A New Species of Saurichthys from the Middle Triassic (Anisian)
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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. -
Albertiana 45 39 a CANDIDATE GSSP for the BASE of the ANISIAN from KÇIRA, ALBANIA
Albertiana 45 39 Research Article A CANDIDATE GSSP FOR THE BASE OF THE ANISIAN FROM KÇIRA, ALBANIA Giovanni Muttoni1*, Alda Nicora1, Marco Balini1, Miriam Katz2, Morgan Schaller2, Dennis V. Kent3, Matteo Maron1, Selam Meço4, Roberto Rettori5, Viktor Doda6, and Shaquir Nazaj4 1Dipartimento di Scienze della Terra ‘Ardito Desio’, via Mangiagalli 34, 20133 Milan, Italy. 2Department of Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Troy, New York, 12180, USA. 3Earth and Planetary Sciences, Rutgers University, Piscataway, New Jersey, USA and Paleomagnetics Lab, Lamont-Doherty Earth Observatory, Palisades New York 10964, USA. 4Faculty of Geology and Mining, Tiranë, Albania. 5Dipartimento di Scienze della Terra, Piazza Università, 06100 Perugia, Italy. 6Albanian Geological Survey, Myslym Keta, Tiranë, Albania. *Corresponding author, Email: [email protected] Abstract– We present a summary of previously published Olenekian–Anisian boundary magnetostratigraphic and biostratigraphic results from the Kçira area of northern Albania. We focus on the stratigraphically complete Kçira-A section that represents a potential candidate Global Boundary Stratotype Section and Point (GSSP) for the base of the Anisian Stage of the Triassic System. The previously published conodont biostratigraphy from Kçira-A and ancillary sections located nearby has been updated using modern taxonomic criteria and correlated to the available ammonoid and benthic foraminifera biostratigraphy. Previously published magnetobiostratigraphic data reveal the occurrence at Kçira-A, and ancillary sections, of a well-defined magnetic polarity reversal pattern of primary origin that allows global correlations ensuring the exportability of biostratigraphic datums (e.g., the first occurrence of conodontChiosella timorensis) falling close to the Kclr/Kc2n polarity transition. A suite of pilot samples has also been studied for bulk carbon and oxygen isotopes stratigraphy, yielding reasonable values that suggest good preservation of primary material. -
Early Triassic (Induan) Radiolaria and Carbon-Isotope Ratios of a Deep-Sea Sequence from Waiheke Island, North Island, New Zealand Rie S
Available online at www.sciencedirect.com Palaeoworld 20 (2011) 166–178 Early Triassic (Induan) Radiolaria and carbon-isotope ratios of a deep-sea sequence from Waiheke Island, North Island, New Zealand Rie S. Hori a,∗, Satoshi Yamakita b, Minoru Ikehara c, Kazuto Kodama c, Yoshiaki Aita d, Toyosaburo Sakai d, Atsushi Takemura e, Yoshihito Kamata f, Noritoshi Suzuki g, Satoshi Takahashi g , K. Bernhard Spörli h, Jack A. Grant-Mackie h a Department of Earth Sciences, Graduate School of Science and Engineering, Ehime University 790-8577, Japan b Department of Earth Sciences, Faculty of Culture, Miyazaki University, Miyazaki 889-2192, Japan c Center for Advanced Marine Core Research, Kochi University 783-8502, Japan d Department of Geology, Faculty of Agriculture, Utsunomiya University, Utsunomiya 321-8505, Japan e Geosciences Institute, Hyogo University of Teacher Education, Hyogo 673-1494, Japan f Research Institute for Time Studies, Yamaguchi University, Yamaguchi 753-0841, Japan g Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan h Geology, School of Environment, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand Received 23 June 2010; received in revised form 25 November 2010; accepted 10 February 2011 Available online 23 February 2011 Abstract This study examines a Triassic deep-sea sequence consisting of rhythmically bedded radiolarian cherts and shales and its implications for early Induan radiolarian fossils. The sequence, obtained from the Waipapa terrane, Waiheke Island, New Zealand, is composed of six lithologic Units (A–F) and, based on conodont biostratigraphy, spans at least the interval from the lowest Induan to the Anisian. -
