Development of the Pollen in the Antarctic Flowering Plant Colobanthus Quitensis (Kunth) Bartl

Total Page:16

File Type:pdf, Size:1020Kb

Development of the Pollen in the Antarctic Flowering Plant Colobanthus Quitensis (Kunth) Bartl ACTA AGROBOTANICA Vol. 60 (2): 3–8 2007 DEVELOPMENT OF THE POLLEN IN THE ANTARCTIC FLOWERING PLANT COLOBANTHUS QUITENSIS (KUNTH) BARTL. Irena Giełwanowska 1, 2, Anna Bochenek 1, Ewa Szczuka 3 1Department of Plant Physiology and Biotechnology, University of Warmia and Mazury, Oczapowskiego 1A, 10-719 Olsztyn, Poland e-mail:[email protected] 2Department of Antarctic Biology, Polish Academy of Sciences, Ustrzycka 10/12, 02-141 Warsaw, Poland 3Department of Plant Anatomy and Cytology, UMCS University, Akademicka 19, 20-033 Lublin, Poland Received: 20.10.2007 Summary The summer season is considered to last for abo- Colobanthus quitensis (Kunth) Bartl. produced two ty- ut 5 months, more or less from November to March, ta- pes very small bisexual fl owers. In the Antarctic natural con- king especially day and night length into account. Con- ditions chasmogamic and cleistogamic fl owers most often form sidering the length of the snow-cover period in the areas fi ve stamina with short fi laments. Two microsporangia with uncovered by ice, the growth season of seminiferous a three-layer wall form in the anther. Microspore mother cells, plants occurring here may be shortened by 1-2 months. which develop into microspores after meiosis, form inside the Irrespective of other factors affecting the plants, this microsporangium. Microsporocytes of Colobanthus quitensis time is critical for the formation of generative cells and are surrounded with a thick callose layer, the special wall. After seeds (Edwards, 1974; G i e ł wanowska et al. meiosis, the callose wall is dissolved and microspores are rele- 2006). ased from the tetrad. The production of proorbicules, orbicules Macroscopic observations of fl ower and seed and peritapetal membrane, and the construction of a complex development in Antarctic pearlwort and Antarctic hair sporoderm with numerous apertural sites were observed. When grass were conducted in various areas of the Maritime microspore and pollen protoplasts underwent necrosis, probably Antarctic and in different growth seasons. Greene and as a result of temperature and osmotic stress, sporoderm lay- ers formed around microspores, and the cell tapetum did not Holtom (1971) described the fl ower formation in Co- disintegrate. However, woody wall layers did not accumulate in lobanthus quitensis and Deschampsia antarctica on the endothecium cells. South Orkney Islands. Brown (1912) and H oldga- t e (1964) observed specimens of Antarctic pearlwort and hair grass which fl owered and dispersed seeds in Key words: Colobanthus quitensis, microsporangia, microsporo- the communities of South Georgia, while Holtom and genesis, male gametophytes, tapetal cells Greene (1967) on some of the South Shetland Is- lands. INTRODUCTION As only few descriptions of generative cell deve- lopment in Antarctic fl owering plants have been publi- Colobanthus quitensis (Kunth) Bartl. is the only shed (G i e ł wanowska, 2005; G i e ł wanowska fl owering dicot of the Antarctica. It has grown together et al. 2005; G i e ł wanowska et al. 2006), in this with Deschampsia antarctica Desv. (Poaceae) for a few work we present some stages of microsporogenesis and thousand years. It effectively colonises surfaces of the pollen development in Colobanthus quitensis. Antarctic geobotanical zone uncovered by melting ice (Edwards, 1974; A lberdi et al. 2002). In the MATERIALS AND METHODS extremely hostile Antarctic conditions, Colobanthus quitensis (Caryophyllaceae) fl owers profusely almost The experimental materials were fl ower buds of every year. After pollination and fertilization it produc- Colobanthus quitensis in different development stages. es seeds. Antarctic pearlwort seeds are often dead due The materials were collected during the 26th expedition to unfavourable microhabitat