Introduction and Bibliography
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Polskaakademianauk Instytutpaleobiologii
POLSKA AKADEMIA NAUK INSTYTUT PALEOBIOLOGII im. Romana Kozłowskiego SILURIAN AND DEVONIAN HETEROSTRACI FROM POLAND AND HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS Sylurskie i dewońskie Heterostraci z Polski oraz efektywność hydrodynamiczna psammosteidów Marek Dec Dissertation for degree of doctor of Earth and related environmental sciences, presented at the Institute of Paleobiology of Polish Academy of Sciences Rozprawa doktorska wykonana w Instytucie Paleobiologii Polskiej Akademii Nauk pod kierunkiem prof. dr hab. Magdaleny Borsuk-Białynickiej w celu uzyskania stopnia doktora w dyscyplinie Nauki o Ziemi oraz środowisku Warszawa 2020 CONTENTS ACKNOWLEDGMENTS…………………………………………………………….….... 3 STRESZCZENIE………………………………………………………………….....….. 4 SUMMARY……………………………………………………………………….…….. 8 CHAPTER I…………………………………………………………………………….. 13 TRAQUAIRASPIDIDAE AND CYATHASPIDIDAE (HETEROSTRACI) FROM LOWER DEVONIAN OF POLAND CHAPTER II……………………………………………………………………….…… 24 A NEW TOLYPELEPIDID (AGNATHA, HETEROSTRACI) FROM THE LATE SILURIAN OF POLAND CHAPTER III…………………………………………………………………………... 41 REVISION OF THE EARLY DEVONIAN PSAMMOSTEIDS FROM THE “PLACODERM SANDSTONE” - IMPLICATIONS FOR THEIR BODY SHAPE RECONSTRUCTION CHAPTER IV……………………………………………………………………….….. 82 NEW MIDDLE DEVONIAN (GIVETIAN) PSAMMOSTEID FROM HOLY CROSS MOUNTAINS (POLAND) CHAPTER V……………………………………………………………………………109 HYDRODYNAMIC PERFORMANCE OF PSAMMOSTEIDS: NEW INSIGHTS FROM COMPUTATIONAL FLUID DYNAMICS SIMULATIONS 2 ACKNOWLEDGMENTS First and foremost I would like to say thank you to my supervisor Magdalena -
Annotated Checklist of Fossil Fishes from the Smoky Hill Chalk of the Niobrara Chalk (Upper Cretaceous) in Kansas
Lucas, S. G. and Sullivan, R.M., eds., 2006, Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin 35. 193 ANNOTATED CHECKLIST OF FOSSIL FISHES FROM THE SMOKY HILL CHALK OF THE NIOBRARA CHALK (UPPER CRETACEOUS) IN KANSAS KENSHU SHIMADA1 AND CHRISTOPHER FIELITZ2 1Environmental Science Program and Department of Biological Sciences, DePaul University,2325 North Clifton Avenue, Chicago, Illinois 60614; and Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601;2Department of Biology, Emory & Henry College, P.O. Box 947, Emory, Virginia 24327 Abstract—The Smoky Hill Chalk Member of the Niobrara Chalk is an Upper Cretaceous marine deposit found in Kansas and adjacent states in North America. The rock, which was formed under the Western Interior Sea, has a long history of yielding spectacular fossil marine vertebrates, including fishes. Here, we present an annotated taxo- nomic list of fossil fishes (= non-tetrapod vertebrates) described from the Smoky Hill Chalk based on published records. Our study shows that there are a total of 643 referable paleoichthyological specimens from the Smoky Hill Chalk documented in literature of which 133 belong to chondrichthyans and 510 to osteichthyans. These 643 specimens support the occurrence of a minimum of 70 species, comprising at least 16 chondrichthyans and 54 osteichthyans. Of these 70 species, 44 are represented by type specimens from the Smoky Hill Chalk. However, it must be noted that the fossil record of Niobrara fishes shows evidence of preservation, collecting, and research biases, and that the paleofauna is a time-averaged assemblage over five million years of chalk deposition. -
From the Crato Formation (Lower Cretaceous)
