Formal System of Dispersed Leaf Cuticles of Pteridosperms (Peltaspermaceae) from the Permian and Triassic of the Russian Platform E
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A New Genus Navipelta (Peltaspermales, Pteridospermae) from the Permian/Triassic Boundary Deposits of the Moscow Syneclise E
ISSN 0031-0301, Paleontological Journal, 2009, Vol. 43, No. 10, pp. 1262–1271. © Pleiades Publishing, Ltd., 2009. A New Genus Navipelta (Peltaspermales, Pteridospermae) from the Permian/Triassic Boundary Deposits of the Moscow Syneclise E. V. Karasev Borissiak Paleontological Institute of the Russian Academy of Sciences, 117997, Profsoyuznaya, 123, Moscow e-mail: [email protected] Received January 25, 2009 Abstract—A new genus of peltaspermalean ovuliferous organs Navipelta gen. nov. is described from the ter- restrial deposits of the Nedubrovo locality (village of Nedubrovo, Vologda Region, Russia), belonging to the base of Vetlugian Group (Upper Permian–Lower Triassic). Data on the anatomy of the peltate bilateral ovulif- erous organs are obtained for the first time. Vascular strands in the peltoid depart from that of a stalk and branch up to three times distally. Transfusion tissue around the vascular strands is well developed. The new genus had a system of radially arranged resin canals, broaden into large secretory cavities. Key words: Peltaspermaceae, ovuliferous organs, Peltaspermum, Autunia, Permian/Triassic boundary, Vetlu- gian Group, systematics. DOI: 10.1134/S0031030109100086 INTRODUCTION angium Zhao ex Gomankov et Meyen and Autuniopsis Poort et Kerp) or on the basis of their association with The family Peltaspermaceae attracts attention of different foliage (Peltaspermopsis buevichiae Goman- many researchers, because its members were the main kov et. Meyen and Meyenopteris, Poort et Kerp) component of the Late Permian Angaraland floras. (Gomankov and Meyen, 1986; Poort and Kerp, 1990). They escaped the global crisis on the Permian/Triassic boundary and transited in the Mesozoic, where domi- The morphology and epidermal structure of seed- nated during the Middle and Late Triassic of the North- bearing organs in the Peltaspermaceae were studied rel- ern as well as Southern hemispheres. -
Ecological Sorting of Vascular Plant Classes During the Paleozoic Evolutionary Radiation
i1 Ecological Sorting of Vascular Plant Classes During the Paleozoic Evolutionary Radiation William A. DiMichele, William E. Stein, and Richard M. Bateman DiMichele, W.A., Stein, W.E., and Bateman, R.M. 2001. Ecological sorting of vascular plant classes during the Paleozoic evolutionary radiation. In: W.D. Allmon and D.J. Bottjer, eds. Evolutionary Paleoecology: The Ecological Context of Macroevolutionary Change. Columbia University Press, New York. pp. 285-335 THE DISTINCTIVE BODY PLANS of vascular plants (lycopsids, ferns, sphenopsids, seed plants), corresponding roughly to traditional Linnean classes, originated in a radiation that began in the late Middle Devonian and ended in the Early Carboniferous. This relatively brief radiation followed a long period in the Silurian and Early Devonian during wrhich morphological complexity accrued slowly and preceded evolutionary diversifications con- fined within major body-plan themes during the Carboniferous. During the Middle Devonian-Early Carboniferous morphological radiation, the major class-level clades also became differentiated ecologically: Lycopsids were cen- tered in wetlands, seed plants in terra firma environments, sphenopsids in aggradational habitats, and ferns in disturbed environments. The strong con- gruence of phylogenetic pattern, morphological differentiation, and clade- level ecological distributions characterizes plant ecological and evolutionary dynamics throughout much of the late Paleozoic. In this study, we explore the phylogenetic relationships and realized ecomorphospace of reconstructed whole plants (or composite whole plants), representing each of the major body-plan clades, and examine the degree of overlap of these patterns with each other and with patterns of environmental distribution. We conclude that 285 286 EVOLUTIONARY PALEOECOLOGY ecological incumbency was a major factor circumscribing and channeling the course of early diversification events: events that profoundly affected the structure and composition of modern plant communities. -
Fundamentals of Palaeobotany Fundamentals of Palaeobotany