conditions and the short to the Antarctic, organized by the Department of An- cold summer (Convey, 1996; G i e ł wanowska et tarctic Biology, Polish Academy of Sciences in Warsaw. al. 2006). Flower buds of Colobanthus quitensis were collected 4 Irena Giełwanowska, Anna Bochenek, Ewa Szczuka during the Antarctic summer, from December 2001 moved from various areas of the tapetum towards pollen to March 2002, in the vicinity of the Arctowski Polar grains, and in the form of bigger structures, orbicules, Station (62º09.8´ S and 58º28.5´W). joined the developing sporoderm (Fig. 5 ). A dozen or so Light and electron microscopy of apertural sites devoid of electron-dense sporopollenin The material for light and electron microsco- material (Fig. 5, ap) differentiated in the forming sporo- py was prepared by a standard method, i.e. fi xed in an derm. In the semi-thin sections, stained with toluidine osmic acid-glutaraldehyde solution. The material was blue, proorbicules and orbicules were visible in the form dehydrated in an alcohol-acetone series, and embedded of blue-green drops (Fig. 5 and Fig. 6). Orbicules settled in Poly Bed 812 epoxy resin. Semi-thin and ultra-thin on the surface of pollen grains until the fi nal stage of sections were prepared in a Leica (Ultracut R) ultrami- tapetal disintegration and atrophy. At the same time, en- crotome, using glass and diamond knives, stained with dothecium with conspicuous ridge-like wall thickenings toluidine blue, and toluidine blue and azure B, following was already fully developed in the microsporangium Pearse (1962), and then examined and photographed wall (Fig. 5). under a light microscope, models Olympus and Nikon It is worth noting that, in the case of microspo- Optiphot II. All preparations to be photographed un- re or pollen protoplast necrosis, as a result of tempe- der a light microscope were mounted in glycerin. Ultra- rature or osmotic stress, tapetum did not disintegrate, -thin sections (60 – 90 nm) were placed onto a copper and endothecium with woody ridges did not develop, wire gauze (300 meshes) and contrasted with a saturated although layers were almost normally deposited on the aqueous solution of uranyl acetate and lead citrate, fol- sporoderm (Fig. 3). lowing Reynolds (1973). Observations and electro- When pollen was mature and contained a bicel- nograms were made in a JEOL JEM 100S transmission lular and tricellular male gametophyte, Colobanthus electron microscope. quitensis microsporangia burst open at a specifi c site, stomium, on the inner (adaxial) side of the anther (Fig. RESULTS 4 and Fig. 7). After anther dehiscence some pollen re- ached the surface of the receptive cells on the fi ve-part Colobanthus quitensis fl owers usually produced feathery stigma, while some remained inside the micro- 5 stamina with short fi laments. sporangium and germinated (Fig. 4). In the anther there were two microsporangia, which had a regular circular shape in cross section. Four DISCUSSION cell layers were visible in the microsporangium wall. The most external layer was epidermis under which, A small number of microspore mother cells diffe- almost on its entire length, there was a layer of starch- rentiated in each of the two microsporangia of the Colo- -fi lled cells which transformed into endothecium. Only banthus quitensis anther. However, already in the early at some places there was a middle layer of parenchyma. fi rst meiotic prophase these cells were surrounded with A nutritive tissue, tapetum (Fig. 1), developed inside. a thick callose wall and were isolated in this way until The central part of the microsporangium was occupied the tetrad stage. Callose began to hydrolise when the by archesporial tissue from which, as a result of meiosis, construction of sporoderm started, just as in other plants microspores were formed. Before meiosis began, micro- (Heslop-Harrison et al. 1986 ). spore mother cells constructed special callose walls. Cal- Microsporgenesis in Deschampsia antarctica was lose surrounded microsporocytes