Die Flechten Im Nationalpark Harz Titelbild: Dr
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Checklist of Calicioid Lichens and Fungi for Genera with Members in Temperate Western North America Draft: 2012-03-13
Draft: 2012-03-13 Checklist of Calicioids – E. B. Peterson Checklist of Calicioid Lichens and Fungi For Genera with Members in Temperate Western North America Draft: 2012-03-13 by E. B. Peterson Calicium abietinum, EBP#4640 1 Draft: 2012-03-13 Checklist of Calicioids – E. B. Peterson Genera Acroscyphus Lév. Brucea Rikkinen Calicium Pers. Chaenotheca Th. Fr. Chaenothecopsis Vainio Coniocybe Ach. = Chaenotheca "Cryptocalicium" – potentially undescribed genus; taxonomic placement is not known but there are resemblances both to Mycocaliciales and Onygenales Cybebe Tibell = Chaenotheca Cyphelium Ach. Microcalicium Vainio Mycocalicium Vainio Phaeocalicium A.F.W. Schmidt Sclerophora Chevall. Sphinctrina Fr. Stenocybe (Nyl.) Körber Texosporium Nádv. ex Tibell & Hofsten Thelomma A. Massal. Tholurna Norman Additional genera are primarily tropical, such as Pyrgillus, Tylophoron About the Species lists Names in bold are believed to be currently valid names. Old synonyms are indented and listed with the current name following (additional synonyms can be found in Esslinger (2011). Names in quotes are nicknames for undescribed species. Names given within tildes (~) are published, but may not be validly published. Underlined species are included in the checklist for North America north of Mexico (Esslinger 2011). Names are given with authorities and original citation date where possible, followed by a colon. Additional citations are given after the colon, followed by a series of abbreviations for states and regions where known. States and provinces use the standard two-letter abbreviation. Regions include: NAm = North America; WNA = western North America (west of the continental divide); Klam = Klamath Region (my home territory). For those not known from North America, continental distribution may be given: SAm = South America; EUR = Europe; ASIA = Asia; Afr = Africa; Aus = Australia. -
Appendix K. Survey and Manage Species Persistence Evaluation
Appendix K. Survey and Manage Species Persistence Evaluation Establishment of the 95-foot wide construction corridor and TEWAs would likely remove individuals of H. caeruleus and modify microclimate conditions around individuals that are not removed. The removal of forests and host trees and disturbance to soil could negatively affect H. caeruleus in adjacent areas by removing its habitat, disturbing the roots of host trees, and affecting its mycorrhizal association with the trees, potentially affecting site persistence. Restored portions of the corridor and TEWAs would be dominated by early seral vegetation for approximately 30 years, which would result in long-term changes to habitat conditions. A 30-foot wide portion of the corridor would be maintained in low-growing vegetation for pipeline maintenance and would not provide habitat for the species during the life of the project. Hygrophorus caeruleus is not likely to persist at one of the sites in the project area because of the extent of impacts and the proximity of the recorded observation to the corridor. Hygrophorus caeruleus is likely to persist at the remaining three sites in the project area (MP 168.8 and MP 172.4 (north), and MP 172.5-172.7) because the majority of observations within the sites are more than 90 feet from the corridor, where direct effects are not anticipated and indirect effects are unlikely. The site at MP 168.8 is in a forested area on an east-facing slope, and a paved road occurs through the southeast part of the site. Four out of five observations are more than 90 feet southwest of the corridor and are not likely to be directly or indirectly affected by the PCGP Project based on the distance from the corridor, extent of forests surrounding the observations, and proximity to an existing open corridor (the road), indicating the species is likely resilient to edge- related effects at the site. -
