GAMMA-KAPPA 765Kv Transmission Line, Western Cape Province
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Plant Species of Special Concern and Vascular Plant Flora of the National
Plant Species of Special Concern and Vascular Plant Flora of the National Elk Refuge Prepared for the US Fish and Wildlife Service National Elk Refuge By Walter Fertig Wyoming Natural Diversity Database The Nature Conservancy 1604 Grand Avenue Laramie, WY 82070 February 28, 1998 Acknowledgements I would like to thank the following individuals for their assistance with this project: Jim Ozenberger, ecologist with the Jackson Ranger District of Bridger-Teton National Forest, for guiding me in his canoe on Flat Creek and for providing aerial photographs and lodging; Jennifer Whipple, Yellowstone National Park botanist, for field assistance and help with field identification of rare Carex species; Dr. David Cooper of Colorado State University, for sharing field information from his 1994 studies; Dr. Ron Hartman and Ernie Nelson of the Rocky Mountain Herbarium, for providing access to unmounted collections by Michele Potkin and others from the National Elk Refuge; Dr. Anton Reznicek of the University of Michigan, for confirming the identification of several problematic Carex specimens; Dr. Robert Dorn for confirming the identification of several vegetative Salix specimens; and lastly Bruce Smith and the staff of the National Elk Refuge for providing funding and logistical support and for allowing me free rein to roam the refuge for plants. 2 Table of Contents Page Introduction . 6 Study Area . 6 Methods . 8 Results . 10 Vascular Plant Flora of the National Elk Refuge . 10 Plant Species of Special Concern . 10 Species Summaries . 23 Aster borealis . 24 Astragalus terminalis . 26 Carex buxbaumii . 28 Carex parryana var. parryana . 30 Carex sartwellii . 32 Carex scirpoidea var. scirpiformis . -
Equisetalean Plant Remains from the Early to Middle Triassic of New South Wales, Australia
Records of the Australian Museum (2001) Vol. 53: 9–20. ISSN 0067-1975 Equisetalean Plant Remains from the Early to Middle Triassic of New South Wales, Australia W.B. KEITH HOLMES “Noonee Nyrang”, Gulgong Road, Wellington NSW 2820, Australia Honorary Research Fellow, Geology Department, University of New England, Armidale NSW 2351, Australia [email protected] Present address: National Botanical Institute, Private Bag X101, Pretoria, 0001, South Africa ABSTRACT. Equisetalean fossil plant remains of Early to Middle Triassic age from New South Wales are described. Robust and persistent nodal diaphragms composed of three zones; a broad central pith disc, a vascular cylinder and a cortical region surrounded by a sheath of conjoined leaf bases, are placed in Nododendron benolongensis n.sp. The new genus Townroviamites is erected for stems previously assigned to Phyllotheca brookvalensis which bear whorls of leaves forming a narrow basal sheath and the number of leaves matches the number of vascular bundles. Finely striated stems bearing leaf whorls consisting of several foliar lobes each formed from four to seven linear conjoined leaves are described as Paraschizoneura jonesii n.sp. Doubts are raised about the presence of the common Permian Gondwanan sphenophyte species Phyllotheca australis and the Northern Hemisphere genus Neocalamites in Middle Triassic floras of Gondwana. HOLMES, W.B. KEITH, 2001. Equisetalean plant remains from the Early to Middle Triassic of New South Wales, Australia. Records of the Australian Museum 53(1): 9–20. The plant Phylum Sphenophyta, which includes the Permian Period, the increasing aridity and decline in the equisetaleans, commonly known as “horse-tails” or vegetation of northern Pangaea was in contrast to that in “scouring rushes”, first appeared during the Devonian southern Pangaea—Gondwana—where flourishing swamp Period (Taylor & Taylor, 1993). -
Plant Fossils and Gondwana Flora