Fundamentals of Palaeobotany Fundamentals of Palaeobotany cuGU .叮 v FimditLU'φL-EjAA ρummmm 吋 eαymGfr 伊拉ddd仇側向iep M d、 況 O C O W Illustrations by the author uc削 ∞叩N Nn凹創 刊,叫MH h 咀 可 白 a aEE-- EEA First published in 1987 by Chapman αndHallLtd 11 New Fetter Lane, London EC4P 4EE Published in the USA by Chα~pman and H all 29 West 35th Street: New Yo地 NY 10001 。 1987 S. V. M秒len Softcover reprint of the hardcover 1st edition 1987 ISBN-13: 978-94-010-7916-7 e-ISBN-13: 978-94-009-3151-0 DO1: 10.1007/978-94-009-3151-0 All rights reserved. No part of this book may be reprinted, or reproduced or utilized in any form or by any electronic, mechanical or other means, now known or hereafter invented, including photocopying and recording, or in any information storage and retrieval system, without permission in writing from the publisher. British Library Cataloguing in Publication Data Mey凹, Sergei V. Fundamentals of palaeobotany. 1. Palaeobotany I. Title 11. Osnovy paleobotaniki. English 561 QE905 Library 01 Congress Catα loging in Publication Data Mey凹, Sergei Viktorovich. Fundamentals of palaeobotany. Bibliography: p. Includes index. 1. Paleobotany. I. Title. QE904.AIM45 561 8ι13000 Contents Foreword page xi Introduction xvii Acknowledgements xx Abbreviations xxi 1. Preservation 抄'pes αnd techniques of study of fossil plants 1 2. Principles of typology and of nomenclature of fossil plants 5 Parataxa and eutaxa S Taxa and characters 8 Peculiarity of the taxonomy and nomenclature of fossil plants 11 The binary (dual) system of fossil plants 12 The reasons for the inflation of generic na,mes 13 The species problem in palaeobotany lS The polytypic concept of the species 17 Assemblage-genera and assemblage-species 17 The cladistic methods 18 3. -
Diversity and Homologies of Corystosperm Seed-Bearing Structures from the Early Cretaceous of Mongolia Aã B,C D E F Gongle Shi , Peter R
Journal of Systematic Palaeontology ISSN: 1477-2019 (Print) 1478-0941 (Online) Journal homepage: https://www.tandfonline.com/loi/tjsp20 Diversity and homologies of corystosperm seed- bearing structures from the Early Cretaceous of Mongolia Gongle Shi, Peter R. Crane, Patrick S. Herendeen, Niiden Ichinnorov, Masamichi Takahashi & Fabiany Herrera To cite this article: Gongle Shi, Peter R. Crane, Patrick S. Herendeen, Niiden Ichinnorov, Masamichi Takahashi & Fabiany Herrera (2019) Diversity and homologies of corystosperm seed- bearing structures from the Early Cretaceous of Mongolia, Journal of Systematic Palaeontology, 17:12, 997-1029, DOI: 10.1080/14772019.2018.1493547 To link to this article: https://doi.org/10.1080/14772019.2018.1493547 Published online: 14 Jan 2019. Submit your article to this journal Article views: 142 View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tjsp20 Journal of Systematic Palaeontology, 2019 Vol. 17, No. 12, 997–1029, http://dx.doi.org/10.1080/14772019.2018.1493547 Diversity and homologies of corystosperm seed-bearing structures from the Early Cretaceous of Mongolia aà b,c d e f Gongle Shi , Peter R. Crane , Patrick S. Herendeen , Niiden Ichinnorov , Masamichi Takahashi and Fabiany Herrerad aState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China; bOak Spring Garden -
Transformative Paleobotany
Chapter 6 Lower Permian Flora of the Sanzenbacher Ranch, Clay County, Texas William A. DiMichele1, Robert W. Hook2, Hans Kerp3, Carol L. Hotton1,4, Cindy V. Looy5 and Dan S. Chaney1 1NMNH Smithsonian Institution, Washington, DC, United States; 2The University of Texas at Austin, Austin, TX, United States; 3Westfälische Wilhelms-Universität Münster, Münster, Germany; 4National Institutes of Health, Bethesda, MD, United States; 5University of California Berkeley, Berkeley, CA, United States 1. INTRODUCTION 1985; Broutin, 1986; Popa, 1999; Steyer et al., 2000; Wagner and Mayoral, 2007; Bercovici and Broutin, 2008; Since 1989, field parties supported by the U.S. National Barthel, 2009; Wagner and Álvarez-Vázquez, 2010; Museum of Natural History have obtained large collections Barthel and Brauner, 2015). Furthermore, because this of mainly Permian plant fossils from north central Texas. locality was collected on three occasions over a time period This work was undertaken to study known localities and to of 50 years and by different parties, comparative analysis of find new fossiliferous deposits that would contribute to a the Sanzenbacher collections provides a basis for assessing better