Foliage of a Broad Leaved Conifer Dammarophyllum from the Cenomanian of Bohemia
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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. -
The Possible Pollen Cone of the Late Triassic Conifer Heidiphyllum/Telemachus (Voltziales) from Antarctica
KU ScholarWorks | http://kuscholarworks.ku.edu Please share your stories about how Open Access to this article benefits you. The Possible Pollen Cone of the Late Triassic Conifer Heidiphyllum/ Telemachus (Voltziales) From Antarctica by Benjamin Bomfleur, Rudolph Serbet, Edith L. Taylor, and Thomas N. Taylor 2011 This is the published version of the article, made available with the permission of the publisher. The original published version can be found at the link below. Bomfleur, B., Serbet, R., Taylor, E., and Taylor, N. 2011. The Possible Pollen Cone of the Late Triassic Conifer Heidiphyllum/Telemachus (Voltziales) From Antarctica. Antarctic Science 23(4): 379-385. Published version: http://dx.doi.org/10.1017/S0954102011000241 Terms of Use: http://www2.ku.edu/~scholar/docs/license.shtml This work has been made available by the University of Kansas Libraries’ Office of Scholarly Communication and Copyright. Antarctic Science 23(4), 379–385 (2011) & Antarctic Science Ltd 2011 doi:10.1017/S0954102011000241 The possible pollen cone of the Late Triassic conifer Heidiphyllum/Telemachus (Voltziales) from Antarctica BENJAMIN BOMFLEUR, RUDOLPH SERBET, EDITH L. TAYLOR and THOMAS N. TAYLOR Division of Paleobotany at the Department of Ecology and Evolutionary Biology, and Natural History Museum and Biodiversity Institute, University of Kansas, Lawrence, KS 66045, USA bbomfl[email protected] Abstract: Fossil leaves of the Voltziales, an ancestral group of conifers, rank among the most common plant fossils in the Triassic of Gondwana. Even though the foliage taxon Heidiphyllum has been known for more than 150 years, our knowledge of the reproductive organs of these conifers still remains very incomplete. Seed cones assigned to Telemachus have become increasingly well understood in recent decades, but the pollen cones belonging to these Mesozoic conifers are rare. -
Araucaria Indica and Two Other Conifers from the Jurassic-Cretaceous Rocks of Madhya Pradesh, India
ARAUCARIA INDICA AND TWO OTHER CONIFERS FROM THE JURASSIC-CRETACEOUS ROCKS OF MADHYA PRADESH, INDIA SUKH-DEV & ZEBA-BANO Birbal Sahni Institute of Palaeobotany, Lucknow-226007, India ABSTRACT This paper reports the occurrence of the living genus Araucaria in the Juras• sic-Lower Cretaceous flora of the Jabalpur Formation, Madhya Pradesh. The species of this genus, Araucaria indica (Sahni) n. comb., is based on leaves and seed-scales. Also, a new genus Satpuria is instituted to accommodate linear conifer leaves, the affinities of which are yet uncertain. Under this genus, S. sehoraensis n. sp. and Satpuria sp. are described from the same formation. INTRODUCTION whose affinities are yet uncertain. These leaves are described here under a new genus Satpuria. Presently two species, S. sehora• INdesh,the UpperdetachedGondwanaslinear leavesof Madhyaof Desmio•Pra• ensis n. sp. and Satpuria sp. are dis• phyllum indicum Sahni (1928) are found tinguished. near jhirnapur, jatarnao, Parsapani, Hasna• pur, Hard River, lmjhiri, Sehora, jabalpur, Bansa and Chandia; near Sehora, Bansa and DESCRIPTION Chandia they are in abundance. Till now Family - ARAUCARIACEAE their affinities were not fully certain. Asso• ciated with Desmiophyllum indicum, in the Genus - Araucaria Jussieu beds of Sehora, jabalpur, Bansa and Chandia detached seed-scales Araucaria Araucaria indica (Sahni) n. comb. pantiana Bose & Maheshwari (1973) are PI. 1, figs. 1-10; Text-fig. lA-J found which were first referred to the lA. Leaves: living genus Araucaria by Pant and Srivastava (1968) on the basis of their 1877 Podozamite9 lanceolatus Schimp. close similarity with seed-scales of Araucaria (Lind!. & Hutt. sp.): Feistmantel, columnaris (Forster) Hooker. -