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, -
The Early Triassic Jurong Fish Fauna, South China Age, Anatomy, Taphonomy, and Global Correlation
Global and Planetary Change 180 (2019) 33–50 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Research article The Early Triassic Jurong fish fauna, South China: Age, anatomy, T taphonomy, and global correlation ⁎ Xincheng Qiua, Yaling Xua, Zhong-Qiang Chena, , Michael J. Bentonb, Wen Wenc, Yuangeng Huanga, Siqi Wua a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China b School of Earth Sciences, University of Bristol, BS8 1QU, UK c Chengdu Center of China Geological Survey, Chengdu 610081, China ARTICLE INFO ABSTRACT Keywords: As the higher trophic guilds in marine food chains, top predators such as larger fishes and reptiles are important Lower Triassic indicators that a marine ecosystem has recovered following a crisis. Early Triassic marine fishes and reptiles Fish nodule therefore are key proxies in reconstructing the ecosystem recovery process after the end-Permian mass extinc- Redox condition tion. In South China, the Early Triassic Jurong fish fauna is the earliest marine vertebrate assemblage inthe Ecosystem recovery period. It is constrained as mid-late Smithian in age based on both conodont biostratigraphy and carbon Taphonomy isotopic correlations. The Jurong fishes are all preserved in calcareous nodules embedded in black shaleofthe Lower Triassic Lower Qinglong Formation, and the fauna comprises at least three genera of Paraseminotidae and Perleididae. The phosphatic fish bodies often show exceptionally preserved interior structures, including net- work structures of possible organ walls and cartilages. Microanalysis reveals the well-preserved micro-structures (i.e. collagen layers) of teleost scales and fish fins. -
Late Permian to Middle Triassic Palaeogeographic Differentiation of Key Ammonoid Groups: Evidence from the Former USSR Yuri D
Late Permian to Middle Triassic palaeogeographic differentiation of key ammonoid groups: evidence from the former USSR Yuri D. Zakharov1, Alexander M. Popov1 & Alexander S. Biakov2 1 Far-Eastern Geological Institute, Russian Academy of Sciences (Far Eastern Branch), Stoletija Prospect 159, Vladivostok, RU-690022, Russia 2 North-East Interdisciplinary Scientific Research Institute, Russian Academy of Sciences (Far Eastern Branch), Portovaja 16, Magadan, RU-685000, Russia Keywords Abstract Ammonoids; palaeobiogeography; palaeoclimatology; Permian; Triassic. Palaeontological characteristics of the Upper Permian and upper Olenekian to lowermost Anisian sequences in the Tethys and the Boreal realm are reviewed Correspondence in the context of global correlation. Data from key Wuchiapingian and Chang- Yuri D. Zakharov, Far-Eastern Geological hsingian sections in Transcaucasia, Lower and Middle Triassic sections in the Institute, Russian Academy of Sciences (Far Verkhoyansk area, Arctic Siberia, the southern Far East (South Primorye and Eastern Branch), Vladivostok, RU-690022, Kitakami) and Mangyshlak (Kazakhstan) are examined. Dominant groups of Russia. E-mail: [email protected] ammonoids are shown for these different regions. Through correlation, it is doi:10.1111/j.1751-8369.2008.00079.x suggested that significant thermal maxima (recognized using geochemical, palaeozoogeographical and palaeoecological data) existed during the late Kun- gurian, early Wuchiapingian, latest Changhsingian, middle Olenekian and earliest Anisian periods. Successive expansions and reductions of the warm– temperate climatic zones into middle and high latitudes during the Late Permian and the Early and Middle Triassic are a result of strong climatic fluctuations. Prime Middle–Upper Permian, Lower and Middle Triassic Bajarunas (1936) (Mangyshlak and Kazakhstan), Popov sections in the former USSR and adjacent territories are (1939, 1958) (Russian northern Far East and Verkhoy- currently located in Transcaucasia (Ševyrev 1968; Kotljar ansk area) and Kiparisova (in Voinova et al. -
