An Updated Checklist of the Mosses of Chile
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Natural Heritage Program List of Rare Plant Species of North Carolina 2016
Natural Heritage Program List of Rare Plant Species of North Carolina 2016 Revised February 24, 2017 Compiled by Laura Gadd Robinson, Botanist John T. Finnegan, Information Systems Manager North Carolina Natural Heritage Program N.C. Department of Natural and Cultural Resources Raleigh, NC 27699-1651 www.ncnhp.org C ur Alleghany rit Ashe Northampton Gates C uc Surry am k Stokes P d Rockingham Caswell Person Vance Warren a e P s n Hertford e qu Chowan r Granville q ot ui a Mountains Watauga Halifax m nk an Wilkes Yadkin s Mitchell Avery Forsyth Orange Guilford Franklin Bertie Alamance Durham Nash Yancey Alexander Madison Caldwell Davie Edgecombe Washington Tyrrell Iredell Martin Dare Burke Davidson Wake McDowell Randolph Chatham Wilson Buncombe Catawba Rowan Beaufort Haywood Pitt Swain Hyde Lee Lincoln Greene Rutherford Johnston Graham Henderson Jackson Cabarrus Montgomery Harnett Cleveland Wayne Polk Gaston Stanly Cherokee Macon Transylvania Lenoir Mecklenburg Moore Clay Pamlico Hoke Union d Cumberland Jones Anson on Sampson hm Duplin ic Craven Piedmont R nd tla Onslow Carteret co S Robeson Bladen Pender Sandhills Columbus New Hanover Tidewater Coastal Plain Brunswick THE COUNTIES AND PHYSIOGRAPHIC PROVINCES OF NORTH CAROLINA Natural Heritage Program List of Rare Plant Species of North Carolina 2016 Compiled by Laura Gadd Robinson, Botanist John T. Finnegan, Information Systems Manager North Carolina Natural Heritage Program N.C. Department of Natural and Cultural Resources Raleigh, NC 27699-1651 www.ncnhp.org This list is dynamic and is revised frequently as new data become available. New species are added to the list, and others are dropped from the list as appropriate. -
Zeitschrift Für Naturforschung / C / 50 (1995)
Notes 311 The Biflavonoid Pattern of the Tortes, Lerida (Spain), 2.11.1991, leg. et det. J.A. Moss Bartramia ithyphylla Löpez-Säez and Puerto de Canencia, Madrid (Bartramiaceae, Musci) (Spain), 10.12.1988, leg. et det. M.E. Ron. Voucher José Antonio López-Sáez, specimens are deposited in the Herbarium of the Marí a José Pérez-Alonso and Department of Plant Biology, Faculty of Biology, Arturo Velasco-Negueruela Complutense University of Madrid (“MACB”). Departamento de Biologfa Vegetal I, Facultad de Bio- logfa, Universidad Complutense, 28040 Madrid, Spain Extraction and isolation Z. Naturforsch. 50c, 311-312 (1995); received October 31, 1994/January 23, 1995 120 g air-dried plant material (freed from for Bartramiaceae, Bartramia ithyphylla Brid., Biflavonoids eign matter) was extracted three times with From Bartramia ithyphylla the following five biflavo M e0H :H 20 (8:2) 5 1 each and twice with 4 1 noids were isolated: philonotisflavone, 2,3-dihydrophilo- Me2C 0 :H 20 (8:2). To eliminate chlorophylls the notisflavone, dicranolomin, 5',3'"-dihydroxyamentofla- combined extracts were evaporated and the resi vone and 5'-hydroxyamentoflavone. due subjected to a four step Craig distribution be tween the upper and lower phases of DMF/HzO/ Et20 (4:1:8). The combined lower phases were re duced in vacuo to a thin syrup (about 100 ml). Bartramia Hedw. is a large moss genus of about After addition of 60 ml dry polyamide-6 powder 100 species and three sections (Corley et al., 1981). it was diluted with 1 1 water. The resulting suspen During a study of the flavonoid patterns of the sion was cautiously poured on top of a 3-1 poly- Bartramiaceae by TLC and HPLC (Löpez-Säez, amide-6-column (wet packed). -
Antarctic Bryophyte Research—Current State and Future Directions
