The Architecture of Permian Glossopterid Ovuliferous Reproductive Organs
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The Formation of Plant Compression Fossils
THE FORMATION OF PLANT COMPRESSION FOSSILS: EXPERIMENTAL AND SEDIMENTOLOGICAL INVESTIGATIONS by G illia n Mary Rex Thesis submitted fo r the degree of Doctor of Philosophy in the University of London Department of Botany Bedford College University of London September 1983 ProQuest Number: 10098497 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest. ProQuest 10098497 Published by ProQuest LLC(2016). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code. Microform Edition © ProQuest LLC. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 To Bob ”The simple^ qudlitab’ive experiments described belcw are only justifiable in so fa r as they give good ideas and they can d isc re d it bad ones. For me they did both”. Professor Tom M. Harris (1974) ABSTRACT The mechanisms and processes that lead to the formation of a plant com pression fossil have been experimentally reproduced and studied in the present investigation. This research has used two main lines of in ve sti gation: f ir s t ly , experimental modelling of the fo ssilisa tio n process; and secondly, a detailed examination of plant compression fo ssils. Early experimental modelling was based on the simplest system possible. -
Biodiversity Journal, 8 (2): 315-389
Biodiversity Journal, 2017, 8 (2): 315–389 MONOGRAPH Revision of the genus Amphiope L. Agassiz, 1840 (Echinoidea Astriclypeidae) with the description of a new species from the Miocene of France Paolo Stara1& Enrico Borghi2 1Centro Studi di Storia Naturale del Mediterraneo - Museo di Storia Naturale Aquilegia and Geomuseo Monte Arci, Masullas, Oristano, Sardinia, Italy; e-mail: [email protected] 2Società Reggiana di Scienze Naturali, Via Tosti 1, 42100 Reggio Emilia, Italy; e-mail: [email protected] ABSTRACT The taxonomy of Amphiope L. Agassiz, 1840 (Echinoidea, Astriclypeidae), an echinoid dis- tributed in the Oligo-Miocene of Central and Southern Europe, is largely unresolved since the description of most species attributed to this genus was based only on the external mor- phological features, while important characters, such as the oral plating and the internal sup- port system, were poorly illustrated or completely omitted. Additionally, the type material of some species was missing or badly preserved and geographical/stratigraphical information about the type-locality was unclear. This was the case also for Amphiope bioculata (Des Moulins, 1837), the type species of the genus. The poor definition of the earlier described species of Amphiope prevented comparison with fossils from other localities and ages, sub- sequently attributed to this genus. A large part of the earlier species of Amphiope, key-taxa for the resolution of the complex taxonomy of this genus, are herein revised by modern meth- ods. For this purpose, the type material available in public institutions has been re-examined and, when possible, new topo-typic material has been collected. As a result, the morphological description of A. -
Florida Fossil Invertebrates 2 (Pdf)
FLORIDA FOSSIL INVERTEBRATES Parl2 JANUARY 2OO2 SINGLE ISSUE: $z.OO OLIGOCENE AND MIOCENE ECHINOIDS CRAIG W. OYEN1 and ROGER W. PORTELL, lDeparlment of Geography and Earth Science Shippensburg U niversity 1871 Old Main Drive Shippensburg, PA 17257 -2299 e-mail: cwoyen @ ark.ship.edu 2Florida Museum of Natural History University of Florida P. O. Box 117800 Gainesville, FL 32611 -7800 e-mail: portell @flmnh.ufl.edu A PUBLICATTON OF THE FLORTDA PALEONTOLOGTCAL SOCIETY tNC. r,q)-.'^ .o$!oLo"€n)- .l^\ z*- il--'t- ' .,vn\'9t\ x\\I ^".{@^---M'Wa*\/i w*'"'t:.&-.d te\ 3t tu , l ". (. .]tt f-w#wlW,/ \;,6'#,/ FLORIDA FOSSIL INVERTEBRATES tssN 1536-5557 Florida Fossil lnvertebrafes is a publication of the Florida Paleontological Society, Inc., and is intended as a guide for identification of the many, common, invertebrate fossils found around the state. lt will deal solely with named species; no new taxonomic work will be included. Two parts per year will be completed with the first three parts discussing echinoids. Part 1 (published June 2001) covered Eocene echinoids, Parl2 (January 2002 publication) is about Oligocene and Miocene echinoids, and Part 3 (June 2002 publication) will be on Pliocene and Pleistocene echinoids. Each issue will be image-rich and, whenever possible, specimen images will be at natural size (1x). Some of the specimens figured in this series soon will be on display at Powell Hall, the museum's Exhibit and Education Center. Each part of the series will deal with a specific taxonomic group (e.9., echinoids) and contain a brief discussion of that group's life history along with the pertinent geological setting. -
