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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). -
IGCP 632, the Jurassic–Cretaceous Transition In
IGCP 79 IGCP 632, The Jurassic–Cretaceous transition in North Eastern China (western Liaoning and Inner Mongolia): An IGCP meeting and field excursion on the conti- nental Jurassic Jingeng Sha1, Yanhong Pan1, Enpu Gong2, and Vivi Vajda3* 1 LPS, Nanjing Institute of Geology & Paleontology, Nanjing 210008, China 2 Northeastern University, Shenyang 110004, China 3 Swedish Museum of Natural History, Frescativägen 40, 114 18 Stockholm, Sweden, *Corresponding author, E-mail: [email protected] Exposures of strata spanning the Jurassic–Cretaceous boundary been discovered. However, the correlation of the various lithostrati- occur within several basins in western Liaoning and adjacent Inner graphic units in this area is complicated due to patchy exposures and Mongolia. These continental successions host world-renowned plant the scarcity of radiometric constraints, which pose a challenge to researchers and animal fossils including feathered dinosaurs and the oldest flow- working on these deposits. ering plant, Archaeofructus. The first feathered dinosaurs from north- To understand the stratigraphy and context of the Jurassic–Creta- eastern China where found about 20 years ago and created a major ceous biota in Liaoning province, the second IGCP-632 symposium impact in science and the media. Since then, many new specimens have was organized in Liaoning, including a two-day presentation (Sep- Figure 1. (A) Sketch map over the field excursion area in north-eastern China. (B) enlargement of the field region showing the localities of the field stops. Episodes Vol. 40, no. 1 80 intracontinental orogenic system, the Yanshan Movement, and creating a new basin-range system in east Asia. Vivi Vajda presented new results (Peterffy et al., 2015; Vajda et al., 2016) where she compre- hensively analyzed the end-Triassic mass extinc- tion and aftermath and its causal mechanisms, particularly stressing the affects of Jurassic vol- canism in disrupting the major ecosystems but also its importance for fossilization. -
The Jurassic Fossil Wood Diversity from Western Liaoning, NE China
Jiang et al. Journal of Palaeogeography (2019) 8:1 https://doi.org/10.1186/s42501-018-0018-y Journal of Palaeogeography RESEARCH Open Access The Jurassic fossil wood diversity from western Liaoning, NE China Zi-Kun Jiang1,2, Yong-Dong Wang2,3*, Ning Tian4,5, Ao-Wei Xie2,6, Wu Zhang7, Li-Qin Li2 and Min Huang1 Abstract Western Liaoning is a unique region in China that bears diverse types of Jurassic plants, including leaves, fern rhizomes, and wood, providing significant proxy for vegetation and palaeoenvironment reconstruction of the well-known Yanliao Flora in East Asia. In particular, the silicified wood is very abundant in the fossil Lagerstätte of the Jurassic Tiaojishan Formation in Beipiao, western Liaoning. Previous and recent systematic investigations documented a high diversity of the Jurassic wood assemblages. These assemblages are dominated by conifers, followed by cycads and ginkgoaleans. In total, about 30 species belonging to 21 genera of fossil wood have been recorded so far, which are represented by Cycadopsida, Ginkgopsida, Coniferopsida, and Gymnospermae incertae sedis. The evolutionary implications of several distinctive fossil wood taxa as well as palaeoclimate implications are summarized based on their anatomical structures and growth ring patterns. This work approaches the vegetation development and evolutionary significances of the wood taxa and their relatives, and provides clues for the further understanding of the diversity of the Jurassic Yanliao Flora in East Asia. Keywords: Fossil wood, Diversity, Evolution, Tiaojishan Formation, Jurassic 1 Introduction 2004;Wangetal.,2009). Among these localities, western Fossil floras are a significant record for the vegetation Liaoning is a well-known fossil Lagerstätte with diverse and for the palaeoenvironment reconstructions of the and well-preserved fossil plant foliages and wood (Zhang Mesozoic. -
Plant Mobility in the Mesozoic Disseminule Dispersal Strategies Of
