And Ultrastructural Investigations of Labile Tissues in Deep Time
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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). -
New Theropod, Thyreophoran, and Small Sauropod Tracks from the Middle Jurassic Bagå Formation, Bornholm, Denmark
New theropod, thyreophoran, and small sauropod tracks from the Middle Jurassic Bagå Formation, Bornholm, Denmark JESPER MILÀN Milàn, J. 2011. New theropod, thyreophoran, and small sauropod tracks from the Middle Jurassic Bagå Formation, Bornholm, Denmark © 2011 by Bulletin of the Geological Society of Denmark, Vol. 59, pp. 51–59. ISSN 0011–6297. (www.2dgf.dk/publikationer/bulletin) https://doi.org/10.37570/bgsd-2011-59-06 Three new dinosaur tracks are described from the Middle Jurassic Bagå Formation of Bornholm, Denmark. The tracks are all preserved as natural casts on the underside of fluvial sandstone blocks originating from the old Hasle Klinkefabrik’s clay pit, now called Pyritsøen. The new tracks are from a medium-sized theropod, a thyreophoran, and a small sauropod. Together with a thyreophoran track and large sauropod tracks described in 2005, the Middle Jurassic dinosaur fauna of Bornholm now comprises theropods, two sizes of sauropods and at least one type of thyreophoran dinosaur. This is important additional data for the very scarce Middle Jurassic dinosaurian skeletal record of Europe. Received 22 November 2010 Accepted in revised form Key words: Dinosaur fauna, trace fossils, Middle Jurassic, theropod, thyreophoran, sauropod. 21 September 2011 Published online Jesper Milàn [[email protected]], GeomuseumFaxe, Østsjællands Museum, Østervej 2, DK-4640 Faxe, 30 September 2011 Denmark. Also Department of Geography and Geology, University of Copenhagen, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark. Remains of Mesozoic terrestrial vertebrates are scarce Dinosaur remains are more commonly encountered in Denmark and have so far only been found in the in the southern part of Sweden, where numerous di- few Mesozoic outcrops along the west and southwest nosaur tracks and trackways of theropod dinosaurs, a coast of the Baltic island of Bornholm (Fig. -
Estimating the Evolutionary Rates in Mosasauroids and Plesiosaurs: Discussion of Niche Occupation in Late Cretaceous Seas
Estimating the evolutionary rates in mosasauroids and plesiosaurs: discussion of niche occupation in Late Cretaceous seas Daniel Madzia1 and Andrea Cau2 1 Department of Evolutionary Paleobiology, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland 2 Independent, Parma, Italy ABSTRACT Observations of temporal overlap of niche occupation among Late Cretaceous marine amniotes suggest that the rise and diversification of mosasauroid squamates might have been influenced by competition with or disappearance of some plesiosaur taxa. We discuss that hypothesis through comparisons of the rates of morphological evolution of mosasauroids throughout their evolutionary history with those inferred for contemporary plesiosaur clades. We used expanded versions of two species- level phylogenetic datasets of both these groups, updated them with stratigraphic information, and analyzed using the Bayesian inference to estimate the rates of divergence for each clade. The oscillations in evolutionary rates of the mosasauroid and plesiosaur lineages that overlapped in time and space were then used as a baseline for discussion and comparisons of traits that can affect the shape of the niche structures of aquatic amniotes, such as tooth morphologies, body size, swimming abilities, metabolism, and reproduction. Only two groups of plesiosaurs are considered to be possible niche competitors of mosasauroids: the brachauchenine pliosaurids and the polycotylid leptocleidians. However, direct evidence for interactions between mosasauroids and plesiosaurs is scarce and limited only to large mosasauroids as the Submitted 31 July 2019 predators/scavengers and polycotylids as their prey. The first mosasauroids differed Accepted 18 March 2020 from contemporary plesiosaurs in certain aspects of all discussed traits and no evidence Published 13 April 2020 suggests that early representatives of Mosasauroidea diversified after competitions with Corresponding author plesiosaurs. -