until the tetrad stage. completely different. In the microsporocyte cell walls After meiosis, when callose disintegrated, microspores of the Antarctic hair grass, deposition of a thick callose were released from the tetrads, and a complex cell wall, layer was not observed. From the stage of sporogenic sporoderm, formed on the surface of their protoplasts. tissue cells, through all the meiotic stages, to tetrads, The developing mother cells of the male game- microsporocyte cell walls of the Antarctic hair grass tophyte, from the premeiotic stage, through meiosis, remained thin. This feature distinguishes Deschampsia to the stage of double-cell pollen grains (Fig. 2), were antarctica from other grasses, in which callose special surrounded and nourished by the cell tapetum. Cells walls of meiotic cells are common (McQuade and of the secretory tapetum contained one or two nuclei. Young-Rottler, 1984; Rodkiewicz et al. They retained their individuality until the gametophy- 1996), as in other angiosperms (P a cini et al. 1985). te stage. In the thick cytoplasm of tapetal cells, before In the microspore of Colobanthus quitensis, af- microspores were released from the tetrads, osmophillic ter the fi rst mitosis, the formed generative nucleus does droplets appeared and moved inside the pollen sac (Fig. not break off the sporoderm, but remains fi rmly attached 3). Apart from small lipid droplets, vast areas containing to the inner surface of the pollen wall. After mitosis, the such material visible within the cytoplasm and on the generative cell stays close to the sporoderm, but it is se- borderline with the pollen sac, could be observed in the parated from the vegetative cell by a very delicate wall tapetal cells. This material, in the form of proorbicules, with a little amount of fi brous material. The typical wall Development of the pollen in the Antarctic fl owering plant Colobanthus quitensis (Kunth) Bartl. 5 Fig. 1. Fragment of a microsporangium in Colobanthus quitensis. Layers of the wall; tapetum (ta), parenchymal middle layer (ml) and epidermis (ep). Very thick callose walls (arrows) of the microspore mother cells are visible. 1200 x. Fig. 2. Binucleate pollen grains are visible in the microsporangium. Tapetum is disintegrated (ta). 2000 x. Fig. 3. Microsporangium with disturbed pollen development. There is no developed endotecium in the microsporangium wall.
Recommended publications
  • Evaluation of a Proposed Significant Natural Area at Mt Iron, Wanaka
    EVALUATION OF A PROPOSED SIGNIFICANT NATURAL AREA AT MT IRON, WANAKA R3762 EVALUATION OF A PROPOSED SIGNIFICANT NATURAL AREA AT MT IRON, WANAKA Coprosma shrubland on the southwest faces at the Allenby Farms site, Mt Iron. Contract Report No. 3762 March 2017 (Revised and updated) Project Team: Kelvin Lloyd - Report author: vegetation and flora Mandy Tocher - Report author: herpetofauna Brian Patrick - Report author: invertebrates Prepared for: Allenby Farms Ltd P.O. Box 196 Wanaka 9343 DUNEDIN OFFICE: 764 CUMBERLAND STREET, DUNEDIN 9016 Ph 03-477-2096, 03-477-2095 HEAD OFFICE: 99 SALA STREET, P.O. BOX 7137, TE NGAE, ROTORUA Ph 07-343-9017, 07-343-9018; email [email protected], www.wildlands.co.nz CONTENTS 1. INTRODUCTION 1 2. SITE CONTEXT 1 3. METHODS 1 4. ECOLOGICAL CONTEXT 4 5. INDIGENOUS VEGETATION AND HABITATS 5 5.1 Kānuka scrub and shrubland 5 5.2 Coprosma scrub and shrubland 6 5.3 Exotic grassland and herbfield 7 5.4 Swale turf 8 5.5 Cushionfield 8 6. FLORA 8 6.1 Species richness 8 6.2 Threatened and At Risk plant species 12 6.3 Pest plants 12 7. BIRDS 13 8. LIZARDS 14 8.1 Overview 14 8.2 “Remove from SNA” zone 14 8.3 Alternate SNA 18 9. INVERTEBRATES 18 9.1 Overview 18 9.2 Mixed Coprosma-dominant shrubland 18 9.3 Kānuka scrub and shrubland 19 9.4 Rock outcrop habitats 19 9.5 Open grassland and turf 19 10. PEST ANIMALS 20 11. ECOLOGICAL VALUES 20 11.1 District Plan (2009) - Section 6c Significance 20 11.2 Proposed District Plan - Section 6c Significance from Policy 33.2.1.9 22 11.3 Significance summary 23 12.