Article in Press
Türkiye Jeoloji Bülteni Geological Bulletin of Turkey 64 (2021) 267-276 doi: 10.25288/tjb.854704 The First Report of Gangamopteris rajaensis from Rajmahal Gondwana Basin (Jharkhand, India) Arun Joshi1 , Raj Kumar Priya2* 1 Council of Scientific and Industrial Research (CSIR) and SGRR (P.G.) College, Dehradun, India 2 Department of Geology, Sikkim University, Gangtok, Sikkim, India • Geliş/Received: 05.01.2021 • Düzeltilmiş Metin Geliş/Revised Manuscript Received: 13.05.2021 • Kabul/Accepted: 14.05.2021 • Çevrimiçi Yayın/Available online: 29.06.2021 • Baskı/Printed: 25.08.2021 Research Article/Araştırma Makalesi Türkiye Jeol. Bül. / Geol. Bull. Turkey Abstract: The present study deals with the systematic description of macro and miofloral analysis ofGangamopteris rajaensis and Glossopteris indica from the carbonaceous shale-coal bearing sequences of the Rajmahal Open Cast Mine, Rajmahal Basin, Jharkhand, India. The floral diversity, age correlation, and the paleoenvironment of the Barakar Formation were well described. Morphological analysis revealed the reticulate venation pattern, anastomosing of veins, and the absence of the midrib in Gangamopteris rajaensis. The recovered megafloral assemblages of Gangamopteris rajaensis and Glossopteris indica suggest a late early Permian (Artiskian-Kungurian) age for the Barakar strata of Rajmahal coal mine and the prevalence of a moderately warm climate during their deposition. Earlier the species was reported from the Barakar Formation of Damodar and Mahanadi Gondwana basins in India. However, this is the first detailed systematic investigation of this species from the Rajmahal Gondwana Basin, Jharkhand, India. Keywords: Barakar Formation, Early Permian, Gangamopteris rajaensis, Rajmahal Gondwana Basin. INTRODUCTION the Permo-Carboniferous period (Mukhopadhyay The warm and humid climate after the Late et al., 2010). -
An Anatomically Preserved Glossopterid Megasporophyll from the Upper Permian of Skaar Ridge, Transantarctic Mountains, Antarctica
Int. J. Plant Sei. 174(3):396^05. 2013. © 2013 by The University of Chicago. All rights reserved. 1058-5893/2013/17403-0012$15.00 DOI: 10.1086/668222 LONCHIPHYLLUM APLOSPERMUM GEN. ET SP. NOV.: AN ANATOMICALLY PRESERVED GLOSSOPTERID MEGASPOROPHYLL FROM THE UPPER PERMIAN OF SKAAR RIDGE, TRANSANTARCTIC MOUNTAINS, ANTARCTICA Patricia E. Ryberg^'* and Edith L. Taylor* *Department of Ecology and Evolutionary Biology and Natural History Museum and Biodiversity Institute, University of Kansas, Lawrence, Kansas 66045, U.S.A. A new anatomically preserved megasporophyll, Lonchiphyllum aplospermum, is described from perminer- alized peat collected on Skaar Ridge in the central Transantarctic Mountains. This new genus contains vascular features similar to those of the leaf genus Glossopteris schopfii, which is the exclusive leaf genus in the specimens in which the sporophylls were found. The vasculature of the sporophyll consists of a central vascular region with bordered pitting and anastomosing lateral bundles with helical-scalariform thickenings. Ovules are attached oppositely to suboppositely to lateral veins on the adaxial surface of the sporophyll. There is an abundance of bisaccate pollen of the Protohaploxypinus type at the base of the ovules. The ovules of Lonchiphyllum are small (1.1 mm X 0.97 mm) and ovate and have an unornamented integument. Comparison with anatomically known ovules from Skaar Ridge, i.e., Plectilospermum elliotii, Choanostoma verruculosum, and Lakkosia kerasata and Homevaleia gouldii from the Bowen Basin of Australia, supports the classification of Lonchiphyllum as a glossopterid. The differences in the sarcotesta and sclerotesta of all the Skaar Ridge ovules may indicate specialization for pollination or dispersal. -
Southeastern Part of the Texas Coastal Plain
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPER 335 GEOLOGY AND UNDERGROUND WATERS OF THE SOUTHEASTERN PART OF THE TEXAS COASTAL PLAIN BY ALEXANDER DEUSSEN WASHINGTON GOVERNMENT PRINTING OFFICE 1914 CONTENTS. Page. Introduction.............................................................. 13 Physiography.............................................................. 14 General character..................................................... 14 Topographic features.................................................. 16 Relief............................................................ 16 Coast prairie.................................................. 16 Kisatchie Wold............................................... 16 Nacogdoches Wold............................................ 16 Corsicana Cuesta and White Rock Escarpment................... 18 Bottom lands................................................. 18 Mounds and pimple plains...................................... 19 Drainage.......................................................... 19 Timber............................................................... 21 General geologic features................................................... 21 Relation of geology to the occurrence of underground water............... 21 Principles of stratigraphy.............................................. 22 Erosion and sedimentation.......................................... 22 The geologic column.............................................. 22 Subdivision -
