Creation Matters Volume 22 Number 3
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Devonian Bryozoans of the Holy Cross Mountains, Poland
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. XVIII 1973 No.4 MARIA KIEPURA DEVONIAN BRYOZOANS OF THE HOLY CROSS MOUNTAINS, POLAND. PART II. CYCLOSTOMATA AND CYSTOPORATA Abstract. - Descriptions are given of 33, species of Middle Devonian Bryozoa from the Holy Cross Mts., belonging to the orders Cyclostomata and Cystoporata. Cyclo stomata are represented by 26 species (4 new: Corynotrypa (Corynotrypa) skalensis, C. (C.) basiplata, Stomatopora varigemmata and Diversipora bitubulata n. gen.). Cystoporata are represented by 7 new species: Ceramoporella orbiculata, C. grandi cystica, Favositella integrimuralis, Fistulipora boardmani, F. emphantica, Cyclotrypa nekhoroshevi and Fistuliramus astrovae. The systematic assignment of the genus Hederella Hall, 1881 has been discussed and the "tabulate-like" microstructure of the zooecial walls of this genus examined. In addition, the epifauna and associated assemblages have been characterized as well as the geological and palaeoecological conditions in which the described Bryozoa occurred. INTRODUCTION Among the Middle Devonian Bryozoa of the Holy Cross Mts., the present author has, up to now, described Ctenostomata (Kiepura, 1965). The present paper is a continuation of her investigations on the Middle Devonian Bryozoa of this region and contains descriptions of 33 species belonging to 9 genera of the orders Cyclostomata and Cystoporata occur ring in the Grzegorzowice - Skaly profile. The bryozoan collection of the Palaeozoological Institute of the Polish Academy of Sciences also contains a rich material representing the orders Trepostomata and Cryptostomata from the Middle Devonian of the Holy Cross Mts., which will be described at a future date. The material described in the present paper was collected by the author during several years of fieldwork (1950-1954). -
001-012 Primeras Páginas
PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9. -
Introduction to the Trilobites: Morphology, Ecology, Macroevolution and More by Michelle M
Introduction to the Trilobites: Morphology, Ecology, Macroevolution and More By Michelle M. Casey1, Perry Kennard2, and Bruce S. Lieberman1, 3 1Biodiversity Institute, University of Kansas, Lawrence, KS, 66045, 2Earth Science Teacher, Southwest Middle School, USD497, and 3Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS 66045 Middle level laboratory exercise for Earth or General Science; supported provided by National Science Foundation (NSF) grants DEB-1256993 and EF-1206757. Learning Goals and Pedagogy This lab is designed for middle level General Science or Earth Science classes. The learning goals for this lab are the following: 1) to familiarize students with the anatomy and terminology relating to trilobites; 2) to give students experience identifying morphologic structures on real fossil specimens 3) to highlight major events or trends in the evolutionary history and ecology of the Trilobita; and 4) to expose students to the study of macroevolution in the fossil record using trilobites as a case study. Introduction to the Trilobites The Trilobites are an extinct subphylum of the Arthropoda (the most diverse phylum on earth with nearly a million species described). Arthropoda also contains all fossil and living crustaceans, spiders, and insects as well as several other extinct groups. The trilobites were an extremely important and diverse type of marine invertebrates that lived during the Paleozoic Era. They only lived in the oceans but occurred in all types of marine environments, and ranged in size from less than a centimeter to almost a meter across. They were once one of the most successful of all animal groups and in certain fossil deposits, especially in the Cambrian, Ordovician, and Devonian periods, they are extremely abundant. -
Biodiversity, Distribution and Patterns of Extinction of the Last Odontopleuroid Trilobites During the Devonian (Givetian, Frasnian)