    [Show full text]
  • A New Parasite Species of Deschampsia Antarctica (Poaceae) Described to Antarctica
    Anais da Academia Brasileira de Ciências (2016) 88(3 Suppl.): 1967-1969 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201620150779 www.scielo.br/aabc Phaeosphaeria deschampsii (Ascomycota): A new parasite species of Deschampsia antarctica (Poaceae) described to Antarctica JAIR PUTZKE1 and ANTONIO B. PEREIRA2 1Universidade de Santa Cruz do Sul/UNISC, Instituto Nacional de Ciência e Tecnologia Antártico de Pesquisas Ambientais/INCT-APA, Av. Independência, 2293, 96815-900 Santa Cruz do Sul, RS, Brasil 2Universidade Federal do Pampa/UNIPAMPA, Instituto Nacional de Ciência e Tecnologia Antártico de Pesquisas Ambientais/INCT-APA, Av. Antonio Trilha, 1847, 97300-000 São Gabriel, RS, Brasil Manuscript received on November 11, 2015; accepted for publication on April 18, 2016 ABSTRACT This study presents the description of Phaeosphaeria deschampsii, which was found in plant communities from Half Moon Island, South Shetland Archipelago, Antarctica, in February 2014. Many patches of Deschampsia antarctica (Poaceae), the only indigenous Poaceae specie in Antarctic, were found dead, parasitized by a fungi pathogen. Based on the shape of its perithecia, with oblique neck, erumpent in the grass tissues, ascospore form and septation, the specie was identified as new to science. Key words: Antarctica, Ascomycota, grass, phytopathology. INTRODUCTION monocot plants. Some species are very specialized while others have a large host spectrum (Stchigel Plant pathogens are little known from the Antarctic et al. 2004). region, generally reported from lichens and mosses During field work done in the Antarctic (Half more than from angiosperms. The fanerogams are Moon Island), we collected many samples of dead restricted to only two species in this continent: D.
    [Show full text]
  • Generative Reproduction of Antarctic Grasses, the Native Species Deschampsia Antarctica Desv
    vol. 36, no. 3, pp. 261–279, 2015 doi: 10.1515/popore−2015−0016 Generative reproduction of Antarctic grasses, the native species Deschampsia antarctica Desv. and the alien species Poa annua L. Irena GIEŁWANOWSKA1,2* and Wioleta KELLMANN−SOPYŁA1 1Katedra Fizjologii, Genetyki i Biotechnologii Roślin, Wydział Biologii i Biotechnologii, Uniwersytet Warmińsko−Mazurski w Olsztynie, ul. Oczapowskiego 1A, 10−719 Olsztyn, Poland 2 Instytut Biochemii i Biofizyki PAN, Zakład Biologii Antarktyki i Polska Stacja Antarktyczna “H. Arctowski”, ul. Ustrzycka 10/12, 02−141 Warszawa, Poland * corresponding author <[email protected]> Abstract: The embryology of two species, Deschampsia antarctica, a native species, and Poa annua, an alien species in the Antarctic we studied. Flowering buds of plants growing in their natural habitats on King George Island and generative tissues of both plant species grown in a greenhouse were analyzed. Adaptations to autogamy and anemogamy were ob− served in the flower anatomy of both species. The microsporangia of the evaluated grasses produce a small number of three−celled pollen grains. Numerous pollen grains do not leave the microsporangium and germinate in the thecae. Deschampsia antarctica and P. annua plants harvested in Antarctica developed a particularly small number of microspores in pol− len chambers. In D. antarctica, male gametophytes were produced at a faster rate: genera− tive cells in pollen did not become detached from the wall of the pollen grain, they were not embedded in the cytoplasm of vegetative cells, and they divided into two sperm cells situ− ated close to the wall. The monosporous Polygonum type of embryo sac development was observed in the studied species.