UNIT 12 PLANT FOSSILS AND GONDWANA FLORA Structure_____________________________________________________ 12.1 Introduction Vertebraria Expected Learning Outcomes Thinnfeldia 12.2 Plant Fossils Sigillaria Definition Nilssonia Classification Williamsonia Modes of Preservation Ptilophyllum Significance 12.5 Activity 12.3 Gondwana Flora of India 12.6 Summary 12.4 Descriptions of some Plant 12.7 Terminal Questions Fossils 12.8 References Glossopteris 12.9 Further/Suggested Readings Gangamopteris 12.10 Answers 12.1 INTRODUCTION The animals, plants and micro-organisms are the three main life forms surviving today. Even their fossilised remains are found in rocks that tell us about their past history. The animals comprise invertebrates and vertebrates. In Block 4, you will read about the invertebrates and their geological history that began in the latest Precambrian time. You also read about the microfossils in Unit 10 that too have a long geological record beginning from Precambrian onwards. In Unit 11, you read the evolutionary history of one of the vertebrate groups i.e., horse. In this unit, you will read the plant fossils and the Gondwana flora of India. Introduction to Palaeontology Block……………………………………………………………………………………………….….............….…........ 3 Like the kingdom Animalia, plants also form a separate kingdom known as the Plantae. It is thought that plants appeared first in the Precambrian, but their fossil record is poor. It is also proposed that earliest plants were aquatic and during the Ordovician period a transition from water to land took place that gave rise to non-vascular land plants. However, it was during the Silurian period, that the vascular plants appeared first on the land. The flowering plants emerged rather recently, during the Cretaceous period. -
Clippety Clop), Kwelera, East London, Great Kei Municipality, Eastern Cape
PALAEONTOLOGICAL ASSESSMENT: COMBINED FIELD ASSESSMENT AND DESKTOP STUDY Proposed development of Portion 3 of Farm 695 (Clippety Clop), Kwelera, East London, Great Kei Municipality, Eastern Cape. JOHN E. ALMOND (PhD, Cantab) Natura Viva cc, PO Box 12410 Mill Street, CAPE TOWN 8010, RSA. [email protected] October 2011 1. SUMMARY The proposed holiday housing development on Portion 3 of Farm 695 (Clippety Clop), Kwelera, East London, is situated on the northern banks of the tidal Kwelera River, some 20 km northeast of East London, Eastern Cape. The development footprint is largely underlain by Late Permian continental sediments of the Adelaide Subgroup (Lower Beaufort Group, c. 253-251 million years old). These rocks are overlain by Early Triassic sandstones of the Katberg Formation (Tarkastad Subgroup) that build the cliffs and higher ground to the northeast. South of the river the Beaufort Group sediments are intruded and baked by Early Jurassic igneous intrusions of the Karoo Dolerite Suite. The Balfour Formation fluvial sediments are potentially fossiliferous, having yielded elsewhere a wide range of terrestrial vertebrates (bones and teeth of pareiasaurs, therapsids, amphibians et al.), bivalves, trace fossils and vascular plants. The overall impact of this project on local palaeontological heritage is likely to be very minor, however, because the potentially fossiliferous Beaufort Group sediments here are (a) deeply weathered, (b) sparsely fossiliferous, (c) have probably been extensively baked by nearby dolerite intrusions, and (d) are mostly covered with a thick (> 3m) mantle of fossil-poor alluvium. No fossils were observed within good exposures of the Balfour Formation rocks at the coast and in excellent roadcuts inland. -
The Stratigraphy and Structure of the Kommadagga Subgroup and Contiguous Rocks
THE STRATIGRAPHY AND STRUCTURE OF THE KOMMADAGGA SUBGROUP AND CONTIGUOUS ROCKS by ROGER SWART B.Sc . (Hons) Thesis presented in fulfilment of the requirements for the degree of Master of Science in the Department of Geology, Rhodes University ,Grahamstown. January 1982 ABSTRACT The Lake Mentz and Kommadagga Subgroups were deposited i n a marine environment and are characterised by a heterogeneous sequence of sediments, which range in grain size from clays to grits . During the first phase of deposition the Kwee~ vlei Shale and Floriskraal Formations were deposited in a prograding shoreline environment, whereas the succeeding Waaipoort Shale Formation is interpreted as represnting a reworked shoreline. The final phase of deposition of the Cape Supergroup was a regressive one in which the Kommadagga Subgroup wa s fo rmed. The coa rs eni ng upward cycle of thi s subgroup represents a deltaic deposit. A significant time gap appears to exist before the deposition of the glacial-marine Dwyka Tillite Formation. Structurally, the area was subjected to deformation by buckle folding at about 250 Ma into a series of folds with southward dipping axial planes. Only one phase of deformation is recognised in the study area . A decrease in pore space, mineral overgrowths,formation of silica and calcite cements and development of aut~igenic minerals such as opal, stilpnomelane; analcite, prehnite, muscovite and various clay minerals are the characteristic diagenetic features of the sediments.The mineralogical evidence suggests that the maximum temperature -