Review Articlemiddle Triassic (Anisian-Ladinian) Tejra Red Beds
Marine and Petroleum Geology 79 (2017) 222e256 Contents lists available at ScienceDirect Marine and Petroleum Geology journal homepage: www.elsevier.com/locate/marpetgeo Review article Middle Triassic (Anisian-Ladinian) Tejra red beds and Late Triassic (Carnian) carbonate sedimentary records of southern Tunisia, Saharan Platform: Biostratigraphy, sedimentology and implication on regional stratigraphic correlations * Mohamed Soussi a, , Grzegorz Niedzwiedzki b, Mateusz Tałanda c, Dawid Drozd_ z_ c, d, Tomasz Sulej d, Kamel Boukhalfa a, e, Janusz Mermer c,Błazej_ Błazejowski_ d a University of Tunis El Manar, Faculty of Sciences, Department of Geology, 2092 Tunis, Tunisia b Uppsala University, Department of Organismal Biology, Evolutionary Biology Center, Norbyvagen€ 18A, 752 36 Uppsala, Sweden c _ University of Warsaw, Faculty of Biology, Department of Paleobiology and Evolution, Biological and Chemical Research Centre, Zwirki i Wigury 101, 02-089 Warszawa, Poland d Polish Academy of Sciences, Institute of Paleobiology, Twarda 51/55, 00-818 Warsaw, Poland e University of Gabes, Faculty of Sciences of Gabes, City Riadh, Zerig 6029, Gabes, Tunisia article info abstract Article history: The “red beds” of the Triassic succession outcropping at Tejra-Medenine (southern Tunisia, Saharan Received 10 July 2016 Platform) have yielded rich fossil assemblages of both freshwater and brackish-marine invertebrates and Received in revised form vertebrates. The new discovered fauna indicates an Anisian-Lower Ladinian age for the Tejra section. Its 11 October 2016 lowermost part is considered as equivalent of Ouled Chebbi Formation, while the medium and upper Accepted 20 October 2016 parts are considered as equivalent of the Kirchaou Formation. Both sedimentological characteristics and Available online 22 October 2016 fossil assemblages indicate the increasing marine influences within the middle part of the section and the migration of brackish and freshwater fauna into the lacustrine/playa environment at the top. -
GEOLOGIC TIME SCALE V
GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE -
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). -
ISPH-PROGRAM-And-ABSTRACT-BOOK.Pdf
- ISPH 2015 logo (front cover) designed by Jasmina Wiemann. The logo highlights several aspects well suited for the Bonn, 2015 meeting. The dwarf sauropod dinosaur, Europasaurus, stands in front of a histology-filled silhouette of the main dome of Poppelsdorf Palace, the main venue for ISPH 2015. This Late Jurassic sauropod is a fitting representative, as it was discovered in Lower Saxony, Germany, and its dwarf status was verified with histological investigations. - Cover, program and abstract book designed by Aurore Canoville and Jessica Mitchell. - Program and abstract book editors: Aurore Canoville, Jessica Mitchell, Koen Stein, Dorota Konietzko-Meier, Elzbieta Teschner, Anneke van Heteren, and P. Martin Sander. ISPH 2015 – Bonn, Germany ISPH 2015 – Bonn, Germany Table of Contents TABLE OF CONTENTS Symposium Organizers and Acknowledgements ...................................................... 4 Welcome Address ........................................................................................................ 5 Program ........................................................................................................................ 6 Main Events ........................................................................................................ 6 Venues ................................................................................................................ 8 Scientific Sessions / Oral Presentations ........................................................... 11 Scientific Sessions / List of Posters ................................................................. -
New Evidence of Saurichthys from the Lower Triassic with an Evaluation of Early Saurichthyid Diversity