ORYCTOS.Vol. 3 : 3 - 8. Décembre2000 FIRSTRECORD OT CALAMOPLEU RUS (ACTINOPTERYGII:HALECOMORPHI: AMIIDAE) FROMTHE CRATO FORMATION (LOWER CRETACEOUS) OF NORTH-EAST BRAZTL David M. MARTILL' and Paulo M. BRITO'z 'School of Earth, Environmentaland PhysicalSciences, University of Portsmouth,Portsmouth, POl 3QL UK. 2Departmentode Biologia Animal e Vegetal,Universidade do Estadode Rio de Janeiro, rua SâoFrancisco Xavier 524. Rio de Janeiro.Brazll. Abstract : A partial skeleton representsthe first occurrenceof the amiid (Actinopterygii: Halecomorphi: Amiidae) Calamopleurus from the Nova Olinda Member of the Crato Formation (Aptian) of north east Brazil. The new spe- cimen is further evidencethat the Crato Formation ichthyofauna is similar to that of the slightly younger Romualdo Member of the Santana Formation of the same sedimentary basin. The extended temporal range, ?Aptian to ?Cenomanian,for this genus rules out its usefulnessas a biostratigraphic indicator for the Araripe Basin. Key words: Amiidae, Calamopleurus,Early Cretaceous,Brazil Première mention de Calamopleurus (Actinopterygii: Halecomorphi: Amiidae) dans la Formation Crato (Crétacé inférieur), nord est du Brésil Résumé : la première mention dans le Membre Nova Olinda de la Formation Crato (Aptien ; nord-est du Brésil) de I'amiidé (Actinopterygii: Halecomorphi: Amiidae) Calamopleurus est basée sur la découverted'un squelettepar- tiel. Le nouveau spécimen est un élément supplémentaireindiquant que I'ichtyofaune de la Formation Crato est similaire à celle du Membre Romualdo de la Formation Santana, située dans le même bassin sédimentaire. L'extension temporelle de ce genre (?Aptien à ?Cénomanien)ne permet pas de le considérer comme un indicateur biostratigraphiquepour le bassin de l'Araripe. Mots clés : Amiidae, Calamopleurus, Crétacé inférieu4 Brésil INTRODUCTION Araripina and at Mina Pedra Branca, near Nova Olinda where cf. -
35-51 New Data on Pleuropholis Decastroi (Teleostei, Pleuropholidae)
Geo-Eco-Trop., 2019, 43, 1 : 35-51 New data on Pleuropholis decastroi (Teleostei, Pleuropholidae), a “pholidophoriform” fish from the Lower Cretaceous of the Eurafrican Mesogea Nouvelles données sur Pleuropholis decastroi (Teleostei, Pleuropholidae), un poisson “pholidophoriforme” du Crétacé inférieur de la Mésogée eurafricaine Louis TAVERNE 1 & Luigi CAPASSO 2 Résumé: Le crâne et le corps de Pleuropholis decastroi, un poisson fossile de l’Albien (Crétacé inférieur) du sud de l’Italie, sont redécrits en détails. P. decastroi diffère des autres espèces du genre par ses deux nasaux en contact médian et qui séparent complètement le dermethmoïde ( = rostral) des frontaux. Avec son maxillaire extrêmement élargi qui couvre la mâchoire inférieure et son supramaxillaire fortement réduit, P. decastroi semble plus nettement apparenté avec Pleuropholis cisnerosorum, du Jurassique supérieur du Mexique, qu’avec les autres espèces du genre. Par ses mâchoires raccourcies et ses nombreux os orbitaires, Pleuropholis apparaît également comme le genre le plus spécialisé de la famille. La position systématique des Pleuropholidae au sein du groupe des « pholidophoriformes » est discutée. Mots-clés: Pleuropholis decastroi, Albien, Italie du sud, Pleuropholis, Pleuropholidae, “Pholidophoriformes”, ostéologie, position systématique. Abstract: The skull and the body of Pleuropholis decastroi, a fossil fish from the marine Albian (Lower Cretaceous) of southern Italy, are re-described in details. P. decastroi differs from the other species of the genus by their two nasals that are in contact along the mid-line, completely separating the dermethmoid (= rostral) from the frontals. With its extremely broadened maxilla that covers the lower jaw and its strongly reduced supramaxilla, P. decastroi seems more closely related to Pleuropholis cisnerosorum, from the Upper Jurassic of Mexico, than to the other species of the genus. -