Joint Geological Survey/University of Cape Town MARINE GEOSCIENCE UNIT TECHNICAL ^REPORT NO. 13 PROGRESS REPORTS for the YEARS 1
Joint Geological Survey/University of Cape Town MARINE GEOSCIENCE UNIT TECHNICAL ^REPORT NO. 13 PROGRESS REPORTS FOR THE YEARS 1981-1982 Marine Geoscience Group Department of Geology University of Cape Town December 1982 NGU-Tfc—Kh JOINT GEOLOGICAL SURVEY/UNIVERSITY OF CAPE TOWN MARINE GEOSCIENCE UNIT TECHNICAL REPORT NO. 13 PROGRESS REPORTS FOR THE YEARS 1981-1982 Marine Geoscience Group Department of Geology University of Cape Town December 1982 The Joint Geological Survey/University of Cape Town Marine Geoscience Unit is jointly funded by the two parent organizations to promote marine geoscientific activity in South Africa. The Geological Survey Director, Mr L.N.J. Engelbrecht, and the University Research Committee are thanked for their continued generous financial and technical support for this work. The Unit was established in 1975 by the amalgamation of the Marine Geology Programme (funded by SANCOR until 1972) and the Marine Geophysical Unit. Financial ?nd technical assistance from the South African National Committee for Oceanographic Research, and the National Research Institute for Oceanology (Stellenbosch) are also gratefully acknowledged. It is the policy of the Geological Survey and the University of Cape Town that the data obtained may be presented in the form of theses for higher degrees and that completed projects shall be published without delay in appropriate media. The data and conclusions contained in this report are made available for the information of the international scientific community with tl~e request that they be not published in any manner without written permission. CONTENTS Page INTRODUCTION by R.V.Dingle i PRELIMINARY REPORT ON THE BATHYMETRY OF PART OF 1 THE TRANSKEI BASIN by S.H. -
Revealing the Beattie Magnetic Anomaly and the Anatomy Of
11th SAGA Biennial Technical Meeting and Exhibition Swaziland, 16 - 18 September 2009, pages 490 - 499 Revealing the Beattie Magnetic Anomaly and the anatomy of the crust of southernmost Africa: Geophysics and deep sub- surface geology where the Cape Fold Belt and Karroo Basin meet A. S. Lindeque1,2,3, M.J. de Wit4 1. Now at Alfred Wegener Institute for Polar and Marine Research, Geophysics, Building D3280, Am Alten Hafen 26, 27568 Bremerhaven, Germany, [email protected] 2. Council for Geoscience, Western Cape, P.O. Box 572, Bellville 7535, Cape Town, South Africa 3. GeoForschungsZentrum Potsdam, Section 2.2, Telegrafenberg, 14473 Potsdam, Germany 4. AEON - Africa Earth Observatory Network and Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa, [email protected] ABSTRACT The deep crust of the southernmost margin of Africa contains unresolved tectonic features such as the Paleozoic Cape Fold Belt (CFB), the Paleozoic-Mesozoic Karroo Basin and the largest terrestrial magnetic anomaly, the Beattie Magnetic Anomaly (BMA). Without resolving these structures, our understanding of the evolution of the southern margin will be incomplete and limited. Under the auspices of the Inkaba yeAfrica framework, several geophysical datasets were acquired from 2004 to 2007, along two transects across the margin and its unique tectonic features. This research presents a tectonic model and crustal geometry, at the centre 100 km of the western transect. The model is derived from the joint interpretation of: surface geology, aeromagnetic data, nearby deep boreholes, teleseismic receiver functions, impedance spectroscopy measurements on borehole samples, near vertical reflection seismic data (NVR), shallow P- and S-wave velocity data, wide angle refraction data and magnetotelluric data. -
Fundamentals of Palaeobotany Fundamentals of Palaeobotany
