The Phylogeny of Antiarch Placoderms
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Cambridge University Press 978-1-107-17944-8 — Evolution And
Cambridge University Press 978-1-107-17944-8 — Evolution and Development of Fishes Edited by Zerina Johanson , Charlie Underwood , Martha Richter Index More Information Index abaxial muscle,33 Alizarin red, 110 arandaspids, 5, 61–62 abdominal muscles, 212 Alizarin red S whole mount staining, 127 Arandaspis, 5, 61, 69, 147 ability to repair fractures, 129 Allenypterus, 253 arcocentra, 192 Acanthodes, 14, 79, 83, 89–90, 104, 105–107, allometric growth, 129 Arctic char, 130 123, 152, 152, 156, 213, 221, 226 alveolar bone, 134 arcualia, 4, 49, 115, 146, 191, 206 Acanthodians, 3, 7, 13–15, 18, 23, 29, 63–65, Alx, 36, 47 areolar calcification, 114 68–69, 75, 79, 82, 84, 87–89, 91, 99, 102, Amdeh Formation, 61 areolar cartilage, 192 104–106, 114, 123, 148–149, 152–153, ameloblasts, 134 areolar mineralisation, 113 156, 160, 189, 192, 195, 198–199, 207, Amia, 154, 185, 190, 193, 258 Areyongalepis,7,64–65 213, 217–218, 220 ammocoete, 30, 40, 51, 56–57, 176, 206, 208, Argentina, 60–61, 67 Acanthodiformes, 14, 68 218 armoured agnathans, 150 Acanthodii, 152 amphiaspids, 5, 27 Arthrodira, 12, 24, 26, 28, 74, 82–84, 86, 194, Acanthomorpha, 20 amphibians, 1, 20, 150, 172, 180–182, 245, 248, 209, 222 Acanthostega, 22, 155–156, 255–258, 260 255–256 arthrodires, 7, 11–13, 22, 28, 71–72, 74–75, Acanthothoraci, 24, 74, 83 amphioxus, 49, 54–55, 124, 145, 155, 157, 159, 80–84, 152, 192, 207, 209, 212–213, 215, Acanthothoracida, 11 206, 224, 243–244, 249–250 219–220 acanthothoracids, 7, 12, 74, 81–82, 211, 215, Amphioxus, 120 Ascl,36 219 Amphystylic, 148 Asiaceratodus,21 -
Upper Devonian) of Latvia
Estonian Journal of Earth Sciences, 2021, 70, 1, 3–17 https://doi.org/10.3176/earth.2021.01 Revision of asterolepidoid antiarch remains from the Ogre Formation (Upper Devonian) of Latvia Ervīns Lukševičs Department of Geology, University of Latvia, Raiņa Boulevard 19, Riga LV1586, Latvia; [email protected] Received 3 June 2020, accepted 8 September 2020, available online 15 December 2020 Abstract. The Frasnian (Upper Devonian) antiarch Walterilepis speciosa was first described in 1933 (as Taeniolepis) on the basis of a single specimen. The newly collected material has allowed the head to be described in a more detail, especially the nuchal and paranuchal plates. Other newly described elements include bones of the pectoral appendages and trunk armour, demonstrating a rather high and short trunk armour. The shape and proportions of the head and trunk armour suggest the attribution of Walterilepis to the family Pterichthyodidae; it is most probably closely related to Lepadolepis from the Late Frasnian of Germany. Whilst W. speciosa is endemic to the Latvian part of the Baltic Devonian Basin, the connection to the Rheinisches Schiefergebirge is probably closer than previously presumed. Walterilepis fits into the biostratigraphical column at the same level as Bothriolepis maxima and B. evaldi, indicating the high diversity of antiarchs during Pamūšis time. Key words: Frasnian, biostratigraphy, morphology, placoderm, Baltic Devonian basin. INTRODUCTION noted that the generic name of Gross (1932, 1933a) is preoccupied by the sarcopterygian name Taeniolepis The wellknown Baltic German palaeontologist Walter Trautschold, 1874, and he erected the replacement name Gross, who was born in the close vicinity of Riga, made Walterilepis (Moloshnikov 2001). -
Ornamentation of Dermal Bones of Placodermi from the Lower Devonian of Morocco As a Measure of Biodiversity
