Ostrich Eggshell Bead Strontium Isotopes Reveal Persistent Macroscale Social Networking Across Late Quaternary Southern Africa
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Biodiversity and Ecology of Afromontane Rainforests with Wild Coffea Arabica L
Feyera Senbeta Wakjira (Autor) Biodiversity and ecology of Afromontane rainforests with wild Coffea arabica L. populations in Ethiopia https://cuvillier.de/de/shop/publications/2260 Copyright: Cuvillier Verlag, Inhaberin Annette Jentzsch-Cuvillier, Nonnenstieg 8, 37075 Göttingen, Germany Telefon: +49 (0)551 54724-0, E-Mail: [email protected], Website: https://cuvillier.de General introduction 1 GENERAL INTRODUCTION 1.1 Background The term biodiversity is used to convey the total number, variety and variability of living organisms and the ecological complexes in which they occur (Wilson 1988; CBD 1992; Rosenzweig 1995). The concept of biological diversity can be applied to a wide range of spatial and organization scales, including genetics, species, community, and landscape scales (Noss 1990; Austin et al. 1996; Tuomisto et al. 2003). It is becoming increasingly apparent that knowledge of the role of patterns and processes that determine diversity at different scales is at the very heart of an understanding of variation in biodiversity. Processes influencing diversity operate at different spatial and temporal scales (Rosenzweig 1995; Gaston 2000). A variety of environmental events and processes, including past evolutionary development, biogeographic processes, extinctions, and current influences govern the biodiversity of a particular site (Brown and Lomolino 1998; Gaston 2000; Ricklefs and Miller 2000). Biodiversity is valued and has been studied largely because it is used, and could be used better, to sustain and improve human well-being (WWF 1993; WCMC 1994). However, there has been a rapid decline in the biodiversity of the world during the past two to three decades (Wilson 1988; Whitmore and Sayer 1992; Lugo et al. -
Tulbagh Renosterveld Project Report
BP TULBAGH RENOSTERVELD PROJECT Introduction The Cape Floristic Region (CFR) is the smallest and richest floral kingdom of the world. In an area of approximately 90 000km² there are over 9 000 plant species found (Goldblatt & Manning 2000). The CFR is recognized as one of the 33 global biodiversity hotspots (Myers, 1990) and has recently received World Heritage Status. In 2002 the Cape Action Plan for the Environment (CAPE) programme identified the lowlands of the CFR as 100% irreplaceable, meaning that to achieve conservation targets all lowland fragments would have to be conserved and no further loss of habitat should be allowed. Renosterveld , an asteraceous shrubland that predominantly occurs in the lowland areas of the CFR, is the most threatened vegetation type in South Africa . Only five percent of this highly fragmented vegetation type still remains (Von Hase et al 2003). Most of these Renosterveld fragments occur on privately owned land making it the least represented vegetation type in the South African Protected Areas network. More importantly, because of the fragmented nature of Renosterveld it has a high proportion of plants that are threatened with extinction. The Custodians of Rare and Endangered Wildflowers (CREW) project, which works with civil society groups in the CFR to update information on threatened plants, has identified the Tulbagh valley as a high priority for conservation action. This is due to the relatively large amount of Renosterveld that remains in the valley and the high amount of plant endemism. The CAPE program has also identified areas in need of fine scale plans and the Tulbagh area falls within one of these: The Upper Breede River planning domain. -
Comparison of Extent and Transformation of South Africa's