    [Show full text]
  • Evolution of Cold Acclimation in Temperate Grasses (Pooideae)
    bioRxiv preprint doi: https://doi.org/10.1101/210021; this version posted October 27, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-ND 4.0 International license. Evolution of cold acclimation in temperate grasses (Pooideae) Marian Schubert*,1, Lars Grønvold*,2, Simen R. Sandve3, Torgeir R. Hvidsten2,4 and Siri Fjellheim1,† 1Faculty of Biosciences, Norwegian University of Life Sciences, Ås NO-1432, Norway. 2Faculty of Chemistry, Biotechnology and Food Science, Norwegian University of Life Sciences, Ås NO-1432, Norway. 3Centre for Integrative Genetics (CIGENE), Faculty of Biosciences, Norwegian University of Life Sciences, Ås NO- 1432, Norway. 4Umeå Plant Science Centre, Department of Plant Physiology, Umeå University, Umeå SE-90187, Sweden. *Contributed equally † Author for correspondence: [email protected] 1 bioRxiv preprint doi: https://doi.org/10.1101/210021; this version posted October 27, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-ND 4.0 International license. Abstract In the past 50 million years climate cooling has triggered the expansion of temperate biomes. During this period, many extant plant lineages in temperate biomes evolved from tropical ancestors and adapted to seasonality and cool conditions. Among the Poaceae (grass family), one of the subfamilies that successfully shifted from tropical to temperate biomes is the Pooideae (temperate grasses).
    [Show full text]
  • Cuverville Island Lecointe Is
    Gourdin Astrolabe Island Island Mikklesen Harbor oker Passage Cr Hydrurga Cierva Cove Dallmann Bay Rocks Two Hummock Is Brabant Is. Cuverville Island Lecointe Is. ANTARCTICMelchior Brialmont Islands TREATY Sprightly Cove Islands Cuverville Island visitor site guide 64˚41’S, 62˚38’W - North Errera Channel Gerlache Strait Enterprise Is. The Waifs Portal Point Key features Anvers Is. Foyn Harbour Spigot Peak Orne Harbour Gouvernøren Harbour - Extensive colony of gentoo penguins in the Nansen Is. Orne Is. Charlotte Bay Georges Point Wilhelmina Bay Antarctic Peninsula CUVERVILLE IS. - Glacial and ice scenery Ronge Is. Arthur Danco Is. Harbour Neumayer Channel Beneden Head (Palmer Station) Dorian Bay Waterboat Point Jougla Pt. Doumer Is. Priest Is. Paradise Py Point Bay Andvord Bay Neko Harbour Peltier Channel Wiencke Is. Almirante la Brown Station ctic Peninsu Antar Description Lemaire Channel TOPOGRAPHY This 2km by 2.5km island is a steep-sided dome, two-thirds of which is covered by a permanent ice-cap. The northern shore is a beach of cobbles and boulders, approx 1.5km long, backed by steep vegetation- covered cliffs toward the east and gentler slopes to the west. FAUNA Confirmed breeders: gentoo penguin (Pygoscelis papua), kelp gull (Larus dominicanus), Antarctic tern (Sterna vittata), snowy sheathbill (Chionis alba), blue-eyed shag (Phalacrocorax atriceps), Wilson’s storm- petrel (Oceanites oceanicus), skuas (Catharacta spp.), snow petrel (Pagodroma nivea), pintado petrel (Daption capense). Weddell seals (Leptonychotes weddellii) and Antarctic fur seals (Arctocephalus gazella) regularly haul out. Leopard seals (Hydrurga leptonyx) often hunt near-shore. FLORA Deschampsia antarctica, Colobanthus quitensis; swards of moss species; and lichen species including Xanthoria spp., Buellia spp., Caloplaca spp.