Geol. Mag. 144 (5), 2007, pp. 777–796. c 2007 Cambridge University Press 777 doi:10.1017/S0016756807003779 First published online 13 August 2007 Printed in the United Kingdom Biodiversity, distribution and patterns of extinction of the last odontopleuroid trilobites during the Devonian (Givetian, Frasnian) ∗ RAIMUND FEIST & KENNETH J. MCNAMARA† ∗Laboratoire de Paleontologie,´ Institut des Sciences de l’Evolution, Universite´ Montpellier II, Cc 062, Place E. Bataillon, 34095 Montpellier, France †Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK (Received 18 September 2006; accepted 22 February 2007) Abstract – Biostratigraphical ranges and palaeogeographical distribution of mid-Givetian to end- Frasnian odontopleurids are investigated. The discovery of Leonaspis rhenohercynica sp. nov. in mid-Givetian strata extends this genus unexpectedly up to the late Middle Devonian. New material of Radiaspis radiata (Goldfuss, 1843) and the first koneprusiine in Britain, Koneprusia? sp., are described from the famous Lummaton shell-bed, Torquay, Devon. New taxa of Koneprusia, K. serrensis, K. aboussalamae, K. brevispina,andK. sp. A and K. sp. B are defined. Ceratocephala (Leonaspis) harborti Richter & Richter, 1926, is revised and reassigned to Gondwanaspis Feist, 2002. Two new species of Gondwanaspis, G. dracula and G. spinosa, plus three others left in open nomenclature, are described from the late Frasnian of Western Australia. A further species of Gondwanaspis, G. prisca, is described from the early Frasnian of Montagne Noire. Species of Gondwanaspis are shown to possess a number of paedomorphic features. A functional analysis suggests that, unlike other odontopleurids, Gondwanaspis actively fed and rested with the same cephalic orientation. The sole odontopleurid survivors of the severe terminal mid-Givetian biocrisis (‘Taghanic Event’) belong to the koneprusiine Koneprusia in the late Givetian and Frasnian, and, of cryptogenic origin, the acidaspidine Gondwanaspis in the Frasnian. -
Introduction to the Trilobites: Morphology, Macroevolution and More by Michelle M
Introduction to the Trilobites: Morphology, Macroevolution and More By Michelle M. Casey1 and Bruce S. Lieberman1,2, 1Biodiversity Institute and 2Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS 66045 Undergraduate laboratory exercise for sophomore/junior level paleontology course Learning Goals and Pedagogy This lab is intended for an upper level paleontology course containing sophomores and juniors who have already taken historical geology or its equivalent; however it may be suitable for introductory biology or geology students familiar with geological time, phylogenies, and trace fossils. This lab will be particularly helpful to those institutions that lack a large teaching collection by providing color photographs of museum specimens. Students may find previous exposure to phylogenetic methods and terminology helpful in completing this laboratory exercise. The learning goals for this lab are the following: 1) to familiarize students with the anatomy and terminology relating to trilobites; 2) to give students experience identifying morphologic structures on real fossil specimens, not just diagrammatic representations; 3) to highlight major events or trends in the evolutionary history and ecology of Trilobita; and 4) to expose students to the study of macroevolution in the fossil record using trilobites as a case study. Introduction to the Trilobites The Trilobites are an extinct subphylum of the Arthropoda (the most diverse phylum on earth with nearly a million species described). Arthropoda also contains all fossil and living crustaceans, spiders, and insects as well as several other solely extinct groups. The trilobites were an extremely important and diverse type of marine invertebrates that lived during the Paleozoic Era. They were exclusively marine but occurred in all types of marine environments, and ranged in size from less than a centimeter to almost a meter. -