understanding of floral and paleoenvironmental sites that have comparable histories. changes within the region during the early Permian. From the outset, the effort was interdisciplinary and grew, through the contributions of nearly 20 paleobotanists, 2. GEOLOGY palynologists, invertebrate and vertebrate paleontologists, Clay County is the only county in the Permo-Carboniferous and sedimentary geologists of several subdisciplines, to be outcrop belt of north central Texas that lacks marine rocks. quite comprehensive. Our reporting of results, however, has These alluvial sediments accumulated east of a broad been influenced by unexpected developments, including the coastal plain that bordered the Eastern Shelf of the Midland discovery of new plant-fossil assemblages in areas once Basin. -
Habit and Ecology of the Petriellales, an Unusual Group of Seed Plants from the Triassic of Gondwana Author(S): Benjamin Bomfleur, Anne-Laure Decombeix, Andrew B
Habit and Ecology of the Petriellales, an Unusual Group of Seed Plants from the Triassic of Gondwana Author(s): Benjamin Bomfleur, Anne-Laure Decombeix, Andrew B. Schwendemann, Ignacio H. Escapa, Edith L. Taylor, Thomas N. Taylor, Stephen McLoughlin Source: International Journal of Plant Sciences, Vol. 175, No. 9 (November/December 2014), pp. 1062-1075 Published by: The University of Chicago Press Stable URL: http://www.jstor.org/stable/10.1086/678087 . Accessed: 08/12/2014 09:32 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The University of Chicago Press is collaborating with JSTOR to digitize, preserve and extend access to International Journal of Plant Sciences. http://www.jstor.org This content downloaded from 130.242.24.193 on Mon, 8 Dec 2014 09:32:01 AM All use subject to JSTOR Terms and Conditions Int. J. Plant Sci. 175(9):1062–1075. 2014. q 2014 by The University of Chicago. All rights reserved. 1058-5893/2014/17509-0008$15.00 DOI:10.1086/678087 HABIT AND ECOLOGY OF THE PETRIELLALES, AN UNUSUAL GROUP OF SEED PLANTS FROM THE TRIASSIC OF GONDWANA Benjamin Bomfleur,1,*,† Anne-Laure Decombeix,‡ Andrew B. -
Iop Newsletter 113
IOP NEWSLETTER 113 June 2017 CONTENTS Letter from the president IBC 2017 Shenzhen (China): latest news Young Scientist Representative Emese Bodor Obituary of Prof. Manju Banerjee Prof. David Dilcher receives award Report of the 34th Midcontinent Paleobotanical Colloquium Rhynie Chert Meeting 2017 Upcoming meetings 2017-2018 New publications 1 Letter from the president Dear Colleagues, I hope this season brings you some time to enjoy palaeobotanical research, whether field work, laboratory/museum investigations or participating in conferences. This is an active time for field work and conferences in many regions. I look forward to meeting with colleagues at the International Botanical Congress (IBC) in Shenzhen next month. Palaeobotanically themed symposia planned for IBC include: “Using fossil evidence to explore the plant evolution, diversity, and their response to global changes;” “New data on early Cretaceous seed plants;” “Ecological and biogeographic implications of Asian Oligocene and Neogene fossil floras;” “Plant conservation, learning from the past”, and “The Origin of Plants: rocks, genomes and geochemistry.” Details of presenters and scheduling of general symposia as well as invited keynote lectures are found at the conference website: http://www.ibc2017.cn/Program/. Please see the note below with details on the social gathering for paleobotanists at IBC. We welcome Kelly Matsunaga (photograph by courtesy of Kelly), Graduate Student at University of Michigan as IOP Student Representative for North America, recently confirmed by Christopher Liu. She joins Han Meng (China), Emese Bodor (Hungary; see p. 3 in the newsletter), and Maiten A. Lafuente Diaz (Argentina) as current student representtatives. The excel- lence of these and other young members of IOP foretells a bright future for our discipline. -
Fossilized Pollination Droplet in a New Seed Genus from the Middle Triassic of Nidpur, India
