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The Palaeobotanist 61(2012): 387-405 0031-0174/2012 $2.00 Sporophyll morphology and reconstruction of the heterosporous lycopod Tomiostrobus radiatus Neuburg emend. from the Lower Triassic of Siberia (Russia) SERGE V. NAUGOLNYKH Laboratory of Paleofloristics, Geological Institute, Russian Academy of Sciences, Pyzhevsky per 7, Moscow, 119017, Russia. Corresponding author: [email protected] (Received 5 July, 2011; revised version accepted 18 July, 2012) ABSTRACT Naugolnykh SV 2012. Sporophyll morphology and reconstruction of the heterosporous lycopod Tomiostrobus radiatus Neuburg emend. from the Lower Triassic of Siberia (Russia). The Palaeobotanist 61(2): 387-405. The paper deals with the taxon Tomiostrobus radiatus Neuburg emend., a heterosporous isoetopsid lycopod from the Babiy Kamen Locality of Lower Triassic of Siberia (Russia). Morphological diversity of the T. radiatus sporophylls is described in detail. Interpretation of structure and function of the sporophylls, and analysis of their morphological peculiarities are given. Arguments for attributing the lycopod T. radiatus to the Isoetaceae family have been provided. The reconstruction of T. radiatus is proposed. Origin and evolution of the families Isoetaceae and Pleuromeiaceae are also discussed. Key-words—Triassic, Siberia, lycopods, Tomiostrobus, Isoetaceae, Isoetes. chtk.kqi.kZ vkd`frfoKku rFkk lkbcsfj;k ¼#l½ ds fuEu r`rh;d ls izkIr fo"kechtk.kq ykbdksikWM VkWfevksLVªkscl jsfM,Vl U;wcxZ besaM uoe ds o`n~f/k iz#i dh iqulZajpuk ltZ oh ukSxkWYuh[k lkjka'k ;g 'kks/k&i= lkbcsfj;k ¼#l½ ds fuEu Vªkb,sfld] csch; desu micLrh ls izkIr fo"ke chtk.kq vkblks,VkWfIlM ykbdksikWM] VksfevksLVªkscl jsfM,Vl U;wcxZ besaM uoe tkfr ls lacn~/k gSA Vh-jsfM,Vl chtk.kqi.kZ dh vkdkfjdh; fofo/krk foLr`r #i ls of.kZr dh xbZ gSA lajpuk dh O;k[;k ,oa chtk.kqi.kZ ds izdk;Z rFkk mudh vkdkfjdh; fof’k"Vrkvksa dks crk;k x;k gSA ykbdksikWM Vh-jsfM,Vl dks vkblksbVslh ifjokj dk ekuus gsrq rdZ fn, x, gSaA Vh-jsfM,Vl dh laiw.kZ ikni iqulZajpuk izLrkfor gSA vkblksbVslh ,oa Iywjksek,lh ifjokjksa ds mn~Hko ,oa fodkl dh Hkh ppkZ dh xbZ gSA laDsÿr&'kCn—Vªkb,sfld] lkbcsfj;k] ykbdksikWM] VkWfevksLVªkscl] vkblksbVslh] vkblksbVsl A INTRODUCTION the groups of spore plants, specially regarding the origin of modern lycopod families. The questions related with the he present-day lycopods are represented by non- appearance and origin of the modern lycopod families are still Tarborescent forms only, which are assigned to the families unanswered. The complexity of the issues related to analysis Lycopodiaceae, Selaginellaceae and Isoetaceae. There are of the initial phases of evolution of the modern lycopod families many challenges in systematics and phylogeny of some of arises from superficial interpretation of some fossil lycopod © Birbal Sahni Institute of Palaeobotany, India 388 THE PALAEOBOTANIST representatives. Nevertheless, these taxa play an essential role Academy of Sciences (Moscow). The Babiy Kamen Section is for proper understanding of the evolution of this plant group. well-known as a classic outcrop of the Lower Triassic (Induan) Absence of well-documented morphological features of such deposits and has yielded fossil plants, represented by both key-taxa does not enable them to compare properly with the macrofossils and palynomorphs. recent taxa for consideration of the potential phylogenetic The sporophylls of Tomiostrobus radiatus were collected descendants. from the dark-grey to black siltstones belonging to The present study deals with the Early Triassic lycopod Tarakhanikha packet of the lower part of the Ostashinskaya Tomiostrobus radiatus Neuburg, its systematic position, Formation of the Maltsevka Series. Besides the fossil plants, detailed characteristics of sporophylls and reconstruction. these deposits also contain numerous shells of Special attention is given to the phylogenetic role of this plant conchostraceans, as well as some insects. in the origin of the family Isoetaceae, which can be regarded in The collection includes more than eighty extremely well the modern plant world as a typical example of the “living preserved fossil plant remains. Most of the plant macrofossils fossils”. are sporophylls of the isoetopsid lycopod taxon Tomiostrobus radiatus Neuburg, initially described on the basis of the MATERIAL material found in the Babiy Kamen Locality. The plant fossils are mostly preserved as impressions on