Andrew Leslie
Andrew Leslie [email protected] • (401) 863-5931 • andrewleslielab.com Department of Ecology and Evolutionary Biology • Brown University Box G-W, 80 Waterman Street • Providence, RI 02912 EDUCATION Ph.D., University of Chicago (Chicago, IL) 2010 Department of the Geophysical Sciences Dissertation: Forms following functions: exploring the evolution of morphological diversity in seed plant reproductive structures. C. Kevin Boyce (advisor), Peter Crane, David Jablonski, Michael LaBarbera, Manfred Rudat B.A. (with honors), University of Pennsylvania 2004 Geology (honors); Biochemistry (honors) Honors thesis: Leaf development in Carboniferous seed plants. Hermann Pfefferkorn (advisor) CURRENT APPOINTMENT Assistant Professor 2014-present Department of Ecology and Evolutionary Biology, Brown University RESEARCH EXPERIENCE Postdoctoral research associate, Yale University 2010-2014 Projects: Fossil conifer descriptions, conifer phylogenetics, conifer reproductive biology, molecular dating techniques, character evolution (advisors: Peter Crane, Michael Donoghue) Doctoral dissertation research, University of Chicago 2004-2010 Topics: Conifer evolution, pollination biology, functional morphology (advisor: C. Kevin Boyce) Research assistant, University of Chicago 2007-2009 Project: Cretaceous plant fossil descriptions from Upatoi Creek, Georgia (advisor: Peter Crane) Research assistant, University of North Carolina, Chapel Hill 2006 Project: Reproductive morphology of the Devonian plant Rhacophyton (advisor: Patricia Gensel) Leslie CV 1 Research -
Jurassic Flora of Cape 1,Isburne Alaska
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR THE JURASSIC FLORA OF CAPE 1,ISBURNE ALASKA F. H. KNOWLTON Publishecl January 28, 1914 PART D OF PROFESSIONAL PAPER 85, "CONTRIBUTIONS TO GENERAL GEOLOGY 1913" WASHINGTON GOVERNMENT PRINTING OFFICE 1914 CONTENTS. Page . Introduction ............................................................................................ 39 The Corwin formation ..................................................................................... 39 Plant collections ......................................................................................... 40 Age of the plant-bearing beds ............................................................................. 41 Distribution of Jurassic floras ............................................................................. 43 Geographicrange .................................................................................... 43 Means of dispersal ................................................................................... 45 Avenues of dispersal ................................................................................. 45 Probable climatic conditions .......................................................................... 46 .The flora ................................................................................................ 46 ILLUSTRATIONS. Page . PLATESV-VIII . Jurassic flora of Cape Lisburne, Alaska .................................................... 57-64 THE' JUR,ASSIC FLORA OF CAPE -
Revision of the Talbragar Fish Bed Flor (Jurassic)
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS White, Mary E., 1981. Revision of the Talbragar Fish Bed Flora (Jurassic) of New South Wales. Records of the Australian Museum 33(15): 695–721. [31 July 1981]. doi:10.3853/j.0067-1975.33.1981.269 ISSN 0067-1975 Published by the Australian Museum, Sydney naturenature cultureculture discover discover AustralianAustralian Museum Museum science science is is freely freely accessible accessible online online at at www.australianmuseum.net.au/publications/www.australianmuseum.net.au/publications/ 66 CollegeCollege Street,Street, SydneySydney NSWNSW 2010,2010, AustraliaAustralia REVISION OF THE TALBRAGAR FISH BED FLORA (jURASSiC) OF NEW SOUTH WALES MARY E. WH ITE The Australian Museum, Sydney. SUMMARY The three well known form-species of the