Fossilized pollination droplet in a new seed genus from the Middle Triassic of Nidpur, India NUPUR BHOWMIK and SHABNAM PARVEEN Bhowmik, N. and Parveen, S. 2014. Fossilized pollination droplet in a new seed genus from the Middle Triassic of Nidpur, India. Acta Palaeontologica Polonica 59 (2): 491–503. The present article reports a fossilized pollination droplet at the micropylar orifice in a compressed seed Gopadisper- mum papillatus gen. et sp. nov. from the Middle Triassic beds of Nidpur, Madhya Pradesh, India. The shapeless droplet forming a convexity above the micropylar orifice is comprised of a resinous crystalline substance. Entrapped within the droplet are a few saccate pollen grains. The seeds are small, oblong to widely elliptical in shape, about 3 mm long and generally 2 mm broad. The micropylar end shows a short straight beak-like micropyle often extended beyond a persistently adhering wrinkled tissue lying outside the seed coat. The seed is composed of four membranes excluding the adherent tissue. They are the outer and inner cuticles of integument, the nucellar cuticle distally modified to form a dark collar-like pollen chamber and the innermost megaspore membrane. Cuticles of the tissue adhering to seed coat are different from seed coat cuticles. The pollen grains inside the pollen chamber are frequently clumped together forming a pollen mass. Individual pollen grains appear spheroidal to ellipsoidal in shape and are saccate. This is the first report of the preservation of a pollination droplet in a compressed seed specimen from the Nidpur Triassic beds. Preservation of the droplet can be attributed to its supposed resinous constitution and the entrapped organic contents (pollen grains). -
New Glossopterid Polysperms from the Permian La Golondrina Formation (Santa Cruz Province, Argentina): Potential Affinities and Biostratigraphic Implications
Rev. bras. paleontol. 18(3):379-390, Setembro/Dezembro 2015 © 2015 by the Sociedade Brasileira de Paleontologia doi: 10.4072/rbp.2015.3.04 NEW GLOSSOPTERID POLYSPERMS FROM THE PERMIAN LA GOLONDRINA FORMATION (SANTA CRUZ PROVINCE, ARGENTINA): POTENTIAL AFFINITIES AND BIOSTRATIGRAPHIC IMPLICATIONS BÁRBARA CARIGLINO Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, CONICET, Av. Ángel Gallardo 470, C1405DJR, Buenos Aires, Argentina. [email protected] ABSTRACT – Impression fossils of ovuliferous fructifi cations from the Permian La Golondrina Formation in Santa Cruz, Argentina, are described, their affi nities compared, and fi nally, assigned to the Arberiaceae (Glossopteridales). Based on morphological differences from the genera in Arberiaceae, a new taxon is established for some specimens, whereas others are allocated to Arberia madagascariensis (Appert) Anderson & Anderson. This is the fi rst record of Arberiaceae from the La Golondrina Basin. The biostratigraphic implications of the occurrence of this family in this unit are discussed, and suggest that more evidence other than that provided by the megafl oral elements is needed to resolve the age of the constituent members of the La Golondrina Formation. Key words: Arberiaceae, Argentina, biostratigraphy, fructifi cations, Glossopteridales, Gondwana. RESUMO – São descritos impressões fósseis de frutifi cações femininas provenientes da Formação La Golondrina, Permiano de Santa Cruz (Argentina), atribuídas a Arberiaceae (Glossopteridales), segundo a comparação de suas afi nidades. -
Antarctic Palynology and Palaeoclimate – a Review
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by NERC Open Research Archive Bionature, 35 (1 & 2), 2015 : 1-6 © Bionature ANTARCTIC PALYNOLOGY AND PALAEOCLIMATE – A REVIEW VANESSA BOWMAN British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET ABSTRACT The first exciting clues that Antarctica had not always been ice-covered were the leaf fossils of Glossopteris plants that Scott’s party brought back from the Beardmore Glacier region in 1912. Since dated at ~ 250 million years old, it has become evident that Antarctica has been vegetated longer than it has been ice-covered. These first plant fossils from the Beardmore have led to over 100 years of scientific investigation of the rich macro- (e.g. leaves and fossil wood) and micro- (terrestrial and marine palynomorph) fossil record of Antarctica. Palynomorphs from the sedimentary record of Antarctica continue to provide an exceptionally detailed interpretation of high latitude vegetation and climate from Devonian to Neogene times, complementing and extending the macrofossil record. They document the transition from the Glossopteris-dominated Gondwanan flora to more modern conifer and then beech-dominated polar forests, followed eventually by a less diverse and lower stature vegetation as climates cooled and ice sheets became large and relatively stable into the Neogene. Continued research into terrestrial and marine palynomorphs provides essential insight into the environmental sensitivity of the polar regions in a future warmer world. Keywords : Antarctica; palynology; palaeoclimate; vegetation Introduction In addition to finds of plant macrofossils (including leaves and fossil wood), During their ill-fated expedition to the microscopic remains of plants and marine South Pole in 1912 Captain Robert Falcon algae (palynomorphs) are now commonly Scott and his party struggled to carry samples found in the Antarctic sedimentary record of leaf fossils back from the mountains of the (Figure 1). -