Bry. Div. Evo. 043 (1): 221–233 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.16 Antarctic bryophyte research—current state and future directions PAULO E.A.S. CÂMARA1, MicHELine CARVALHO-SILVA1 & MicHAEL STecH2,3 1Departamento de Botânica, Universidade de Brasília, Brazil UnB; �[email protected]; http://orcid.org/0000-0002-3944-996X �[email protected]; https://orcid.org/0000-0002-2389-3804 2Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, Netherlands; 3Leiden University, Leiden, Netherlands �[email protected]; https://orcid.org/0000-0001-9804-0120 Abstract Botany is one of the oldest sciences done south of parallel 60 °S, although few professional botanists have dedicated themselves to investigating the Antarctic bryoflora. After the publications of liverwort and moss floras in 2000 and 2008, respectively, new species were described. Currently, the Antarctic bryoflora comprises 28 liverwort and 116 moss species. Furthermore, Antarctic bryology has entered a new phase characterized by the use of molecular tools, in particular DNA sequencing. Although the molecular studies of Antarctic bryophytes have focused exclusively on mosses, molecular data (fingerprinting data and/or DNA sequences) have already been published for 36 % of the Antarctic moss species. In this paper we review the current state of Antarctic bryological research, focusing on molecular studies and conservation, and discuss future questions of Antarctic bryology in the light of global challenges. Keywords: Antarctic flora, conservation, future challenges, molecular phylogenetics, phylogeography Introduction The Antarctic is the most pristine, but also most extreme region on Earth in terms of environmental conditions. -
Fossil Mosses: What Do They Tell Us About Moss Evolution?
Bry. Div. Evo. 043 (1): 072–097 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.7 Fossil mosses: What do they tell us about moss evolution? MicHAEL S. IGNATOV1,2 & ELENA V. MASLOVA3 1 Tsitsin Main Botanical Garden of the Russian Academy of Sciences, Moscow, Russia 2 Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia 3 Belgorod State University, Pobedy Square, 85, Belgorod, 308015 Russia �[email protected], https://orcid.org/0000-0003-1520-042X * author for correspondence: �[email protected], https://orcid.org/0000-0001-6096-6315 Abstract The moss fossil records from the Paleozoic age to the Eocene epoch are reviewed and their putative relationships to extant moss groups discussed. The incomplete preservation and lack of key characters that could define the position of an ancient moss in modern classification remain the problem. Carboniferous records are still impossible to refer to any of the modern moss taxa. Numerous Permian protosphagnalean mosses possess traits that are absent in any extant group and they are therefore treated here as an extinct lineage, whose descendants, if any remain, cannot be recognized among contemporary taxa. Non-protosphagnalean Permian mosses were also fairly diverse, representing morphotypes comparable with Dicranidae and acrocarpous Bryidae, although unequivocal representatives of these subclasses are known only since Cretaceous and Jurassic. Even though Sphagnales is one of two oldest lineages separated from the main trunk of moss phylogenetic tree, it appears in fossil state regularly only since Late Cretaceous, ca. -
Bryophytes: Indicators and Monitoring Agents of Pollution
NeBIO (2010) Vol. 1(1) Govindapyari et al . 35-41 GENERAL ARTICLE Bryophytes: indicators and monitoring agents of pollution H. Govindapyari, M. Leleeka, M. Nivedita and P. L. Uniyal Department of Botany, University of Delhi, Delhi – 110 007 Author for correspondence: [email protected], [email protected] Received: 17 September 2009; Revised and Accepted: 2 January 2010 ABSTRACT Bryophyte proves to be a potential bio-indicator of air pollution. The habitat diversity, structural simplicity, totipotency, rapid rate of multiplication and high metal accumulation capacity make bryophytes an ideal organism for pollution studies. The decline and absence of bryophyte populations especially epiphytes is a phenomenon primarily induced by air pollution caused by gaseous and particulate pollutants. Bryophytes are reliable indicators and monitors of air pollution as they are easy to handle and show a vast range of specific sensitivity and visible symptoms to pollutants greatly exceeding that of higher plants. KEY WORDS: Bryophyte, bio-indicator, air pollution, pollutants. Bryophytes are green land plants which lack a • which have the capacity to absorb and retain vascular system and are simple both morpho- pollutants in quantities much higher than those logically and anatomically. The growth potential in absorbed by other plant groups growing in the bryophytes is not as highly polarized as vascular same habitat. These plants trap and prevent plants. Bryophytes grow in a variety of habitats recycling of such pollutants in the ecosystem especially in moist places on soil, rocks, trunks and for different periods of time. Analysis of such branches of trees and fallen log. They obtain plants gives a fair idea about the degree of nutrients directly from substances dissolved in metal pollution. -
