Annual Report 2011
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Timeline of Natural History
Timeline of natural history This timeline of natural history summarizes significant geological and Life timeline Ice Ages biological events from the formation of the 0 — Primates Quater nary Flowers ←Earliest apes Earth to the arrival of modern humans. P Birds h Mammals – Plants Dinosaurs Times are listed in millions of years, or Karo o a n ← Andean Tetrapoda megaanni (Ma). -50 0 — e Arthropods Molluscs r ←Cambrian explosion o ← Cryoge nian Ediacara biota – z ←Earliest animals o ←Earliest plants i Multicellular -1000 — c Contents life ←Sexual reproduction Dating of the Geologic record – P r The earliest Solar System -1500 — o t Precambrian Supereon – e r Eukaryotes Hadean Eon o -2000 — z o Archean Eon i Huron ian – c Eoarchean Era ←Oxygen crisis Paleoarchean Era -2500 — ←Atmospheric oxygen Mesoarchean Era – Photosynthesis Neoarchean Era Pong ola Proterozoic Eon -3000 — A r Paleoproterozoic Era c – h Siderian Period e a Rhyacian Period -3500 — n ←Earliest oxygen Orosirian Period Single-celled – life Statherian Period -4000 — ←Earliest life Mesoproterozoic Era H Calymmian Period a water – d e Ectasian Period a ←Earliest water Stenian Period -4500 — n ←Earth (−4540) (million years ago) Clickable Neoproterozoic Era ( Tonian Period Cryogenian Period Ediacaran Period Phanerozoic Eon Paleozoic Era Cambrian Period Ordovician Period Silurian Period Devonian Period Carboniferous Period Permian Period Mesozoic Era Triassic Period Jurassic Period Cretaceous Period Cenozoic Era Paleogene Period Neogene Period Quaternary Period Etymology of period names References See also External links Dating of the Geologic record The Geologic record is the strata (layers) of rock in the planet's crust and the science of geology is much concerned with the age and origin of all rocks to determine the history and formation of Earth and to understand the forces that have acted upon it. -
8. Archosaur Phylogeny and the Relationships of the Crocodylia
8. Archosaur phylogeny and the relationships of the Crocodylia MICHAEL J. BENTON Department of Geology, The Queen's University of Belfast, Belfast, UK JAMES M. CLARK* Department of Anatomy, University of Chicago, Chicago, Illinois, USA Abstract The Archosauria include the living crocodilians and birds, as well as the fossil dinosaurs, pterosaurs, and basal 'thecodontians'. Cladograms of the basal archosaurs and of the crocodylomorphs are given in this paper. There are three primitive archosaur groups, the Proterosuchidae, the Erythrosuchidae, and the Proterochampsidae, which fall outside the crown-group (crocodilian line plus bird line), and these have been defined as plesions to a restricted Archosauria by Gauthier. The Early Triassic Euparkeria may also fall outside this crown-group, or it may lie on the bird line. The crown-group of archosaurs divides into the Ornithosuchia (the 'bird line': Orn- ithosuchidae, Lagosuchidae, Pterosauria, Dinosauria) and the Croco- dylotarsi nov. (the 'crocodilian line': Phytosauridae, Crocodylo- morpha, Stagonolepididae, Rauisuchidae, and Poposauridae). The latter three families may form a clade (Pseudosuchia s.str.), or the Poposauridae may pair off with Crocodylomorpha. The Crocodylomorpha includes all crocodilians, as well as crocodi- lian-like Triassic and Jurassic terrestrial forms. The Crocodyliformes include the traditional 'Protosuchia', 'Mesosuchia', and Eusuchia, and they are defined by a large number of synapomorphies, particularly of the braincase and occipital regions. The 'protosuchians' (mainly Early *Present address: Department of Zoology, Storer Hall, University of California, Davis, Cali- fornia, USA. The Phylogeny and Classification of the Tetrapods, Volume 1: Amphibians, Reptiles, Birds (ed. M.J. Benton), Systematics Association Special Volume 35A . pp. 295-338. Clarendon Press, Oxford, 1988. -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
University of Birmingham the Earliest Bird-Line Archosaurs and The
University of Birmingham The earliest bird-line archosaurs and the assembly of the dinosaur body plan Nesbitt, Sterling; Butler, Richard; Ezcurra, Martin; Barrett, Paul; Stocker, Michelle; Angielczyk, Kenneth; Smith, Roger; Sidor, Christian; Niedzwiedzki, Grzegorz; Sennikov, Andrey; Charig, Alan DOI: 10.1038/nature22037 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Nesbitt, S, Butler, R, Ezcurra, M, Barrett, P, Stocker, M, Angielczyk, K, Smith, R, Sidor, C, Niedzwiedzki, G, Sennikov, A & Charig, A 2017, 'The earliest bird-line archosaurs and the assembly of the dinosaur body plan', Nature, vol. 544, no. 7651, pp. 484-487. https://doi.org/10.1038/nature22037 Link to publication on Research at Birmingham portal Publisher Rights Statement: Checked for eligibility: 03/03/2017. General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. -