11701-19-A0558 RVH Landmarke 4 Engl
Landmark 4 Brocken ® On the 17th of November, 2015, during the 38th UNESCO General Assembly, the 195 member states of the United Nations resolved to introduce a new title. As a result, Geoparks can be distinguished as UNESCO Global Geoparks. As early as 2004, 25 European and Chinese Geoparks had founded the Global Geoparks Network (GGN). In autumn of that year Geopark Harz · Braunschweiger Land · Ostfalen became part of the network. In addition, there are various regional networks, among them the European Geoparks Network (EGN). These coordinate international cooperation. 22 Königslutter 28 ® 1 cm = 26 km 20 Oschersleben 27 18 14 Goslar Halberstadt 3 2 1 8 Quedlinburg 4 OsterodeOsterodee a.H.a.Ha H.. 9 11 5 13 15 161 6 10 17 19 7 Sangerhausen Nordhausen 12 21 In the above overview map you can see the locations of all UNESCO Global Geoparks in Europe, including UNESCO Global Geopark Harz · Braunschweiger Land · Ostfalen and the borders of its parts. UNESCO-Geoparks are clearly defi ned, unique areas, in which geosites and landscapes of international geological importance are found. The purpose of every UNESCO-Geopark is to protect the geological heritage and to promote environmental education and sustainable regional development. Actions which can infl ict considerable damage on geosites are forbidden by law. A Highlight of a Harz Visit 1 The Brocken A walk up the Brocken can begin at many of the Landmark’s Geopoints, or one can take the Brockenbahn from Wernigerode or Drei Annen-Hohne via Schierke up to the highest mountain of the Geopark (1,141 meters a.s.l.). -
11701-19-A0655 RVH Landmarke 11 Englisch
Landmark 11 Old Fortress Osterode ® On the 17th of November, 2015, during the 38th UNESCO General Assembly, the 195 member states of the United Nations resolved to introduce a new title. As a result, Geoparks can be distinguished as UNESCO Global Geoparks. As early as 2004, 25 European and Chinese Geoparks had founded the Global Geoparks Network (GGN). In autumn of that year Geopark Harz · Braunschweiger Land · Ostfalen became part of the network. In addition, there are various regional networks, among them the European Geoparks Network (EGN). These coordinate international cooperation. 22 Königslutter 28 ® 1 cm = 26 km 20 Oschersleben 27 18 14 Goslar Halberstadt 3 2 1 8 Quedlinburg 4 OsterodeOOssterorodd a.H. 9 1111 5 13 15 16 6 10 17 19 7 Sangerhausen Nordhausen 12 21 In the above overview map you can see the locations of all UNESCO Global Geoparks in Europe, including UNESCO Global Geopark Harz · Braunschweiger Land · Ostfalen and the borders of its parts. UNESCO-Geoparks are clearly defi ned, unique areas, in which geosites and landscapes of international geological importance are found. The purpose of every UNESCO-Geopark is to protect the geological heritage and to promote environmental education and sustainable regional development. Actions which can infl ict considerable damage on geosites are forbidden by law. River Gravel & Gypsum Mortar 1 Old Fortress and Town Wall Originally the „Alte Burg” (“Old Fortress“) served to defend the crossing point over the Söse stream and the adjacent market settlement. Since its first documented mention in the 12th century it was in Welp possession. In the 14th/15th centuries it was therewith also the seat of the dukes who reigned over the principality of Grubenhagen and then, finally, it was the widows’ residence. -