Talbragar Fish Bed Flora-Podozamites lanceolatus, Elatocladus planus and Taeniopteris spa tu lata - are redescribed as Agathis jurassica sp. nov., Rissikia talbragarensis sp. novo and Pentoxylon australica sp. novo respectively. The minor components of the assemblage are described and illustrated, and in some cases, reclassified. Additions are made to the list of plants recorded from the horizon. INTRODUCTION The Talbragar Fish Beds are characterised by their beautifully preserved fish and plant remains which occur in great profusion throughout the shale lens which comprises the Beds. The ochre-coloured shale is ferruginous, with impressions of plants and fish, white in colour, standing out dramatically. The weathering of the outer layers of blocks of the shale has resulted in contrasting bands of iron-rich stain framing many of the specimens and enhancing their appearance. Specimens are much prized by collectors. The fossil locality is the valley ofthe Talbragar River, about twenty miles due North of Home Rule Mine in the Cassilis District, "on the southern boundary of Boyce's selection" (Anderson 1889). -
The Jurassic Plants from Shitaka (The Maizuru Coal-Field), Prov
Title The Jurassic Plants from Shitaka (the Maizuru Coal-field), Prov. Tango (Kyôto Prefecture), Japan Author(s) Ôishi, Saburô Citation Journal of the Faculty of Science, Hokkaido Imperial University. Ser. 4, Geology and mineralogy, 2(1), 1-14 Issue Date 1932-11 Doc URL http://hdl.handle.net/2115/35750 Type bulletin (article) File Information 2(1)_1-14.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP THE YURASSXC PLAN arS FROM SwnllTAKA (THE MAXZURU'COALpFXELD), PROV. TANGO (KYOTO A PREFEC'ffrURE), JAPAN By Sabur6 AOIsm valth 3 Plates ancl 1 Text-PiguTe. The geology of the so-ca]Ied Maizuru eoal-field, about 8 km. SWW ' of ]YIaizuru, and the surrounding area was first mentioned by D. YAMA- smTA in 1895 in the IExpianatory Text to the Geological Map in 11200,OeO; Sheet Hieizan. But he did not announce the occurrence of any Mesozoic fossil plants there, and only correlated the coal seams to those of the Cretaceous age developed in the Islands of Amakusa. In l897, Dr. [[7. 0GAwA(') also touched upon the geology of the ]Mresozoic area in his study on the basie eruptive rocks of northern Tamba and ealled the coal-bearing series, in which he found some fossil plants, the Shitaka Series. He enumerated the following fossil plants col- lected from Shital<a where the main anthraeite searns are being worked now and mentioned that they indicate the Mesozoic age of the plant-beds; they are: Zamiophyllum sp. Podozamites lanceolatus Aspleniu7n ToesseTti ? Taeniopteris Of these Zamiophyllum sp. may be a fragment of Cfr. -
(Nestares Formation) in Northern Patagonia, Argentina. Part 1. Terrestrial Species
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 40 (4): 545-558. Buenos Aires, 30-12-2003 ISSN 0002-7014 Palynostratigraphy and paleoenvironments of Early Jurassic strata (Nestares Formation) in northern Patagonia, Argentina. Part 1. Terrestrial species Ana María ZAVATTIERI1 and Wolfgang VOLKHEIMER1 Abstract. A palynologic analysis is presented of the Early Jurassic Nestares Formation at its type locality, on both sides of the Limay river, Alicurá dam, at Neuquén and Río Negro provinces boundary, northern Patagonia, Argentina. In this first part the terrestrial species (spores and pollen grains) of the microflora are listed, illustrated and, in some cases, commented on. The geologic context is reviewed and different paleoenvironmental interpretations, one as a paralic sequence and another as an anastomosing fluvial sys- tem, both based on earlier sedimentologic studies, are considered. The microflora is compared with the known record of the megaflora and the botanical affinities of the components of the microflora are pro- posed. Thirty nine of the species of miospores illustrated and listed are recorded for the first time in the Early Jurassic of Argentina. The terrestrial