Mateusz Antczak, Błażej Berkowski Geologos 23, 2 (2017): 65–73 doi: 10.1515/logos-2017-0009 Ornamentation of dermal bones of Placodermi from the Lower Devonian of Morocco as a measure of biodiversity Mateusz Antczak1*, Błażej Berkowski1 1Adam Mickiewicz University, Faculty of Geographical and Geological Sciences, Institute of Geology, Department of Palaeontology and Stratigraphy, Krygowskiego 12, 61-680 Poznań, Poland * corresponding author, e-mail: [email protected] Abstract Dermal bones are formed early during growth and thus constitute an important tool in studies of ontogenetic and evo- lutionary changes amongst early vertebrates. Ornamentation of dermal bones of terrestrial vertebrates is often used as a taxonomic tool, for instance in Aetosauria, extant lungfishes (Dipnoi) and ray-finned fishes (Actinopterygii), for which it have been proved to be of use in differentiating specimens to species level. However, it has not been utilised to the same extent in placoderms. Several features of the ornamentation of Early Devonian placoderms from Hamar Laghdad (Morocco) were examined using both optical and scanning electron microscopy to determine whether it is possible to distinguish armoured Palaeozoic fishes. Four distinct morphotypes, based on ornamentation of dermal bones, are dif- ferentiated. These distinct types of ornamentation may be the result of either different location of dermal plates on the body or of ontogenetic (intraspecific) and/or interspecific variation. Keywords: Arthrodira, interspecific variation, ontogeny, fishes, North Africa 1. Introduction both between species and ontogenetic stages (Tri- najstic, 1999); acanthodians are almost exclusively Dermal bones, or membranous bones, form known by scale taxa (Brazeau & Friedman, 2015), as without a chondral stage; in extant fish taxa these are many sharks (e.g., Martin, 2009). -
Copyrighted Material
06_250317 part1-3.qxd 12/13/05 7:32 PM Page 15 Phylum Chordata Chordates are placed in the superphylum Deuterostomia. The possible rela- tionships of the chordates and deuterostomes to other metazoans are dis- cussed in Halanych (2004). He restricts the taxon of deuterostomes to the chordates and their proposed immediate sister group, a taxon comprising the hemichordates, echinoderms, and the wormlike Xenoturbella. The phylum Chordata has been used by most recent workers to encompass members of the subphyla Urochordata (tunicates or sea-squirts), Cephalochordata (lancelets), and Craniata (fishes, amphibians, reptiles, birds, and mammals). The Cephalochordata and Craniata form a mono- phyletic group (e.g., Cameron et al., 2000; Halanych, 2004). Much disagree- ment exists concerning the interrelationships and classification of the Chordata, and the inclusion of the urochordates as sister to the cephalochor- dates and craniates is not as broadly held as the sister-group relationship of cephalochordates and craniates (Halanych, 2004). Many excitingCOPYRIGHTED fossil finds in recent years MATERIAL reveal what the first fishes may have looked like, and these finds push the fossil record of fishes back into the early Cambrian, far further back than previously known. There is still much difference of opinion on the phylogenetic position of these new Cambrian species, and many new discoveries and changes in early fish systematics may be expected over the next decade. As noted by Halanych (2004), D.-G. (D.) Shu and collaborators have discovered fossil ascidians (e.g., Cheungkongella), cephalochordate-like yunnanozoans (Haikouella and Yunnanozoon), and jaw- less craniates (Myllokunmingia, and its junior synonym Haikouichthys) over the 15 06_250317 part1-3.qxd 12/13/05 7:32 PM Page 16 16 Fishes of the World last few years that push the origins of these three major taxa at least into the Lower Cambrian (approximately 530–540 million years ago). -
Tesis De Grado Valentina Blandon 201511522
Reconstrucción científica del Macizo Devónico de Floresta, ilustrada en un diorama. Por Valentina Blandón Hurtado 201511522 Director Dr. Leslie F. Noè Uniandes Co director Dr. Jaime Reyes Abril S.G.C. Universidad de los Andes Facultad de Ciencias Departamento de Geociencias Bogotá, Colombia Noviembre 2019 Leslie F. Noè Jaime A. Reyes Valentina Blandón Hurtado II Tabla de contenido Dedicación .................................................................................................................................V Agradecimiento ..........................................................................................................................V