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THREE-DIMENSIONAL MUSCLE PRESERVATION IN JURASSIC FISHES OF CHILE Museum 01 Natural History, and Department 01 Systematics and Ecology, HANS-PETER SCHULTZE The University 01 Kansas, Lawrence, Kansas 66045-2454, U.S.A. ABSTRACT Late Jurassic fishes of Northern Chile are preserved in calcareous concretions within black shales of Oxfordian age. Co-occurring invertebrates (decapod crustaceans, ostrean bivalves, and algae) indicate benthic life. Soft tissues of the fishes were impregnated by calcium phosphate during life, whereas the decay of the remaining soft tissue induced the formation of the calcareous concretions around the fishes. Occurrence of vitamin 03 or a hydroxylated form of Ihis vitamin is postulated to have occurred in Ihe Jurassic phytoplankton; vitamin 03 induced a break-down of the regulation of the calcium metabolism in the fishes as is the case in calcinosis 01 cattle. High concentration of phosphate in phytoplankton 01 the upwelling zone on the western margin of the shelf of South America could explain the additional supply of phosphate in the fossil fishes which is missing from surrounding concretions and sediment. Key words: Preservation, 50ft tissue,lmpregnation in lite (calcinosis), Teleostean fishes, Oxtordian, Northern Chile. RESUMEN Los peces del Jurásico Superior del norte de Chile están preservados en lutitas negras. La presencia de invertebra dos (crustáceos decápodos, ostras y algas) junto con los peces es indicio de vida bentónica. Los tejidos blandos de los peces se impregnaron con fosfato de calcio en vida de los individuos, mientras que la descomposición de otros tejidos blandos indujo a la formación de concreciones calcáreas alrededor de los peces. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
The Scales of Mesozoic Actinopterygians
Mesozoic Fishes – Systematics and Paleoecology, G. Arratia & G. Viohl (eds.): pp. 83-93, 6 figs. © 1996 by Verlag Dr. Friedrich Pfeil, München, Germany – ISBN 3-923871–90-2 The scales of Mesozoic actinopterygians Hans-Peter SCHULTZE Abstract Cycloid scales (elasmoid scales with circuli) are a unique character of teleosts above the level of Pholidophorus and Pholidophoroides. Cycloid scales have two layers. A bony layer, usually acellular, is superimposed on a basal plate composed of partially mineralized layers of plywoodlike laminated collagen fibres. The tissue of the basal layer is refered to here as elasmodin. Basal teleosts (sensu PATTERSON 1973) possess rhombic scales with a bony base overlain by ganoin (lepidosteoid ganoid scale). Amioid scales (elasmoid scales with longitudinally to radially arranged ridges or rods on the overlapped field) are found within halecomorphs. This scale type evolved more than once within primitive actinopterygians and other osteichthyan fishes. It may have even developed twice within halecomorphs, in Caturidae and Amiidae, from rhombic scales of lepidosteoid type. Some basal genera of halecomorphs show remains of a dentine layer between ganoin and bone that is characteristic of actinopterygians below the halecostome level. The Semionotidae placed at the base of the Halecostomi, exhibit scale histology transitional between the palaeoniscoid and lepidosteoid scale type. Introduction Actinopterygians, from primitive Coccolepididae to advanced teleosts, are represented in the Solnhofen lithographic limestone. These are fishes with rhombic and round scales. Ganoid scales of the lepidosteoid type are found in the following fishes: semionotid Lepidotes and Heterostrophus, macrosemiids Histionotus, Macrosemius, Notagogus and Propterus, ophiopsid Ophiopsis, caturids Furo and Brachyichthys, aspido- rhynchid Belonostomus, pleuropholid Pleuropholis, and pholidophorid Pholidophorus. -
Ichthyodectiform Fishes from the Late Cretaceous
Mesozoic Fishes 5 – Global Diversity and Evolution, G. Arratia, H.-P. Schultze & M. V. H. Wilson (eds.): pp. 247-266, 12 figs., 2 tabs. © 2013 by Verlag Dr. Friedrich Pfeil, München, Germany – ISBN 978-3-89937-159-8 Ichthyodectiform fi shes from the Late Cretaceous (Campanian) of Arkansas, USA Kelly J. IRWIN and Christopher FIELITZ Abstract Several specimens of the ichthyodectiform fishes Xiphactinus audax and Saurocephalus cf. S. lanciformis are reported from the Upper Cretaceous (Campanian) Brownstown Marl and Ozan formations of southwestern Arkansas, U.S.A. Seven individuals of Xiphactinus, based on incomplete specimens, are represented by various elements: disarticu- lated skull