Trachycystis Montissalinarum Spec
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Chapter 4 Major Vegetation Types of the Soutpansberg Conservancy and the Blouberg Nature Reserve
Chapter 4 Major Vegetation Types of the Soutpansberg Conservancy and the Blouberg Nature Reserve (Research paper submitted for publication in Koedoe) 25 Major Vegetation Types of the Soutpansberg Conservancy and the Blouberg Nature Reserve T.H.C. Mostert1, G.J. Bredenkamp1, H.L. Klopper1, C. Verwey1, R.E. Mostert2 and N. Hahn3 1. African Vegetation and Plant Diversity Research Centre, Department of Botany, University of Pretoria, Pretoria, 0002. 2. South African Biodiversity Institute, Private Bag X101, Pretoria, 0001. 3. Herbarium Soutpansbergensis, P.O. Box 1734, Makhado, 0920. Abstract The Major Vegetation Types and plant communities of the Soutpansberg Centre of Endemism are described in detail with special reference to the Soutpansberg Conservancy and the Blouberg Nature Reserve. Phytosociological data from 466 sample plots were ordinated using a Detrended Correspondence Analysis (DECORANA) and classified using Two–way Indicator Species Analysis (TWINSPAN). The resulting classification was further refined with table–sorting procedures based on the Braun–Blanquet floristic–sociological approach of vegetation classification using MEGATAB. Eight Major Vegetation Types were identified and described as Eragrostis lehmanniana var. lehmanniana–Sclerocarya birrea subsp. caffra BNR Northern Plains Bushveld, Euclea divinorum–Acacia tortilis BNR Southern Plains Bushveld, Englerophytum magalismontanum–Combretum molle BNR Mountain Bushveld, Adansonia digitata–Acacia nigrescens Soutpansberg Arid Northern Bushveld, Catha edulis–Flueggia virosa Soutpansberg Moist Mountain Thickets, Diplorhynchus condylocarpon–Burkea africana Soutpansberg Leached Sandveld, Rhus rigida var. rigida–Rhus magalismontanum subsp. coddii Soutpansberg Mistbelt Vegetation and Xymalos monospora–Rhus chirendensis Soutpansberg Forest Vegetation. 26 Introduction The Soutpansberg Conservancy (SC) and the Blouberg Nature Reserve (BNR) reveal extremely rich diversities of plant communities relative to the sizes of these conservation areas (Van Wyk & Smith 2001). -
Major Vegetation Types of the Soutpansberg Conservancy and the Blouberg Nature Reserve, South Africa
Original Research MAJOR VEGETATION TYPES OF THE SOUTPANSBERG CONSERVANCY AND THE BLOUBERG NATURE RESERVE, SOUTH AFRICA THEO H.C. MOSTERT GEORGE J. BREDENKAMP HANNES L. KLOPPER CORNIE VERWEy 1African Vegetation and Plant Diversity Research Centre Department of Botany University of Pretoria South Africa RACHEL E. MOSTERT Directorate Nature Conservation Gauteng Department of Agriculture Conservation and Environment South Africa NORBERT HAHN1 Correspondence to: Theo Mostert e-mail: [email protected] Postal Address: African Vegetation and Plant Diversity Research Centre, Department of Botany, University of Pretoria, Pretoria, 0002 ABSTRACT The Major Megetation Types (MVT) and plant communities of the Soutpansberg Centre of Endemism are described in detail, with special reference to the Soutpansberg Conservancy and the Blouberg Nature Reserve. Phytosociological data from 442 sample plots were ordinated using a DEtrended CORrespondence ANAlysis (DECORANA) and classified using TWo-Way INdicator SPecies ANalysis (TWINSPAN). The resulting classification was further refined with table-sorting procedures based on the Braun–Blanquet floristic–sociological approach of vegetation classification using MEGATAB. Eight MVT’s were identified and described asEragrostis lehmanniana var. lehmanniana–Sclerocarya birrea subsp. caffra Blouberg Northern Plains Bushveld, Euclea divinorum–Acacia tortilis Blouberg Southern Plains Bushveld, Englerophytum magalismontanum–Combretum molle Blouberg Mountain Bushveld, Adansonia digitata–Acacia nigrescens Soutpansberg -