Palaeogeography, Palaeoclimatology, Palaeoecology 515 (2019) 47–69 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Plant mobility in the Mesozoic: Disseminule dispersal strategies of Chinese and Australian Middle Jurassic to Early Cretaceous plants T ⁎ Stephen McLoughlina, , Christian Potta,b a Palaeobiology Department, Swedish Museum of Natural History, Box 50007, 104 05 Stockholm, Sweden b LWL - Museum für Naturkunde, Westfälisches Landesmuseum mit Planetarium, Sentruper Straße 285, D-48161 Münster, Germany ARTICLE INFO ABSTRACT Keywords: Four upper Middle Jurassic to Lower Cretaceous lacustrine Lagerstätten in China and Australia (the Daohugou, Seed dispersal Talbragar, Jehol, and Koonwarra biotas) offer glimpses into the representation of plant disseminule strategies Zoochory during that phase of Earth history in which flowering plants, birds, mammals, and modern insect faunas began to Anemochory diversify. No seed or foliage species is shared between the Northern and Southern Hemisphere fossil sites and Hydrochory only a few species are shared between the Jurassic and Cretaceous assemblages in the respective regions. Free- Angiosperms sporing plants, including a broad range of bryophytes, are major components of the studied assemblages and Conifers attest to similar moist growth habitats adjacent to all four preservational sites. Both simple unadorned seeds and winged seeds constitute significant proportions of the disseminule diversity in each assemblage. Anemochory, evidenced by the development of seed wings or a pappus, remained a key seed dispersal strategy through the studied interval. Despite the rise of feathered birds and fur-covered mammals, evidence for epizoochory is minimal in the studied assemblages. Those Early Cretaceous seeds or detached reproductive structures bearing spines were probably adapted for anchoring to aquatic debris or to soft lacustrine substrates. -
Nomenclatural Notes on Some Ginkgoalean Fossil Plants from China
植 物 分 类 学 报 45 (6): 880–883(2007) doi:10.1360/aps07015 Acta Phytotaxonomica Sinica http://www.plantsystematics.com Nomenclatural notes on some ginkgoalean fossil plants from China WU Xiang-Wu ZHOU Zhi-Yan* WANG Yong-Dong (Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing 210008, China) Abstract Two morphotaxa of ginkgoalean fossil plants from China bear illegitimate specific names, viz. Sphenobaiera biloba S. N. Feng (1977) and S. rugata Z. Q. Wang (Dec. 1984), that are heterotypic later homonyms of S. biloba Prynada (1938) and S.? rugata Z. Y. Zhou (Mar. 1984) respectively. Under Art. 53.1 and 7.3 of the Vienna Code, new specific names are proposed to supersede these illegitimate names. Two other names, viz. Baiera ziguiensis F. S. Meng (1987) and Ginkgoites elegans S. Yang, B. N. Sun & G. L. Shen (1988), were not validly published, because no nomenclatural type was definitely indicated. New species are instituted for the two morphotaxa here. Although the specific name Ginkgoites elegans Cao (1992) was antedated by Ginkgoites elegans S. Yang, B. N. Sun & G. L. Shen (1988), it still remains available for use, as the latter name has no status under the Vienna Code (Art. 12, 37) and thus no priority over Ginkgoites elegans Z. Y. Cao. Key words Ginkgoales, Ginkgoites, Baiera, Sphenobaiera, morphospecies, nomenclature. In compiling the Chinese record of fossil plants described since 1865, several illegitimate and/or not validly published names of ginkgoalean morphotaxa were found. They are either later homonyms or were published without a definite indication of the type (Art. -
A Translation of the Linnaean Dissertation the Invisible World
BJHS 49(3): 353–382, September 2016. © British Society for the History of Science 2016 doi:10.1017/S0007087416000637 A translation of the Linnaean dissertation The Invisible World JANIS ANTONOVICS* AND JACOBUS KRITZINGER** Abstract. This study presents the first translation from Latin to English of the Linnaean disser- tation Mundus invisibilis or The Invisible World, submitted by Johannes Roos in 1769. The dissertation highlights Linnaeus’s conviction that infectious diseases could be transmitted by living organisms, too small to be seen. Biographies of Linnaeus often fail to mention that Linnaeus was correct in ascribing the cause of diseases such as measles, smallpox and syphilis to living organisms. The dissertation itself reviews the work of many microscopists, especially on zoophytes and insects, marvelling at the many unexpected discoveries. It then discusses and quotes at length the observations of Münchhausen suggesting that spores from fungi causing plant diseases germinate to produce animalcules, an observation that Linnaeus claimed to have confirmed. The dissertation then draws parallels between these findings and the conta- giousness of many human diseases, and urges further studies of this ‘invisible world’ since, as Roos avers, microscopic organisms may cause more destruction than occurs in all wars. Introduction Here we present the first translation from Latin to English of the Linnaean dissertation published in 1767 by Johannes Roos (1745–1828) entitled Dissertatio academica mundum invisibilem, breviter delineatura and republished by Carl Linnaeus (1707– 1778) several years later in the Amoenitates academicae under the title Mundus invisibi- lis or The Invisible World.1 Roos was a student of Linnaeus, and the dissertation is important in highlighting Linnaeus’s conviction that infectious diseases could be trans- mitted by living organisms. -