SURNAMES in CHILE a Study of the Population of Chile Through
Page 1 of 31 American Journal of Physical Anthropology 1 2 3 SURNAMES IN CHILE 4 5 A study of the population of Chile through isonymy 6 I. Barrai, A. Rodriguez-Larralde 2, J. Dipierri 1, E.Alfaro 1, N. Acevedo 3, 7 8 E. Mamolini, M. Sandri, A.Carrieri and C. Scapoli. 9 10 Dipartimento di Biologia ed Evoluzione, Università di Ferrara, 44121- Ferrara, Italy 11 1Instituto de Biología de la Altura, Universidad Nacional de Jujuy, 4600 – San Salvador De Jujuy, 12 13 Argentina. 14 2 15 Centro de Medicina Experimental, Laboratorio de Genetica Humana, IVIC, 1020A -Caracas, 16 Venezuela. 17 18 3Museo Nacional de Ciencias Naturales, Santiago, Chile 19 20 21 Running title: Surnames in Chile 22 23 24 25 26 Correspondence to: 27 Chiara Scapoli 28 Department of Biology and Evolution 29 30 University of Ferrara, 31 Via L. Borsari 46, - I-44121 Ferrara, Italy. 32 Telephone: +39 0532 455744; FAX: : +39 0532 249761 33 Email: [email protected] 34 35 36 Number of text pages: 15 37 Literature pages: 4 38 39 Number of Tables : 2 40 41 Number of Figures: 7 42 43 44 KEYWORDS : Chile, Population Structure, Isonymy, Inbreeding, Isolation by distance 45 46 47 ACKNOWLEDGMENTS: The authors are grateful to the Director of the Servicio Electoral de la 48 49 Republica de Chile Sr. Juan Ignacio Garcia Rodríguez, who made the data available, and to Sr. 50 51 Dr.Ginés Mario Gonzalez Garcia, Embajador de la Republica Argentina en Chile. The work was 52 supported by grants of the Italian Ministry of Universities and Research (MIUR) to Chiara Scapoli. -
Bryophytes of Azorean Parks and Gardens (I): “Reserva Florestal De Recreio Do Pinhal Da Paz” - São Miguel Island
Arquipelago - Life and Marine Sciences ISSN: 0873-4704 Bryophytes of Azorean parks and gardens (I): “Reserva Florestal de Recreio do Pinhal da Paz” - São Miguel Island CLARA POLAINO-MARTIN, ROSALINA GABRIEL, PAULO A.V. BORGES, RICARDO CRUZ AND ISABEL S. ALBERGARIA Polaino-Martin, C.P., R. Gabriel, P.A.V. Borges, R. Cruz and I.S. Albergaria 2020. Bryophytes of Azorean parks and gardens (I): “Reserva Florestal de Recreio do Pinhal da Paz” - São Miguel Island. Arquipelago. Life and Marine Sciences 37: 1 – 20. https://doi.org/10.25752/arq.23643 Historic urban parks and gardens are increasingly being considered as interesting refuges for a great number of species, including some rare taxa, otherwise almost absent from urban areas, such as many bryophytes and other biota that are not their main focus. After a bibliographic work, the "Reserva Florestal de Recreio do Pinhal da Paz" (RFR-PP), in São Miguel Island (Azores), stood out as one of the least studied areas of the region, without any bryophyte’ references. Thus, the aim of this study was to identify the most striking bryophyte species present along the main visitation track of RFR-PP, in order to increase its biodiversity knowledge. Bryophytes growing on rocks, soil or tree bark were collected ad- hoc, in 17 sites, ca. 100 m apart from each other. In total, 43 species were identified: 23 mosses, 19 liverworts, and one hornwort, encompassing five classes, 15 orders and 27 families. Seven species are endemic from Europe and three from Macaronesia. No invasive bryophytes were found in the surveyed area. -
NEW DATA ABOUT MOSSES on the SVALBARD GLACIERS Olga