Taxonomy of Cladonia Angustiloba and Related Species
Taxonomy of Cladonia angustiloba and related species Raquel PINO-BODAS, Ana Rosa BURGAZ, Teuvo AHTI, Soili STENROOS R. Pino-Bodas, Real Jardín Botánico de Madrid, CSIC, Spain, [email protected] A.R. Burgaz, Departamento de Biología Vegetal 1, Universidad Complutense de Madrid, Spain T. Ahti, S. Stenroos, Museum, Finnish Museum of Natural History, FI-00014 University of Helsinki, Finland Abstract: The lichen species Cladonia angustiloba is characterized by a well- developed primary thallus, and narrow squamules, which show deep incisions and presence of usnic and fumarprotocetraric acids. Morphologically it is similar to C. foliacea and C. convoluta, from which it can be distiguished by the squamule size and morphology. In this study, the species delimitation within the C. foliacea complex has been studied by sequencing three loci, ITS rDNA, cox1 and rpb2. The data were analyzed by means of phylogenetic and species delimitation methods (GMYC, PTP, ABGD and BPP). Our results show that none of the three species is monophyletic. Most of the species delimitation methods did not support the current species as evolutionary lineages. Only some of the BPP analyses supported that C. angustiloba is a different species from C. foliacea and C. convoluta. However, the hypothesis that considers the C. foliacea complex as constituted by a unique species obtained the best Bayes Factor value. Therefore, C. angustiloba and C. convoluta are synonymized with C. foliacea. A new, thoroughly checked synonymy with typifications of the whole C. foliacea complex is presented. An updated survey of the world distribution data was compiled. Key words: Cladonia, lichens, Macaronesia, molecular systematics, species delimitation Introduction 1 Cladonia is one of the most diverse macrolichen genera, with 470 species recognized at present (Ahti 2017, pers. -
BLS Bulletin 111 Winter 2012.Pdf
1 BRITISH LICHEN SOCIETY OFFICERS AND CONTACTS 2012 PRESIDENT B.P. Hilton, Beauregard, 5 Alscott Gardens, Alverdiscott, Barnstaple, Devon EX31 3QJ; e-mail [email protected] VICE-PRESIDENT J. Simkin, 41 North Road, Ponteland, Newcastle upon Tyne NE20 9UN, email [email protected] SECRETARY C. Ellis, Royal Botanic Garden, 20A Inverleith Row, Edinburgh EH3 5LR; email [email protected] TREASURER J.F. Skinner, 28 Parkanaur Avenue, Southend-on-Sea, Essex SS1 3HY, email [email protected] ASSISTANT TREASURER AND MEMBERSHIP SECRETARY H. Döring, Mycology Section, Royal Botanic Gardens, Kew, Richmond, Surrey TW9 3AB, email [email protected] REGIONAL TREASURER (Americas) J.W. Hinds, 254 Forest Avenue, Orono, Maine 04473-3202, USA; email [email protected]. CHAIR OF THE DATA COMMITTEE D.J. Hill, Yew Tree Cottage, Yew Tree Lane, Compton Martin, Bristol BS40 6JS, email [email protected] MAPPING RECORDER AND ARCHIVIST M.R.D. Seaward, Department of Archaeological, Geographical & Environmental Sciences, University of Bradford, West Yorkshire BD7 1DP, email [email protected] DATA MANAGER J. Simkin, 41 North Road, Ponteland, Newcastle upon Tyne NE20 9UN, email [email protected] SENIOR EDITOR (LICHENOLOGIST) P.D. Crittenden, School of Life Science, The University, Nottingham NG7 2RD, email [email protected] BULLETIN EDITOR P.F. Cannon, CABI and Royal Botanic Gardens Kew; postal address Royal Botanic Gardens, Kew, Richmond, Surrey TW9 3AB, email [email protected] CHAIR OF CONSERVATION COMMITTEE & CONSERVATION OFFICER B.W. Edwards, DERC, Library Headquarters, Colliton Park, Dorchester, Dorset DT1 1XJ, email [email protected] CHAIR OF THE EDUCATION AND PROMOTION COMMITTEE: S. -