    [Show full text]
  • Studies of Plant Communities of the Antarctic Peninsula Near Palmer
    combining our raw concentration data with depth adjusted Allnutt. 1982-a. Comparative ecology of plankton communities in estimates of water body volume. In conjunction with loading seven Antarctic oasis lakes. Journal of Plankton Research, 4(2), 271-286. estimates, we will then estimate nutrient residence times, to Parker, B.C., G.M. Simmons, Jr., R.A. Wharton, Jr., K.G. Seaburg, and gain some sense of nitrogen and phosphorus dynamics in these F.G. Love. 1982-b. Removal of organic and inorganic matter from lakes. Antarctic lakes by aerial escape of blue-green algal mats. Journal of Work in the future will center on modeling of diffusion pro- Phycology, 18, 72-78. Rast, W., and G.F. cesses for nutrients within the lakes. Specifically, we will be Lee. 1978. Summary analysis of the North American (U.S. Portion) OFCD eutrophication project: Nutrient loading—lake response looking at the rate of diffusion of ammonia into the upper waters relationships and trophic state indices. (U.S. EPA. EPA-G0013-78-008.) of Lake Fryxell and its conversion to available (and limiting) Corvallis, Oregon: Corvallis Environmental Research Laboratory. nitrate. This will permit comparison of internal versus external Simmons, G.M., Jr., B.C. Parker, F.C.T. Allnutt, D.P. Brown, D.D. loading and will further aid in determining why this lake is Cathey, and K.G. Seaburg. 1980. Ecosystem comparison of oasis more productive than its oligotrophic neighbor, Lake Hoare. lakes and soils. Antarctic Journal of the U.S., 14(5), 181-183. We wish to thank George Simmons and his students for their Strickland, J.D.H., and T.R.
    [Show full text]
  • Global Southern Limit of Flowering Plants and Moss Peat Accumulation Peter Convey,1 David W
    RESEARCH/REVIEW ARTICLE Global southern limit of flowering plants and moss peat accumulation Peter Convey,1 David W. Hopkins,2,3,4 Stephen J. Roberts1 & Andrew N. Tyler3 1 British Antarctic Survey, National Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK 2 Scottish Crop Research Institute, Invergowrie, Dundee DD2 5DA, UK 3 Environmental Radioactivity Laboratory, School of Biological and Environmental Sciences, University of Stirling, Stirling FK9 4LA, UK 4 School of Life Sciences, Heriot-Watt University, Riccarton, Edinburgh EH14 4AS, UK Keywords Abstract Antarctic plants; distribution limits; peat accumulation; dating. The ecosystems of the western Antarctic Peninsula, experiencing amongst the most rapid trends of regional climate warming worldwide, are important ‘‘early Correspondence warning’’ indicators for responses expected in more complex systems else- Peter Convey, British Antarctic Survey, where. Central among responses attributed to this regional warming are National Environment Research Council, widely reported population and range expansions of the two native Antarctic High Cross, Madingley Road, Cambridge flowering plants, Deschampsia antarctica and Colobanthus quitensis. However, CB3 0ET, UK. E-mail: [email protected] confirmation of the predictions of range expansion requires baseline knowl- edge of species distributions. We report a significant southwards and westwards extension of the known natural distributions of both plant species in this region, along with several range extensions in an unusual moss community, based on a new survey work in a previously unexamined and un-named low altitude peninsula at 69822.0?S71850.7?W in Lazarev Bay, north-west Alexander Island, southern Antarctic Peninsula. These plant species therefore have a significantly larger natural range in the Antarctic than previously thought.
    [Show full text]
  • Co-Extinction of Mutualistic Species – an Analysis of Ornithophilous Angiosperms in New Zealand
    DEPARTMENT OF BIOLOGICAL AND ENVIRONMENTAL SCIENCES CO-EXTINCTION OF MUTUALISTIC SPECIES An analysis of ornithophilous angiosperms in New Zealand Sandra Palmqvist Degree project for Master of Science (120 hec) with a major in Environmental Science ES2500 Examination Course in Environmental Science, 30 hec Second cycle Semester/year: Spring 2021 Supervisor: Søren Faurby - Department of Biological & Environmental Sciences Examiner: Johan Uddling - Department of Biological & Environmental Sciences “Tui. Adult feeding on flax nectar, showing pollen rubbing onto forehead. Dunedin, December 2008. Image © Craig McKenzie by Craig McKenzie.” http://nzbirdsonline.org.nz/sites/all/files/1200543Tui2.jpg Table of Contents Abstract: Co-extinction of mutualistic species – An analysis of ornithophilous angiosperms in New Zealand ..................................................................................................... 1 Populärvetenskaplig sammanfattning: Samutrotning av mutualistiska arter – En analys av fågelpollinerade angiospermer i New Zealand ................................................................... 3 1. Introduction ............................................................................................................................... 5 2. Material and methods ............................................................................................................... 7 2.1 List of plant species, flower colours and conservation status ....................................... 7 2.1.1 Flower Colours .............................................................................................................