NEW DATA ABOUT MOSSES ON THE SVALBARD GLACIERS Olga Belkina Polar-Alpine Botanical Garden-Institute, Kola Science Center of the Russian Academy of Sciences, Apatity, Murmansk Province, Russia; e-mail: [email protected] Rapid melting and retreat of glaciers in the Arctic is a cause of sustainable long‐ In Svalbard moss populations were found on 9 glaciers. In 2012, during re‐examination of the populations a few term existence of ablation zone on them. Sometimes these areas are the habitats In 2007 B.R.Mavlyudov collected one specimen on individuals of Bryum cryophilum Mårtensson and some plants of some mosses partly due to good availability of water and cryoconite Bertilbreen (Paludella squarrosa (Hedw.) Brid.) and of Sanionia uncinata were found among H. polare shoots in substratum. 14 species were found in this unusual habitat on Alaska and Iceland: some specimens on Austre Grønfjordbreen (Ceratodon some large cushions. Therefore the next stage of cushion Andreaea rupestris Hedw., Ceratodon purpureus (Hedw.) Brid., Ditrichum purpureus (Hedw.) Brid., Warnstorfia sarmentosa succession had begun –emergence of a di‐ and multi‐species flexicaule (Schwaegr.) Hampe, Pohlia nutans (Hedw.) Lindb., Polytrichum (Wahlenb.) Hedenäs, Sanionia uncinata (Hedw.) community. A similar process was observed earlier on the juniperinum Hedw. (Benninghoff, 1955), Racomitrium fasciculare (Hedw.) Brid. Loeske, Hygrohypnella polare (Lindb.) Ignatov & bone of a mammal that was lying on the same glacier. (=Codriophorus fascicularis (Hedw.) Bendarek‐Ochyra et Ochyra) (Shacklette, Ignatova.). Ceratodon purpureus settled in center of almost spherical 1966), Drepanocladus berggrenii (C.Jens.) Broth. (Heusser, 1972), Racomitrium In 2009 populations of two latter species were studied cushion of Sanionia uncinata on the both butt‐ends of the crispulum var. -
Volume 1, Chapter 2-7: Bryophyta
Glime, J. M. 2017. Bryophyta – Bryopsida. Chapt. 2-7. In: Glime, J. M. Bryophyte Ecology. Volume 1. Physiological Ecology. Ebook 2-7-1 sponsored by Michigan Technological University and the International Association of Bryologists. Last updated 10 January 2019 and available at <http://digitalcommons.mtu.edu/bryophyte-ecology/>. CHAPTER 2-7 BRYOPHYTA – BRYOPSIDA TABLE OF CONTENTS Bryopsida Definition........................................................................................................................................... 2-7-2 Chromosome Numbers........................................................................................................................................ 2-7-3 Spore Production and Protonemata ..................................................................................................................... 2-7-3 Gametophyte Buds.............................................................................................................................................. 2-7-4 Gametophores ..................................................................................................................................................... 2-7-4 Location of Sex Organs....................................................................................................................................... 2-7-6 Sperm Dispersal .................................................................................................................................................. 2-7-7 Release of Sperm from the Antheridium..................................................................................................... -
Unidades Sedimentarias Cenozoicas De La Cuenca Del Rio Loa En La Pampa Del Tamarugal, Region De Antofagasta, Chile
ESTRATlGRAFIA DE LAS -UNIDADES SEDIMENTARIAS CENOZOICAS DE LA CUENCA DEL RIO LOA EN LA PAMPA DEL TAMARUGAL, REGION DE ANTOFAGASTA, CHILE. JOSE A. NARANJO Servo Nac. Geol. y Minería, Casilla 10465, Santigo, Chile. ROLAND. P. PASKOFF Département de Géographie, Université de Tunis, 94, Bd. du 9 avril1938, Túnez. RESUMEN El relleno sedimentario de la cuenca del río Loa, en la Pampa del Tamarugal, es de gran complejidad. En él es posible distinguir al menos seis unidades diferentes. Su génesis se explicaría por la intervención e interacción de cambios climáticos en un ambiente árido, y de movimientos tectónicos durante el Cenozoico. ABSTRACT The sedimentary filling of the Pampa del Tamarugal in the Río Loa basin is compleXo At lcast six different units can be distinguished. Interferences between climatic changes in an arid environment and tectonic move ments