2014 / Published: 10 June 2014 Abstract: Reptiles are among the oldest known amniotes and are highly diverse in their morphology and ecological niches. These animals have an evolutionarily ancient innate-immune system that is of great interest to scientists trying to identify new and useful antimicrobial peptides. Significant work in the last decade in the fields of biochemistry, proteomics and genomics has begun to reveal the complexity of reptilian antimicrobial peptides. Here, the current knowledge about antimicrobial peptides in reptiles is reviewed, with specific examples in each of the four orders: Testudines (turtles and tortosises), Sphenodontia (tuataras), Squamata (snakes and lizards), and Crocodilia (crocodilans). Examples are presented of the major classes of antimicrobial peptides expressed by reptiles including defensins, cathelicidins, liver-expressed peptides (hepcidin and LEAP-2), lysozyme, crotamine, and others. Some of these peptides have been identified and tested for their antibacterial or antiviral activity; others are only predicted as possible genes from genomic sequencing. Bioinformatic analysis of the reptile genomes is presented, revealing many predicted candidate antimicrobial peptides genes across this diverse class. The study of how these ancient creatures use antimicrobial peptides within their innate immune systems may reveal new understandings of our mammalian innate immune system and may also provide new and powerful antimicrobial peptides as scaffolds for potential therapeutic development. -
Reptile” Diversity and Evolution George A
“Reptile” Diversity and Evolution George A. Lozano Department of Biology University of Ottawa Summary Sauropsids Turtles Diapsids/Saurians Plesiosaurs † and ichthyosaurs † Lepidosaurs Tuatara Squamates (snakes, geckos, iguanas, monitors ) Archosaurs (crocodiles, dinosaurs, pterosaurs ) Dinosaurs 2 George A. Lozano Amniota Synapsida Sauropsida Diapsida Turtles Ancestral amniotes & Turtles Turtles - Testudina 250 species Carapace (vertebrae and ribs) Appendicular girdles INSIDE the shell Beak, no teeth (along with aves) Ear ossicle columella (ind?) 4 George A. Lozano Sauropsida Diapsida/Sauria Turtles 250 Archosaurs Ichthyosaurs† Lepidosaurs Plesiosaurs† 9.1K 7K Ear ossicle collumella, 3 rd ind. evol.) Lepidosaurs “scaly” reptiles 6700 species : 4000 lizards, 2700 snakes Tuatara: ancestral diapsid skull Squamata: derived diapsid skull, hemipenes Iguanas Geckos Snakes Skinks Gila monsters, monitor lizards, Komodo dragon 6 George A. Lozano Tuatara Turtles Squamates Modified Euryapsid: Aves diapsid Plesiosaur Ichthyosaur Snakes 8 George A. Lozano Sauropsida Diapsida Turtles Archosaurs Crocodiles Dinosaurs Pterosaurs† Dinosaurs Ornithischians† Saurischians •Ceratopsids •Duck-billed dino Sauropods† Theropods •Stegosaurus •Ankylosaurus Dinosaurs Ornithischians† Saurischians •-ceratops (uni, tri…) •Duck-billed dino Sauropods† Theropods •Stegosaurus •Diplodocus •Ankylosaurus •Brachiosaurus T. rex † Velociraptor † Birds 12 George A. Lozano Sauropod and ornithischian (ankylosaurus) 13 George A. Lozano 14 George A. Lozano Dinosaurs -
What Are Dinosaurs?
Tote Hughes, 140819 [email protected] Dinosaurs 1/20 What Are Dinosaurs? The following are not dinosaurs∗: • Things that aren’t organisms—There is no rock that is a dinosaur. • Things that existed before the Triassic period† • Pterosaurs The following are dinosaurs: • Birds (Aves) The following contain dinosaurs: • Archosaurs (X.Archosauria) • Reptiles (Reptilia) Dinosaur Overview A discussion of the important dinosaur clades. Dinosaurs are divided into two main groups: the eusaurischians‡ and ornithischians. Eusaurischians • Sauropods – Apatasaurus: diplodocoidean – Barosaurus: diplodocoidean – Brachiosaurus: macronarian – Diplodocus: diplodocoidean • Theropods – Allosaurus: carnosaurian – Archaeopteryx: maniraptor – Giganotosaurus: carnosaurian – Megalosaurus: megalosaurid – Spinosaurus: megalosaurid – Tyrannosaurus: tyrannosauroid – Velociraptor: maniraptor ∗See the Dinosaur Encyclopedia section for details on terms. †See Appendix: Time for details on geological time. ‡These are commonly called saurischians, but since almost every interesting saurischian is actually in the subclade X.Eusaurischia, I’ve taken the liberty of breaking the standard. I hope you will grow to understand and accept my decision. 1/20 Tote Hughes, 140819 [email protected] Dinosaurs 2/20 Ornithischians • Eurypodans (thyreophor) – Ankylosaurus: ankylosaurian – Stegosaurus: stegosaurian • Marginocephalians (cerapod) – Pachycephalosaurus: pachycephalosaurian – Triceratops: ceratopsian • Ornithopods (cerapod) – Hadrosaurus: hadrosauriform – Iguanodon: hadrosauriform -
Diversity in Rhynchocephalian Clevosaurus Skulls Based on CT Reconstruction of Two Late Triassic Species from Great Britain