The Bushveld Igneous Complex
The Bushveld Igneous Complex THE GEOLOGY OF SOUTH AFRICA’S PLATINUM RESOURCES By C. A. Cousins, MSC. Johannesburg Consolidated Investment Company Limited A vast composite body of plutonic and volcanic rock in the central part of the Transvaal, the Bushveld igneous complex includes the platinum reef worked by Rustenburg Platinum Mines Limited and constituting the world’s greatest reserve of the platinum metals. This article describes the geological and economic aspects of this unusually interesting formation. In South Africa platinum occurs chiefly in square miles. Two of these areas lie at the the Merensky Reef, which itself forms part of eastern and western ends of the Bushveld and the Bushveld igneous complex, an irregular form wide curved belts, trending parallel to oval area of some 15,000 square miles occupy- the sedimentary rocks which they overlie, and ing a roughly central position in the province dipping inwards towards the centre of the of the Transvaal. A geological map of the Bushveld at similar angles. The western belt area, which provides the largest known has a flat sheet-like extension reaching the example of this interesting type of formation, western boundary of the Transvaal. The is shown on the facing page. third area extends northwards and cuts out- The complex rests upon a floor of sedi- side the sedimentary basin. Its exact relation- mentary rocks of the Transvaal System. This ship to the other outcrops within the basin floor is structurally in the form of an immense has not as yet been solved. oval basin, three hundred miles long and a As the eastern and western belts contain hundred miles broad. -
The Uranium Potential of the Bushveld Igneous Complex
(GEA748| June 1987 THE URANIUM POTENTIAL OF THE BUSHVELD IGNEOUS COMPLEX A CRITICAL REAPPRAISAL Investigators: MAG Andreoli R J Hart H J Brynard F A G M Camisani-Calzolari ATOMIC ENERGY CORPORATION OF SOUTH AFRICA LIMITED PRETORIA THIS DOCUMENT MAY NOT BE COPIED IN ANY WAY WHATSOEVER PER 158 GEA 748 ATOMIC ENERGY CORPORATION/UNIVERSITY OF PRETORIA WORKING GROUP ON URANIUM IN THE BUSHVELD COMPLEX Progress Report No. 4 THE URANIUM POTENTIAL OF THE BUSHVELD IGNEOUS COMPLEX A CRITICAL REAPPRAISAL Investigators: MAG Andreoli R J Hart H J Beynard F A G M Camisani-Calzolari POSTAL ADDRESS: Department of Geotechnology P 0 Box 582 PELINDABA PRETORIA June 1987 0001 ISBN 0 86960 848 7 PER-158 GEA-748 ATOMIC ENERGY CORPORATION/UNIVERSITY OF PRETORIA WORKING GROUP ON URANIUM IN THE BUSHVELD COMPLEX Progress Report No. 4 THE URANIUM POTENTIAL OF THE BUSHVELD IGNEOUS COMPLEX A CRITICAL REAPPRAISAL Investigators: MAG Andreoli R J Hart H J Brynard F A G M Camisani-Calzolari DEPARTMENT OF GEOTECHNOLOGY ATOMIC ENERGY CORPORATION OF SOUTH AFRICA LIMITED P 0 BOX 582, PRETORIA (0001) June 1987 ISBN 086960 848 7 PER-158- i - CONTENTS Page Samevatting/Abstract vi LIST OF ABBREVIATIONS ii-iii LIST OF TABLES iv LIST OF FIGURES v 1 INTRODUCTION 1 2 ON THE POSSIBILITY OF A GIANT OLYMPIC DAM-TYPE DEPOSIT JN THE BUSHVELD COMPLEX 3 3 THE WATERBERG COVER: A TARGET FOR UNCOMFORMITY-TYPE DEPOSITS? 19 4 ADDITIONAL TARGETS FOR URANIUM EXPLORATION 25 5 DISCUSSION & RECOMMENDATIONS 27 6 ACKNOWLEDGEMENTS 30 7 REFERENCES 30 LIST OP IBBEKVIAÏIOIIS All allanite amp amphibole -
Abstract Booklet
DSI-NRF CIMERA Annual COLLOQUIUM 26-27 NOVEMBER 2020 ABSTRACT BOOKLET Image: Transvaal Supergroup, banded iron formation, Kuruman Kop, Northern Cape. 26-27 November 2020 ONLINE & IN PERSON School of Tourism and Hospitality (STH) University of Johannesburg Auckland Park Bunting Road Campus 2 Dear All, Dear All, We would like to extend a warm welcome to the annual DSI-NRF CIMERA Colloquium, hosted by the University of We would like to extend a warm welcome to the annual DSI-NRF CIMERA Colloquium, hosted by the University of Johannesburg. Johannesburg. DSI-NRF Centre of Excellence (CoE) for Integrated Mineral and Energy Resource Analysis (CIMERA) is hosted by the Department DSI-NRF Centre of Excellence (CoE) for Integrated Mineral and Energy Resource Analysis (CIMERA) is hosted by the Department of Geology at the University of Johannesburg (UJ), and co-hosted by the School of Geosciences at the University of the of Geology