Reproductive Biology of the Permian Glossopteridalesand Their
Proc. Natd. Acad. Sci. USA Vol. 89, pp. 11495-11497, December 1992 Plant Biology Reproductive biology of the Permian Glossopteridales and their suggested relationship to flowering plants (Gndwan/seed fen/p d peat/phogy) EDITH L. TAYLOR AND THOMAS N. TAYLOR Byrd Polar Research Center and Department of Plant Biology, Ohio State University, Columbus, OH 43210 Communicated by Henry N. Andrews, August 27, 1992 ABSTRACT The discovery of pn rid reproductive organs fm Le ard- mr Glacier regV_io Antarctica proides anato l eidene for the ada iat- tachment of the seeds to the megasporophyll in this Impant group of Late Paeooic seed plants. The position of the seeds is in direct contradiction to many earlier Pbs predominantly on impression/compressIon remains. The at- tachment of the ovules on the adaxial surface of a leaf-like megasftiorophyfl, combinedwithotherfetre, suchasm g- metophyte development, sugs a sler reproductive biology in this group than has prev been hypothesized. These findings confirm the of the Glessopteridales as seed ferns and are important coider- FIG. 1. Cross section of megasporophyll (below) showing three ato in dc ons f the of the group, cldg ovules attached to the adaxial (upper) surface. Arrow points to ovule phylogey that has been broken off and is reoriented with the micropyle facing their suggestd role as close relatives or possible c of the megasporophyll. Note circular pads of resistant tissue around the a osperms. micropyle. Arrowheads delimit outer edge of megasporophyll. (x15.) The Glossopteridales are a group of extinct gymnospermous plants that dominated many terrestrial habitats in Gondwana locality along Skaar Ridge in the Beardmore Glacier region of during Permian times. -
Palynology of the Permian Sanangoe
PALYNOLOGY OF THE PERMIAN SANANGOE- MEFIDEZI COAL BASIN,TETE PROVINCE, MOZAMBIQUE AND CORRELATIONS WITH GONDWANAN MICROFLORAL ASSEMBLAGES Kierra Caprice Mahabeer A Dissertation submitted to the Faculty of Science, University of the Witwatersrand, in partial fulfilment of the requirements for the Degree of Master of Science June, 2017 The financial assistance of the National Research Foundation (NRF) towards this research is hereby acknowledged. Opinions expressed and conclusions arrived at, are those of the author and are not necessarily to be attributed to the NRF. Declaration I hereby certify that this Dissertation is my own unaided work. It is being submitted for the degree of Master of Science at the University of the Witwatersrand, Johannesburg. It has not been submitted before for any degree or examination at any other University. aT Kierra Caprice Mahabeer June 2017 n Acknowledgements My deepest gratitude goes to my supervisors Prof. Marion Bamford and Dr. Natasha Barbolini. Without their help and guidance this dissertation would not be possible. Thank you for always pushing me further and making me a better researcher. Thanks also goes to Dr. Jennifer Fitchett for the R script as well as for training in the statistical programs used in this study. Thank you to Eurasian Natural Resources Corporation (Mozambique Limitada) for access to core. Thank you to Dr. John Hancox for always being willing to assist with any questions and for facilitating access to core and for providing geological core logs. Thanks also goes to Prosper Bande for assistance with laboratory preparation. I am grateful for the financial assistance from the National Research Foundation the Palaeontological Scientific Trust (PAST) and the University of the Witwatersrand. -
Variation in Growth Pattern in the Sand Dollar, Echinarachnius Parma, (Lamarck)