Lichens and Associated Fungi from Glacier Bay National Park, Alaska
The Lichenologist (2020), 52,61–181 doi:10.1017/S0024282920000079 Standard Paper Lichens and associated fungi from Glacier Bay National Park, Alaska Toby Spribille1,2,3 , Alan M. Fryday4 , Sergio Pérez-Ortega5 , Måns Svensson6, Tor Tønsberg7, Stefan Ekman6 , Håkon Holien8,9, Philipp Resl10 , Kevin Schneider11, Edith Stabentheiner2, Holger Thüs12,13 , Jan Vondrák14,15 and Lewis Sharman16 1Department of Biological Sciences, CW405, University of Alberta, Edmonton, Alberta T6G 2R3, Canada; 2Department of Plant Sciences, Institute of Biology, University of Graz, NAWI Graz, Holteigasse 6, 8010 Graz, Austria; 3Division of Biological Sciences, University of Montana, 32 Campus Drive, Missoula, Montana 59812, USA; 4Herbarium, Department of Plant Biology, Michigan State University, East Lansing, Michigan 48824, USA; 5Real Jardín Botánico (CSIC), Departamento de Micología, Calle Claudio Moyano 1, E-28014 Madrid, Spain; 6Museum of Evolution, Uppsala University, Norbyvägen 16, SE-75236 Uppsala, Sweden; 7Department of Natural History, University Museum of Bergen Allégt. 41, P.O. Box 7800, N-5020 Bergen, Norway; 8Faculty of Bioscience and Aquaculture, Nord University, Box 2501, NO-7729 Steinkjer, Norway; 9NTNU University Museum, Norwegian University of Science and Technology, NO-7491 Trondheim, Norway; 10Faculty of Biology, Department I, Systematic Botany and Mycology, University of Munich (LMU), Menzinger Straße 67, 80638 München, Germany; 11Institute of Biodiversity, Animal Health and Comparative Medicine, College of Medical, Veterinary and Life Sciences, University of Glasgow, Glasgow G12 8QQ, UK; 12Botany Department, State Museum of Natural History Stuttgart, Rosenstein 1, 70191 Stuttgart, Germany; 13Natural History Museum, Cromwell Road, London SW7 5BD, UK; 14Institute of Botany of the Czech Academy of Sciences, Zámek 1, 252 43 Průhonice, Czech Republic; 15Department of Botany, Faculty of Science, University of South Bohemia, Branišovská 1760, CZ-370 05 České Budějovice, Czech Republic and 16Glacier Bay National Park & Preserve, P.O. -
Taxonomy of Bryoria Section Implexae (Parmeliaceae, Lecanoromycetes) in North America and Europe, Based on Chemical, Morphological and Molecular Data
Ann. Bot. Fennici 51: 345–371 ISSN 0003-3847 (print) ISSN 1797-2442 (online) Helsinki 22 September 2014 © Finnish Zoological and Botanical Publishing Board 2014 Taxonomy of Bryoria section Implexae (Parmeliaceae, Lecanoromycetes) in North America and Europe, based on chemical, morphological and molecular data Saara Velmala1,*, Leena Myllys1, Trevor Goward2, Håkon Holien3 & Pekka Halonen4 1) Botanical Museum, Finnish Museum of Natural History, P.O. Box 7, FI-00014 University of Helsinki, Finland (*corresponding author’s e-mail: [email protected]) 2) UBC Herbarium, Beaty Museum, University of British Columbia, Vancouver, BC V6T 1Z4, Canada (mailing address: Enlichened Consulting Ltd., 5369 Clearwater Valley Road, Upper Clearwater, BC V0E 1N1, Canada) 3) Nord-Trøndelag University College, Serviceboks 2501, N-7729 Steinkjer, Norway 4) Botanical Museum, Department of Biology, P.O. Box 3000, FI-90014 University of Oulu, Finland Received 31 Jan. 2014, final version received 13 June 2014, accepted 18 June 2014 Velmala, S., Myllys, L., Goward, T., Holien, H. & Halonen, P. 2014: Taxonomy of Bryoria section Implexae (Parmeliaceae, Lecanoromycetes) in North America and Europe, based on chemical, morphological and molecular data. — Ann. Bot. Fennici 51: 345–371. Ninety-seven ingroup