at the University of Johannesburg (UJ), and co-hosted by the School of Geosciences at the University of the DearWitwatersrand All, (Wits). DSI-NRF CIMERA is a virtual centre of research that concentrates existing research excellence, capacity Witwatersrand (Wits). DSI-NRF CIMERA is a virtual centre of research that concentrates existing research excellence, capacity Weand extend resources a warm welcome to enable to the researchersannual DSI-NRF toCIMERA collaborate Colloquium, across hosted disciplinesby the University and of Johannesburg. institutions on long-term projects of economic and/ or and resources to enable researchersThe to Colloquiumcollaborate will acrossrun as a hybriddisciplines event this and year, institutions triggered by the on COVID-19 long-term pandemic projects lockdown of economic situation and and/ or societal benefit in geology, that are locally relevant and internationally competitive. -
Timeline of Natural History
Timeline of natural history Main articles: History of the Earth and Geological his- chondrules,[1] are a key signature of a supernova ex- tory of Earth plosion. See also: Geologic time scale and Timeline of evolution- ary history of life • 4,567±3 Ma: Rapid collapse of hydrogen molecular For earlier events, see Timeline of the formation of the cloud, forming a third-generation Population I star, Universe. the Sun, in a region of the Galactic Habitable Zone This timeline of natural history summarizes signifi- (GHZ), about 25,000 light years from the center of the Milky Way Galaxy.[2] • 4,566±2 Ma: A protoplanetary disc (from which Earth eventually forms) emerges around the young Sun, which is in its T Tauri stage. • 4,560–4,550 Ma: Proto-Earth forms at the outer (cooler) edge of the habitable zone of the Solar Sys- tem. At this stage the solar constant of the Sun was only about 73% of its current value, but liquid wa- ter may have existed on the surface of the Proto- Earth, probably due to the greenhouse warming of high levels of methane and carbon dioxide present in the atmosphere. Early bombardment phase begins: because the solar neighbourhood is rife with large planetoids and debris, Earth experiences a number of giant impacts that help to increase its overall size. Visual representation of the history of life on Earth as a spiral 2 Hadean Eon cant geological and biological events from the formation of the Earth to the rise of modern humans. Times are listed in millions of years, or megaanni (Ma). -
Crewnewsletter
newsletter CREW Volume 14 • April 2018 National CREW overview he pages of this newsletter highlight the work of the Custodians of Rare and CREW, the Custodians of Rare and Endangered Endangered Wildflowers (CREW) pro- Wildflowers, is a programme that involves Tgramme’s citizen scientists during 2017. volunteers from the public in the monitoring and The depth of experience of our volunteers, many whom have been with the programme for over 10 conservation of South Africa’s threatened plants. years, and the long term commitment of the staff CREW aims to capacitate a network of volunteers that manage this programme shows clearly in the excellent information being gathered and the ever from a range of socio-economic backgrounds to increasing spin-off benefits that this programme is monitor and conserve South Africa’s threatened generating for South African plant conservation. plant species. The programme links volunteers CREW continues to grow and we are very pleased to welcome the two new groups that have been in- with their local conservation agencies and itiated in the summer rainfall region (more about particularly with local land stewardship this in Suvarna’s update Page 16). initiatives to ensure the conservation of key Since its inception, CREW has been determined sites for threatened plant species. Funded not only to monitor threatened plants’ popula- jointly by the Botanical Society of South Africa tions, but also to support the conservation of criti- cal habitats for plant conservation. This is achieved and the South African National Biodiversity in two ways; firstly by supporting the expansion Institute, CREW is an integral part of the work on of protected areas via provincial stewardship pro- grammes and secondly by contributing highly monitoring threatened species for South Africa. -
Resources in the Upper Zone of the Bushveld Complex, South Africa