account for their genesis. INTRODUCCION Durante mucho tiempo se ha pensado que el voluminoso relleno de depósitos aluviales y evapo ríticos de la depresión seguida por el río Loa, entre Calama y Quillagua (Fig. 1), correspondería a una sola formación, la Formación El Loa (Brüggen, 1950; Fuenzalida, 1957). Esta opinión prevalece todavía en estudios geológicos recientes (Boben rieth, 1980; Boric, 1980; Maksaev y Marinovic 1980), pese a que, en 1975, Rieu llamó la atención sobre la complejidad de los depósitos que rellenan la cuenca. Efectivamente, es posible distinguir va rias unidades estratigráficas, claramente separadas por discordancias de erosión (Fig. 2). Recientemente, Naranjo y Paskoff (1981) han caracterizado la estratigrafía del Cenozoico del sec tor comprendido entre Chiuchiu y Calama (22°20'- 22°27'S). -
An Annotated Checklist of Tasmanian Mosses
15 AN ANNOTATED CHECKLIST OF TASMANIAN MOSSES by P.I Dalton, R.D. Seppelt and A.M. Buchanan An annotated checklist of the Tasmanian mosses is presented to clarify the occurrence of taxa within the state. Some recently collected species, for which there are no published records, have been included. Doubtful records and excluded speciei. are listed separately. The Tasmanian moss flora as recognised here includes 361 species. Key Words: mosses, Tasmania. In BANKS, M.R. et al. (Eds), 1991 (3l:iii): ASPECTS OF TASMANIAN BOTANY -- A TR1BUn TO WINIFRED CURTIS. Roy. Soc. Tasm. Hobart: 15-32. INTRODUCTION in recent years previously unrecorded species have been found as well as several new taxa described. Tasmanian mosses received considerable attention We have assigned genera to families followi ng Crosby during the early botanical exploration of the antipodes. & Magill (1981 ), except where otherwise indicated in One of the earliest accounts was given by Wilson (1859), the case of more recent publications. The arrangement who provided a series of descriptions of the then-known of families, genera and species is in alphabetic order for species, accompanied by coloured illustrations, as ease of access. Taxa known to occur in Taslnania ami Part III of J.D. Hooker's Botany of the Antarctic its neighbouring islands only are listed; those for Voyage. Although there have been a number of papers subantarctic Macquarie Island (politically part of since that time, two significant compilations were Tasmania) are not treated and have been presented published about the tum of the century. The first was by elsewhere (Seppelt 1981). -
Total of 10 Pages Only May Be Xeroxed
CENTRE FOR NEWFOUNDLAND STUDIES TOTAL OF 10 PAGES ONLY MAY BE XEROXED (Without Author's Permission) ,, l • ...J ..... The Disjunct Bryophyte Element of the Gulf of St. Lawrence Region: Glacial and Postglacial Dispersal and Migrational Histories By @Rene J. Belland B.Sc., M.Sc. A thesis submitted to the School of Graduate Studies in partial fulfilment of the requirements for the degree of Doctor of Philosophy Department of Biology Memorial University of Newfoundland December, 1Q84 St. John's Newfoundland Abstract The Gulf St. Lawrence region has a bryophyte flora of 698 species. Of these 267 (38%) are disjunct to this region from western North America, eastern Asia, or Europe. The Gulf of St. Lawrence and eastern North American distributions of the disjuncts were analysed and their possible migrational and dispersal histories during and after the Last Glaciation (Wisconsin) examined. Based on eastern North American distribution patterns, the disjuncts fell into 22 sub elements supporting five migrational/ dispersal histories or combinations of these : (1) migration from the south, (2) migration from the north, (3) migration from the west, (4) survival in refugia, and (5) introduction by man. The largest groups of disjuncts had eastern North American distributions supporting either survival of bryophytes in Wisconsin ice-free areas of the Gulf of St. Lawrence or postglacial migration to the Gulf from the south. About 26% of the disjuncts have complex histories and their distributions support two histories. These may have migrated to the Gulf from the west and/or north, or from the west and/or survived glaciation in Gulf ice-free areas.