Resumen ...................................................................................................................................VI Abstract ...................................................................................................................................VII Introducción ................................................................................................................................1 Metodología y Materiales ...........................................................................................................5 Resultados y Discusiones ...........................................................................................................7 Devónico Inferior – Formación El Tibet ....................................................................................7 Descripción organismos Formación El Tibet .........................................................................8 -
The Earliest Phyllolepid (Placodermi, Arthrodira) from the Late Lochkovian (Early Devonian) of Yunnan (South China)
Geol. Mag. 145 (2), 2008, pp. 257–278. c 2007 Cambridge University Press 257 doi:10.1017/S0016756807004207 First published online 30 November 2007 Printed in the United Kingdom The earliest phyllolepid (Placodermi, Arthrodira) from the Late Lochkovian (Early Devonian) of Yunnan (South China) V. DUPRET∗ &M.ZHU Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, P.O. Box 643, Xizhimenwai Dajie 142, Beijing 100044, People’s Republic of China (Received 1 November 2006; accepted 26 June 2007) Abstract – Gavinaspis convergens, a new genus and species of the Phyllolepida (Placodermi: Arthrodira), is described on the basis of skull remains from the Late Lochkovian (Xitun Formation, Early Devonian) of Qujing (Yunnan, South China). This new form displays a mosaic of characters of basal actinolepidoid arthrodires and more derived phyllolepids. A new hypothesis is proposed concerning the origin of the unpaired centronuchal plate of the Phyllolepida by a fusion of the paired central plates into one single dermal element and the loss of the nuchal plate. A phylogenetic analysis suggests the position of Gavinaspis gen. nov. as the sister group of the Phyllolepididae, in a distinct new family (Gavinaspididae fam. nov.). This new form suggests a possible Chinese origin for the Phyllolepida or that the common ancestor to Phyllolepida lived in an area including both South China and Gondwana, and in any case corroborates the palaeogeographic proximity between Australia and South China during the Devonian Period. Keywords: Devonian, China, Placodermi, phyllolepids, biostratigraphy, palaeobiogeography. 1. Introduction 1934). Subsequently, they were considered as either sharing an immediate common ancestor with the The Phyllolepida are a peculiar group of the Arthrodira Arthrodira (Denison, 1978), belonging to the Actin- (Placodermi), widespread in the Givetian–Famennian olepidoidei (Long, 1984), or being of indetermined of Gondwana (Australia, Antarctica, Turkey, South position within the Arthrodira (Goujet & Young,1995). -
Devonian Daniel Childress Parkland College
Parkland College A with Honors Projects Honors Program 2019 Did You Know: Devonian Daniel Childress Parkland College Recommended Citation Childress, Daniel, "Did You Know: Devonian" (2019). A with Honors Projects. 252. https://spark.parkland.edu/ah/252 Open access to this Poster is brought to you by Parkland College's institutional repository, SPARK: Scholarship at Parkland. For more information, please contact [email protected]. GENUS PHYLUM CLASS ORDER SIZE ENVIROMENT DIET: DIET: DIET: OTHER D&D 5E “PERSONAL NOTES” # CARNIVORE HERBIVORE SIZE ACANTHOSTEGA Chordata Amphibia Ichthyostegalia 58‐62 cm Marine (Neritic) Y ‐ ‐ small 24in amphibian 1 ACICULOPODA Arthropoda Malacostraca Decopoda 6‐8 cm Marine (Neritic) Y ‐ ‐ tiny Giant Prawn 2 ADELOPHTHALMUS Arthropoda Arachnida Eurypterida 4‐32 cm Marine (Neritic) Y ‐ ‐ small “Swimmer” Scorpion 3 AKMONISTION Chordata Chondrichthyes