bones, jaw fragments, pectoral fin-rays, or vertebrae. The circular vertebral centra are diagnostic for X. audax rather than X. vetus. The specimen of Saurocephalus consists of a three-dimensional skull, lacking much of the skull roof bones. It is identified as Saurocephalus based on the shape of the predentary bone. This specimen provides the first record of entopterygoid teeth in Saurocephalus. These specimens represent new geographic and geologic distribution records of these taxa from the western Gulf Coastal Plain, which biogeographically links records from the eastern Gulf Coastal Plain with those from the Western Interior Sea. Introduction LEIDY (1854) was the first to report the presence of Cretaceous marine vertebrate fossils from Arkansas, yet in the intervening 150+ years, the body of work on the paleoichthyofauna of Arkansas remains limited (WILSON & BRUNER 2004). BARDACK (1965), GOODY (1976), CASE (1978), and RUSSELL (1988) re- ported geographic and geologic distributions for specific taxa, but few descriptive works on fossil fishes are available (see HUSSAKOF 1947; MEYER 1974; BECKER et al. -
Geological Survey of Ohio
GEOLOGICAL SURVEY OF OHIO. VOL. I.—PART II. PALÆONTOLOGY. SECTION II. DESCRIPTIONS OF FOSSIL FISHES. BY J. S. NEWBERRY. Digital version copyrighted ©2012 by Don Chesnut. THE CLASSIFICATION AND GEOLOGICAL DISTRIBUTION OF OUR FOSSIL FISHES. So little is generally known in regard to American fossil fishes, that I have thought the notes which I now give upon some of them would be more interesting and intelligible if those into whose hands they will fall could have a more comprehensive view of this branch of palæontology than they afford. I shall therefore preface the descriptions which follow with a few words on the geological distribution of our Palæozoic fishes, and on the relations which they sustain to fossil forms found in other countries, and to living fishes. This seems the more necessary, as no summary of what is known of our fossil fishes has ever been given, and the literature of the subject is so scattered through scientific journals and the proceedings of learned societies, as to be practically inaccessible to most of those who will be readers of this report. I. THE ZOOLOGICAL RELATIONS OF OUR FOSSIL FISHES. To the common observer, the class of Fishes seems to be well defined and quite distin ct from all the other groups o f vertebrate animals; but the comparative anatomist finds in certain unusual and aberrant forms peculiarities of structure which link the Fishes to the Invertebrates below and Amphibians above, in such a way as to render it difficult, if not impossible, to draw the lines sharply between these great groups. -
THE CLASSIFICATION and EVOLUTION of the HETEROSTRACI Since 1858, When Huxley Demonstrated That in the Histological Struc
ACTA PALAEONT OLOGICA POLONICA Vol. VII 1 9 6 2 N os. 1-2 L. BEVERLY TARLO THE CLASSIFICATION AND EVOLUTION OF THE HETEROSTRACI Abstract. - An outline classification is given of the Hetero straci, with diagnoses . of th e following orders and suborders: Astraspidiformes, Eriptychiiformes, Cya thaspidiformes (Cyathaspidida, Poraspidida, Ctenaspidida), Psammosteiformes (Tes seraspidida, Psarnmosteida) , Traquairaspidiformes, Pteraspidiformes (Pte ras pidida, Doryaspidida), Cardipeltiformes and Amphiaspidiformes (Amphiaspidida, Hiber naspidida, Eglonaspidida). It is show n that the various orders fall into four m ain evolutionary lineages ~ cyathaspid, psammosteid, pteraspid and amphiaspid, and these are traced from primitive te ssellated forms. A tentative phylogeny is pro posed and alternatives are discussed. INTRODUCTION Since 1858, when Huxley demonstrated that in the histological struc ture of their dermal bone Cephalaspis and Pteraspis were quite different from one another, it has been recognized that there were two distinct groups of ostracoderms for which Lankester (1868-70) proposed the names Osteostraci and Heterostraci