University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Summer 1964 VARIATION IN GROWTH PATTERN IN THE SAND DOLLAR, ECHINARACHNIUS PARMA, (LAMARCK) PRASERT LOHAVANIJAYA University of New Hampshire, Durham Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation LOHAVANIJAYA, PRASERT, "VARIATION IN GROWTH PATTERN IN THE SAND DOLLAR, ECHINARACHNIUS PARMA, (LAMARCK)" (1964). Doctoral Dissertations. 2339. https://scholars.unh.edu/dissertation/2339 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. This dissertation has been 65-950 microfilmed exactly as received LOHAVANIJAYA, Prasert, 1935- VARIATION IN GROWTH PATTERN IN THE SAND DOLLAR, ECHJNARACHNIUS PARMA, (LAMARCK). University of New Hampshire, Ph.D., 1964 Zoology University Microfilms, Inc., Ann Arbor, Michigan VARIATION IN GROWTH PATTERN IN THE SAND DOLLAR, EC’HINARACHNIUS PARMA, (LAMARCK) BY PRASERT LOHAVANUAYA B. Sc. , (Honors), Chulalongkorn University, 1959 M.S., University of New Hampshire, 1961 A THESIS Submitted to the University of New Hampshire In Partial Fulfillment of The Requirements for the Degree of Doctor of Philosophy Graduate School Department of Zoology June, 1964 This thesis has been examined and approved. May 2 2, 1 964. Date An Abstract of VARIATION IN GROWTH PATTERN IN THE SAND DOLLAR, ECHINARACHNIUS PARMA, (LAMARCK) This study deals with Echinarachnius parma, the common sand dollar of the New England coast. Some problems concerning taxonomy and classification of this species are considered. -
Early Permian Palaeofloras from Southern Brazilian Gondwana: a Palaeoclimatic Approach
Revista Brasileira de Geociências 30(3):486-490, setembro de 2000 EARLY PERMIAN PALAEOFLORAS FROM SOUTHERN BRAZILIAN GONDWANA: A PALAEOCLIMATIC APPROACH MARGOT GUERRA-SOMMER AND MIRIAM CAZZULO-KLEPZIG ABSTRACT In evaluating the parameters supplied by the taphofloras from different sedimentary facies in the Early Permian sedimentary sequences of the southern part of the Paraná basin, Brazil, it has become evident that the palaeofloristic evolution was related to palaeoecological and palaeoclimatic evolution. The homogeneous composition of Early Permian floral assemblages, which are characterized mainly by herbaceous to shrub-like plants considered to be relicts from the rigorous climate of an ice age (e.g. Botrychiopsis plantiana) suggest the persistence of the cold climate. The dominance of Rubidgea and Gangamopteris leaves with palmate venation associated with glossopterids with penate venation seems to indicate a gradual warming of climate. In roof-shales of coalbearing strata pinnate glossopterids related to Glossopteris are common, while Gangamopteris and Rubidgea (palmate forms) are poorly represented. The sudden enrichment of herbaceous articulates and filicoids fronds is characteristic of this stage and trunks of arborescents lycophytes become important elements. These antrocophilic paleofloras are characterized by typical elements of the "Glossopteris flora" associated to tree lycophytes and ferns communities. Therefore, the cool seasonal climate of Early Permian changed into the moist seasonal interval during the Artinskian-Kungurian. This climatic change was significant to the meso-hygrophitic to hygrophitic vegetation registered in roof-shale ferns of the Gondwana Southern Brazilian coalbearing strata. Keywords: roof-shale floras, Gondwana, Southern Brazil, Paraná basin, Glossopteris Flora INTRODUCTION The intracratonic Paraná basin, with a total area proposed by Milani et al. -
Morphology and Affinities of Glossopteris
MORPHOLOGY AND AFFINITIES OF GLOSSOPTERIS K. R. SURANGE & SHALLA CHANDRA Birbal Sahni Institute of Palaeobotany, Lucknow-226007, India ABSTRACT Reproductive organs of glossopterids, viz., Eretmonia, Glossotlleea, Kendos• trobus, Lidgettonia, Partlla, Russangea, M ooia, Rigbya, Denkania, Venustostrobus, Plumsteadiostrobus, Dietyopteridium and Jambadostrobus are briefly described. Their morphology and affinities are discussed. In the Permian of the southern hemis• phere atleast two distinct orders of gymnosperms, viz., Pteridospermales and Glos• sopteridales were dominating the landscape. genera bore sporangia terminally on ultimate GLOSSOPTERISAustralia were firstleavesrecordedfrom Indiaby Brong•and branches whereas the third genus bore niart in 1828. From 1845 to 1905, sporangia crowded on a cylindrical axis. a number of new species of Glossopteris were discovered from different continents of Eretmonia Du Toit Gondwanaland. From 1905 to 1950 there PI. 1. figs. 3,4; PI. 2, fig. 2; PI. 3, figs. 2,3 were only a few records, but from 1950 onwards Glossopteris again attracted the Fertile scale leaves of Eretmonia (see attention of many palaeobotanists. At first, Chandra & Surange, 1977, text-fig. 1) are of Glos90pteris were regarded as ferns but different shapes and sizes and five species later they turned out to be seed .plants. have been recognized on this basis. The In recent years our knowledge of the fertile bracts are ovate (E. ovoides Surange reproductive structures of glossopterids has & Chandra, 1974), spathulate with acute increased to such an extent that one can apex (E. hingridaensis Surange & Mahesh• get some idea as to what type of plants wari, 1970), triangular (E. emarginata they were. Chandra & Surange, 1977), diamond-shaped (E. utkalensis Surange & Maheshwari, 1970) HABIT and orbicular (E. -
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.