Symmoriida 47‐50 cm Marine (Neritic) Y ‐ ‐ small ratfish 4 ALKENOPTERUS Arthropoda Arachnida Eurypterida 2‐4 cm Marine (Transitional) Y ‐ ‐ small Sea scorpion 5 ANGUSTIDONTUS Arthropoda Malacostraca Angustidontida 6‐9 cm Marine (Pelagic) Y ‐ ‐ small Primitive shrimp 6 ASTEROLEPIS Chordata Placodermi Antiarchi 32‐35 cm Marine (Transitional) Y ‐ Y small Placo bottom feeder 7 ATTERCOPUS Arthropoda Arachnida Uraraneida 1‐2 cm Marine (Transitional) Y ‐ ‐ tiny Proto‐Spider 8 AUSTROPTYCTODUS Chordata Placodermi Ptyctodontida 10‐12 cm Marine (Neritic) Y ‐ ‐ tiny Half‐Plate 9 BOTHRIOLEPIS Chordata Placodermi Antiarchia 28‐32 cm Marine (Neritic) ‐ ‐ Y tiny Jawed Placoderm 10 -
Journal De L'apf N°74 SOMMAIRE
JJoouurrnnaall ddee ll''AAPPFF nn°°7744 JJuuiilllleett 22001188 La Revue Semestrielle de l’Association Paléontologique Française Numéro spécial : les résumés du Congrès 2018 de l'APF à Bruxelles. L'Association Paléontologique Française Le bureau Eric Buffetaut Nathalie Bardet Laurent Londeix (CNRS) (CNRS) (Univ. Bordeaux) Président Secrétaire Trésorier Damien Germain Claude Monnet Thierry Tortosa (MNHN) (Univ. Lille) (Conseil départemental Conseiller Conseiller des Bouches du Rhône) Conseiller Secrétariat : Cotisation : 1 an : 16 euros, 2 ans : 30 euros, 5 ans : 70 euros Nathalie Bardet Muséum National d'Histoire Naturelle Chèque au Nom de : Département Histoire de la Terre Association Paléontologique Française Centre de Recherche sur la Paléobiodiversité et A adresser à : les Paléoenvironnements (CR2P) UMR 7207 du CNRS Laurent Londeix 8, rue Buffon CP 38 UMR CNRS 5805 EPOC OASU 75005 Paris Université de Bordeaux, Site de Talence Bâtiment B18 Tel. : (+33) 1 40 79 34 55 Allée Geoffroy SaintHilaire FAX : (+33) 1 40 79 35 80 CS 50023, 33615 PESSAC CEDEX email : [email protected] Tel. : (+33) 5 40 00 88 66 FAX : (+33) 5 40 00 33 16 laurent.londeix@ubordeaux.fr 2 Journal de l'APF n°74 SOMMAIRE Editorial .......................................................................... 4 Compterendu du congrès de l'Association Paléontologique Française 2018 ........ 5 Excursion post congrès .................................................. 7 Prix de l'APF 2018 .......................................................... 9 Résumés du congrès ...................................................... -
Belgisch Instituut Voor Natuurwetenschappen
Institut royal des Sciences Koninklijk Belgisch Instituut naturelles de Belgique voor Natuurwetenschappen BULLETIN MEDEDELINGEN Tome XLI, n° 16 Deel XLI, nr 16 Bruxelles, juin 1965. Brussel, juni 1965. ÜBER DIE PLACODERMEN-GATTUNGEN ASTEROLEPIS UND TIARASPIS AUS DEM DEVON BELGIENS UND EINEN FRAGLICHEN TIARASPIS-REST AUS DEM DEVON SPITZBERGENS, von Walter Gross (Tübingen). (Mit 4 Abbildungen und Tafel 1-2.) Die obermitteldevonischen Fische von Bergisch-Gladbach, die T. Orvig (1960, 1960-1961, 1962) entdeckt und beschrieben hat, bilden die formen- reichste und wichtigste Fischfauna des rheinischen Mitteldevons. Sie erinnert sehr an die tiefoberdevonische Wirbeltier-Fauna von Koken- husen in Lettland, die W. Gross in einer Anzahl von Arbeiten darge- stellt hat. In beiden Faunen kommt die Gattung Rhinodipterus zahlreich vor. Rhinodipterus ist nun kiirzlich auch von E. I. White (1963) in einer Kollektion mitteldevonischer Fische aus dem höchsten Mitteldevon von Belgien entdeckt worden. Neben den gut erhaltenen Resten von Rhinodipterus enthàlt die Kollektion aus Belgien auch Antiarchi- und Crossopterygier-Reste, die bereits E. Asselberghs (1936) unter den Namen Bothriolepis und Osteolepis erwâhnt. Antiarchi-Reste erlangen oft eine grössere biostratigraphische Bedeutung, die sich in der Aufein- anderfolge ihrer Gattungen im Mittel- und Oberdevon Schottlands und anderer Gebiete deutlich widerspiegelt. Reste dieser belgischen Antiarchi, die aus dem Museum in Brüssel entliehen waren, zeigte mir Dr. T. Orvig im Herbst 1963 in Stockholm. Eine Prâparation der Reste liess vermuten, dass es sich um eine Art der Gattung Asterolepis handelt, die bekanntlich fiir das höhere Obermitteldevon charakteristisch ist. Nach einer Anfrage bei Dir. Dr. E. Casier, Brüssel, bot mit Dr. T. Orvig dieses Material 2 w. -