Fundamentals of Palaeobotany Fundamentals of Palaeobotany cuGU .叮 v FimditLU'φL-EjAA ρummmm 吋 eαymGfr 伊拉ddd仇側向iep M d、 況 O C O W Illustrations by the author uc削 ∞叩N Nn凹創 刊,叫MH h 咀 可 白 a aEE-- EEA First published in 1987 by Chapman αndHallLtd 11 New Fetter Lane, London EC4P 4EE Published in the USA by Chα~pman and H all 29 West 35th Street: New Yo地 NY 10001 。 1987 S. V. M秒len Softcover reprint of the hardcover 1st edition 1987 ISBN-13: 978-94-010-7916-7 e-ISBN-13: 978-94-009-3151-0 DO1: 10.1007/978-94-009-3151-0 All rights reserved. No part of this book may be reprinted, or reproduced or utilized in any form or by any electronic, mechanical or other means, now known or hereafter invented, including photocopying and recording, or in any information storage and retrieval system, without permission in writing from the publisher. British Library Cataloguing in Publication Data Mey凹, Sergei V. Fundamentals of palaeobotany. 1. Palaeobotany I. Title 11. Osnovy paleobotaniki. English 561 QE905 Library 01 Congress Catα loging in Publication Data Mey凹, Sergei Viktorovich. Fundamentals of palaeobotany. Bibliography: p. Includes index. 1. Paleobotany. I. Title. QE904.AIM45 561 8ι13000 Contents Foreword page xi Introduction xvii Acknowledgements xx Abbreviations xxi 1. Preservation 抄'pes αnd techniques of study of fossil plants 1 2. Principles of typology and of nomenclature of fossil plants 5 Parataxa and eutaxa S Taxa and characters 8 Peculiarity of the taxonomy and nomenclature of fossil plants 11 The binary (dual) system of fossil plants 12 The reasons for the inflation of generic na,mes 13 The species problem in palaeobotany lS The polytypic concept of the species 17 Assemblage-genera and assemblage-species 17 The cladistic methods 18 3. -
New Ephedroid Plant from the Lower Cretaceous Koonwarra Fossil Bed, Victoria, Australia
New ephedroid plant from the Lower Cretaceous Koonwarra Fossil Bed, Victoria, Australia V. A. KRASSILOV, D. L. DILCHER, AND 1. G. DOUGLAS KAA~~lLOv, VA., DlLCHeR. D.L.. & Douou.~, J.G.. 1998:03:31. New ephedroid plant from the Lower Cretaceous Koonwarra Fossil Bed. ViCloria, Aurualia. Alcheringa 22, 123-133. ISSN 0311 5518. A revision of the Lower Cretaceous Koonwarra mll1erial fint allSigned to angiosperms and subse quently to sphenopsids shows morphological and analOmical <:hanlcIen typical ofe:Phedroid (gnetophyte) affinities. Shoots are preserved lUI clayey-ferruginous films deposited beneath the cuticle reflecting eitherthe interior reliefofthe epidermal cell panem orsubepidermal sclerencbymow stlaI1ds (rugulJue striations) and vascular tissue of the internodes. The articulate aho<xs are similar to Ephedra foliata and some Olher extant species with 3-4 decussate, basally camate leaves III each node, sunken stomllla in interoostal zones, allernating large and small vasallarbWldles. paired leaf traces, and the morphol. ogy oftracheary elements. but differ in the leafnurnber per node ranging from two to eight and in the oonsiderably lowerratio of leaves to internode vlUlCUlar bWldles. A new genus and speciesLeongalhia elegans is described. The oo-occurrence of gnetophytes and early angiosperms in the lower Aptian of Koonwarra is of cerUlin evolutionary and palaeoecological significance. The KOOllwarra material in crealles the known diversity of the Cretaceous gnela1eans by presenting a hitherto unrecordedEphe dra-like shO<XlDorphology. VA. Kra.ssilov, PalaeonUJlogical 1nsuluJe, 123 Profsojusnaya, Moscow. 117647, RUSSUl .. D. L. Dilchu. Florida Museum of Nalwa1 History, Universiry ofFlorida, Gainesville. FL. 32611, USA .. J. G. Douglas, 41 Gril!Ve SI., Wamlambool, VICtoria 3280, Ausrralia . -
Taphonomy As an Aid to African Palaeontology*
Palaeont. afr., 24 (1981 ) PRESIDENTIAL ADDRESS: TAPHONOMY AS AN AID TO AFRICAN PALAEONTOLOGY* by C.K. Brain Transvaal Museum, P.O. Box 413, Pretoria 0001 SUMMARY Palaeontology has its roots in both the earth and life sciences. Its usefulness to geology comes from the light which the understanding of fossils may throw on the stratigraphic re lationships of sediments, or the presence of economic deposits such as coal or oil. In biology, the study of fossils has the same objectives as does the study of living animals or plants and such objectives are generally reached in a series of steps which may be set out as follows: STEP I. Discovering what forms of life are, or were, to be found in a particular place at a particular time. Each form is allocated a name and is fitted into a system of classification. These contributions are made by the taxonomist or the systematist. STEP 2. Gaining afuller understanding ofeach described taxon as