Upper Cretaceous Deposits in the Northwest of Saratov Region, Part 2: Problems of Chronostratigraphy and Regional Geological History A
ISSN 0869-5938, Stratigraphy and Geological Correlation, 2008, Vol. 16, No. 3, pp. 267–294. © Pleiades Publishing, Ltd., 2008. Original Russian Text © A.G. Olfer’ev, V.N. Beniamovski, V.S. Vishnevskaya, A.V. Ivanov, L.F. Kopaevich, M.N. Ovechkina, E.M. Pervushov, V.B. Sel’tser, E.M. Tesakova, V.M. Kharitonov, E.A. Shcherbinina, 2008, published in Stratigrafiya. Geologicheskaya Korrelyatsiya, 2008, Vol. 16, No. 3, pp. 47–74. Upper Cretaceous Deposits in the Northwest of Saratov Region, Part 2: Problems of Chronostratigraphy and Regional Geological History A. G. Olfer’eva, V. N. Beniamovskib, V. S. Vishnevskayab, A. V. Ivanovc, L. F. Kopaevichd, M. N. Ovechkinaa, E. M. Pervushovc, V. B. Sel’tserc, E. M. Tesakovad, V. M. Kharitonovc, and E. A. Shcherbininab a Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia b Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia c Saratov State University, Astrakhanskaya ul., 83, Saratov, 410012 Russia d Moscow State University, Vorob’evy Gory, Moscow, 119991 Russia Received November 7, 2006; in final form, March 21, 2007 Abstract—Problems of geochronological correlation are considered for the formations established in the study region with due account for data on the Mezino-Lapshinovka, Lokh and Teplovka sections studied earlier on the northwest of the Saratov region. New paleontological data are used to define more precisely stratigraphic ranges of some stratigraphic subdivisions, to consider correlation between standard and local zones established for different groups of fossils, and to suggest how the Upper Cretaceous regional scale of the East European platform can be improved. -
Reconstruction of Belemnite Evolution Using Formal Concept Analysis
Reconstruction of Belemnite Evolution Using Formal Concept Analysis Radim Belohlavek,1,2∗ Martin Koˇst’´ak3†, and Petr Osicka2 1State University of New York at Binghamton, Binghamton, NY [email protected] 2Palacky University, Olomouc, Czech Republic 3Charles University, Prague, Czech Republic Abstract The paper presents results on using for- mal concept analysis in the problem of identification of taxa and reconstructing evolution from paleontological data. We present results of experiments performed with belemnites—a group of extinct marine cephalophods which seems particularly suit- Figure 1: Schematic sketch of belemnite body with able for such a purpose. We demonstrate position of the internal shell. Apical grey part repre- that the methods of formal concept analysis sents the rostrum. are capable of revealing taxa and relation- ships among them which are relevant from a paleobiological point of view. Coleoid cephalopods played an important role in the Cretaceous ecosystem in both the Northern and Southern hemispheres. Inside this diverse group, es- 1 Introduction and Problem Setting pecially belemnites were a common part of nectonic An important system-theoretic concept is that of a assemblages in marine shallower water ecosystems. taxonomy, i.e. a classification scheme arranged in They belong to coleoids with internal shell. The ex- a hierarchical structure. Biological taxonomies and ternal morphology of belemnites resembles partly Re- the methods of devising them are perhaps the best cent squids and their behavior—larger sets of spec- known and most widely studied. There exist sev- imens concentrated probably during spawning acts. eral approaches to biological classification, with phy- However, the internal shell characteristic is strongly logenetics (cladistics) and phenetics (numerical taxon- different in both, non related cephalopod groups. -
Late Cretaceous) of Morocco : Palaeobiological and Behavioral Implications Remi Allemand