Editors' choice Diversity in rhynchocephalian Clevosaurus skulls based on CT reconstruction of two Late Triassic species from Great Britain SOFIA A.V. CHAMBI-TROWELL, DAVID I. WHITESIDE, and MICHAEL J. BENTON Chambi-Trowell, S.A.V., Whiteside, D.I., and Benton M.J. 2019. Diversity in rhynchocephalian Clevosaurus skulls based on CT reconstruction of two Late Triassic species from Great Britain. Acta Palaeontologica Polonica 64 (1): 41–64. Clevosaurus was an early sphenodontian, known from many specimens and species from the Late Triassic and Early Jurassic. Here we describe and compare the cranial morphology of Clevosaurus hudsoni, the type species, and Clevosaurus cambrica, both from the UK, based on digital reconstructions from segmented CT scan data of two skulls. C. hudsoni has been described in some detail, but the CT data reveal new information on cranial anatomy, and C. cambrica is a newly described species for which the CT scans enable us to identify many previously undescribed bones, re-identify bones whose identity had previously been uncertain, and refine certain cranial elements. The near complete preservation of the left side of the skull of C. cambrica, and the preservation of much of the left side of the skull of C. hudsoni, provided us with the opportunity to fully reconstruct both species’ skulls in three dimensions. For the first time, coronoid bones are identified in Clevosaurus species from the British Isles. These two species show the diversity of morphology in the genus Clevosaurus. We provide evidence for two morphotypes of C. hudsoni based on study of the dentary dentition of the syntypes and other attributed specimens. -
A New Sphenodontian (Lepidosauria: Rhynchocephalia)
View metadata, citation and similar papersDownloaded at core.ac.uk from http://rspb.royalsocietypublishing.org/ on February 13, 2017 brought to you by CORE provided by CONICET Digital A new sphenodontian (Lepidosauria: Rhynchocephalia) from the Late Triassic of Argentina and the early origin of the herbivore opisthodontians rspb.royalsocietypublishing.org Ricardo N. Martı´nez1, Cecilia Apaldetti1,2, Carina E. Colombi1,2, Angel Praderio1, Eliana Fernandez1,2, Paula Santi Malnis1,2, 1,2 1 1 Research Gustavo A. Correa , Diego Abelin and Oscar Alcober 1Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan, Avenida Espan˜a 400 Norte, Cite this article: Martı´nez RN, Apaldetti C, 5400 San Juan, Argentina Colombi CE, Praderio A, Fernandez E, Malnis 2Consejo Nacional de Investigaciones Cientı´ficas y Te´cnicas, CONICET, Buenos Aires, Argentina PS, Correa GA, Abelin D, Alcober O. 2013 A new sphenodontian (Lepidosauria: Rhyncho- Sphenodontians were a successful group of rhynchocephalian reptiles that dominated the fossil record of Lepidosauria during the Triassic and Jurassic. cephalia) from the Late Triassic of Argentina Although evidence of extinction is seen at the end of the Laurasian Early and the early origin of the herbivore Cretaceous, they appeared to remain numerically abundant in South America opisthodontians. Proc R Soc B 280: 20132057. until the end of the period. Most of the known Late Cretaceous record in http://dx.doi.org/10.1098/rspb.2013.2057 South America is composed of opisthodontians, the herbivorous branch of Sphenodontia, whose oldest members were until recently reported to be from the Kimmeridgian–Tithonian (Late Jurassic). Here, we report a new sphenodontian, Sphenotitan leyesi gen. -
Mirnas Support an Archosaur, Not Lepidosaur, Affinity for Turtles
EVOLUTION & DEVELOPMENT 16:4, 189–196 (2014) DOI: 10.1111/ede.12081 Toward consilience in reptile phylogeny: miRNAs support an archosaur, not lepidosaur, affinity for turtles Daniel J. Field,a,b,* Jacques A. Gauthier,a Benjamin L. King,c Davide Pisani,d,e Tyler R. Lyson,a,b and Kevin J. Petersonf,* a Department of Geology and Geophysics, Yale University, 210 Whitney Avenue, New Haven, CT 06511, USA b Department of Vertebrate Zoology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA c Mount Desert Island Biological Laboratory, Salisbury Cove, ME 04672, USA d School of Earth Sciences, University of Bristol, Queen's Road, Bristol BS8 1RJ, United Kingdom e School of Biological Sciences, University of Bristol, Woodland Road, Bristol BS8 1UG, United Kingdom f Department of Biological Sciences, Dartmouth College, Hanover, NH 03755, USA *Authors for correspondence (e‐mail: [email protected], daniel.fi[email protected]) SUMMARY Understanding the phylogenetic position of for a turtle lepidosaur sister‐relationship; instead, we recover þ crown turtles (Testudines) among amniotes has been a source strong support for turtles sharing a more recent common of particular contention. Recent morphological analyses ancestor with archosaurs. We further test this result by suggest that turtles are sister to all other reptiles, whereas analyzing a super‐alignment of precursor miRNA sequences the vast majority of gene sequence analyses support turtles as for every miRNA inferred to have been present in the most being inside Diapsida, and usually as sister to crown recent common ancestor of tetrapods. This analysis yields a Archosauria (birds and crocodilians).