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by South East Academic Libraries System (SEALS) Research in Action South African Journal of Science 97, May/June 2001 179 remote sensing applications in South Comparison of extent and Africa. This is a hierarchical framework designed to suit South African conditions, transformation of South Africa’s and incorporates known land-cover types that can be identified in a consistent woodland biome from two national and repetitive manner from high- resolution satellite imagery such as Land- databases sat TM and SPOT.The ‘natural’vegetation classes are based on broad, structural M.W. Thompsona*, E.R. Vinka, D.H.K. Fairbanksb,c, A. Ballancea types only, and are not intended to be and C.M. Shackletona,d equivalent to a floristic or ecological vege- tation classification. It is important to understand that a HE RECENT COMPLETION OF THE SOUTH Fairbanks et al.5 combination of both the NLC database’s TAfrican National Land-Cover Database This paper compares the distribution ‘Woodland’ and ‘Thicket, Bushland, and the Vegetation Map of South Africa, and location of woodland and bushveld- Bush-Clump & Tall Fynbos’ land-cover Swaziland and Lesotho, allows for the first type vegetation categories defined within classes were used in the comparison with time a comparison to be made on a national scale between the current and potential the NLC data, and the equivalent the DEAT defined ‘Savanna Biome’. The distribution of ‘natural’ vegetation resources. ‘Savanna Biome’ class defined within the inclusion of the NLC’s ‘Thicket, Bushland This article compares the distribution and DEAT’s ‘VegetationMap’ data. -
National Forests Act: List of Protected Tree Species
6 No. 37037 GOVERNMENT GAZETTE, 22 NOVEMBER 2013 GOVERNMENT NOTICES GOEWERMENTSKENNISGEWINGS DEPARTMENT OF AGRICULTURE, FORESTRY AND FISHERIES DEPARTEMENT VAN LANDBOU, BOSBOU EN VISSERYE No. 877 22 November 2013 NOTICE OFOF THETHE LISTLIST OFOF PROTECTEDPROTECTED TREE TREE SPECIES SPECIES UNDER UNDER THE THE NATIONAL NATIONAL FORESTS ACT, 19981998 (ACT(ACT NO No. 84 84 OF OF 1998) 1998) By virtue of powers vested in me under Section 15(3) of the National Forests Act, 1998, I, Tina Joemat-Pettersson, Minister of Agriculture, Forestry and Fisheries hereby publish a list of all protected trees belonging to a particular species under Section 12(1) (d) set out in Schedule below. The effect of this declaration is that in terms of Section 15(1) of the National Forests Act, 1998, no person may cut, disturb, damage or destroy any protected tree or possess, collect, remove, transport, export, purchase, sell, donate or in any other manner acquire or dispose of any protected tree or any forest product derived from a protected tree, except under a licence or exemption granted by the Minister to an applicant and subject to such period and conditions as may be stipulated. Contravention of this declaration is regarded as a first category offence that may result in a person who is found guilty of being sentenced to a fine or imprisonment for a period up to three years, or to both a fine and imprisonment. SCHEDULE A / BYLAE A Botanical Name English Other Common Names National Common Afrikaans (A), Northern SothoTree Names (NS),SouthernSotho (S),Number Tswana (T), Venda (V), Xhosa (X), Zulu (Z) Acacia erioloba Camel thorn Kameeldoring (A) / Mogohlo (NS) / 168 Mogotlho (T) Acacia haematoxylon Grey camel thorn Vaalkameeldoring (A) / Mokholo (T) 169 Adansonia digitata Baobab Kremetart (A) /Seboi (NS)/ Mowana 467 (T) Afzelia quanzensis Pod mahogany Peulmahonie (A) / Mutokota (V) / 207 lnkehli (Z) Balanites subsp. -
Maloti-Drakensberg Park, Lesotho & South Africa
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Maloti-Drakensberg Park - 2020 Conservation Outlook Assessment Maloti-Drakensberg Park 2020 Conservation Outlook Assessment SITE INFORMATION Country: Lesotho, South Africa Inscribed in: 2000 Criteria: (i) (iii) (vii) (x) The Maloti-Drakensberg Park is a transboundary site composed of the uKhahlamba Drakensberg National Park in South Africa and the Sehlathebe National Park in Lesotho. The site has exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts as well as visually spectacular sculptured arches, caves, cliffs, pillars and rock pools. The site's diversity of habitats protects a high level of endemic and globally important plants. The site harbors endangered species such as the Cape vulture (Gyps coprotheres) and the bearded vulture (Gypaetus barbatus). Lesotho’s Sehlabathebe National Park also harbors the Maloti minnow (Pseudobarbus quathlambae), a critically endangered fish species only found in this park. This spectacular natural site contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. They represent the spiritual life of the San people, who lived in this area over a period of 4,000 years. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 01 Dec 2020 SIGNIFICANT CONCERN The conservation outlook for Maloti-Drakensberg Park is of significant concern. The EKZNW management staff are highly dedicated and experienced and there is also significant appreciation for the values of the Maloti Drakensberg by communities living nearby as evidenced, for example, by the vehemently strong opposition to the possibility of oil and gas exploration in the area. -