Endocranial microtomographic study of marine reptiles (Plesiosauria and Mosasauroidea) from the Turonian (Late Cretaceous) of Morocco : palaeobiological and behavioral implications Remi Allemand To cite this version: Remi Allemand. Endocranial microtomographic study of marine reptiles (Plesiosauria and Mosasauroidea) from the Turonian (Late Cretaceous) of Morocco : palaeobiological and behavioral implications. Paleontology. Museum national d’histoire naturelle - MNHN PARIS, 2017. English. NNT : 2017MNHN0015. tel-02375321 HAL Id: tel-02375321 https://tel.archives-ouvertes.fr/tel-02375321 Submitted on 22 Nov 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MUSEUM NATIONAL D’HISTOIRE NATURELLE Ecole Doctorale Sciences de la Nature et de l’Homme – ED 227 Année 2017 N° attribué par la bibliothèque |_|_|_|_|_|_|_|_|_|_|_|_| THESE Pour obtenir le grade de DOCTEUR DU MUSEUM NATIONAL D’HISTOIRE NATURELLE Spécialité : Paléontologie Présentée et soutenue publiquement par Rémi ALLEMAND Le 21 novembre 2017 Etude microtomographique de l’endocrâne de reptiles marins (Plesiosauria et Mosasauroidea) du Turonien (Crétacé supérieur) du Maroc : implications paléobiologiques et comportementales Sous la direction de : Mme BARDET Nathalie, Directrice de Recherche CNRS et les co-directions de : Mme VINCENT Peggy, Chargée de Recherche CNRS et Mme HOUSSAYE Alexandra, Chargée de Recherche CNRS Composition du jury : M. -
Caudal Fin Skeleton of the Late Cretaceous Lamniform Shark, Cretoxyrhina Mantelli, from the Niobrara Chalk of 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. 185 CAUDAL FIN SKELETON OF THE LATE CRETACEOUS LAMNIFORM SHARK, CRETOXYRHINA MANTELLI, FROM THE NIOBRARA CHALK OF KANSAS KENSHU SHIMADA1, STEPHEN L. CUMBAA2, AND DEANNE VAN ROOYEN3 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; 2Paleobiology, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada; 3Department of Earth Sciences, Carleton University, 2240 Herzberg Laboratories, 1125 Colonel By Drive, Ottawa, Ontario K1S 5B6, Canada. Abstract—The caudal fin morphology of the Late Cretaceous lamniform shark, Cretoxyrhina mantelli (Agassiz), was previously inferred from scale morphology, which suggested that it was capable of fast swimming. A specimen from the Niobrara Chalk of western Kansas is described here and offers new insights into the morphology of the caudal fin of the taxon. The specimen preserves the posterior half of the vertebral column and a series of hypochordal rays. These skeletal elements exhibit features suggesting that C. mantelli had a lunate tail and a caudal peduncle with a lateral fluke. The specimen also supports the idea that the body form of C. mantelli resembled that of the extant white shark, Carcharodon carcharias (Linneaus). Given a total vertebral count in Cretoxyrhina mantelli of about 230, this specimen suggests that the transition between precaudal and caudal vertebrae was somewhere between the 140th and 160th vertebrae. -
A First Estimation of Storage Potential for Selected Aquifer Cases
A first estimation of storage potential for selected aquifer cases Ane Lothe, Benjamin Emmel, Per Bergmo, Gry Möl Mortensen, Peter Frykman NORDICCS Technical Report D 6.3.1302 (D25) April 2014 Summary This report D 6.3.1302 "A first estimation of storage potential for selected aquifer cases (D25)" was in the beginning named “Estimation of improved capacity and quantification of capacity and sealing properties (D25)”. The aim with this report is to present updated estimates on storage potential for some selected aquifers in the Nordic countries. The storage aquifers are selected on specified criteria as defined in the memo by Bergmo (Bergmo 2014). From Norway modelling and simulation of the Gassum Formation in the Skagerrak area and the Garn Formation at the Trøndelag Platform, offshore Mid‐Norway has been carried out. From Denmark the geological model building of the Vedsted structure in northeast Denmark and the Hanstholm structure, offshore Denmark is reported. From Sweden the Faludden sandstone located in the south‐east Baltic Sea is described, together with the Arnager Greensand located