taxonomic diversity is represented by 48 species of Bryophyte/Pteridophyte spores and 23 species of Gymnospermous pollen grains, versus five species of Pteridophytes and 17 Gymnosperm species known from the the megaflora; thus the microfloristic biodi- versity record is larger than the megafloristic one. Resumen. PALINOESTRATIGRAFÍA Y PALEOAMBIENTES DE ESTRATOS DEL JURÁSICO TEMPRANO (FORMACIÓN NESTARES) EN EL NORTE DE PATAGONIA, ARGENTINA. Parte 1. Especies Terrestres. Se presenta un analisis pali- nológico de la Formación Nestares (Jurásico Temprano) en su localidad tipo, a ambos lados del río Limay, represa de Alicurá en el límite de las provincias de Neuquén y Río Negro, norte de Patagonia, Argentina. -
An Unexpected Noncarpellate Epigynous Flower from the Jurassic
RESEARCH ARTICLE An unexpected noncarpellate epigynous flower from the Jurassic of China Qiang Fu1, Jose Bienvenido Diez2, Mike Pole3, Manuel Garcı´aA´ vila2,4, Zhong-Jian Liu5*, Hang Chu6, Yemao Hou7, Pengfei Yin7, Guo-Qiang Zhang5, Kaihe Du8, Xin Wang1* 1CAS Key Laboratory of Economic Stratigraphy and Paleogeography, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing, China; 2Departamento de Geociencias, Universidad de Vigo, Vigo, Spain; 3Queensland Herbarium, Brisbane Botanical Gardens Mt Coot-tha, Toowong, Australia; 4Facultade de Bioloxı´a, Asociacio´n Paleontolo´xica Galega, Universidade de Vigo, Vigo, Spain; 5State Forestry Administration Key Laboratory of Orchid Conservation and Utilization at College of Landscape Architecture, Fujian Agriculture and Forestry University, Fuzhou, China; 6Tianjin Center, China Geological Survey, Tianjin, China; 7Key Laboratory of Vertebrate Evolution and Human Origin of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Beijing, China; 8Jiangsu Key Laboratory for Supramolecular Medicinal Materials and Applications, College of Life Sciences, Nanjing Normal University, Nanjing, China Abstract The origin of angiosperms has been a long-standing botanical debate. The great diversity of angiosperms in the Early Cretaceous makes the Jurassic a promising period in which to anticipate the origins of the angiosperms. Here, based on observations of 264 specimens of 198 *For correspondence: individual flowers preserved on 34 slabs in various states and orientations, from the South [email protected] (Z-JL); Xiangshan Formation (Early Jurassic) of China, we describe a fossil flower, Nanjinganthus [email protected] (XW) dendrostyla gen. -
Supplementary Information 1. Supplementary Methods
Supplementary Information 1. Supplementary Methods Phylogenetic and age justifications for fossil calibrations The justifications for each fossil calibration are presented here for the ‘hornworts-sister’ topology (summarised in Table S2). For variations of fossil calibrations for the other hypothetical topologies, see Supplementary Tables S1-S7. Node 104: Viridiplantae; Chlorophyta – Streptophyta: 469 Ma – 1891 Ma. Fossil taxon and specimen: Tetrahedraletes cf. medinensis [palynological sample 7999: Paleopalynology Unit, IANIGLA, CCT CONICET, Mendoza, Argentina], from the Zanjón - Labrado Formations, Dapinigian Stage (Middle Ordovician), at Rio Capillas, Central Andean Basin, northwest Argentina [1]. Phylogenetic justification: Permanently fused tetrahedral tetrads and dyads found in palynomorph assemblages from the Middle Ordovician onwards are considered to be of embryophyte affinity [2-4], based on their similarities with permanent tetrads and dyads found in some extant bryophytes [5-7] and the separating tetrads within most extant cryptogams. Wellman [8] provides further justification for land plant affinities of cryptospores (sensu stricto Steemans [9]) based on: assemblages of permanent tetrads found in deposits that are interpreted as fully terrestrial in origin; similarities in the regular arrangement of spore bodies and size to extant land plant spores; possession of thick, resistant walls that are chemically similar to extant embryophyte spores [10]; some cryptospore taxa possess multilaminate walls similar to extant liverwort spores [11]; in situ cryptospores within Late Silurian to Early Devonian bryophytic-grade plants with some tracheophytic characters [12,13]. The oldest possible record of a permanent tetrahedral tetrad is a spore assigned to Tetrahedraletes cf. medinensis from an assemblage of cryptospores, chitinozoa and acritarchs collected from a locality in the Rio Capillas, part of the Sierra de Zapla of the Sierras Subandinas, Central Andean Basin, north-western Argentina [1]. -
