Flora of the Late Triassic
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Gymnosperm Foliage from the Upper Triassic of Lunz, Lower Austria: an Annotated Check List and Identification Key
Geo.Alp, Vol. 7, S. 19–38, 2010 GYMNOSPERM FOLIAGE FROM THE UPPER TRIASSIC OF LUNZ, LOWER AUSTRIA: AN ANNOTATED CHECK LIST AND IDENTIFICATION KEY Christian Pott1 & Michael Krings2 With 7 figures and 1 table 1 Naturhistoriska riksmuseet, Sektionen för paleobotanik, Box 50007, SE-104 05 Stockholm, Sweden; [email protected] 2 Department für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Ludwig-Maximilians-Universität, and Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, 80333 München, Germany; [email protected] Abstract The famous Lunz flora from Lower Austria is one of the richest and most diverse Late Triassic floras of the Northern He- misphere. The historical outcrops (mainly coal mines) are no longer accessible, but showy fossils can still be collected from natural exposures around the town of Lunz-am-See and from several of the old spoil tips. This paper presents an annotated check list with characterisations of all currently recognised gymnosperm foliage taxa in the Lunz flora. The descriptions are exemplified by illustrations of typical specimens and diagnostic features of the leaf morphology and epidermal anatomy. Moreover, a simple identification key for the taxa based on macromorphological features is provided that facilitates identification of newly collected specimens. 1. Introduction The Carnian (Late Triassic) flora from Lunz in Lo- ments (i.e. reproductive structures) among the fossils wer Austria is one of only a few well-preserved flo- (see e.g., Krasser, 1917, 1919; Kräusel, 1948, 1949, ras from the Alpine Triassic (Cleal, 1993; Dobruskina, 1953; Pott et al., 2010), the most striking feature of 1998). -
The Origin and Early Evolution of Vascular Plant Shoots and Leaves Rstb.Royalsocietypublishing.Org C
Downloaded from http://rstb.royalsocietypublishing.org/ on January 22, 2018 The origin and early evolution of vascular plant shoots and leaves rstb.royalsocietypublishing.org C. Jill Harrison 1 and Jennifer L. Morris 2 1School of Biological Sciences, and 2School of Earth Sciences, University of Bristol, 24 Tyndall Avenue, Bristol BS8 1TQ, UK Review CJH, 0000-0002-5228-600X; JLM, 0000-0002-7453-3841 Cite this article: Harrison CJ, Morris JL. 2017 The morphology of plant fossils from the Rhynie chert has generated long- standing questions about vascular plant shoot and leaf evolution, for The origin and early evolution of vascular plant instance, which morphologies were ancestral within land plants, when did shoots and leaves. Phil. Trans. R. Soc. B 373 : vascular plants first arise and did leaves have multiple evolutionary origins? 20160496. Recent advances combining insights from molecular phylogeny, palaeobotany http://dx.doi.org/10.1098/rstb.2016.0496 and evo–devo research address these questions and suggest the sequence of morphological innovation during vascular plant shoot and leaf evolution. The evidence pinpoints testable developmental and genetic hypotheses relat- Accepted: 11 August 2017 ing to the origin of branching and indeterminate shoot architectures prior to the evolution of leaves, and demonstrates underestimation of polyphyly in One contribution of 18 to a discussion meeting the evolution of leaves from branching forms in ‘telome theory’ hypotheses issue ‘The Rhynie cherts: our earliest terrestrial of leaf evolution. This review discusses fossil, developmental and genetic ecosystem revisited’. evidence relating to the evolution of vascular plant shoots and leaves in a phylogenetic framework. This article is part of a discussion meeting issue ‘The Rhynie cherts: our Subject Areas: earliest terrestrial ecosystem revisited’. -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Asterotheca Meriani (Brongn.) Stur and Its Spores from the Upper Triassic of Lunz (Austria)
ASTEROTHECA MERIANI (BRONGN.) STUR AND ITS SPORES FROM THE UPPER TRIASSIC OF LUNZ (AUSTRIA) D. C. BHARDWAJ & HARI PALL SINGH Birbal Sahni Institute of Palaeobotany, Lucknow ABSTRACT Horizon-Lunzer Schichten, UpperTriassic. This paper deals with the morphological study of The compressions were examined under A ste"otheca rneriani (Brongn.) Stur, a species of strong reflected light. The transfer prepara ferns from the Upper Triassic of Lunz, Austria. tions were made following Walton's transfer well preserved in the form of carbonaceous crust on the shales. The frond is bipinnate. Pinnules method ( WALTON, 1923 ) and studied under are longer than broad and the venation is typically strong reflected ligh t. The synangia were of Pecopteris type. Synangia are circular, borne picked up with the help of a needle from the intramarginally, comprising 4 sessile sporangia in transfers and treated separately with com close cohesion at the anterior end but slightly apart at the apical end. Spores are bilateral, circular to mercial nitric acid for about 24 hours. Then oval in polar view and indisputably show a longi the oxidized products were washed with tudinal ( monolete) slit, slightly bent in the middle. water and followed by a treatment with 10 The spore exine is thick and finely granulose. per cent potassium hydroxide solution for 4 hours. After several washings with water, INTRODUCTION till the residue was free from alkali, the spores thus recovered were mounted in OR the last few decades the study of Canada balsam. For the recovery of the plant microfossils, especially the spores cuticles, the organic crust in the transfers F and pollen grains from the sedimen was separated with the help of xylol and tary strata such as shales and coals is being passed through alcohol to bring it to water. -