offshore Skåne in Sweden and finally the Höganäs‐Rya sequence, also deposited in the same area, close to Danish border. Preliminary capacity estimates are carried out for all the selected sites, but modelling has only been performed for the two Norwegian sites. Authors Ane Lothe, Sintef, Norway, [email protected] Benjamin U. Emmel, SINTEF, Norway, [email protected] Per Bergmo, SINTEF Petroleum Research, Norway, [email protected] Gry Møl Mortensen, Geological Survey of Sweden, Sweden, [email protected] Peter Frykman, GEUS, Denmark, [email protected] Date April 2014 About NORDICCS Nordic CCS Competence Centre, NORDICCS, is a networking platform for increased CCS deployment in the Nordic countries. -
Dinosaur Tracks in Lower Jurassic Coastal Plain Sediments (Sose Bugt Member, Rønne Formation) on Bornholm, Denmark
Dinosaur tracks in Lower Jurassic coastal plain sediments (Sose Bugt Member, Rønne Formation) on Bornholm, Denmark LARS B. CLEMMENSEN, JESPER MILAN, GUNVER K. PEDERSEN, ANNE B. JOHANNESEN AND CONNIE LARSEN Clemmensen, L.B., Milan, J., Pedersen, G.K., Johannesen, A.B. & Larsen, C. 2014: Dinosaur tracks in Lower Jurassic coastal plain sediments (Sose Bugt Member, Rønne Formation) on Bornholm, Denmark. Lethaia,Vol. 47, pp. 485–493. Fluvial palaeochannels of coastal plain sediments of the Lower Jurassic Sose Bugt Member of the Rønne Formation exposed in the coastal cliffs at Sose Bugt, Bornholm, contain abundant dinosaur or other large vertebrate tracks in the form of deformation structures exposed in vertical section. The tracks are represented by steep-walled, flat- to-concave-bottomed depressions, with a raised ridge at each side. The tracks are filled with laminated sediments, draping the contours of the bottom of the depression. Un- derprints, stacked concave deformations beneath the prints, are present beneath each track. Contemporary Upper Triassic – Lower Jurassic strata from southern Sweden and Poland contain a diverse track fauna, supporting our interpretation. This is the earliest evidence of dinosaur activity in Denmark. □ Bornholm, coastal plain, dinosaur tracks, lake sediments, Lower Jurassic. Lars B. Clemmensen [[email protected]], Jesper Milan [[email protected]], Anne B. Joh- annesen [[email protected]], and Connie Larsen [[email protected]], Depart- ment for Geosciences and Natural Resource Managements, University of Copenhagen, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark; Jesper Milan [[email protected]], Geomuseum Faxe/Østsjællands Museum, Østervej 2, DK-4640 Faxe, Denmark; Gunver K. Pedersen [[email protected]], GEUS Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark; manuscript received on 12/04/2013; manuscript accepted on 04/12/2013. -
Back Matter (PDF)
Index Page numbers in italic denote figures. Page numbers in bold denote tables. Aachenia sp. [gymnosperm] 211, 215, 217 selachians 251–271 Abathomphalus mayaroensis [foraminifera] 311, 314, stratigraphy 243 321, 323, 324 ash fall and false rings 141 actinopterygian fish 2, 3 asteroid impact 245 actinopterygian fish, Sweden 277–288 Atlantic opening 33, 128 palaeoecology 286 Australosomus [fish] 3 preservation 280 autotrophy 89 previous study 277–278 avian fossils 17 stratigraphy 278 study method 281 bacteria 2, 97, 98, 106 systematic palaeontology 281–286 Balsvik locality, fish 278, 279–280 taphonomy and biostratigraphy 286–287 Baltic region taxa and localities 278–280 Jurassic palaeogeography 159 Adventdalen Group 190 Baltic Sea, ice flow 156, 157–158 Aepyornis [bird] 22 barite, mineralization in bones 184, 185 Agardhfjellet Formation 190 bathymetry 315–319, 323 see also depth Ahrensburg Glacial Erratics Assemblage 149–151 beach, dinosaur tracks 194, 202 erratic source 155–158 belemnite, informal zones 232, 243, 253–255 algae 133, 219 Bennettitales 87, 95–97 Amerasian Basin, opening 191 leaf 89 ammonite 150 root 100 diversity 158 sporangia 90 amniote 113 benthic fauna 313 dispersal 160 benthic foraminifera 316, 322 in glacial erratics 149–160 taxa, abundance and depth 306–310 amphibian see under temnospondyl 113–122 bentonite 191 Andersson, Johan G. 20, 25–26, 27 biostratigraphy angel shark 251, 271 A˚ sen site 254–255 angiosperm 4, 6, 209, 217–225 foraminifera 305–312 pollen 218–219, 223 palynology 131 Anomoeodus sp. [fish] 284 biota in silicified -