respectively. Although these groups are generally considered to be related to on e another, Lankester belie ved that "the Heterostraci are at present associated with the Osteostraci because they are found in the same beds, because they have, like Cepha laspis, a large head shield, and because there is nothing else with which to associate them". In 1889, Cop e united these two groups in the Ostracodermi which, together with the modern cyclostomes, he placed in the Class Agnatha, and although this proposal was at first opposed by Traquair (1899) and Woodward (1891b), subsequent work has shown that it was correct as both the Osteostraci and the Heterostraci were agnathous. -
(Early Cretaceous, Araripe Basin, Northeastern Brazil): Stratigraphic, Palaeoenvironmental and Palaeoecological Implications
Palaeogeography, Palaeoclimatology, Palaeoecology 218 (2005) 145–160 www.elsevier.com/locate/palaeo Controlled excavations in the Romualdo Member of the Santana Formation (Early Cretaceous, Araripe Basin, northeastern Brazil): stratigraphic, palaeoenvironmental and palaeoecological implications Emmanuel Faraa,*, Antoˆnio A´ .F. Saraivab, Dio´genes de Almeida Camposc, Joa˜o K.R. Moreirab, Daniele de Carvalho Siebrab, Alexander W.A. Kellnerd aLaboratoire de Ge´obiologie, Biochronologie, et Pale´ontologie humaine (UMR 6046 du CNRS), Universite´ de Poitiers, 86022 Poitiers cedex, France bDepartamento de Cieˆncias Fı´sicas e Biologicas, Universidade Regional do Cariri - URCA, Crato, Ceara´, Brazil cDepartamento Nacional de Produc¸a˜o Mineral, Rio de Janeiro, RJ, Brazil dDepartamento de Geologia e Paleontologia, Museu Nacional/UFRJ, Rio de Janeiro, RJ, Brazil Received 23 August 2004; received in revised form 10 December 2004; accepted 17 December 2004 Abstract The Romualdo Member of the Santana Formation (Araripe Basin, northeastern Brazil) is famous for the abundance and the exceptional preservation of the fossils found in its early diagenetic carbonate concretions. However, a vast majority of these Early Cretaceous fossils lack precise geographical and stratigraphic data. The absence of such contextual proxies hinders our understanding of the apparent variations in faunal composition and abundance patterns across the Araripe Basin. We conducted controlled excavations in the Romualdo Member in order to provide a detailed account of its main stratigraphic, sedimentological and palaeontological features near Santana do Cariri, Ceara´ State. We provide the first fine-scale stratigraphic sequence ever established for the Romualdo Member and we distinguish at least seven concretion-bearing horizons. Notably, a 60-cm-thick group of layers (bMatraca˜oQ), located in the middle part of the member, is virtually barren of fossiliferous concretions. -
Using Information in Taxonomists' Heads to Resolve Hagfish And
This article was downloaded by: [Max Planck Inst fuer Evolutionsbiologie] On: 03 September 2013, At: 07:01 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Historical Biology: An International Journal of Paleobiology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ghbi20 Using information in taxonomists’ heads to resolve hagfish and lamprey relationships and recapitulate craniate–vertebrate phylogenetic history Maria Abou Chakra a , Brian Keith Hall b & Johnny Ricky Stone a b c d a Department of Biology , McMaster University , Hamilton , Canada b Department of Biology , Dalhousie University , Halifax , Canada c Origins Institute, McMaster University , Hamilton , Canada d SHARCNet, McMaster University , Hamilton , Canada Published online: 02 Sep 2013. To cite this article: Historical Biology (2013): Using information in taxonomists’ heads to resolve hagfish and lamprey relationships and recapitulate craniate–vertebrate phylogenetic history, Historical Biology: An International Journal of Paleobiology To link to this article: http://dx.doi.org/10.1080/08912963.2013.825792 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information.