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. -
Dr. Sahanaj Jamil Associate Professor of Botany M.L.S.M. College, Darbhanga
Subject BOTANY Paper No V Paper Code BOT521 Topic Taxonomy and Diversity of Seed Plant: Gymnosperms & Angiosperms Dr. Sahanaj Jamil Associate Professor of Botany M.L.S.M. College, Darbhanga BOTANY PG SEMESTER – II, PAPER –V BOT521: Taxonomy and Diversity of seed plants UNIT- I BOTANY PG SEMESTER – II, PAPER –V BOT521: Taxonomy and Diversity of seed plants Classification of Gymnosperms. # Robert Brown (1827) for the first time recognized Gymnosperm as a group distinct from angiosperm due to the presence of naked ovules. BENTHAM and HOOKSER (1862-1883) consider them equivalent to dicotyledons and monocotyledons and placed between these two groups of angiosperm. They recognized three classes of gymnosperm, Cyacadaceae, coniferac and gnetaceae. Later ENGLER (1889) created a group Gnikgoales to accommodate the genus giankgo. Van Tieghem (1898) treated Gymnosperm as one of the two subdivision of spermatophyte. To accommodate the fossil members three more classes- Pteridospermae, Cordaitales, and Bennettitales where created. Coulter and chamberlain (1919), Engler and Prantl (1926), Rendle (1926) and other considered Gymnosperm as a division of spermatophyta, Phanerogamia or Embryoptyta and they further divided them into seven orders: - i) Cycadofilicales ii) Cycadales iii) Bennettitales iv) Ginkgoales v) Coniferales vi) Corditales vii) Gnetales On the basis of wood structure steward (1919) divided Gymnosperm into two classes: - i) Manoxylic ii) Pycnoxylic The various classification of Gymnosperm proposed by various workers are as follows: - i) Sahni (1920): - He recognized two sub-divison in gymnosperm: - a) Phylospermae b) Stachyospermae BOTANY PG SEMESTER – II, PAPER –V BOT521: Taxonomy and Diversity of seed plants ii) Classification proposed by chamber lain (1934): - He divided Gymnosperm into two divisions: - a) Cycadophyta b) Coniterophyta iii) Classification proposed by Tippo (1942):- He considered Gymnosperm as a class of the sub- phylum pteropsida and divided them into two sub classes:- a) Cycadophyta b) Coniferophyta iv) D. -
Ginkgoites Ticoensis</Italic>
Leaf Cuticle Anatomy and the Ultrastructure of Ginkgoites ticoensis Archang. from the Aptian of Patagonia Author(s): Georgina M. Del Fueyo, Gaëtan Guignard, Liliana Villar de Seoane, and Sergio Archangelsky Reviewed work(s): Source: International Journal of Plant Sciences, Vol. 174, No. 3, Special Issue: Conceptual Advances in Fossil Plant Biology Edited by Gar Rothwell and Ruth Stockey (March/April 2013), pp. 406-424 Published by: The University of Chicago Press Stable URL: http://www.jstor.org/stable/10.1086/668221 . Accessed: 15/03/2013 17:43 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 on Fri, 15 Mar 2013 17:43:56 PM All use subject to JSTOR Terms and Conditions Int. J. Plant Sci. 174(3):406–424. 2013. Ó 2013 by The University of Chicago. All rights reserved. 1058-5893/2013/17403-0013$15.00 DOI: 10.1086/668221 LEAF CUTICLE ANATOMY AND THE ULTRASTRUCTURE OF GINKGOITES TICOENSIS ARCHANG. FROM THE APTIAN OF PATAGONIA Georgina M. Del Fueyo,1,* Gae¨tan Guignard,y Liliana Villar de Seoane,* and Sergio Archangelsky* *Divisio´n Paleobota´nica, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia,’’ CONICET, Av. -
Taxonomic Utility of Old Names in Current Fungal Classification and Nomenclature: Conflicts, Confusion & Clarifications
Mycosphere 7 (11): 1622–1648 (2016) www.mycosphere.org ISSN 2077 7019 Article – special issue Doi 10.5943/mycosphere/7/11/2 Copyright © Guizhou Academy of Agricultural Sciences Taxonomic utility of old names in current fungal classification and nomenclature: Conflicts, confusion & clarifications Dayarathne MC1,2, Boonmee S1,2, Braun U7, Crous PW8, Daranagama DA1, Dissanayake AJ1,6, Ekanayaka H1,2, Jayawardena R1,6, Jones EBG10, Maharachchikumbura SSN5, Perera RH1, Phillips AJL9, Stadler M11, Thambugala KM1,3, Wanasinghe DN1,2, Zhao Q1,2, Hyde KD1,2, Jeewon R12* 1Center of Excellence in Fungal Research, Mae Fah Luang University, Chiang Rai 57100, Thailand 2Key Laboratory for Plant Biodiversity and Biogeography of East Asia (KLPB), Kunming Institute of Botany, Chinese Academy of Science, Kunming 650201, Yunnan China3Guizhou Key Laboratory of Agricultural Biotechnology, Guizhou Academy of Agricultural