Gastropoda: Pulmonata: Achatinellidae) 1
Published online: 29 May 2015 ISSN (online): 2376-3191 Records of the Hawaii Biological Survey for 2014. Part I: 49 Articles. Edited by Neal L. Evenhuis & Scott E. Miller. Bishop Museum Occasional Papers 116: 49 –51 (2015) Rediscovery of Auriculella pulchra Pease, 1868 (Gastropoda: Pulmonata: Achatinellidae) 1 NORINe W. Y eUNg 2, D ANIel CHUNg 3 Bishop Museum, 1525 Bernice Street, Honolulu, Hawai‘i 96817-2704, USA; emails: [email protected], [email protected] DAvID R. S ISCHO Department of Land and Natural Resources, 1151 Punchbowl Street, Rm. 325, Honolulu, Hawai‘i 96813, USA; email: [email protected] KeNNetH A. H AYeS 2,3 Howard University, 415 College Street NW, Washington, DC 20059, USA; email: [email protected] Hawaii supports one of the world’s most spectacular land snail radiations and is a diversity hotspot (Solem 1983, 1984, Cowie 1996a, b). Unfortunately, much of the Hawaiian land snail fauna has been lost, with overall extinction rates as high as ~70% (Hayes et al ., unpubl. data). However, the recent rediscovery of an extinct species provides hope that all is not lost, yet continued habitat destruction, impacts of invasive species, and climate change, necessi - tate the immediate development and deployment of effective conservation strategies to save this biodiversity treasure before it vanishes entirely (Solem 1990, Rég nier et al . 2009). Achatinellidae Auriculella pulchra Pease 1868 Notable rediscovery Auriculella pulchra (Fig. 1) belongs in the Auriculellinae, a Hawaiian endemic land snail subfamily of the Achatinellidae with 32 species (Cowie et al . 1995). It was originally described from the island of O‘ahu in 1868 and was subsequently recorded throughout the Ko‘olau Mountain range. -
Eskom Holdings SOC Limited
Eskom Holdings SOC Limited Environmen tal Impact Assessment for the Proposed 1x40 0kV Tabor-Bokmakirie (Nzhelele) and 4 X 250MVA 400kV/132kV Nzhelele Mai n Transmission Station, Limpopo Province SOCIO-ECONOMIC IMPACT REPORT DEA EIA Reference Number: 14/12/16/3/3/2/317 NEAS Ref Number: DEA/EIA/0001132/2012 LDEDET Ref Number: 12/1/9/E-V178 Date: February 2013 Report Version: Draft 1 Lidwala Consulting Engineers (SA) (Pty) Ltd Randburg Office: Pretoria Office: 11th Church Avenue, Ruiterhof, Randburg, 2194, 1121 Hertzog Street, Office F005, Waverley, Pretoria, 0186, PO Box 4221, Northcliff, 2115. PO Box 32497, Waverley, Pretoria, 0135, Tel: 0861 543 9252 Tel/faxs: 0861 543 9252 Polokwane Office : Nelspruit Office: 128 Marshall Street, Amy Park no. 5, Polokwane 39 Emkhe Street, Nelpruit, 1200 PO Box 3558, Polokwane, 0700 PO Box 2930, Nelspruit, 1200 Tel: 0861 543 9252 Tel: 0861 543 9252 TABLE OF CONTENTS 1. Introduction 5 1.1. Methodology 5 2. Social impacts expected during all project stages: 5 3. Description of the socio-economic setting – demographic information regarding the area in which the proposed line will be constructed: 6 3.1 Demographic profiles 7 3.2 Economic activities, Tourism and farming: 9 3.2.2 Tourism 9 3.2.3 Farming in the MLM 10 3.3 Employment rates and livelihoods 12 3.4 Access to services 12 3.4.1 Electricity 12 3.4.2. Access to water and sanitation facilities 13 3.4.3 Waste management 14 3.4.4 Transport 14 3.4.5 Educational facilities and libraries 14 3.4.6 Health facilities 15 3.4.7 Telecommunication and Postal Services 15 3.5 Conclusions from the social and economic environment within which the new power line is planned 16 4. -