specimens of Bryoria section Implexae (Parmeliaceae, Leca- noromycetes) were studied using molecular, chemical, morphological and geographic characters. The molecular data included nuclear ribosomal markers (ITS, IGS) and the partial glyceraldehyde-3-phosphate dehydrogenase (GAPDH) gene. In addition to par- simony analyses, a haplotype network was constructed. Phylogenetic analyses strongly supported the monophyly of the section Implexae. The specimens were grouped into two monophyletic clades. Clade 1 encompassed all esorediate material from North America, whereas Clade 2 included both sorediate North American material and all European material. -
Lichens and Allied Fungi of the Indiana Forest Alliance
2017. Proceedings of the Indiana Academy of Science 126(2):129–152 LICHENS AND ALLIED FUNGI OF THE INDIANA FOREST ALLIANCE ECOBLITZ AREA, BROWN AND MONROE COUNTIES, INDIANA INCORPORATED INTO A REVISED CHECKLIST FOR THE STATE OF INDIANA James C. Lendemer: Institute of Systematic Botany, The New York Botanical Garden, Bronx, NY 10458-5126 USA ABSTRACT. Based upon voucher collections, 108 lichen species are reported from the Indiana Forest Alliance Ecoblitz area, a 900 acre unit in Morgan-Monroe and Yellowwood State Forests, Brown and Monroe Counties, Indiana. The lichen biota of the study area was characterized as: i) dominated by species with green coccoid photobionts (80% of taxa); ii) comprised of 49% species that reproduce primarily with lichenized diaspores vs. 44% that reproduce primarily through sexual ascospores; iii) comprised of 65% crustose taxa, 29% foliose taxa, and 6% fruticose taxa; iv) one wherein many species are rare (e.g., 55% of species were collected fewer than three times) and fruticose lichens other than Cladonia were entirely absent; and v) one wherein cyanolichens were poorly represented, comprising only three species. Taxonomic diversity ranged from 21 to 56 species per site, with the lowest diversity sites concentrated in riparian corridors and the highest diversity sites on ridges. Low Gap Nature Preserve, located within the study area, was found to have comparable species richness to areas outside the nature preserve, although many species rare in the study area were found only outside preserve boundaries. Sets of rare species are delimited and discussed, as are observations as to the overall low abundance of lichens on corticolous substrates and the presence of many unhealthy foliose lichens on mature tree boles. -
<I> Lecanoromycetes</I> of Lichenicolous Fungi Associated With
Persoonia 39, 2017: 91–117 ISSN (Online) 1878-9080 www.ingentaconnect.com/content/nhn/pimj RESEARCH ARTICLE https://doi.org/10.3767/persoonia.2017.39.05 Phylogenetic placement within Lecanoromycetes of lichenicolous fungi associated with Cladonia and some other genera R. Pino-Bodas1,2, M.P. Zhurbenko3, S. Stenroos1 Key words Abstract Though most of the lichenicolous fungi belong to the Ascomycetes, their phylogenetic placement based on molecular data is lacking for numerous species. In this study the phylogenetic placement of 19 species of cladoniicolous species lichenicolous fungi was determined using four loci (LSU rDNA, SSU rDNA, ITS rDNA and mtSSU). The phylogenetic Pilocarpaceae analyses revealed that the studied lichenicolous fungi are widespread across the phylogeny of Lecanoromycetes. Protothelenellaceae One species is placed in Acarosporales, Sarcogyne sphaerospora; five species in Dactylosporaceae, Dactylo Scutula cladoniicola spora ahtii, D. deminuta, D. glaucoides, D. parasitica and Dactylospora sp.; four species belong to Lecanorales, Stictidaceae Lichenosticta alcicorniaria, Epicladonia simplex, E. stenospora and Scutula epiblastematica. The genus Epicladonia Stictis cladoniae is polyphyletic and the type E. sandstedei belongs to Leotiomycetes. Phaeopyxis punctum and Bachmanniomyces uncialicola form a well supported clade in the Ostropomycetidae. Epigloea soleiformis is related to Arthrorhaphis and Anzina. Four species are placed in Ostropales, Corticifraga peltigerae, Cryptodiscus epicladonia, C. galaninae and C. cladoniicola -