Pterosaurs Flight in the Age of Dinosaurs Now Open 2 News at the Museum 3
Member Magazine Spring 2014 Vol. 39 No. 2 Pterosaurs Flight in the Age of Dinosaurs now open 2 News at the Museum 3 From the After an unseasonably cold, snowy winter, will work to identify items from your collection, More than 540,000 Marine Fossils the Museum is pleased to offer a number of while also displaying intriguing specimens from President springtime opportunities to awaken the inner the Museum’s own world-renowned collections. Added to Paleontology Collection naturalist in us all. This is the time of year when Of course, fieldwork and collecting have Ellen V. Futter Museum scientists prepare for the summer been hallmarks of the Museum’s work since Collections at a Glance field season as they continue to pursue new the institution’s founding. What has changed, discoveries in their fields. It’s also when Museum however, is technology. With a nod to the many Over nearly 150 years of acquisitions and Members and visitors can learn about their ways that technology is amplifying how scientific fieldwork, the Museum has amassed preeminent own discoveries during the annual Identification investigations are done, this year, ID Day visitors collections that form an irreplaceable record Day in Theodore Roosevelt Memorial Hall. can learn how scientists use digital fabrication of life on Earth. Today, 21st-century tools— Held this year on May 10, Identification Day to aid their research and have a chance to sophisticated imaging techniques, genomic invites visitors to bring their own backyard finds have their own objects scanned and printed on analyses, programs to analyze ever-growing and curios for identification by Museum scientists. -
Cuticle Ultrastructure in Brachyphyllum Garciarum Sp. Nov (Lower Cretaceous, Argentina) Reveals Its Araucarian Affinity
Review of Palaeobotany and Palynology 269 (2019) 104–128 Contents lists available at ScienceDirect Review of Palaeobotany and Palynology journal homepage: www.elsevier.com/locate/revpalbo Cuticle ultrastructure in Brachyphyllum garciarum sp. nov (Lower Cretaceous, Argentina) reveals its araucarian affinity Martin A. Carrizo a,⁎, Maiten A. Lafuente Diaz a, Georgina M. Del Fueyo a, Gaëtan Guignard b a División Paleobotánica, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, CONICET. Av. Ángel Gallardo 470, 1405 Buenos Aires, Argentina b Université Lyon 1, CNRS, UMR 5023 LEHNA, 7-9 rue Raphaël Dubois, Villeurbanne cedex F-69622, Lyon, France article info abstract Article history: A detailed and extensive study of a new species, Brachyphyllum garciarum sp. nov., was carried out through the Received 28 February 2019 analysis of the gross morphology and the cuticle fine details, structure and ultrastructure characters of its leaves Received in revised form 14 June 2019 using light microscope and scanning and transmission electron microscope. The fossils consist of compressions of Accepted 19 June 2019 incomplete twigs with well-preserved cuticle, collected from pelitic levels of the Springhill Formation (lower Hauterivian/lower Barremian) at the Río Correntoso locality in the Santa Cruz province, Argentina. The twigs Keywords: have adpressed scale-like leaves spirally disposed. Leaves have a rhomboidal to pyramidal shape, a width and Foliar cuticle length always in a 1:1 ratio, margin entire and apex mostly rounded. Leaves are amphistomatic with stomatal ap- Ultrastructure paratuses occurring in groups of narrow-wedge shape along the leaf axis. Stomatal apparatuses are close to each Taxonomy other with subsidiary cells in contact; the guard cells are sunken, with marked polar extensions and thickened Brachyphyllum mouth. -
Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia Emily Simpson East Tennessee State University