fine-grained dark-grey The material under examination was collected in 2001 from siltstone, however, several fossils are partly preserved as the Babiy Kamen (“Women’s Stone”) Section, located in the compressions having limonitizied tissues. Kuznetsk coal basin, on the right bank of Tom River (Fig. 1) The sporophylls of Tomiostrobus radiatus from this and was provided to the present author by D.E. Scherbakov, collection can be grouped into several categories according who is a researcher of the Palaeontological Institute of Russian to mode of their preservation. The first category includes Fig. 1—Geographical position of the Babiy Kamen Locality. The locality is marked by asterisk. Geological map modified after: http://jurassic.ucoz.ru. NAUGOLNYKH—TOMIOSTROBUS RADIATUS NEUBURG EMEND. FROM THE LOWER TRIASSIC OF SIBERIA 389 argued for its interpretation as a conductive strand of the sporophyll. From my viewpoint, the rib-like extenuation, without any doubt, corresponds to the position of the conductive strand in the sporophyll, but nonetheless is not identical to it. I think that the adaxial surface of the sporophyll, both in its basal part and under the sporangium, has a small prolonged rib-like elevation expressed in relief of the sporophyll as a positive linear structure. This elevation is Fig. 2—Tomiostrobus radiatus Neuburg, sporophyll diversity: a – 4851/ Fig. 3—Tomiostrobus radiatus Neuburg, sporophyll diversity: a – 4851/ 113; b – 4851/114; c – 4851/115a; d – 4851/115b; e – 4851/ 122; b – 4851/118; c – 4851/116; d – 4851/121. Lower Triassic, 127; f – 4851/119a; g – 4851/128. Lower Triassic, Induan Induan Stage. Babiy Kamen Locality. Scale – 1 cm. Stage. Babiy Kamen Locality. Scale – 1 cm. virtually completely preserved sporophylls or their imprints to estimate the main modes of intraspecific variability of the with the observed fertile (proximal) and sterile (distal) parts. most important diagnostic features. This approach has been The second category includes proximal (fertile) parts of found to be very effective and productive both for the sporophylls without distal segments, which were most systematics and taxonomy, not only for the palaeobotanical probably detached naturally as generally happens with the but also for the palaeozoological studies (Serezhnikova, 2008). extant representatives of the genus Isoetes L. (see the Some of the sporophylls are photographed in different modes “Discussion” part below). The third category includes the for an adequate demonstration of their morphological features. proximal (fertile) parts of the Tomiostrobus radiatus sporophylls, also without distal (sterile) segment, but in this MORPHOLOGY OF THE SPOROPHYLLS OF case the distal segment was lost as a result of mechanical TOMIOSTROBUS RADIATUS NEUBURG damage of the specimens. Isolated distal segments of the sporophylls are assigned to the fourth category. Despite a very high morphological variability, the The approach of monotopic site analysis as suggested sporophylls of Tomiostrobus radiatus of the present collection by Meyen (1966) is applied in the present study as a have been assigned to one and the same natural or “botanical’ methodological basis for description of the Tomiostrobus species. Using typological basis/approach for Tomiostrobus radiatus sporophylls. This approach was based on the radiatus taxonomy (based on the structure of sporophylls), multisubjective study of plant macrofossils collected from one one can divide these sporophylls into several formal morpho- and the same locality (from one and the same layer or taxa, but this way can hardly be accepted as biologically depositional surface), presumably all these macrofossils valuable. The observed differences can be explained as represent the same natural community or population (in case reflections of (1) a different position of the sporophylls on of monospecies locality). The monotopic site approach enables protocorm; (2) a different age (or onthogenetic stage) of the 390 THE PALAEOBOTANIST Fig. 4—Tomiostrobus radiatus Neuburg, sporophyll diversity: a – 4851/ Fig. 5—Tomiostrobus radiatus Neuburg, several sporophylls belonged 123; b – 4851/124; c – 4851/126; e – 4851/127; f – 4851/ to one and the same parent plant; 4851/161. Lower Triassic, 119a; g – 4851/128. Lower Triassic, Induan Stage. Babiy Kamen Induan Stage. Babiy Kamen Locality. Scale – 1 cm. Locality. Scale – 1 cm. parent plants; (3) a natural intraspecific or intra-population