Family-Group Names of Fossil Fishes
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Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR013 Features and paleoecological significance of the shark fauna from the Upper Cretaceous Hinoshima Formation, Himenoura Group, Southwest Japan Accepted Naoshi Kitamura 4-8-7 Motoyama, Chuo-ku Kumamoto, Kumamoto 860-0821, Japan (e-mail: [email protected]) Abstract. The shark fauna of the Upper Cretaceous Hinoshima Formation (Santonian: 86.3–83.6 Ma) of the manuscriptHimenoura Group (Kamiamakusa, Kumamoto Prefecture, Kyushu, Japan) was investigated based on fossil shark teeth found at five localities: Himedo Park, Kugushima, Wadanohana, Higashiura, and Kotorigoe. A detailed geological survey and taxonomic analysis was undertaken, and the habitat, depositional environment, and associated mollusks of each locality were considered in the context of previous studies. Twenty-one species, 15 genera, 11 families, and 6 orders of fossil sharks are recognized from the localities. This assemblage is more diverse than has previously been reported for Japan, and Lamniformes and Hexanchiformes were abundant. Three categories of shark fauna are recognized: a coastal region (Himedo Park; probably a breeding site), the coast to the open sea (Kugushima and Wadanohana), and bottom-dwelling or near-seafloor fauna (Kugushima, Wadanohana, Higashiura, and Kotorigoe). -
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 -
A Framework of Ichthyofaunal Ecostratigraphy of the Oligocene–Early Miocene Strata of the Polish Outer Carpathian Basin
Annales Societatis Geologorum Poloniae (2006), vol. 76: 1–111. A FRAMEWORK OF ICHTHYOFAUNAL ECOSTRATIGRAPHY OF THE OLIGOCENE–EARLY MIOCENE STRATA OF THE POLISH OUTER CARPATHIAN BASIN Janusz KOTLARCZYK1, Anna JERZMAÑSKA2, Ewa ŒWIDNICKA2 & Teresa WISZNIOWSKA2 1 Department of General and Mathematical Geology, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Kraków, Poland 2 Department of Palaeozoology, Institute of Zoology, University of Wroc³aw, Sienkiewicza, 21, 50-335 Wroc³aw, Poland Kotlarczyk, J., Jerzmañska, A., Œwidnicka, E. & Wiszniowska, T., 2006. A framework of ichthyofaunal ecostrati- graphy of the Oligocene–Early Miocene strata of the Polish Outer Carpathian basin. Annales Societatis Geologorum Poloniae, 76: 1–111. Abstract: The paper presents the results of an analysis of ichthyofaunal variability throughout the section of the Menilite-Krosno Series (MKS) in the Outer Carpathians of Poland. The studied tanathocoenoses were formed at the bottom of a more than 2,000 m deep northern basin of the Tethys, being largely represented by the continental rise and bottoms of its narrow furrows, and – to a lesser degree – the continental slope and slopes of a submarine high. Lateral variability of statististically representative assemblages of tanathocoenoses hosted in thin, isochro- nous horizons is interpreted as a result of both local changes of ichthyocoenoses and the influence of post-mortem relocation of fishes that mainly dwelled the shelf and upper continental slope. Vertical variability, in turn, is considered as a resulting from changeable conditions of the ecological environment, the input and outflow of taxa whose evolution proceeded in the Indo-Pacific area, and the species extinction. Changeability of ichthyofauna within a ca. -
Evolution of the Cretaceous Lamnoid Sharks of the Genus Eostriatolamia L
Paleontological Journal, Vol. 32, No. 4, 1998, pp. 376–384. Translated from Paleontologicheskii Zhurnal, No. 4, 1998, pp. 54–62. Original Russian Text Copyright © 1998 by Glickman, Averianov. English Translation Copyright © 1998 by åÄàä ç‡Û͇ /Interperiodica Publishing (Russia). Evolution of the Cretaceous Lamnoid Sharks of the Genus Eostriatolamia L. S. Glickman* and A. O. Averianov** * Pr. Elizarova 1, kv. 30, St. Petersburg, 193029 Russia ** Zoological Institute, Russian Academy of Sciences, Universitetskaya nab. 1, St. Petersburg, 199034 Russia Received April 9, 1997 Abstract—The “archaic” tooth form and comparatively few tooth rows are characteristic of the Cretaceous sharks of the genus Eostriatolamia (Odontaspididae). This is in contrast to the conditions in the Cenozoic sand sharks and thus makes it possible to regard this as a valid genus. The evolution and systematics of Eostriatola- mia