Morphology and Affinities of Glossopteris
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Plant Fossils and Gondwana Flora
UNIT 12 PLANT FOSSILS AND GONDWANA FLORA Structure_____________________________________________________ 12.1 Introduction Vertebraria Expected Learning Outcomes Thinnfeldia 12.2 Plant Fossils Sigillaria Definition Nilssonia Classification Williamsonia Modes of Preservation Ptilophyllum Significance 12.5 Activity 12.3 Gondwana Flora of India 12.6 Summary 12.4 Descriptions of some Plant 12.7 Terminal Questions Fossils 12.8 References Glossopteris 12.9 Further/Suggested Readings Gangamopteris 12.10 Answers 12.1 INTRODUCTION The animals, plants and micro-organisms are the three main life forms surviving today. Even their fossilised remains are found in rocks that tell us about their past history. The animals comprise invertebrates and vertebrates. In Block 4, you will read about the invertebrates and their geological history that began in the latest Precambrian time. You also read about the microfossils in Unit 10 that too have a long geological record beginning from Precambrian onwards. In Unit 11, you read the evolutionary history of one of the vertebrate groups i.e., horse. In this unit, you will read the plant fossils and the Gondwana flora of India. Introduction to Palaeontology Block……………………………………………………………………………………………….….............….…........ 3 Like the kingdom Animalia, plants also form a separate kingdom known as the Plantae. It is thought that plants appeared first in the Precambrian, but their fossil record is poor. It is also proposed that earliest plants were aquatic and during the Ordovician period a transition from water to land took place that gave rise to non-vascular land plants. However, it was during the Silurian period, that the vascular plants appeared first on the land. The flowering plants emerged rather recently, during the Cretaceous period. -
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. -
Three New Fern Fronds from the Glossopteris Flora of India
THREE NEW FERN FRONDS FROM THE GLOSSOPTERIS FLORA OF INDIA P. K. MAITHY Birbal Sahni Institute of Palaeobotany, Lucknow-226007 ABSTRACT of dates, Damudopteris becomes synonym A new species of Neomariopteris and a new to Neomariopteris, because the former form species of Dichotomopteris is recorded. In addition has been published one month later. to this a new genus Santhalea is instituted. INTRODUCTION Neomariopteris khanU sp. novo Diagnosis - Fronds large, at least tri• the ferns from the Lower Gondwanas knowledge on the morphology of pinnate; catadromic, rachis winged, secon• OURof India has been advanced consider• dary rachis broad, emerge alternately at an ably from the recent work of Maithy (1974a, angle of ± 60°; pinnae lanceolate; attached 1974b, 1975), Pant and Misra (1976) and alternate, sub-opposite or opposite from Pant and Khare (1974). Recently Maithy secondary rachis; lateral pinnules ovate, has revised the Lower Gondwana ferns from 1'0 cm long and 0'4 mm broad at base, i.e. India. On the basis of his revision, he has the length and breadth ratio of the pinnules instituted two new genera Neomariopteris is 2·5: I, lateral pinnules alternately and Dichotomopteris and an unrecorded form arranged, standing at right angles to rachis, Dizeugotheca. Pant and Khare (1974) and decurrent, attached by broad bases, lateral Pant and Misra (1976) have reported two fusion of two pinnules margin is ± 1/4 length new genera Damudopteris and Asansolia from of the pinnules from the base; apex acute; the Raniganj Coalfield. margin entire; both the margins show out• The present paper deals with three new ward curvature; terminal pinnules smaller fern fronds collected recently from than lateral pinnules, triangular in shape. -
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. -
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. -
The Architecture of Permian Glossopterid Ovuliferous Reproductive Organs