Palaeontological Society of Japan
ISSN 0031-0204 Transactions and Proceedings of the Palaeontological Society of Japan New Series No. 148 Palaeontological Society of Japan September 30, 1986 Co-Editors Hisayoshi 100 and Takashi HAMADA Officers for 1985-1986 President: Toshimasa TANAI Honorary President: Teiichi KOBAYASHI Councillors; Kiyotaka GHINZEI, Takashi HAMADA, Tetsuro HANAI, Yoshikazu HASEGAWA, Itaru HAYAMI, Hisayoshi IGO, Junji ITOIGAWA, Tadao KAMEl, Tatsuaki KIMURA, Tamio KOTAKA, Kei MORI, Ikuwo OBATA, Tsunemasa SAITO, Yokichi TAKAYANAGI, Toshimasa TAN AI Members of Standing Committee: Kiyotaka CHINZEI (Membership), Takashi HAMADA (Co Editor of Transactions), Yoshikazu HASEGAWA (Foreign Affairs), Itaru HAY AMI (Planning), Hisayoshi IGO (Co-Editor of Transactions), Tatsuaki KIMURA (Finance), Ikuwo OBATA (General Affairs), Yokichi TAKAYANAGI (Editor of "Fossils"), Juichi YANAGIDA (Editor of Special Papers) Secretary: Hiroshi NODA (Editor of Transactions) Auditor: Yoshiaki MA TSUSHIMA The fossil on the cover is Unuma (Spinunuma) echinatus ICHIKAWA and YAO, a Middle Jurassic multisegmented radiolaria from Unuma, Gifu Prefecture, central Japan (photo by A. YAO, x 260). All communication relating to this journal should be addressed to the PALAEONTOLOGICAL SOCIETY OF JAPAN c/o Business Center for Academic Societies, Yayoi 2-4-16, Bunkyo-ku, Tokyo 113, Japan Trans. Proc. Palaeont. Soc. Japan, N.S., No. 143, pp. 409-421, pis. 81-85, September 30,1986 816. SOME INOCERAMIDS (BIV AL VIA) FROM THE CENOMANIAN (CRETACEOUS) OF JAPAN-I NEW OR LITTLE KNOWN FOUR SPECIES FROM HOKKAIDO AND KYUSHU* TATSURO MATSUMOTO c/o Department of Geology, Kyushu University 33, Fukuoka 812 and MASAYUKINODA Minami·Oita Junior High School, Oita 870 Abstract. In a series of papers in 3 parts some new and little known ino· ceramid species from the Cenomanian of Japan are to be described. -
Paralejurus Colossicus N. Sp. Und Paralejurus Flickorum N. Sp
Jb. nass. Ver. Naturkde. 140 S. 7-45 6 Abb. 6 Taf. Wiesbaden Paralejurus colossicus n. sp. und Paralejurus flickorum n. sp. (Trilobita, Scutelluidae) aus dem basalen Rupbach-Schiefer (Ober-Emsium; Rheinisches Schiefergebirge) Mirco Alberti Taunus, Ober-Emsium, Rupbach-Schiefer, Trilobiten, Paralejurus sp. Kurzfassung: Mit Paralejurus colossicus n. sp. und Paralejurus flickorum n. sp. werden zwei scutelluide Trilobiten aus dem basalen Rupbach-Schiefer des Steinbruchs an der Heckel- mann Mühle beschrieben und mit dem bislang aus jüngeren Rupbach-Schiefern be kann ten Paralejurus cameratus (Maurer 1876) verglichen. Paralejurus sp. S aus dem basalen Rupbach- Schiefer des Schieferlagers der Grube „Schöne Aussicht“ lässt sich erhaltungsbedingt nicht nä- her zuordnen. Paralejurus flickorum n sp. ist der älteste Vertreter seiner Gattung im Rupbach- Schiefer. Die Großwüchsigkeit des etwas jüngeren Paralejurus colossicus n. sp. wird auf be son- ders günstige Lebensbedingungen in seinem Lebensumfeld zurückgeführt. Die beschriebenen Taxa gehören zu den späten Formen ihrer Gattung. Für die spätere Entwick lungs geschichte von Paralejurus wird ein möglicher Trend von einer ursprünglich semi-endobenthischen hin zu einer eher epibenthischen Lebensweise diskutiert. Paralejurus colossicus n. sp. and Paralejurus flickorum n. sp. (Trilobita, Scutelluidae) from the basal Rupbach Shales (Upper Emsium; Rhenish Slate Mountains) Taunus mountains, Upper Emsium, Rupbach Shales, trilobites, Paralejurus sp. A b s t r a c t : The scutelluid trilobites Paralejurus colossicus n. sp. and Paralejurus flickorum n. sp. from the basal Rupbach Shales in the quarry near the Heckelmann mill are described and compared with Paralejurus cameratus (Maurer 1876) so far known from the lower Rupbach Shales. Paralejurus sp. S from the basal Rupbach Shales corresponding to the beds of “Schöne Aussicht” mine cannot be effectively matched with the other taxa due to its poor preservation. -
4. the Phylogeny and Disparity of the Odontopleurida (Trilobita)