Discovery O F a Podocarpaceous Plant from the Lower Cretaceous O F
No. 81 Proc. Japan Acad., 64, Ser. B (1988) 213 54. Discovery of a Podocarpaceous Plant from the Lower Cretaceous of Kochi Prefecture, in the Outer Zone o f Southwest Japan' By Tatsuaki KIMURA,**'Tamiko GHANA,**)and Kenji MIMOT0***' (Communicatedby TeiichiKoBAYASHI, M.J. A.,Oct. 12, 1988) Extant genera of Podocarpaceae (Conif erales) are confined in distribution to the Southern Hemisphere except for the genus Podocarpus which extends northward. The genus Podocarpus consisting of extant 70 species was divided into 8 sections (Buchholz and Gray, 1948) . Of these, Section Nageia is charac- terized by having the leaves with many parallel veins and its extant species have been known from Indonesia, Philippines, Taiwan and Burma (Florin, 1931) and also from Japan. Very recently many leafy-branches, detached leaves and an organically con- nected seed all referable to Podocarpus (Nageia) were collected from the new locality (Fig. 1) corresponding to the lower part of the Monobe Formation of marine origin (lower Barremian; Tashiro and Kozai, 1984; Tashiro, 1987). The finding of this podocarpaceous plant is significant for the Cretaceous palaeobotany and phytogeography in Japan and its adjacent regions, because this is not only the first finding of a classifiable conifer in the Ryoseki-type floras (e, g. Kimura, 1987) in Japan, but also the existence of the species belonging to the Section Nageia of Podocarpus can be traced back to the early Barremian age in Southwest Japan. Besides this new finding, many new bennettitalean and cycadalean taxa were found from the same locality. They will be described in the separate papers. Description. -
Exceptionally Well-Preserved Early Cretaceous Leaves of Nilssoniopteris from Central Mongolia
Acta Palaeobotanica 58(2): 135–157, 2018 e-ISSN 2082-0259 DOI: 10.2478/acpa-2018-0016 ISSN 0001-6594 Exceptionally well-preserved Early Cretaceous leaves of Nilssoniopteris from central Mongolia FABIANY HERRERA1,5,*, GONGLE SHI2, GOMBOSUREN TSOLMON3, NIIDEN ICHINNOROV 3, MASAMICHI TAKAHASHI4, PETER R. CRANE5,6 and PATRICK S. HERENDEEN1 1 Chicago Botanic Garden, Glencoe, Illinois 60022 USA; e-mails: [email protected]; [email protected] 2 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008 People’s Republic of China; e-mail: [email protected] 3 Institute of Paleontology and Geology, Mongolian Academy of Sciences, Ulaanbaatar-51, Mongolia; e-mails: [email protected]; [email protected] 4 Department of Environmental Sciences, Niigata University, Ikarashi, Nishi-ku, Niigata 950-2181 Japan; e-mail: [email protected] 5 Oak Spring Garden Foundation, Upperville, Virginia 20184 USA 6 School of Forestry and Environmental Studies, Yale University, New Haven, Connecticut 06511 USA; e-mail: [email protected] Received 20 June 2018; accepted for publication 25 October 2018 ABSTRACT. Two new Early Cretaceous (Aptian-Albian) species of fossil bennettitalean leaves are described from central Mongolia and assigned to the genus Nilssoniopteris. Nilssoniopteris tomentosa F.Herrera, G.Shi, Tsolmon, Ichinnorov, Takahashi, P.R.Crane, et Herend. sp. nov., isolated from bulk sediment samples collected for mesofossils in the Tevshiingovi Formation at the Tevshiin Govi opencast coal mine, is distinctive in having a dense, well-developed indumentum composed of branched, flattened multicellular trichomes on the abaxial leaf surface.