Alcheringa: An Australasian Journal of Palaeontology ISSN: 0311-5518 (Print) 1752-0754 (Online) Journal homepage: https://www.tandfonline.com/loi/talc20 The architecture of Permian glossopterid ovuliferous reproductive organs Stephen Mcloughlin & Rose Prevec To cite this article: Stephen Mcloughlin & Rose Prevec (2019) The architecture of Permian glossopterid ovuliferous reproductive organs, Alcheringa: An Australasian Journal of Palaeontology, 43:4, 480-510, DOI: 10.1080/03115518.2019.1659852 To link to this article: https://doi.org/10.1080/03115518.2019.1659852 Published online: 01 Oct 2019. Submit your article to this journal Article views: 138 View related articles View Crossmark data Citing articles: 1 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=talc20 The architecture of Permian glossopterid ovuliferous reproductive organs STEPHEN MCLOUGHLIN and ROSE PREVEC MCLOUGHLIN,S.&PREVEC, R. 20 September 2019. The architecture of Permian glossopterid ovuliferous reproductive organs. Alcheringa 43, 480–510. ISSN 0311-5518 A historical account of research on glossopterid ovuliferous reproductive structures reveals starkly contrasting interpretations of their architecture and homologies from the earliest investigations. The diversity of interpretations has led to the establishment of a multitude of genera for these fossil organs, many of the taxa being synonymous. We identify a need for taxonomic revision of these genera to clearly demarcate taxa before they can be used effectively as palaeobiogeographic or biostratigraphic indices. Our assessment of fructification features based on extensive studies of adpression and permineralized fossils reveals that many of the character states for glossopterids used in previous phylogenetic analyses are erroneous. -
Plant Evolution
Conquering the land The rise of plants Ordovician Spores Algae (algal mats) Green freshwater algae Bacteria Fungae Bryophytes Moses? Liverworts? Little body fossil evidence Silurian Wenlock Stage 423-428mya Psilophytes Rhyniopsidsa important later in early Devonian Cooksonia Rhynia Branching stems, flattened sporangia at tips No leaves, no roots short 30 cms rhizoids Zosterophylls Early stem group of Lycopodiophytes Ancestors of Class Lycopsida (clubmosses) Prevalent in Devonian Spores at tips and on branches Lycopsids (?) Baragwanathia with microphylls in Australia Zosterophylls Silurian Cooksonia Development of Soil Fungae Bacteria Algae Organic matter Arthropods and annelids Change in erosion Change in CO2 Devonian Devonian Early Devonian simple structure Rhynie Chert (Rhyniophytes) Trimerophytes First with main shoot Give rise to Ferns and Progymnosperms Up to 3m tall Animal life (mainly arthropods) Late Devonian Forests First true wood (lignin) Forest structure develops (stories) Sphenopsids (Calamites) Lycopsids (Lepidodendron) Seed Ferns (Pteridosperm) Progymnosperm Archaeopteris Cladoxylopsid First vertebrates present Upper Devonian Lycopsida 374-360 mya Leaves and roots differentiated Most ancient with living relatives Megaphylls branching in on plane Photosynthetic webbing Shrub size vertical growth limited (weak) Lateral (secondary) growth (woody) Development of roots Homosporous Heterosporous Upper Devonian Calamites (Sphenopsid) Horestail Sphenophyta (Calamites-Annularia) Devonian Archaeopteris Ur. Devonian - Lr. Carboniferous -
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. -
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. -
1 Relationships of Angiosperms To
Relationships of Angiosperms to 1 Other Seed Plants Seed plants are of fundamental importance both evolution- all gymnosperms (living and extinct) together are not arily and ecologically. They dominate terrestrial landscapes, monophyletic. Importantly, several fossil lineages, Cayto- and the seed has played a central role in agriculture and hu- niales, Bennettitales, Pentoxylales, and Glossopteridales man history. There are fi ve extant lineages of seed plants: (glossopterids), have been proposed as putative close rela- angiosperms, cycads, conifers, gnetophytes, and Ginkgo. tives of the angiosperms based on phylogenetic analyses These fi ve groups have usually been treated as distinct (e.g., Crane 1985; Rothwell and Serbet 1994; reviewed in phyla — Magnoliophyta (or Anthophyta), Cycadophyta, Doyle 2006, 2008, 2012; Friis et al. 2011). These fossil lin- Co ni fe ro phyta, Gnetophyta, and Ginkgophyta, respec- eages, sometimes referred to as the para-angiophytes, will tively. Cantino et al. (2007) used the following “rank- free” therefore be covered in more detail later in this chapter. An- names (see Chapter 12): Angiospermae, Cycadophyta, other fossil lineage, the corystosperms, has been proposed Coniferae, Gnetophyta, and Ginkgo. Of these, the angio- as a possible angiosperm ancestor as part of the “mostly sperms are by far the most diverse, with ~14,000 genera male hypothesis” (Frohlich and Parker 2000), but as re- and perhaps as many as 350,000 (The Plant List 2010) to viewed here, corystosperms usually do not appear as close 400,000 (Govaerts 2001) species. The conifers, with ap- angiosperm relatives in phylogenetic trees. proximately 70 genera and nearly 600 species, are the sec- The seed plants represent an ancient radiation, with ond largest group of living seed plants.