University of Bath PHD Trilobita: phylogeny and evolutionary patterns Pollitt, Jessica R. Award date: 2006 Awarding institution: University of Bath Link to publication Alternative formats If you require this document in an alternative format, please contact: [email protected] General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Download date: 10. Oct. 2021 TRILOBITA: PHYLOGENY AND EVOLUTIONARY PATTERNS Jessica R. Pollitt A thesis submitted for the degree of Doctor of Philosophy University of Bath Department of Biology & Biochemistry September 2006 COPYRIGHT Attention is drawn to the fact that copyright of this thesis rests with its author. This copy of the thesis has been supplied on condition that anyone who consults it is understood to recognise that its copyright rests with its author and that no quotation from the thesis and no information derived from it may be published without the prior written consent of the author. -
Introduction to the Trilobites: Morphology, Macroevolution and More by Michelle M
Introduction to the Trilobites: Morphology, Macroevolution and More By Michelle M. Casey1 and Bruce S. Lieberman1,2, 1Biodiversity Institute and 2Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS 66045 Undergraduate laboratory exercise for sophomore/junior level paleontology course Learning Goals and Pedagogy This lab is intended for an upper level paleontology course containing sophomores and juniors who have already taken historical geology or its equivalent; however it may be suitable for introductory biology or geology students familiar with geological time, phylogenies, and trace fossils. This lab will be particularly helpful to those institutions that lack a large teaching collection by providing color photographs of museum specimens. Students may find previous exposure to phylogenetic methods and terminology helpful in completing this laboratory exercise. The learning goals for this lab are the following: 1) to familiarize students with the anatomy and terminology relating to trilobites; 2) to give students experience identifying morphologic structures on real fossil specimens, not just diagrammatic representations; 3) to highlight major events or trends in the evolutionary history and ecology of the Trilobita; and 4) to expose students to the study of macroevolution in the fossil record using trilobites as a case study. Introduction to the Trilobites The Trilobites are an extinct subphylum of the Arthropoda (the most diverse phylum on earth with nearly a million species described). Arthropoda also contains all fossil and living crustaceans, spiders, and insects as well as several other solely extinct groups. The trilobites were an extremely important and diverse type of marine invertebrates that lived during the Paleozoic Era. -
The Collection of Type Fossils of the Natural Science Museum of the University of Zaragoza (Spain)
The collection of type fossils of the Natural Science Museum of the University of Zaragoza (Spain) José Ignacio Canudo Natural Science Museum of the University of Zaragoza, Plaza Basilio Paraíso 4 50005 Zaragoza, Spain Abstract The Natural Science Museum of the University of Zaragoza houses one of the most important collections in Spain of fossils published in scientific journals. It is a new museum, which has brought together the fossil collections of the Palaeontological Museum of the University of Zaragoza with the University’s historical collections. It harbours 33,561 fossils, which have been studied in 524 scientific publications (dissertations, books and journals), and of which 243 are holotypes. All the material is inventoried in a FileMaker database and is available for consultation by any researcher who applies to do so. The type-fossil collection is mainly from the Autonomous Region of Aragón in Spain (comprising the provinces of Zaragoza, Huesca and Teruel), with a small proportion from other Spanish regions (less than 10%) and from other countries (less than 1%). The collection is diverse on what concerns taxonomic groups, with arthropods, brachiopods, echinoderms and vertebrates standing out in