Geological Inventory of the Maremani Nature Reserve
Geological Inventory Of The Maremani Nature Reserve Professor Jay Barton Department of Geology, Rand Afrikaans University (RAU) P.O. Box 524, Auckland Park 2006, South Africa Telephone: 27-11-489-2304 FAX: 27-11-489-2309 E-mail: [email protected] Introduction The Maremani Nature Reserve is presently being established and this document is intended as a summary of aspects of the geology within the boundaries of the Reserve. I have taken the liberty also to express my opinions with regard to possible roles that the Reserve might fulfill with regard to promoting geological awareness, education and research. The geology of the area covered by the Reserve was mapped in 1976 by Gunther Brandl and W. O. Willoughby of the Geological Survey of South Africa (presently the Council For Geo- science) at a scale of 1:50 000 for compilation at a scale of 1:250 000 (Brandl, 1981). The western portion to 30o 15’ east was previously mapped at a scale of 1:10 000 for compilation at scales of 1:50 000 and 1:125 000 by P. G. Söhnge (1946; Söhnge et al., 1948). Also locally within the western portion of the Reserve, maps at the scale of 1:5 000 were compiled by Messina Transvaal Development Corporation on farms and prospects investigated by the staff of the Messina Copper Mine. These maps are presently archived with me at RAU. Peter Horrocks wrote a PhD thesis on the geology of part of the western portion of what is now the Reserve (Horrocks, 1981). Charles Guerin in the late 1970’s worked on an unfin- ished MSc thesis on the calc-silicate rocks exposed in an area south of that studied by Peter Horrocks, some of which occur within the Reserve. -
To Be a Forum for the Nation to Present, Explore, and Preserve the Heritage
G.12 ANNUAL REPORT 2008/09 TONGAREWA PAPA TE ZEALAND NEW OF MUSEUM To be a forum for the nation to present, explore, and preserve the heritage of its cultures and knowledge of the natural environment in order to better understand and treasure the past, enrich the present, and meet the challenges of the future… Directory TE RÄRANGI INGOA MUSEUM OF NEW ZEALAND TE PAPA TONGAREWA Cable Street PO Box 467 Wellington 6140 New Zealand TORY STREET RESEARCH AND COLLECTION STORAGE FACILITY 169 Tory Street Wellington 6011 Telephone + 64 4 381 7000 Facsimile + 64 4 381 7070 Email [email protected] Website http://www.tepapa.govt.nz Auditors Audit New Zealand, Wellington, on behalf of the Auditor-General Bankers Westpac Banking Corporation Photography by Te Papa staff photographers, unless otherwise credited ISSN: 1179 – 0024 1 MUSEUM OF NEW OF MUSEUM Museum of New Zealand Te Papa Tongarewa Annual Report 2008/09 Te Pürongo ä-Tau 2008/09 In accordance with section 44 of the Public Finance Act 1989, this annual report of the Museum of TONGAREWA PAPA TE ZEALAND New Zealand Te Papa Tongarewa for 2008/09 is presented to the House of Representatives. Contents Ngä Ihirangi ANNUAL Part one Overview Statements Ngä Tauäki Tirohanga Whänui 3 Chairman’s Statement 4 REPORT Acting Chief Executive/Kaihautü Statement 6 Tribute to the late Dr Seddon Bennington (1947–2009) 7 2008/09 Performance at a Glance He Tirohanga ki ngä Whakatutukitanga 8 Part two Operating Framework Te Anga Whakahaere 12 Concept 12 Corporate Principles 12 Functions and Alignment with Government -