are reconsidered, in particular, on the basis of statistical methods. The cluster and principal component analyses were used to process a large quantity of teeth from 17 samples from the Albian-Campanian. Six or seven species are included in the genus Eostriatolamia: E. gracilis (Albian of Europe and Kazakhstan), E. stri- atula (Aptian–Albian of Europe), E. subulata (=E. amonensis?) (Cenomanian of Europe, Kazakhstan and ?USA), E. venusta (=E. samhammeri?, =E. sanguinei?) (Santonian–Early Campanian of Europe, ? Late Cam- panian of USA), E. segedini (=E. aktobensis?) (Santonian–Early Campanian of Kazakhstan), ?E. lerichei (the latest Early Campanian–beginning of the Late Campanian of Kazakhstan) and E. holmdelensis (Late Campa- nian of the USA). INTRODUCTION chondrichthyan fishes (Capetta, 1987) the genus Teeth of small sand sharks of the family Odontaspi- Eostriatolamia is questionably synonymized with the didae often dominate in the Cretaceous marine verte- genus Synodontaspis White, 1931 (the senior available brate oryctocomplexes. -
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). -
The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution. -
'Placoderm' (Arthrodira)
Jobbins et al. Swiss J Palaeontol (2021) 140:2 https://doi.org/10.1186/s13358-020-00212-w Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access A large Middle Devonian eubrachythoracid ‘placoderm’ (Arthrodira) jaw from northern Gondwana Melina Jobbins1* , Martin Rücklin2, Thodoris Argyriou3 and Christian Klug1 Abstract For the understanding of the evolution of jawed vertebrates and jaws and teeth, ‘placoderms’ are crucial as they exhibit an impressive morphological disparity associated with the early stages of this process. The Devonian of Morocco is famous for its rich occurrences of arthrodire ‘placoderms’. While Late Devonian strata are rich in arthrodire remains, they are less common in older strata. Here, we describe a large tooth-bearing jaw element of Leptodontich- thys ziregensis gen. et sp. nov., an eubrachythoracid arthrodire from the Middle Devonian of Morocco. This species is based on a large posterior superognathal with a strong dentition. The jawbone displays features considered syna- pomorphies of Late Devonian eubrachythoracid arthrodires, with one posterior and one lateral row of conical teeth oriented postero-lingually. μCT-images reveal internal structures including pulp cavities and dentinous tissues. The posterior orientation of the teeth and the traces of a putative occlusal contact on the lingual side of the bone imply that these teeth were hardly used for feeding. Similar to Compagopiscis and Plourdosteus, functional teeth were pos- sibly present during an earlier developmental stage and have been worn entirely. The morphological features of the jaw element suggest a close relationship with plourdosteids. Its size implies that the animal was rather large. Keywords: Arthrodira, Dentition, Food web, Givetian, Maïder basin, Palaeoecology Introduction important to reconstruct character evolution in early ‘Placoderms’ are considered as a paraphyletic grade vertebrates. -
Leo Semenovich Berg and the Biology of Acipenseriformes: a Dedication
Environmental Biology of Fishes 48: 15–22, 1997. 1997 Kluwer Academic Publishers. Printed in the Netherlands. Leo Semenovich Berg and the biology of Acipenseriformes: a dedication Vadim J. Birstein1 & William E. Bemis2 1 The Sturgeon Society, 331 West 57th Street, Suite 159, New York, NY 10019, U.S.A. 2 Department of Biology and Graduate Program in Organismic and Evolutionary Biology, University of Massachusetts, Amherst, MA 01003, U.S.A. Received 5.3.1996 Accepted 23.5.1996 Key words: T. Dobzhansky, A. Sewertzoff, T. Lysenko, Paleonisciformes, biogeography This volume is dedicated to the memory of Leo Semenovich Berg (1876–1950), a Russian ichthyologist and geographer. In the foreword to the English translation of Berg’s remarkable treatise, ‘Nomogenesis or evolu- tion according to law’, Theodosius Dobzhansky wrote: ‘Berg was one of the outstanding intellects among Russian scientists. The breadth of his interests and the depth as well as the amplitude of his scholarship were remarkable. He had the reputation of being a ‘walking library’, because of the amount of information he could produce from his memory’ (Dobzhansky 