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2019 Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia Emily Simpson East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Paleontology Commons Recommended Citation Simpson, Emily, "Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia" (2019). Electronic Theses and Dissertations. Paper 3590. https://dc.etsu.edu/etd/3590 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia ________________________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences with a concentration in Paleontology _______________________________ by Emily Michelle Bruff Simpson May 2019 ________________________________ Dr. Chris Widga, Chair Dr. Blaine W. Schubert Dr. Andrew Joyner Key Words: Paleoecology, land-use, grassy balds, stable isotope ecology, Whitetop Mountain ABSTRACT Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia by Emily Michelle Bruff Simpson Land-use, feeding habits, and response to seasonality by Quaternary megaherbivores in Saltville, Virginia, is poorly understood. Stable isotope analyses of serially sampled Bootherium and Equus enamel from Saltville were used to explore seasonally calibrated (δ18O) patterns in megaherbivore diet (δ13C) and land-use (87Sr/86Sr). -
Palaeogeograph Y, Palaeoclimatology, Palaeoecology , 17(1975): 157--172 © Elsevier Scientific Publishing Company, Amsterdam -- Printed in the Netherlands
Palaeogeograph y, Palaeoclimatology, Palaeoecology , 17(1975): 157--172 © Elsevier Scientific Publishing Company, Amsterdam -- Printed in The Netherlands CLIMATIC CHANGES IN EASTERN ASIA AS INDICATED BY FOSSIL FLORAS. II. LATE CRETACEOUS AND DANIAN V. A. KRASSILOV Institute of Biology and Pedology, Far-Eastern Scientific Centre, U.S.S.R. Academy of Sciences, Vladivostok (U.S.S.R.) (Received June 17, 1974; accepted for publication November 11, 1974) ABSTRACT Krassilov, V. A., 1975. Climatic changes in Eastern Asia as indicated by fossil floras. II. Late Cretaceous and Danian. Palaeogeogr., Palaeoclimatol., Palaeoecol., 17:157--172. Four Late Cretaceous phytoclimatic zones -- subtropical, warm--temperate, temperate and boreal -- are recognized in the Northern Hemisphere. Warm--temperate vegetation terminates at North Sakhalin and Vancouver Island. Floras of various phytoclimatic zones display parallel evolution in response to climatic changes, i.e., a temperature rise up to the Campanian interrupted by minor Coniacian cooling, and subsequent deterioration of cli- mate culminating in the Late Danian. Cooling episodes were accompanied by expansions of dicotyledons with platanoid leaves, whereas the entire-margined leaf proportion increased during climatic optima. The floristic succession was also influenced by tectonic events, such as orogenic and volcanic activity which commenced in Late Cenomanian--Turonian times. Major replacements of ecological dominants occurred at the Maastrichtian/Danian and Early/Late Danian boundaries. INTRODUCTION The principal approaches to the climatic interpretation of fossil floras have been outlined in my preceding paper (Krassilov, 1973a). So far as Late Creta- ceous floras are concerned, extrapolation (i.e. inferences from tolerance ranges of allied modern taxa) is gaining in importance and the entire/non-entire leaf type ratio is no less expressive than it is in Tertiary floras. -
Seed Plant Phylogeny: Demise of the Anthophyte Hypothesis? Michael J
bb10c06.qxd 02/29/2000 04:18 Page R106 R106 Dispatch Seed plant phylogeny: Demise of the anthophyte hypothesis? Michael J. Donoghue* and James A. Doyle† Recent molecular phylogenetic studies indicate, The first suggestions that Gnetales are related to surprisingly, that Gnetales are related to conifers, or angiosperms were based on several obvious morphological even derived from them, and that no other extant seed similarities — vessels in the wood, net-veined leaves in plants are closely related to angiosperms. Are these Gnetum, and reproductive organs made up of simple, results believable? Is this a clash between molecules unisexual, flower-like structures, which some considered and morphology? evolutionary precursors of the flowers of wind-pollinated Amentiferae, but others viewed as being reduced from Addresses: *Harvard University Herbaria, 22 Divinity Avenue, Cambridge, Massachusetts 02138, USA. †Section of Evolution and more complex flowers in the common ancestor of Ecology, University of California, Davis, California 95616, USA. angiosperms, Gnetales and Mesozoic Bennettitales [1]. E-mail: [email protected] These ideas went into eclipse with evidence that simple [email protected] flowers really are a derived, rather than primitive, feature Current Biology 2000, 10:R106–R109 of the Amentiferae, and that vessels arose independently in angiosperms and Gnetales. Vessels in angiosperms 0960-9822/00/$ – see front matter seem derived from tracheids with scalariform pits, whereas © 2000 Elsevier Science Ltd. All rights reserved. in Gnetales they resemble tracheids with circular bor- dered pits, as in conifers. Gnetales are also like conifers in These are exciting times for those interested in plant lacking scalariform pitting in the primary xylem, and in evolution. -
JUDD W.S. Et. Al. (2002) Plant Systematics: a Phylogenetic Approach. Chapter 7. an Overview of Green