Triassic Floras of Antarctica: Plant Diversity and Distribution in High Paleolatitude Communities
PALAIOS, 2011, v. 26, p. 522–544 Research Article DOI: 10.2110/palo.2010.p10-122r TRIASSIC FLORAS OF ANTARCTICA: PLANT DIVERSITY AND DISTRIBUTION IN HIGH PALEOLATITUDE COMMUNITIES IGNACIO H. ESCAPA,1,2* EDITH L. TAYLOR,1 RUBE´ NCU´ NEO,2 BENJAMIN BOMFLEUR,1,3 JULIE BERGENE,1 RUDOLPH SERBET,1 and THOMAS N. TAYLOR 1 1Department of Ecology and Evolutionary Biology, and Natural History Museum and Biodiversity Institute, University of Kansas, Lawrence 66045-7534, USA, [email protected], [email protected], [email protected], [email protected], [email protected]; 2CONICET—Museo Paleontolo´gico Egidio Feruglio, Trelew, Chubut, 9100, Argentina, [email protected]; 3Forschungsstelle fu¨r Pala¨obotanik am Institut fu¨r Geologie und Pala¨ontologie, Westfa¨lische Wilhelms-Universita¨t Mu¨nster, Hindenburgplatz 57, D-48143 Mu¨nster, Germany, [email protected] ABSTRACT number of Antarctic plant fossils during his career. His collection—now at the University of Kansas—includes plants preserved as impressions Continental Triassic sequences in Antarctica are among the most and compressions, palynological samples, and silicified wood from continuous and best represented in Gondwana. Triassic fossil plants have numerous sites, including southern and northern Victoria Land (SVL, been collected sporadically from Antarctica since the beginning of the NVL) and the CTM. twentieth century, but our knowledge of the vegetation during this time Certainly one of the most significant contributions of Schopf’s has dramatically increased during the last three decades. Here we review fieldwork in Antarctica was the discovery of permineralized peat from the fossil record of Triassic plants as representatives of natural groups two sites in the CTM (Schopf, 1970, 1978). -
Extinction and Recovery Patterns of the Vegetation Across
Review of Palaeobotany and Palynology 144 (2007) 99–112 www.elsevier.com/locate/revpalbo Extinction and recovery patterns of the vegetation across the Cretaceous–Palaeogene boundary — a tool for unravelling the causes of the end-Permian mass-extinction ⁎ Vivi Vajda a, , Stephen McLoughlin b a GeoBiosphere Science Centre, Lund University, Sölvegatan 12, SE-223 62, Lund, Sweden b School of Natural Resource Sciences, Queensland University of Technology, PO Box 2434, Brisbane, Q. 4001, Australia Received 22 December 2004; received in revised form 14 September 2005; accepted 14 September 2005 Available online 12 July 2006 Abstract High-resolution palynofloral signatures through the Cretaceous–Palaeogene boundary succession show several features in common with the Permian–Triassic transition but there are also important differences. Southern Hemisphere Cretaceous– Palaeogene successions, to date studied at high resolution only in New Zealand, reveal a diverse palynoflora abruptly replaced by fungi-dominated assemblages that are in turn succeeded by low diversity suites dominated by fern spores, then gymnosperm- and angiosperm-dominated palynofloras of equivalent diversity to those of the Late Cretaceous. This palynofloral signature is interpreted to represent instantaneous (days to months) destruction of diverse forest communities associated with the Chicxulub impact event. The pattern of palynofloral change suggests wholesale collapse of vascular plant communities and short-term proliferation of saprotrophs followed by relatively rapid successional recovery of pteridophyte and seed–plant communities. The Permian–Triassic transition records global devastation of gymnosperm-dominated forests in a short zone synchronous with one or more peaks of the fungal/algal palynomorph Reduviasporonites. This zone is typically succeeded by assemblages rich in lycophyte spores and/or acritarchs.