    [Show full text]
  • From Cacti to Carnivores: Improved Phylotranscriptomic Sampling And
    Article Type: Special Issue Article RESEARCH ARTICLE INVITED SPECIAL ARTICLE For the Special Issue: Using and Navigating the Plant Tree of Life Short Title: Walker et al.—Phylotranscriptomic analysis of Caryophyllales From cacti to carnivores: Improved phylotranscriptomic sampling and hierarchical homology inference provide further insight into the evolution of Caryophyllales Joseph F. Walker1,13, Ya Yang2, Tao Feng3, Alfonso Timoneda3, Jessica Mikenas4,5, Vera Hutchison4, Caroline Edwards4, Ning Wang1, Sonia Ahluwalia1, Julia Olivieri4,6, Nathanael Walker-Hale7, Lucas C. Majure8, Raúl Puente8, Gudrun Kadereit9,10, Maximilian Lauterbach9,10, Urs Eggli11, Hilda Flores-Olvera12, Helga Ochoterena12, Samuel F. Brockington3, Michael J. Moore,4 and Stephen A. Smith1,13 Manuscript received 13 October 2017; revision accepted 4 January 2018. 1 Department of Ecology & Evolutionary Biology, University of Michigan, 830 North University Avenue, Ann Arbor, MI 48109-1048 USA 2 Department of Plant and Microbial Biology, University of Minnesota-Twin Cities, 1445 Gortner Avenue, St. Paul, MN 55108 USA 3 Department of Plant Sciences, University of Cambridge, Cambridge CB2 3EA, UK 4 Department of Biology, Oberlin College, Science Center K111, 119 Woodland Street, Oberlin, OH 44074-1097 USA 5 Current address: USGS Canyonlands Research Station, Southwest Biological Science Center, 2290 S West Resource Blvd, Moab, UT 84532 USA 6 Institute of Computational and Mathematical Engineering (ICME), Stanford University, 475 Author Manuscript Via Ortega, Suite B060, Stanford, CA, 94305-4042 USA This is the author manuscript accepted for publication and has undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process, which may lead to differences between this version and the Version of Record.
    [Show full text]
  • Diversity and Origin of the Central Mexican Alpine Flora
    diversity Article Diversity and Origin of the Central Mexican Alpine Flora Victor W. Steinmann 1, Libertad Arredondo-Amezcua 2, Rodrigo Alejandro Hernández-Cárdenas 3 and Yocupitzia Ramírez-Amezcua 2,* 1 Facultad de Ciencias Naturales, Universidad Autónoma de Querétaro, Av. de las Ciencias s/n, Del. Sta. Rosa Jáuregui, Querétaro 76230, Mexico; [email protected] or [email protected] 2 Private Practice, Pátzcuaro, Michoacán 61600, Mexico; [email protected] 3 Herbario Metropolitano, División de Ciencias Biológicas y de la Salud, Departamento de Biología, Universidad Autónoma Metropolitana-Iztapalapa, Avenida San Rafael Atlixco #186, Colonia Vicentina, Iztapalapa, Ciudad de México 09340, Mexico; [email protected] * Correspondence: [email protected] Abstract: Alpine vegetation is scarce in central Mexico (≈150 km2) and occurs on the 11 highest peaks of the Trans-Mexican Volcanic Belt (TMVB). Timberline occurs at (3700) 3900 m, and at 4750 m vascular plants cease to exist. The alpine vascular flora comprises 237 species from 46 families and 130 genera. Asteraceae (44), Poaceae (42), and Caryophyllaceae (21) possess 45% of the species; none of the remaining families have more than 10 species. Four species are strict endemics, and eight others are near endemics. Thirteen species are restricted to alpine vegetation but also occur outside the study area. Seventy-seven species are endemic to Mexico, 35 of which are endemic to the TMVB. In terms of biogeography, the strongest affinities are with Central or South America. Fifteen species are also native to the Old World. Size of the alpine area seems to not be the determining factor for its floristic diversity. Instead, the time since and extent of the last volcanic activity, in addition to the distance from other alpine islands, appear to be important factors affecting diversity.