a living entity. Here the input is from the anatomist, developmental biologist, genetIcIst, physi ologist or ethologist and the information gained is likely to modify earlier decisions taken on the systematic position of the forms involved. STEP 3. Understanding the position ofeach form in the living community or ecosystem. This step is usually taken by a population biologist or ecologist. Hopefully, any competent neo- or palaeobiologist (I use the latter term deliberately in this context in preference to "palaeontologist") should be able to contribute to more than one of the steps outlined above. Although the taxonomic and systematic steps have traditionally been taken in museums or related institutions, it is encouraging to see that some of the steps subsequent to these very basic classificatory ones are now also being taken by museum biol ogists. -
Rademan Radiometric 2018.Pdf (11.89Mb)
Radiometric dating and stratigraphic reassessment of the Elliot and Clarens formations; near Maphutseng and Moyeni, Kingdom of Lesotho, southern Africa Ms. Zandri Rademan, 16964063 Thesis presented in partial fulfilment of the requirements for the degree of Masters of Science at University of Stellenbosch Supervisor: Dr. R. T. Tucker (University of Stellenbosch) Co-advisor: Dr. E. M. Bordy (University of Cape Town) Department of Earth Sciences Faculty of Science RSA December 2018 Stellenbosch University https://scholar.sun.ac.za DECLARATION By submitting this dissertation electronically, I declare that the entirety of the work contained herein is my own, original work, that I am the sole author thereof (except where explicitly otherwise stated), that reproduction and publication thereof by Stellenbosch University will not infringe any third-party rights and that I have not previously in its entirety or in part submitted it for obtaining any qualification. Date: December 2018 Copyright © 2018 Stellenbosch University All rights reserved Stellenbosch University https://scholar.sun.ac.za ACKNOWLEDGEMENTS Firstly, I would like to thank my supervisor, Dr. R. T. Tucker (University of Stellenbosch), for his guidance throughout this project. Thank you for allowing this paper to be my own work; yet, steering me in the right direction whenever I hit a speed-bump and careened off the path. Thank you for your patience through all the blood, sweat and tears, it’s been quite the journey. My utmost gratitude goes to Dr. E. M. Bordy (University of Cape Town) for taking me under her wing and granting me the opportunity to tackle this project, as well as graciously offering advice and aid from her great well of expertise. -
Stratigraphy, Sedimentary Facies and Diagenesis of the Ecca Group, Karoo Supergroup in the Eastern Cape, South Africa
STRATIGRAPHY, SEDIMENTARY FACIES AND DIAGENESIS OF THE ECCA GROUP, KAROO SUPERGROUP IN THE EASTERN CAPE, SOUTH AFRICA By Nonhlanhla Nyathi Dissertation submitted in fulfilment of the requirements for the degree of Master of Science In Geology FACULTY OF SCIENCE AND AGRICULTURE UNIVERSITY OF FORT HARE SUPERVISOR: PROFESSOR K. LIU CO-SUPERVISOR: PROFESSOR O. GWAVAVA APRIL 2014 DECLARATION I, Nonhlanhla Nyathi, hereby declare that the research described in this dissertation was carried out in the field and under the auspices of the Department of Geology, University of Fort Hare, under the supervision of Professor K. Liu and Prof. O. Gwavava. This dissertation and the accompanying photographs represent original work by the author, and have not been submitted, in whole or in part, to any other university for the purpose of a higher degree. Where reference has been made to the work of others, it has been dully acknowledged in the text. N. NYATHI Date signed: 12/04/2014 Place signed: Alice ACKNOWLEDGEMENTS The author is indebted to Professor K. Liu for his guidance, knowledge on all aspects of the project, constant supervision and help in doing field wok. Professor O. Gwavava is much appreciated for being my co-supervisor and helping me obtain financial support from the Goven Mbeki Research Development Centre. I am deeply grateful for the emotional support and encouragement from my parents and family. I express my profound gratitude to Mr Edwin Mutototwa and Mr Eric Madifor always taking time to read through my dissertation. The Rhodes University Geology laboratory technicians are thanked for their assistance in the making of thin sections.