Sciences, Guiyang 550006, Guizhou, China 4Engineering Research Center of Southwest Bio-Pharmaceutical Resources, Ministry of Education, Guizhou University, Guiyang 550025, Guizhou Province, China5Department of Crop Sciences, College of Agricultural and Marine Sciences, Sultan Qaboos University, P.O. Box 34, Al-Khod 123,Oman 6Institute of Plant and Environment Protection, Beijing Academy of Agriculture and Forestry Sciences, No 9 of ShuGuangHuaYuanZhangLu, Haidian District Beijing 100097, China 7Martin Luther University, Institute of Biology, Department of Geobotany, Herbarium, Neuwerk 21, 06099 Halle, Germany 8Westerdijk Fungal Biodiversity Institute, Uppsalalaan 8, 3584CT Utrecht, The Netherlands. 9University of Lisbon, Faculty of Sciences, Biosystems and Integrative Sciences Institute (BioISI), Campo Grande, 1749-016 Lisbon, Portugal. 10Department of Entomology and Plant Pathology, Faculty of Agriculture, Chiang Mai University, 50200, Thailand 11Helmholtz-Zentrum für Infektionsforschung GmbH, Dept. -
The Evolutionary History of Flowering Plants
Journal & Proceedings of the Royal Society of New South Wales, vol. 149, parts 1 & 2, 2016, pp. 65–82. ISSN 0035-9173/16/010065–18 The evolutionary history of flowering plants Charles S.P. Foster1 1 School of Life and Environmental Sciences, University of Sydney, New South Wales 2006, Australia This paper was an RSNSW Scholarship Winner in 2015 Email: [email protected] Abstract In terms of species richness and important ecological roles, there are few biological groups that rival the success of flowering plants (Angiospermae). Angiosperm evolution has long been a topic of interest, with many attempts to clarify their phylogenetic relationships and timescale of evolution. However, despite this attention there remain many unsolved questions surrounding how and when flowers first appeared, and much of the angiosperm diversity remains to be quantified. Here, I review the evolutionary history of angiosperms, and how our understanding of this has changed over time. I begin by summarising the incredible morphological and genetic diversity of flowering plants, and the ways in which this can be studied using phylogenetic inference. I continue by discussing both the relationships between angiosperms and the other major lineages of seed plants, and the relationships between the main groups within angiosperms. In both cases, I outline how our knowledge has changed over time based on factors such as the different conclusions drawn from morphological and genetic data. I then discuss attempts to estimate the timescale of angiosperm evolution and the difficulties of doing so, including the apparent conflict between ages derived from fossil and molecular evidence. Finally, I propose future directions for angiosperm research to help clarify the evolutionary history of one of the most important groups of organisms on the planet. -
132Nd Annual Academy Meeting Abstracts March 25, 2017
132nd Annual Academy Meeting Abstracts March 25, 2017 Page # Anthropology 2 Botany 5 Cell Biology 6 Chemistry 20 Earth Science 49 Ecology 28 Engineering 45 Entomology 40 Environmental Science 47 Micro and Molecular Biology 58 Physics and Astronomy 68 Plant Systematics and Biodiversity 71 Psychology 74 Science Education 75 Zoology 77 1 Anthropology Section An Examination of Midwestern American Indian Female Crania in FORDISC 3.0 with Regard to an Isolated Calotte Found in Indiana Susan Spencer Helfrich, University of Southern Indiana, and Della Collins Cook, Indiana University Isolated crania are a common find in the Midwest and are often broken and incomplete. These fragmentary finds are particularly difficult to identify using traditional forensic techniques. We present on a calotte from Greene County, Indiana, submitted to us as a forensic case. It was missing the face and skull base, allowing for only seven measurements to be entered into FORDISC®3.0 (GOL, XCB, WFB, UFBR, ASB, FRC, PAC). Discrepancies in FORDISC®3.0 results for the Greene County calotte prompted an examination of results for ancient American Indian female crania from the Schild site (AD 700-1250) in west-central Illinois. We learned that (1) ancient Midwestern American Indian females tend to be misclassified in FORDISC®3.0; (2) the likelihood of having a result with a posterior probability above 0.800 increased as the number of measurements entered into FORDISC®3.0 increased; (3) an increased number of measurements entered into FORDISC®3.0 do not guarantee a more accurate result. We propose that the application of FORDISC®3.0 in cases such as the Greene County calotte is unreliable, and should not be used to exclude an ancient American Indian identification.