placed distally in relation to the sporangium. The ligula is variability of the parent plants and natural variability of their observed in very few specimens only (Figs 2g, 5, Pl. 4.1). parts/different organs. Proximal part of the sporophyll distally continues very All general linear parameters of the sporophyll gradually into the distal (sterile) part (distal segment). The morphology have been measured (Fig. 10). If the linear size of distal segment is narrow and possesses long, acute apex (Figs the sporophyll part could not be stated, the cell of the Fig. 10 2f, 2g, 4a-g, 6; Pl. 1.4-5,8-9, Pl. 2.1-4, Pl. 3.3, 4, Pl. 5.1, 2). A distal has been left blank with (-) mark. All the measurements
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    Review of Palaeobotany and Palynology 293 (2021) 104503 Contents lists available at ScienceDirect Review of Palaeobotany and Palynology journal homepage: www.elsevier.com/locate/revpalbo Review papers The Eco-Plant model and its implication on Mesozoic dispersed sporomorphs for Bryophytes, Pteridophytes, and Gymnosperms Jianguang Zhang a,⁎, Olaf Klaus Lenz b, Pujun Wang c,d, Jens Hornung a a Technische Universität Darmstadt, Schnittspahnstraße 9, 64287 Darmstadt, Germany b Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, 60325 Frankfurt/Main, Germany c Key Laboratory for Evolution of Past Life and Environment in Northeast Asia (Jilin University), Ministry of Education, Changchun 130026, China d College of Earth Sciences, Jilin University, Changchun 130061, PR China article info abstract Article history: The ecogroup classification based on the growth-form of plants (Eco-Plant model) is widely used for extant, Ce- Received 15 July 2020 nozoic, Mesozoic, and Paleozoic paleoenvironmental reconstructions. However, for most Mesozoic dispersed Received in revised form 2 August 2021 sporomorphs, the application of the Eco-Plant model is limited because either their assignment to a specific Accepted 3 August 2021 ecogroup remains uncertain or the botanical affinities to plant taxa are unclear. By comparing the unique outline Available online xxxx and structure/sculpture of the wall of dispersed sporomorph to the sporomorph wall of modern plants and fossil plants, 861 dispersed Mesozoic sporomorph genera of Bryophytes, Pteridophytes, and Gymnosperms are Keywords: Botanical affinity reviewed. Finally, 474 of them can be linked to their closest parent plants and Eco-Plant model at family or Ecogroup order level. Based on the demands of the parent plants to different humidity conditions, the Eco-Plant model sep- Paleoenvironment arates between hydrophytes, hygrophytes, mesophytes, xerophytes, and euryphytes.
  • MANUAL of PTERIDOLOGY Typical New Zealand Lowland Rainforest (Westland) with Cyathea Medullaris, C

    MANUAL of PTERIDOLOGY Typical New Zealand Lowland Rainforest (Westland) with Cyathea Medullaris, C

    MANUAL OF PTERIDOLOGY Typical New Zealand lowland rainforest (Westland) with Cyathea medullaris, C. dealbata, Hemithelia Smithii etc., on left: Freycinethia Banksii; Podocarpus dacry­ dioides in background. - Photo I. L. COLLINS. MA UAL OF T IDOLOGY EDITED BY FR. VERDOORN IN COLLABORATION WITH A. H. G. ALSTON, I. ANDERSSON-KoTTO, L. R. ATKINSON, H. BURGEFF, H. G. DU BUY, C. CHRISTENSEN, W. Dopp, W. M. DOCTERS VAN LEEUWEN, H. GAMS, M. J. F. GREGOR, M. HIRMER, R. E. HOLTTUM, R. KRAUSEL, E. L. NUERN­ BERGK, J. C. SCHOUTE, J. WALTON, K. WETZEL, S. WILLIAMS, H. WINKLER AND W. ZIMMERMANN FOREWORD BY F. O. BOWER WITH 121 ILLUSTRATIONS • Springer-Science+Business Media, B.V 1938 ISBN 978-94-017-5743-0 ISBN 978-94-017-6111-6 (eBook) DOI 10.1007/978-94-017-6111-6 Copyright 1938 by Springer Science+Business Media Dordrecht Originally published by Martinus Nijhoff, The Hague, Netherlands in 1938. Softcover reprint ofthe hardcover 1st edition 1938 All rights reserved, including the right to translate or to reproduce this book or parts thereot in any torm CONTENTS CHAPTER I. Morphology Page § 1 HISTORICAL INTRODUCTION . 1 § 2 THE COMMON PRINCIPLES OF PTERIDOPHYTE MORPHOLOGY. 3 § 3 THE PROT HALL US . 4 § 4 THE GAMETANGIA 5 § 5 THE STEM .... 6 A. GENERAL PROPERTIES 6 B. FORM OF STEM .. 7 C. ORIGIN OF STEM. 8 D. RAMIFICATION. 9 .1. KINDS OF RAMIFICATION. 9 II. SPATIAL RELATIONS OF BRANCHES. 10 a. Spatial relations between branches of a branch system. 10 b. Spatial relations to nodes of stem . 12 c. Spatial relations to nodes and to other branches at the same time 12 d.