DWT 2014 - MI 01 Am Grünen Band Von Der Eckerquelle Zum Stausee
Wandern DWT 2014 - MI 01 Am Grünen Band von der Eckerquelle zum Stausee Länge: 18 km Start: Torfhaus Steigung:+ 179 m / - 690 m Ziel: Bad Harzburg Dauer: ca. 7 bis 8 Stunden Überblick passierend, zum und durch den westlich des Scharfensteins gelegenen Eckerstausee. Unterhalb von Harzklub-Wandertipp zum Deutschen Wandertag 2014. Staumauer und dortigem Wasserkraftwerk verläuft die Ecker Hinweis: Die Wanderführer behalten sich vor, beim offiziellen in ihrem Mittellauf durch das tief eingeschnittene Eckertal und DWT-Termin die Tour bei Bedarf zu modifizieren. passiert dabei die westlich befindliche Muxklippe sowie etwas weiter nordöstlich ebenfalls westlich des Flusses die Rabenklippe und östlich gegenüberliegend die Taubenklippe. Ein Stück unterhalb davon fließt sie westlich an der Ruine Ahlsburg vorbei. Anschließend verläuft die Ecker ab der seit dem 19. Jahrhundert im mittleren Eckertal stehenden Pappenfabrik in einem schmalen, aus dem Nationalpark ausgeklammerten Streifen weiter entlang der Naturparkgrenze nach Nordnordosten. Dabei verlässt sie den Harz und den Nationalpark. In ihrem Unterlauf verläuft die Ecker im nördlichen Harzvorland zwischen Eckertal (Ortsteil von Bad Harzburg; Niedersachsen) und Stapelburg (Gemeindeteil von Nordharz; Sachsen-Anhalt) hindurch, von wo an sie sich nach Nordwesten wendet. Danach fließt sie durch Abbenrode (zur Gemeinde Nordharz), wonach sie den Naturpark verlässt. Eckertal Dann unterquert sie die Bundesstraße 6n, einmal die Bahnstrecke Stapelburg-Vienenburg und zweimal Tourbeschreibung die Bahnstrecke -
Flächennutzungsplan Einheitsgemeinde Nordharz
FLÄCHENNUTZUNGSPLAN EINHEITSGEMEINDE NORDHARZ LANDKREIS HARZ BEGRÜNDUNG mit den Ortsteilen Abbenrode Danstedt Heudeber Langeln Schmatzfeld Stapelburg Veckenstedt Wasserleben Conterra Planungsgesellschaft mbH Karsten-Balder-Stieg 9, 38640 Goslar Harzburger Straße 24, 38871 Ilsenburg Tel: 05321/21205 039452/84193 Fax: 05321/29563 039452/84194 E-Mail: [email protected] Internet: www.conterra-goslar.de Stand Entwurf Flächennutzungsplan Einheitsgemeinde Nordharz Landkreis Harz I n h a l t Abkürzungsverzeichnis 5 Gesetzes- Verordnungs- und Normenverzeichnis 6 Quellenverzeichnis 6 Tabellenverzeichnis 6 Teil A Begründung ............................................................................................................................ 7 1 Vorbemerkungen ................................................................................................................................. 7 1.1 Ausgangssituation ........................................................................................................................ 7 1.2 Aufgaben und Ziele der Flächennutzungsplanung ...................................................................... 7 1.3 Rechtliche Grundlagen ................................................................................................................ 8 1.4 Planungsanlass ............................................................................................................................ 9 1.5 Redaktionelle Vorbemerkung ...................................................................................................