HYDROGEOLOGY of GROUNDWATER REGION 7 POLOKWANE/PIETERSBURG PLATEAU JR Vegter
HYDROGEOLOGY OF GROUNDWATER REGION 7 POLOKWANE/PIETERSBURG PLATEAU Prepared for the Water Research Commission by JR Vegter Hydrogeological Consultant WRC Report No. TT 209/03 October 2003 Obtainable from: Water Research Commission Private Bag X03 GEZINA 0031 Pretoria The publication of this report emanates from a project entitled: Hydrogeology of groundwater region 7 Pietersburg Plateau (WRC Consultancy No. K8/466) DISCLAIMER This report has been reviewed by the Water Research Commission (WRC) and approved for publication. Approval does not signify that the contents necessarily reflect the views and policies of the WRC, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. ISBN No. 1-77005-027-2 ISBN Set No. 1-86845-645-5 Printed in the Republic of South Africa EXECUTIVE SUMMARY The more important findings of this study are summarised below under “Statistical analyses”, “Role of geophysical methods” and “Hydrogeological control of drilling operations” General Groundwater Region 7, a rectangular area of about 12 000 km2, is located in the Limpopo Province. Its eastern boundary is the watershed between the Sand River and its tributaries and the eastward draining Letaba and Pafuri Rivers. Its northern boundary is formed by Formations of the Soutpansberg Group that built the mountain range of that name. The western boundary consists from north to south firstly of Waterberg Group sedimentary rocks, followed by mafic Bushveld rocks and lastly by strata of the Wolkberg Group including the Black Reef Formation. These strata build the Highlands Mountains and the east- northeasterly trending Strydpoort Mountains that form the southern boundary. -
Soutpansberg
4 EXECUTIVESUMMARY EXECUTIVESUMMARY EditedbyIanA.W.Macdonald,Ian Gaigher, Retha Gaigher andKatharineBerger fromsubmissionsmadebytheparticipantsinthe Lajuma SynthesisWorkshop,9–10May2003. This executive summary is based on the findings of a and provides a great deal of information about the area’s group of local human and natural scientists on research ecology, medicine, local cultures and cultural and social done in and around the Soutpansberg. The Soutpansberg change and exchange as well as linguistic developments. is, in terms of geological and geographical parameters, Physical remnants of former mission stations, cemeteries, defined as an area of approximately 6 800 km2 in the Lim- hospitals and schools are interesting foci for tourism. Al- popo Province of South Africa stretching from the Blou- most all the missionary denominations of Christianity are berg Massif in the west for about 250 km to Punda Maria represented in the Soutpansberg area and there is also in the Kruger National Park in the east. It includes the en- active development of African Initiated Churches. tire Soutpansberg mountain range and its immediate out- liers. This is South Africa’s most northerly and least The living cultural resources of the Soutpansberg are also widely known mountain range. This workshop was aimed extremely rich. The Venda was the last cultural group to at producing brief syntheses on as many of the compo- be affected by colonialism and the Venda people’s culture nents of the area’s cultural and natural assets as was pos- is still a way of life and is not just an object for material sible. This summary and the series of component gain. -