Climate Forcing of Tree Growth in Dry Afromontane Forest Fragments of Northern Ethiopia: Evidence from Multi-Species Responses Zenebe Girmay Siyum1,2* , J
Siyum et al. Forest Ecosystems (2019) 6:15 https://doi.org/10.1186/s40663-019-0178-y RESEARCH Open Access Climate forcing of tree growth in dry Afromontane forest fragments of Northern Ethiopia: evidence from multi-species responses Zenebe Girmay Siyum1,2* , J. O. Ayoade3, M. A. Onilude4 and Motuma Tolera Feyissa2 Abstract Background: Climate-induced challenge remains a growing concern in the dry tropics, threatening carbon sink potential of tropical dry forests. Hence, understanding their responses to the changing climate is of high priority to facilitate sustainable management of the remnant dry forests. In this study, we examined the long-term climate- growth relations of main tree species in the remnant dry Afromontane forests in northern Ethiopia. The aim of this study was to assess the dendrochronological potential of selected dry Afromontane tree species and to study the influence of climatic variables (temperature and rainfall) on radial growth. It was hypothesized that there are potential tree species with discernible annual growth rings owing to the uni-modality of rainfall in the region. Ring width measurements were based on increment core samples and stem discs collected from a total of 106 trees belonging to three tree species (Juniperus procera, Olea europaea subsp. cuspidate and Podocarpus falcatus). The collected samples were prepared, crossdated, and analyzed using standard dendrochronological methods. The formation of annual growth rings of the study species was verified based on successful crossdatability and by correlating tree-ring widths with rainfall. Results: The results showed that all the sampled tree species form distinct growth boundaries though differences in the distinctiveness were observed among the species. -
Lesotho Fourth National Report on Implementation of Convention on Biological Diversity
Lesotho Fourth National Report On Implementation of Convention on Biological Diversity December 2009 LIST OF ABBREVIATIONS AND ACRONYMS ADB African Development Bank CBD Convention on Biological Diversity CCF Community Conservation Forum CITES Convention on International Trade in Endangered Species CMBSL Conserving Mountain Biodiversity in Southern Lesotho COP Conference of Parties CPA Cattle Post Areas DANCED Danish Cooperation for Environment and Development DDT Di-nitro Di-phenyl Trichloroethane EA Environmental Assessment EIA Environmental Impact Assessment EMP Environmental Management Plan ERMA Environmental Resources Management Area EMPR Environmental Management for Poverty Reduction EPAP Environmental Policy and Action Plan EU Environmental Unit (s) GA Grazing Associations GCM Global Circulation Model GEF Global Environment Facility GMO Genetically Modified Organism (s) HIV/AIDS Human Immuno Virus/Acquired Immuno-Deficiency Syndrome HNRRIEP Highlands Natural Resources and Rural Income Enhancement Project IGP Income Generation Project (s) IUCN International Union for Conservation of Nature and Natural Resources LHDA Lesotho Highlands Development Authority LMO Living Modified Organism (s) Masl Meters above sea level MDTP Maloti-Drakensberg Transfrontier Conservation and Development Project MEAs Multi-lateral Environmental Agreements MOU Memorandum Of Understanding MRA Managed Resource Area NAP National Action Plan NBF National Biosafety Framework NBSAP National Biodiversity Strategy and Action Plan NEAP National Environmental Action -
Comparative Wood Anatomy of Afromontane and Bushveld Species from Swaziland, Southern Africa