    [Show full text]
  • Falkland Islands Species List
    Falkland Islands Species List Day Common Name Scientific Name x 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 1 BIRDS* 2 DUCKS, GEESE, & WATERFOWL Anseriformes - Anatidae 3 Black-necked Swan Cygnus melancoryphus 4 Coscoroba Swan Coscoroba coscoroba 5 Upland Goose Chloephaga picta 6 Kelp Goose Chloephaga hybrida 7 Ruddy-headed Goose Chloephaga rubidiceps 8 Flying Steamer-Duck Tachyeres patachonicus 9 Falkland Steamer-Duck Tachyeres brachypterus 10 Crested Duck Lophonetta specularioides 11 Chiloe Wigeon Anas sibilatrix 12 Mallard Anas platyrhynchos 13 Cinnamon Teal Anas cyanoptera 14 Yellow-billed Pintail Anas georgica 15 Silver Teal Anas versicolor 16 Yellow-billed Teal Anas flavirostris 17 GREBES Podicipediformes - Podicipedidae 18 White-tufted Grebe Rollandia rolland 19 Silvery Grebe Podiceps occipitalis 20 PENGUINS Sphenisciformes - Spheniscidae 21 King Penguin Aptenodytes patagonicus 22 Gentoo Penguin Pygoscelis papua Cheesemans' Ecology Safaris Species List Updated: April 2017 Page 1 of 11 Day Common Name Scientific Name x 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 23 Magellanic Penguin Spheniscus magellanicus 24 Macaroni Penguin Eudyptes chrysolophus 25 Southern Rockhopper Penguin Eudyptes chrysocome chrysocome 26 ALBATROSSES Procellariiformes - Diomedeidae 27 Gray-headed Albatross Thalassarche chrysostoma 28 Black-browed Albatross Thalassarche melanophris 29 Royal Albatross (Southern) Diomedea epomophora epomophora 30 Royal Albatross (Northern) Diomedea epomophora sanfordi 31 Wandering Albatross (Snowy) Diomedea exulans exulans 32 Wandering
    [Show full text]
  • Detection of Ancient Genome Duplications in Several Flowering Plant
    DETECTION OF ANCIENT GENOME DUPLICATIONS IN SEVERAL FLOWERING PLANT LINEAGES AND SYNTE-MOLECULAR COMPARISON OF HOMOLOGOUS REGIONS by JINGPING LI (Under the Direction of Andrew H. Paterson) ABSTRACT Flowering plants have evolved through repeated ancient genome duplications (or paleo- polyploidies) for ~200 million years, a character distinct from other eukaryotic lineages. Paleo-duplicated genomes returned to diploid heredity by means of extensive sequence loss and rearrangement. Therefore repeated paleo-polyploidies have left multiple homeologs (paralogs produced in genome duplication) and complex networks of homeology in modern flowering plant genomes. In the first part of my research three paleo-polyploidy events are discussed. The Solanaceae “T” event was a hexaploidy making extant Solanaceae species rare as having derived from two successive paleo-hexaploidies. The Gossypium “C” event was the first paleo-(do)decaploidy identified. The sacred lotus (Nelumbo nucifera) was the first sequenced basal eudicot, which has a lineage-specific “λ” paleo-tetraploidy and one of the slowest lineage evolutionary rates. In the second part I describe a generalized method, GeDupMap, to simultaneously infer multiple paleo-polyploidy events on a phylogeny of multiple lineages. Based on such inferences the program systematically organizes homeologous regions between pairs of genomes into groups of orthologous regions, enabling synte-molecular analyses (molecular comparison on synteny backbone) and graph representation. Using 8 selected eudicot and monocot
    [Show full text]