1969, p. xi). Berg was prolific, publishing 217 papers and monographs on ichthyology, 30 papers on general zoology and biology, 20 papers on paleontology, 32 papers on zoogeo- graphy, 320 papers and monographs on geography, geology, and ethnography, as well as 290 biographies, obituaries, and popular articles (Berg 1955, Sokolov 1955). Berg was born 120 years ago, on 14 March 1876, in Sciences. Berg was never formally recognized by the town of Bendery. According to laws of the Rus- the Soviet Academy for his accomplishments in sian Empire, Berg could not enter the university as biology, and only later (1946) was he elected a mem- a Jew, so he was baptized and became a Lutheran, ber of the Geography Branch of the Soviet Acade- which allowed him to study and receive his diploma my of Sciences (Figure 1). -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Bibliography of Alexander O
Зоологический институт РАН Лаборатория териологии Bibliography of Alexander O. Averianov A. Monograph 1992. Averianov A.O., Baryschnikov G.F., Garutt W.E., Garutt N.W. & Fomicheva N.L. The Volgian Fauna of Pleistocene Mammals in the Geological-Mineralogical Museum of the Kazan University. Kazan State University, Kazan. 164pp. [In Russian] B. Edited books 2003. [Systematics, Phylogeny and Paleontology of Small Mammals. Proceedings of the International Conference devoted to the 90-th anniversary of Prof. I.M. Gromov] (Edited by A.O. Averianov and N.I. Abramson). Zoologicheskii Institut RAN, St. Petersburg. 246 pp. [papers in Russian and English] 1999. [Materials on the History of Fauna of Eurasia] (Edited by I.S. Darevskii and A.O. Averianov). Trudy Zoologicheskogo Instituta RAN, T. 277. 144 pp. [papers in Russian and English] 1997. Nessov, L.A. [Cretaceous Nonmarine Vertebrates of Northern Eurasia] (Posthumous edition by L.B. Golovneva and A.O. Averianov). 218 pp. Izdatelstvo Sankt-Peterburgskogo Universiteta, Saint Petersburg. [in Russian] C. Refereed Journals 2017. Averianov A.O. and Sues H.-D. 2017. The oldest record of Alvarezsauridae (Dinosauria: Theropoda) in the Northern Hemisphere. PLoS One 12(10): e0186254. 2017. Аверьянов А.О. 2017. Титанозавры: новые данные о возрастной и индивидуальной изменчивости зубов. Природа. № 2. С.83-84. 2017. Averianov A.O. and Archibald J.D. 2017. Therian postcranial bones from the Upper Cretaceous Bissekty Formation of Uzbekistan. Proceedings of the Zoological Institute of the Russian Academy of Sciences 321(4): 433–484. 2017. Lopatin A.V. and Averianov A.O. 2017. The stem placental mammal Prokennalestes from the Early Cretaceous of Mongolia. -
Supporting Information
Supporting Information Clarke et al. 10.1073/pnas.1607237113 Major Axes of Shape Variation and Their Anatomical a comparison: the crown teleost vs. stem teleost comparison on Correlates molecular timescales. Here, the larger SL dataset delivers a All relative warp axes that individually account for >5% of the majority of trees where crown teleosts possess significantly variation across the species sampled are displayed in Table S3. higher rates than stem teleosts, whereas the CS and pruned SL Morphospaces derived from the first three axes, containing all datasets find this result in a large minority (Fig. S3). 398 Mesozoic neopterygian species in our shape dataset, are Overall, these results suggest that choice of size metric is presented in Fig. S1. Images of sampled fossil specimens are also relatively unimportant for our dataset, and that the overall size included in Fig. S1 to illustrate the anatomical correlates of and taxonomic samplings of the dataset are more likely to in- shape axes. The positions of major neopterygian clades in mor- fluence subsequent results, despite those factors having a rela- phospace are indicated by different colors in Fig. S2. Major tively small influence here. Nevertheless, choice of metric may be teleost clades are presented in Fig. S2A and major holostean important for other datasets (e.g., different groups of organisms clades in Fig. S2B. or datasets of other biological/nonbiological structures), because RW1 captures 42.53% of the variance, reflecting changes from it is possible to envisage scenarios where the choice of size metric slender-bodied taxa to deep-bodied taxa (Fig. S1 and Table S3). -
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).