IAWA Bulletin n.s., Vol. 11 (4), 1990: 319-336 COMPARATIVE WOOD ANATOMY OF AFROMONTANE AND BUSHVELD SPECIES FROM SWAZILAND, SOUTHERN AFRICA by J. A. B. Prior 1 and P. E. Gasson 2 1 Department of Biology, Imperial College of Science, Technology & Medicine, London SW7 2BB, U.K. and 2Jodrell Laboratory, Royal Botanic Gardens, Kew, Richmond, Surrey, TW9 3DS, U.K. Summary The habit, specific gravity and wood anat of the archaeological research, uses all the omy of 43 Afromontane and 50 Bushveld well preserved, qualitative anatomical charac species from Swaziland are compared, using ters apparent in the charred modem samples qualitative features from SEM photographs in an anatomical comparison between the of charred samples. Woods with solitary ves two selected assemblages of trees and shrubs sels, scalariform perforation plates and fibres growing in areas of contrasting floristic com with distinctly bordered pits are more com position. Some of the woods are described in mon in the Afromontane species, whereas Kromhout (1975), others are of little com homocellular rays and prismatic crystals of mercial importance and have not previously calcium oxalate are more common in woods been investigated. Few ecological trends in from the Bushveld. wood anatomical features have previously Key words: Swaziland, Afromontane, Bush been published for southern Africa. veld, archaeological charcoal, SEM, eco The site of Sibebe Hill in northwest Swazi logical anatomy. land (26° 15' S, 31° 10' E) (Price Williams 1981), lies at an altitude of 1400 m, amidst a Introduction dramatic series of granite domes in the Afro Swaziland, one of the smallest African montane forest belt (White 1978). -
Early History of South Africa
THE EARLY HISTORY OF SOUTH AFRICA EVOLUTION OF AFRICAN SOCIETIES . .3 SOUTH AFRICA: THE EARLY INHABITANTS . .5 THE KHOISAN . .6 The San (Bushmen) . .6 The Khoikhoi (Hottentots) . .8 BLACK SETTLEMENT . .9 THE NGUNI . .9 The Xhosa . .10 The Zulu . .11 The Ndebele . .12 The Swazi . .13 THE SOTHO . .13 The Western Sotho . .14 The Southern Sotho . .14 The Northern Sotho (Bapedi) . .14 THE VENDA . .15 THE MASHANGANA-TSONGA . .15 THE MFECANE/DIFAQANE (Total war) Dingiswayo . .16 Shaka . .16 Dingane . .18 Mzilikazi . .19 Soshangane . .20 Mmantatise . .21 Sikonyela . .21 Moshweshwe . .22 Consequences of the Mfecane/Difaqane . .23 Page 1 EUROPEAN INTERESTS The Portuguese . .24 The British . .24 The Dutch . .25 The French . .25 THE SLAVES . .22 THE TREKBOERS (MIGRATING FARMERS) . .27 EUROPEAN OCCUPATIONS OF THE CAPE British Occupation (1795 - 1803) . .29 Batavian rule 1803 - 1806 . .29 Second British Occupation: 1806 . .31 British Governors . .32 Slagtersnek Rebellion . .32 The British Settlers 1820 . .32 THE GREAT TREK Causes of the Great Trek . .34 Different Trek groups . .35 Trichardt and Van Rensburg . .35 Andries Hendrik Potgieter . .35 Gerrit Maritz . .36 Piet Retief . .36 Piet Uys . .36 Voortrekkers in Zululand and Natal . .37 Voortrekker settlement in the Transvaal . .38 Voortrekker settlement in the Orange Free State . .39 THE DISCOVERY OF DIAMONDS AND GOLD . .41 Page 2 EVOLUTION OF AFRICAN SOCIETIES Humankind had its earliest origins in Africa The introduction of iron changed the African and the story of life in South Africa has continent irrevocably and was a large step proven to be a micro-study of life on the forwards in the development of the people. -
A Fine-Scale Conservation Plan for Cape Lowlands Renosterveld: Technical Report
A Fine-Scale Conservation Plan for Cape Lowlands Renosterveld: Technical Report MAIN REPORT September 2003 Amrei von Hase Mathieu Rouget Kristal Maze Nick Helme Report No. CCU 2/03 Cape Conservation Unit Botanical Society of South Africa Pvt Bag X 10 7735 Claremont www.botanicalsociety.org.za/ccu Key Partners and Sponsors of the Cape Lowlands Renosterveld Project TABLE MOUNTAIN FUND 2 Acknowledgements Many individuals and organizations have contributed generously to the Cape Lowlands Renosterveld Project to whom the Botanical Society and the project team are greatly indebted. We express our appreciation to you in this section and in addition have provided acknowledgement to others in sections of this report where their contribution was relevant. We are particularly indebted to our key project partners, the Western Cape Nature Conservation Board (WCNCB), for putting their full support behind the project from its inception as well as their many contributions to the project. In Scientific Services we especially thank the late Chris Burgers, Helen de Klerk, Ernst