Papers and Proceedings of the Royal Society of Tasmania, Volume 150(1), 2016 15 Fe-Ti-V-(P) RESOURCES IN THE UPPER ZONE OF THE BUSHVELD COMPLEX, SOUTH AFRICA by L.A. Fischer and Q. Yuan (with four text-figures and two plates) Fischer, L.A. & Yuan, Q. 2016 (31:viii): Fe-Ti-V-(P) resources in the Upper Zone of the Bushveld Complex, South Africa. Papers and Proceedings of the Royal Society of Tasmania 150(1): 15–22. https://doi.org/10.26749/rstpp.150.1.15 ISSN 0080-4703. Institut für Mineralogie, Leibniz Universität Hannover, 30167 Hannover, Germany, and School of Physical Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia (LAF*); Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China, and Department of Geology, University of Liege, 4000 Sart Tilman, Belgium (QY). *Author for correspondence. Email: [email protected] The Bushveld Complex in South Africa is the largest layered intrusion on Earth. Its upper part is known for huge resources of iron, tita- nium, vanadium and phosphorus. Associated with the layered character of the rocks, these resources are enriched at certain levels of the intrusion, which makes it important to understand the formation processes of those layers. In this paper we give an introduction and overview of recent debates and challenges. Key Words: layered intrusion, Bushveld, resources. INTRODUCTION Fe, Ti, V and P never or only rarely occur as native elements in nature. Minerals, rich in one or more of these Iron (Fe), titanium (Ti) and vanadium (V) are important elements are mined and their components are extracted. -
Gardens and Stewardship
GARDENS AND STEWARDSHIP Thaddeus Zagorski (Bachelor of Theology; Diploma of Education; Certificate 111 in Amenity Horticulture; Graduate Diploma in Environmental Studies with Honours) Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy October 2007 School of Geography and Environmental Studies University of Tasmania STATEMENT OF AUTHENTICITY This thesis contains no material which has been accepted for any other degree or graduate diploma by the University of Tasmania or in any other tertiary institution and, to the best of my knowledge and belief, this thesis contains no copy or paraphrase of material previously published or written by other persons, except where due acknowledgement is made in the text of the thesis or in footnotes. Thaddeus Zagorski University of Tasmania Date: This thesis may be made available for loan or limited copying in accordance with the Australian Copyright Act of 1968. Thaddeus Zagorski University of Tasmania Date: ACKNOWLEDGEMENTS This thesis is not merely the achievement of a personal goal, but a culmination of a journey that started many, many years ago. As culmination it is also an impetus to continue to that journey. In achieving this personal goal many people, supervisors, friends, family and University colleagues have been instrumental in contributing to the final product. The initial motivation and inspiration for me to start this study was given by Professor Jamie Kirkpatrick, Dr. Elaine Stratford, and my friend Alison Howman. For that challenge I thank you. I am deeply indebted to my three supervisors Professor Jamie Kirkpatrick, Dr. Elaine Stratford and Dr. Aidan Davison. Each in their individual, concerted and special way guided me to this omega point. -
South Africa's Coalfields – a 2014 Perspective
South Africa's coalfields – a 2014 perspective 1Hancox, P. John and 2,3Götz, Annette E. 1University of the Witwatersrand, School of Geosciences, Private Bag 3, 2050 Wits, South Africa; [email protected] 2University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa; [email protected] 3Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation Highlights • South Africa’s Coalfields are presented. • The role of Gondwanan coals as palaeoclimate archives is stated. • Future research fields include palynology, sequence stratigraphy, basin fill. Abstract For well over a century and a half coal has played a vital role in South Africa’s economy and currently bituminous coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the production of a substantial percentage of the country’s liquid fuels. It furthermore provides a considerable source of foreign revenue from exports. Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review of their exploration and exploitation histories, general geology, and coal seam nomenclature and coal qualities. Within the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up of Gondwana most of the coals bearing successions were intruded by dolerite. These intrusions are important as they may cause devolatilisation and burning of the coal, create structural disturbances and related seam correlation problems, and difficulties in mining operations.