A New Antiarch Fish from the Upper Devonian Zhongning Formation of Ningxia, China
Available online at www.sciencedirect.com Palaeoworld 19 (2010) 136–145 Research paper A new antiarch fish from the Upper Devonian Zhongning Formation of Ningxia, China Lian-Tao Jia ∗, Min Zhu, Wen-Jin Zhao Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Xi Zhi Men Wai Street, 142, PO Box 643, Beijing 100044, China Received 2 April 2009; received in revised form 8 December 2009; accepted 9 February 2010 Available online 17 February 2010 Abstract A new antiarch, Ningxialepis spinosa n. gen. n. sp., is described from the Zhongning Formation (Famennian, Late Devonian) of Shixiagou, Qingtongxia, Ningxia, northwestern China. It is characterized by the presence of X-shaped pit-lines, long obstantic margins, high dorsal median spine of the trunk armour formed from the anterior and posterior median dorsal plates, prominent dorsolateral and ventrolateral ridges of the trunk armour, and the anterior median dorsal plate partly overlapping the anterior dorsolateral plate. Ningxialepis is placed as the sister taxon to Jiangxilepis in the Family Jiangxilepidae from South China, based on a phylogenetic analysis of the Euantiarcha. The Jiangxilepidae is redefined. The close affinity between Ningxialepis and Jiangxilepis further corroborates the geographic proximity between the North China and South China blocks in the Late Devonian. © 2010 Elsevier Ltd and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved. Keywords: Antiarcha; Placodermi; Late Devonian; Phylogeny; Paleogeography 1. Introduction then, abundant fish fossils (mainly antiarchs and petalichthyids) were recovered from four main Devonian Sections in Ningixa, Pan et al. (1980) first reported Devonian vertebrates in i.e., the Shixiagou and Dadaigou sections of Qingtongxia, the Ningxia, and described two antiarchs (Bothriolepis niushousha- Shanghongya Section of Zhongning, and the Hongshiwan Sec- nensis and Remigolepis zhongningensis) from the Shixiagou tion of Zhongwei (Fig. -
Fossils Provide Better Estimates of Ancestral Body Size Than Do Extant
Acta Zoologica (Stockholm) 90 (Suppl. 1): 357–384 (January 2009) doi: 10.1111/j.1463-6395.2008.00364.x FossilsBlackwell Publishing Ltd provide better estimates of ancestral body size than do extant taxa in fishes James S. Albert,1 Derek M. Johnson1 and Jason H. Knouft2 Abstract 1Department of Biology, University of Albert, J.S., Johnson, D.M. and Knouft, J.H. 2009. Fossils provide better Louisiana at Lafayette, Lafayette, LA estimates of ancestral body size than do extant taxa in fishes. — Acta Zoologica 2 70504-2451, USA; Department of (Stockholm) 90 (Suppl. 1): 357–384 Biology, Saint Louis University, St. Louis, MO, USA The use of fossils in studies of character evolution is an active area of research. Characters from fossils have been viewed as less informative or more subjective Keywords: than comparable information from extant taxa. However, fossils are often the continuous trait evolution, character state only known representatives of many higher taxa, including some of the earliest optimization, morphological diversification, forms, and have been important in determining character polarity and filling vertebrate taphonomy morphological gaps. Here we evaluate the influence of fossils on the interpretation of character evolution by comparing estimates of ancestral body Accepted for publication: 22 July 2008 size in fishes (non-tetrapod craniates) from two large and previously unpublished datasets; a palaeontological dataset representing all principal clades from throughout the Phanerozoic, and a macroecological dataset for all 515 families of living (Recent) fishes. Ancestral size was estimated from phylogenetically based (i.e. parsimony) optimization methods. Ancestral size estimates obtained from analysis of extant fish families are five to eight times larger than estimates using fossil members of the same higher taxa.