Mesozoic Fishes 4 – Homology and Phylogeny, G. Arratia, H.-P. Schultze & M. V. H. Wilson (eds.): pp. 103-127, 18 figs., 2 apps. © 2008 by Verlag Dr. Friedrich Pfeil, München, Germany – ISBN 978-3-89937-080-5 New evidence of Saurichthys from the Lower Triassic with an evaluation of early saurichthyid diversity Raoul J. MUTTER, Joan CARTANYÀ & Susan A. U. BASARABA Abstract A new Early Triassic species from the Vega-Phroso Siltstone Member of the Sulphur Mountain Formation of western Canada, Saurichthys toxolepis sp. nov., is described, and we confirm the presence of a second species, Saurichthys dayi, in the same formation. Another species from the Wordy Creek Formation of East Greenland, Saurichthys cf. S. ornatus, is introduced. Our review of the Early-Middle Triassic record of the genus Saurichthys reveals that species with striking differences in skull anatomy and squamation were already present in the Early Triassic. We briefly review saurichthyid evolution and Early-Middle Triassic paleobiogeography. Saurichthys was predominantly marine, and a significant taphonomic bias is identified in the Triassic record. The new evidence highlights the importance of often poorly dated Early Triassic saurichthyids and shows that evolutionary trends are more complex than previously believed. Introduction Saurichthyids share a slender and elongate body with far posteriorly positioned pelvic, anal, and dorsal fins and an oblong-slender, pointed snout, usually with long jaws. Saurichthyid remains have caused much confusion due to the lack of diagnostic especially features in isolated teeth, leaving basically the elongate, slender jaws as the universally accepted diagnostic feature of saurichthyids. Saurichthyids were long known by teeth only. -
Body-Shape Diversity in Triassic–Early Cretaceous Neopterygian fishes: Sustained Holostean Disparity and Predominantly Gradual Increases in Teleost Phenotypic Variety
Body-shape diversity in Triassic–Early Cretaceous neopterygian fishes: sustained holostean disparity and predominantly gradual increases in teleost phenotypic variety John T. Clarke and Matt Friedman Comprising Holostei and Teleostei, the ~32,000 species of neopterygian fishes are anatomically disparate and represent the dominant group of aquatic vertebrates today. However, the pattern by which teleosts rose to represent almost all of this diversity, while their holostean sister-group dwindled to eight extant species and two broad morphologies, is poorly constrained. A geometric morphometric approach was taken to generate a morphospace from more than 400 fossil taxa, representing almost all articulated neopterygian taxa known from the first 150 million years— roughly 60%—of their history (Triassic‒Early Cretaceous). Patterns of morphospace occupancy and disparity are examined to: (1) assess evidence for a phenotypically “dominant” holostean phase; (2) evaluate whether expansions in teleost phenotypic variety are predominantly abrupt or gradual, including assessment of whether early apomorphy-defined teleosts are as morphologically conservative as typically assumed; and (3) compare diversification in crown and stem teleosts. The systematic affinities of dapediiforms and pycnodontiforms, two extinct neopterygian clades of uncertain phylogenetic placement, significantly impact patterns of morphological diversification. For instance, alternative placements dictate whether or not holosteans possessed statistically higher disparity than teleosts in the Late Triassic and Jurassic. Despite this ambiguity, all scenarios agree that holosteans do not exhibit a decline in disparity during the Early Triassic‒Early Cretaceous interval, but instead maintain their Toarcian‒Callovian variety until the end of the Early Cretaceous without substantial further expansions. After a conservative Induan‒Carnian phase, teleosts colonize (and persistently occupy) novel regions of morphospace in a predominantly gradual manner until the Hauterivian, after which expansions are rare.