Fauna of New Zealand Website Copy 2010, Fnz.Landcareresearch.Co.Nz
aua o ew eaa Ko te Aiaga eeke o Aoeaoa IEEAE SYSEMAICS AISOY GOU EESEAIES O ACAE ESEAC ema acae eseac ico Agicuue & Sciece Cee P O o 9 ico ew eaa K Cosy a M-C aiièe acae eseac Mou Ae eseac Cee iae ag 917 Aucka ew eaa EESEAIE O UIESIIES M Emeso eame o Eomoogy & Aima Ecoogy PO o ico Uiesiy ew eaa EESEAIE O MUSEUMS M ama aua Eiome eame Museum o ew eaa e aa ogaewa O o 7 Weigo ew eaa EESEAIE O OESEAS ISIUIOS awece CSIO iisio o Eomoogy GO o 17 Caea Ciy AC 1 Ausaia SEIES EIO AUA O EW EAA M C ua (ecease ue 199 acae eseac Mou Ae eseac Cee iae ag 917 Aucka ew eaa Fauna of New Zealand Ko te Aitanga Pepeke o Aotearoa Number / Nama 38 Naturalised terrestrial Stylommatophora (Mousca Gasooa Gay M ake acae eseac iae ag 317 amio ew eaa 4 Maaaki Whenua Ρ Ε S S ico Caeuy ew eaa 1999 Coyig © acae eseac ew eaa 1999 o a o is wok coee y coyig may e eouce o coie i ay om o y ay meas (gaic eecoic o mecaica icuig oocoyig ecoig aig iomaio eiea sysems o oewise wiou e wie emissio o e uise Caaoguig i uicaio AKE G Μ (Gay Micae 195— auase eesia Syommaooa (Mousca Gasooa / G Μ ake — ico Caeuy Maaaki Weua ess 1999 (aua o ew eaa ISS 111-533 ; o 3 IS -7-93-5 I ie 11 Seies UC 593(931 eae o uIicaio y e seies eio (a comee y eo Cosy usig comue-ase e ocessig ayou scaig a iig a acae eseac M Ae eseac Cee iae ag 917 Aucka ew eaa Māoi summay e y aco uaau Cosuas Weigo uise y Maaaki Weua ess acae eseac O o ico Caeuy Wesie //wwwmwessco/ ie y G i Weigo o coe eoceas eicuaum (ue a eigo oaa (owe (IIusao G M ake oucio o e coou Iaes was ue y e ew eaIa oey oa ue oeies eseac -
Preliminary Biodiversity Conservation Plan For
APPENDIX A – DATASETS USED IN THE P-LCP FEATURES DATASET DATA TYPE DATE DATA SOURCE / CUSTODIAN COMMENT GIS VIEWER Agricultural Fields LP_fields_030507_ll.shp Vector 2007 AGIS Yes Conservation Farms all_conservation_farm_accurate.shp Vector SANBI Data records limited - not representative of whole province Conservation Features Cons_Features.shp Vector 2011 MetroGIS Composite dataset Species: Birds, Plants, Reptiles SANBI / MetroGIS Point data (SANBI) referenced on surrogate data, e.g. steep slopes, ridges, vegetation (grasslands), geology (dolomite) Vegetation 2006 SANBI High Yield Quaternary Catchments DWA Nylsvley - Modimolle corridor 2011 MetroGIS Contours 20m_contours.shp Vector Chief Directorate: Surveys & Used to compile shaded relief map Mapping Critical Biodiversity Areas (C-Plan) Cplan_Union3.shp Vector 2011 MetroGIS, Environomics, 4Life Compiled from Marxan process. Yes Promotions Protected Areas incorporated Development Pressure Mining rights Mining_Rights_all.shp Vector 2010 MetroGIS 5km Buffer around built-up areas Builtup_Final_Buffer_5km.shp Vector 2011 MetroGIS Eco Region vegm2006_Limpopo Vector 2006 SANBI Utilise field name [BIOREGION] Yes Ecological Corridors EcologicalCcorridors2.shp Vector 2011 MetroGIS Yes Farm Portions farm_portion.shp Vector Land-Surveyor Genl Yes High Yield Catchments Quaternary_Catchments_High_Yield.shp Vector DWA Top 10% to be used for high yield Yes interpretation Landcover landcover1.shp Vector 2000 SCIR / DWA / ARC-ISCW Built-up areas updated in places by MetroGIS Limpopo Province Boundary -
Zoologische Mededelingen