UNCORRECTED PAGE PROOFS An Overview of Green Plant Phylogeny he word plant is commonly used to refer to any auto- trophic eukaryotic organism capable of converting light energy into chemical energy via the process of photosynthe- sis. More specifically, these organisms produce carbohydrates from carbon dioxide and water in the presence of chlorophyll inside of organelles called chloroplasts. Sometimes the term plant is extended to include autotrophic prokaryotic forms, especially the (eu)bacterial lineage known as the cyanobacteria (or blue- green algae). Many traditional botany textbooks even include the fungi, which differ dramatically in being heterotrophic eukaryotic organisms that enzymatically break down living or dead organic material and then absorb the simpler products. Fungi appear to be more closely related to animals, another lineage of heterotrophs characterized by eating other organisms and digesting them inter- nally. In this chapter we first briefly discuss the origin and evolution of several separately evolved plant lineages, both to acquaint you with these important branches of the tree of life and to help put the green plant lineage in broad phylogenetic perspective. We then focus attention on the evolution of green plants, emphasizing sev- eral critical transitions. Specifically, we concentrate on the origins of land plants (embryophytes), of vascular plants (tracheophytes), of 1 UNCORRECTED PAGE PROOFS 2 CHAPTER SEVEN seed plants (spermatophytes), and of flowering plants dons.” In some cases it is possible to abandon such (angiosperms). names entirely, but in others it is tempting to retain Although knowledge of fossil plants is critical to a them, either as common names for certain forms of orga- deep understanding of each of these shifts and some key nization (e.g., the “bryophytic” life cycle), or to refer to a fossils are mentioned, much of our discussion focuses on clade (e.g., applying “gymnosperms” to a hypothesized extant groups. -
Paleontologia Em Destaque
Paleontologia em Destaque Boletim Informativo da SBP Ano 34, n° 72, 2019 · ISSN 1807-2550 PALEO, SBPV e SBPI 2018 RELATOS E RESUMOS SOCIEDADE BRASILEIRA DE PALEONTOLOGIA Presidente: Dr. Renato Pirani Ghilardi (UNESP/Bauru) Vice-Presidente: Dr. Annie Schmaltz Hsiou (USP/Ribeirão Preto) 1ª Secretária: Dra. Taissa Rodrigues Marques da Silva (UFES) 2º Secretário: Dr. Rodrigo Miloni Santucci (UnB) 1º Tesoureiro: Me. Marcos César Bissaro Júnior (USP/Ribeirão Preto) 2º Tesoureiro: Dr. Átila Augusto Stock da Rosa (UFSM) Diretor de Publicações: Dr. Sandro Marcelo Scheffler (UFRJ) P a l e o n t o l o g i a e m D e s t a q u e Boletim Informativo da Sociedade Brasileira de Paleontologia Ano 34, n° 72, setembro/2019 · ISSN 1807-2550 Web: http://www.sbpbrasil.org/, Editores: Sandro Marcelo Scheffler, Maria Izabel Lima de Manes Agradecimentos: Aos organizadores dos eventos científicos Capa: Palácio do Museu Nacional após a instalação do telhado provisório. Foto: Sandro Scheffler. 1. Paleontologia 2. Paleobiologia 3. Geociências Distribuído sob a Licença de Atribuição Creative Commons. EDITORIAL As reuniões PALEO são encontros regionais chancelados pela Sociedade Brasileira de Paleontologia (SBP) que têm por objetivo a comunhão entre estudantes de graduação e pós- graduação, pesquisadores e interessados na área de Paleontologia. Estes eventos possuem periodicidade anual e ocorrem em várias regiões do Brasil. Iniciadas em 1999, como uma reunião informal da comunidade de paleontólogos, possuem desde então as seguintes distribuições, de acordo com a região de abrangência: Paleo RJ/ES, Paleo MG, Paleo SP, Paleo RS, Paleo PR/SC, Paleo Nordeste e Paleo Norte. -
Evolution of the Female Conifer Cone Fossils, Morphology and Phylogenetics
DEPARTMENT OF BIOLOGICAL AND ENVIRONMENTAL SCIENCES EVOLUTION OF THE FEMALE CONIFER CONE FOSSILS, MORPHOLOGY AND PHYLOGENETICS Daniel Bäck Degree project for Bachelor of Science with a major in Biology BIO602, Biologi: Examensarbete – kandidatexamen, 15 hp First cycle Semester/year: Spring 2020 Supervisor: Åslög Dahl, Department of Biological and Environmental Sciences Examiner: Claes Persson, Department of Biological and Environmental Sciences Front page: Abies koreana (immature seed cones), Gothenburg Botanical Garden, Sweden Table of contents 1 Abstract ............................................................................................................................... 2 2 Introduction ......................................................................................................................... 3 2.1 Brief history of Florin’s research ............................................................................... 3 2.2 Progress in conifer phylogenetics .............................................................................. 4 3 Aims .................................................................................................................................... 4 4 Materials and Methods ........................................................................................................ 4 4.1 Literature: ................................................................................................................... 4 4.2 RStudio: .....................................................................................................................