Baard, Annelise le Roux, Guy Palmer and Andrew Turner for their guidance in the project planning and initiation stages, particularly on data and GIS matters. We are tremendously grateful to Chris who generously and infectiously shared with us his wealth of knowledge about the lowlands. In Operations we express our appreciation to the business unit managers, extension officers and regional ecologists who played a vital role particularly in shaping the final products of the project. We are especially grateful to Anton Wolfaardt and Chris Martens. Wendy Paisley of the Cape Conservation Unit (CCU) of the Botanical Society provided invaluable administrative and organizational support to the project. -
Upper Mantle P and S Wave Velocity Structure of the Kalahari Craton And
RESEARCH LETTER Upper Mantle P and S Wave Velocity Structure of the 10.1029/2019GL084053 Kalahari Craton and Surrounding Proterozoic Key Points: • Thick cratonic lithosphere extends Terranes, Southern Africa beneath the Rehoboth Province and Kameron Ortiz1, Andrew Nyblade1,5 , Mark van der Meijde2, Hanneke Paulssen3 , parts of the northern Okwa Terrane 4 4 5 2,6 and Magondi Belt Motsamai Kwadiba , Onkgopotse Ntibinyane , Raymond Durrheim , Islam Fadel , • The northern edge of the greater and Kyle Homman1 Kalahari Craton lithosphere lies along the northern boundary of the 1Department of Geosciences, Pennsylvania State University, University Park, PA, USA, 2Faculty for Geo‐information Rehoboth Province and Magondi Science and Earth Observation (ITC), University of Twente, Enschede, Netherlands, 3Department of Earth Sciences, Belt 4 • Cratonic mantle lithosphere Faculty of Geosciences, Utrecht University, Utrecht, Netherlands, Botswana Geoscience Institute, Lobatse, Botswana, 5 6 beneath the Okwa Terrane and School of Geosciences, The University of the Witwatersrand, Johannesburg, South Africa, Geology Department, Faculty Magondi Belt may have been of Science, Helwan University, Ain Helwan, Egypt chemically altered by Proterozoic magmatic events Abstract New broadband seismic data from Botswana and South Africa have been combined with Supporting Information: existing data from the region to develop improved P and S wave velocity models for investigating the • Supporting Information S1 upper mantle structure of southern Africa. Higher craton‐like velocities are imaged beneath the Rehoboth Province and parts of the northern Okwa Terrane and the Magondi Belt, indicating that the Correspondence to: northern edge of the greater Kalahari Craton lithosphere lies along the northern boundary of these A. Nyblade, terranes. -
Pinnacle Point Cave 13B (Western Cape Province, South Africa) in Context: the Cape Floral Kingdom, Shellfish, and Modern Human Originsq
Journal of Human Evolution 59 (2010) 425e443 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Pinnacle Point Cave 13B (Western Cape Province, South Africa) in context: The Cape Floral kingdom, shellfish, and modern human originsq Curtis W. Marean Institute of Human Origins, School of Human Evolution and Social Change, P.O. Box 872402, Arizona State University, Tempe, AZ 85287-2402, USA article info abstract Article history: Genetic and anatomical evidence suggests that Homo sapiens arose in Africa between 200 and 100 ka, Received 15 December 2009 and recent evidence suggests that complex cognition may have appeared between w164 and 75 ka. This Accepted 19 March 2010 evidence directs our focus to Marine Isotope Stage (MIS) 6, when from 195e123 ka the world was in a fluctuating but predominantly glacial stage, when much of Africa was cooler and drier, and when dated Keywords: archaeological sites are rare. Previously we have shown that humans had expanded their diet to include Middle Stone Age marine resources by w164 ka (Æ12 ka) at Pinnacle Point Cave 13B (PP13B) on the south coast of South Mossel Bay Africa, perhaps as a response to these harsh environmental conditions. The associated material culture Origins of modern humans documents an early use and modification of pigment, likely for symbolic behavior, as well as the production of bladelet stone tool technology, and there is now intriguing evidence for heat treatment of lithics. PP13B also includes a later sequence of MIS 5 occupations that document an adaptation that increasingly focuses on coastal resources.