MINISTERIE VAN ONDERWIJS, KUNSTEN EN WETENSCHAPPEN ZOOLOGISCHE MEDEDELINGEN UITGEGEVEN DOOR HET RIJKSMUSEUM VAN NATUURLIJKE HISTORIE TE LEIDEN Deel 40 no. 25 22 juli 1965 TRACHYGYSTIS (DENDROTRICHIA) SYLVICOLA, A NEW SUBGENUS AND SPECIES FROM RHODESIA (MOLLUSCA, GASTROPODA PULMONATA: ENDODONTIDAE) by A. C. van BRUGGEN Natal Museum, Pietermaritzburg, South Africa and B. VERDCOURT Royal Botanic Gardens, Kew, Richmond, England In 1959 the first author (A.C.v.B.) discovered a peculiar snail of the pulmonate family Endodontidae in Rhodesia; on a subsequent expedition more specimens were obtained, so that a series is now available for descrip• tion. The species undoubtedly belongs to the genus Trachycystis Pilsbry, 1893, but a new subgenus has to be created in order to accomodate this particular species. Anatomical data and figures have been supplied by the second author (B.V.), while the first author is responsible for the re• maining part of text and figures. Dendrotrichia subgen. nov. A subgenus of Trachycystis characterised by ramose bristles on the sur• face of the shell; genital anatomy like that of subgenus Chalcocystis. Type species: Trachycystis (Dendrotrichia) sylvicola spec. nov. Trachycystis (Dendrotrichia) sylvicola spec. nov. Shell (pl. 1) small, depressed subconic, umbilicate, thin, somewhat trans• parent, dull, hirsute, corneous. Spire depressed, apex mamillate. Whorls 1 4-4 /2, regularly increasing, nearly flat, bluntly shouldered at periphery, first 1 1 /2 smooth, remainder covered all over with sharp, curved, oblique, trans- 220 ZOOLOGISCHE MEDEDELINGEN 4Ο (1965) Figs. 1-3. Trachycystis (Dendrotrichia) sylvicoh n.sp. 1, ramose bristles; 2, radula, teeth with outline of half row; 3, genitalia. A = atrium, C = common duct, Ε = epiphallus, FO = free oviduct, Ρ = penis, PR = penial retractor, S = sperma- theca, SD = spermathecal duct, V = vas deferens. -
Mollusca: Gastropoda) from Islands Off the Kimberley Coast, Western Australia Frank Köhler1, Vince Kessner2 and Corey Whisson3
RECORDS OF THE WESTERN AUSTRALIAN MUSEUM 27 021–039 (2012) New records of non-marine, non-camaenid gastropods (Mollusca: Gastropoda) from islands off the Kimberley coast, Western Australia Frank Köhler1, Vince Kessner2 and Corey Whisson3 1 Department of Environment and Conservation of Western Australia, Science Division, PO Box 51, Wanneroo, Western Australia 6946; and Australian Museum, 6 College Street, Sydney, New South Wales 2010, Australia. Email: [email protected] 2 162 Haynes Road, Adelaide River, Northern Terrritory 0846, Australia. Email: [email protected] 3 Department of Aquatic Zoology, Western Australian Museum, 49 Kew Street, Welshpool, Western Australia 6106, Australia. Email: [email protected] ABSTRACT – The coast of the Western Australian Kimberley boasts an archipelago that comprises several hundred large islands and thousands much smaller. While the non–marine gastropod fauna of the Kimberley mainland has been surveyed to some extent, the fauna of these islands had never been comprehensively surveyed and only anecdotal and unsystematic data on species occurrences have been available. During the Western Australian Department of Environment and Conservation’s Kimberley Island Survey, 2008–2010, 22 of the largest islands were surveyed. Altogether, 17 species of terrestrial non–camaenid snails were found on these islands. This corresponds to about 75% of all terrestrial, non–camaenid gastropods known from the entire Kimberley region. In addition, four species of pulmonate freshwater snails were found to occur on one or more of four of these islands. Individual islands harbour up to 15, with an average of eight, species each. Species diversity was found to be higher in the wetter parts of the region.