terms of the number of specimens and of holotypes. The fossils date from the Upper Proterozoic to the Pleistocene, the Carboniferous-Triassic being the least-represented period. Particularly noteworthy are the collections of invertebrates from the Cambrian and of mammals from the Aragonian (Tertiary). Key Words: Fossils, Zaragoza University Museum, Spain, Collection management Acknowledgements Management of the collection is subsidized by the Government of Aragón by means of financial support from the government office and by the University of Zaragoza by means of the Vice-Rector’s Office for Cultural Projection. -
Defensive Enrolment in Mantis Shrimp Larvae (Malacostraca: Stomatopoda)
Contributions to Zoology, 83 (3) 185-194 (2014) Defensive enrolment in mantis shrimp larvae (Malacostraca: Stomatopoda) Carolin Haug1, 2, Joachim T. Haug1 1 LMU Munich, Department of Biology II and GeoBio-Center, Großhaderner Str. 2, 82152 Planegg-Martinsried, Germany 2 [email protected] Key words: defensive behaviour, functional morphology, marine larvae, museum material Abstract numerous groups developed escape reactions. Well- known examples of groups with such a reaction are We describe a possible new defensive behaviour of larval stages caridoid eucrustaceans, leaf hoppers, and orthopteran of mantis shrimps (Stomatopoda). Mantis shrimp larvae are insects (e.g., Carew, 2000; Burrows, 2007; Burrows rarely observed in nature, thus the study is based on postures of museum material and functional morphological aspects. Speci- and Picker, 2010). Other defensive strategies involve mens described here are tightly enrolled, their pleon is bent for- the development of defensive structures: the body of ward, and the telson is locked into the frontal margin of the arthropods can be armed with strong spines, serrations shield. This margin has two lobes into which the two postero- or heavily sclerotised dorsal sclerites, or the entire lateral spines of the telson fit. The shield shows further adaptions to enrolment; e.g., the ventral gape of the shield perfectly match- body can be enclosed in large shields. In some arthro- es the width of the pleon and leaves no major gaps when the pods, a combination of several of these defensive as- pleon is bent forward. Based on these observations, we briefly pects can be found. For example, many orthopterans discuss the possibilities to infer behavioural aspects from func- arm their jumping legs, which they use for their escape tional morphological aspects. -
Phacops (Phacops) D
ACTA PALAEONTOLOGI CA POLO NICA Vol. II I 9 5 7 No .1 HALSZKA OS MOLSKA TRILOBITES FROM THE COUVINIAN OF WYDRYSZOW (HOLY CROSS MTS. , POLAND) Abstr act. - This paper deals w it h 13 species of Couvin ia n Tr ilobites from Wydry sz6w. In addidi on to sp ecies previou sly recorded from the Holy Cr oss M ts, the writer describ es so me others not known so far f r om Poland and 3 n ew sp eci es. INTROD UCT ION The material here describe d has been collecte d by the present write r in the Holy Cross Mts., at the locality of Wydryszow, to the north-east of Kielce. The paper has been p rep ared at the P aleozoological Labora tory of the Po lish Academy of Sciences at the inspi ration and under the guidance of Dr. Zofia Kielan to whom sincere thanks are due for he r advice, assistance in the selection of literature and criticism of the ma nuscript. The writ er is also most indeb ted to Mrs. M. Pajchel for her most valuable suggestions concerning the stratigraphy of the deposits from whi ch the s tudied m aterial has been collected. To Miss M. Czar nocka the wri te r is grateful for the photographs. STRATIGRAPHIC AND GEOGRAPHIC DISTRIBUTION OF THE DISCUSSED SPECIES The Couvinian fauna from Wydryszow has been described by the late J. Czarnocki, but both, the respective manuscripts and the collections of this author, were in 1944 destroyed in Warsaw. Czarnecki (1950) has assigned to the Couvinian th e deposits of Wydryszow, regarding this stage as intermediate between the Lower and the Middle Devonian.