An Introduction to the Mesozoic Biotas of Scandinavia and Its Arctic Territories
Downloaded from http://sp.lyellcollection.org/ at Uppsala Universitetsbibliotek on August 1, 2016 An introduction to the Mesozoic biotas of Scandinavia and its Arctic territories BENJAMIN P. KEAR1*, JOHAN LINDGREN2, JØRN H. HURUM3,4, JESPER MILA` N5,6 & VIVI VAJDA2,7 1Museum of Evolution, Uppsala University, Norbyva¨gen 16, 752 36 Uppsala, Sweden 2Department of Geology, Lund University, So¨lvegatan 12, 223 62 Lund, Sweden 3Natural History Museum, University of Oslo, Postboks 1172, Blindern, 0318 Oslo, Norway 4The University Centre in Svalbard, UNIS, Postboks 156, 9171 Longyearbyen, Norway 5Geomuseum Faxe/Østsjællands Museum, Østervej 2, DK-3640 Faxe, Denmark 6Natural History Museum of Denmark, Øster Voldgade 5-7, DK-1350 Copenhagen K, Denmark 7Department of Palaeobiology, Swedish Museum of Natural History, Postboks 50007, SE-104 05 Stockholm, Sweden *Corresponding author (e-mail: [email protected]) Abstract: The Mesozoic biotas of Scandinavia have been studied for nearly two centuries. How- ever, the last 15 years have witnessed an explosive advance in research, most notably on the richly fossiliferous Triassic (Olenekian–Carnian) and Jurassic (Tithonian) Lagersta¨tten of the Norwe- gian Arctic Svalbard archipelago, Late Cretaceous (Campanian) Kristianstad Basin and Vomb Trough of Ska˚ne in southern Sweden, and the UNESCO heritage site at Stevns Klint in Denmark – the latter constituting one of the most complete Cretaceous–Palaeogene (Maastrichtian–Danian) boundary sections known globally. Other internationally significant deposits include earliest (Induan) and latest Triassic (Norian–Rhaetian) strata from the Danish autonomous territory of Greenland, and the Early Jurassic (Sinemurian–Pliensbachian) to Early Cretaceous (Berriasian) rocks of southern Sweden and the Danish Baltic island of Bornholm, respectively. -
Element/Ca, C and O Isotope Ratios in Modern Brachiopods: Species-Specific Signals of Biomineralization
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Open Research Exeter This is the author-formatted version of Ullmann et al, 2017, in Chemical Geology, http://doi.org/10.1016/j.chemgeo.2017.03.034. Element/Ca, C and O isotope ratios in modern brachiopods: species-specific signals of biomineralization C.V. ULLMANN1,*, R. FREI2, C. KORTE2, C. LÜTER3 1University of Exeter, Camborne School of Mines & Environment and Sustainability Institute, Penryn Campus, Penryn, TR10 9FE, United Kingdom 2University of Copenhagen, Department of Geoscience and Natural Resource Management, Øster Voldgade 10, 1350 Copenhagen, Denmark 3Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany *Correspondence: [email protected]; Tel: 0044 1326 259165 Abstract: Fossil brachiopods are of major importance for the reconstruction of palaeoenvironmental conditions, particularly of the Palaeozoic. In order to better understand signals of ancient shell materials, modern analogue studies have to be conducted. Here we present C and O isotope data in conjunction with Mg/Ca, Sr/Ca, Mn/Ca and Fe/Ca data for nine modern rhynchonellid and terebratulid brachiopod species from tropical to intermediate latitudes and shallow to very deep marine settings. C and O isotope signals of most species suggest formation of secondary shell layers near or in isotopic equilibrium with ambient seawater. Some species – especially in the suborder Terebratellidina – show partly distinct disequilibrium signals, suggesting some degree of phylogenetic control on the expression of vital effects. Mn/Ca and Fe/Ca ratios measured in the modern species form a baseline to assess fossil preservation, but also yield environmental information Mg/Ca and Sr/Ca ratios follow previously observed patterns, with all studied brachiopod species comprising low-Mg calcite.