Palaeoenvironmental Studies of the Middle Triassic Uppermost Narrabeen Group, Sydney Basin

Total Page:16

File Type:pdf, Size:1020Kb

Palaeoenvironmental Studies of the Middle Triassic Uppermost Narrabeen Group, Sydney Basin PALAEOENVIRONMENTAL STUDIES OF THE MIDDLE TRIASSIC UPPERMOST NARRABEEN GROUP, SYDNEY BASIN: PALAEOECOLOGICAL CONSTRAINTS WITH PARTICULAR EMPHASIS ON TRACE FOSSIL ASSEMBLAGES by Thann Naing, BSc. (Hons.), Rangoon University. Dip. Appld. Geol. (Hons.), Rangoon University, MSc, (Hons.), Rangoon University. A thesis submitted to Macquarie University in fulfilment of the requirements for the degree of Doctor of Philosophy 1990 Copyright in relation to this Thesis Under the Copyright Act 1968 (several provision of which are referred to below), this material must be used only under the normal conditions of scholarly fair dealing for the purposes of research, criticism or review. In particular no results or conclusions should be extracted from it, nor should it be copied or closely parahrased in whole or in part without the written consent of the author. Proper written acknowledgement should be made for any assistance obtained from this material. Under Section 35 (2) of the Copyright Act 1968 'the author of a literary, dramatic, musical or artistic work is the owner of any copyright subsisting in the work'. By virtue of Section 32 (1) copyright 'subsists in an original literary, dramatic, musical or artistic work that is unpublished' land of which the author was an Australian citizen, an Australian protected person or a person resident in Australia. The Act, by Section 36(1) provides: 'Subject to this Act, the copyright in a literary, dramatic, musical or artistic work is infringed by a person who, not being the owner of the copyright and without the licence of the owner of the copyright, does in Australia, or authorises the doing in Australia of, any act comprised in the copyright'. Section 31 (1) (a) (i) provides that copyright includes the exclusive right to 'reproduce the work in a material form'. Thus, copyright is infringed by a person who, not being the owner of the copyright, reproduces or authorises the reproduction of a work, or of more than a reasonable part of the work, in a material form, unless the reproduction is a 'fair dealing' with the work 'for the purpose of research or study' as further defined in Sections 40 and 41 of the Act. Section 51 (2) provides that "Where a manuscript, or a copy, of material of other similar literary work that has not been published is kept in a library of a university or other similar institution or in an archives, the copyright in the material or other work is not infringed by the making of a copy of the material or other work by or on behalf of the officer in charge of the library or archives if the copy is supplied to a person who satisfies an authorized officer of the library or archives that he requires the copy for the purpose of research or study'. * Thesis' includes ' treatise', ' dissertation' and other similar productions. VOLUME IB BIBLIOGRAPHY AND APPENDIXES BIBLIOGRAPHY 596 BIBLIOGRAPHY Abel, O. , 1935, Vorzeitliche Lebensspuren. Gustav. Fischer (Jena), pp. 644, 530 text-figs. Alf, R.M., 1959, Possible fossils from the Early Proterozoic Bass Formation, Grand Canyon, Arizona. Plateau, vol. 31, p. 60- 63. Allen, E.A. and Curran, H.A., 1974, Biogenic sedimentary structures produced by the Crab in lagoon margin and salt marsh environments near Beaufort, North Carolina. Jour. Sed. Pet., 44(2), 538-548. Allen, J.A.R. and Williams, B.P.J., 1981, Beaconites Antarcticus: A giant channel-associated trace fossil from the Lower Old Red Sandstone of South Wales and the Welsh border. Geol. Jour., vol. 16, p. 255-269. Allen, J.A.R., 1989, Shortpaper: Fossil Vertebrate Tracks and Indenter Mechanics. Jour. Geol. Soc, Lond., vol. 146, p. 600-602, 4 figs. Alpert, S.P., 1974, Systematic review of te genus Skolithos . Jour. Paleont., vol. 48, pp. 661-669. ., 1975, Planolites and Skolithos from the Upper Precambrian - Lower Cambrian, White-Inyo Mountains, California. Jour. Paleont., vol. 49, p. 509-521. Asgaard, W. and Bromley, R.G., 1974 (1973), Sporfossiler fra den meilem Miocaene trangression 1 soby-fasterholt omradet. Geol. Surv. Den. Arsskr., p. 11-19. Baatz, H., 1959, Ophiomorpha Lundgren, eines marines spurenfossil, in Oberen quartzsand Nieder Hessens. Notzbl. Hess. Landesant. Bodenforsch. Wiesbaden. , 87: 168-171. Balme, B.E., 1969, The Permian-Triassic Boundary in Australia. Spec. Pubis. Geol. Aust., 2: 99-112. Banks, M.R., 1978, Correlation chart for the Triassic Systems of Australia. Aust. Bur. Miner. Resour., Geol. Geophys., Bull., 156C: 1-39. Barbour, E.H., 1892, Notice of new Gigantic fossils. Science, vol. 19, p. 99-100. Bassler, R.S., 1941, A supposed jellyfish from the Pre-cambrian of the Grand Canyon: , , Proc., vol. 89, no. 3104, p. 519- 522, illus. U.S. Natl. Muse-am, Bayer, W., Altheimer, E. and Deutsche, W., 1985, Environmental 597 evolution in shallow epicontinental seas: sedimentary cycles and bed formation. Iji U. Bayer & A. Seilacher (eds.) , sedimentary and evolution cycles. Springer-Verlag, p. 347- 381. Beale, R. , 1986, There's a bit of Paracyclotosaurus about: Sydney Morn. Herald. (News Paper on 21-3-86) . Bembrick, C, 1980, Geology of the Blue Mountains, Western Sydney Basin. J-n_ C. Herbert & R. Helby (eds.) , A guide to the Sydney Basin, Dept. Min. Res., Geol. Surv. N.S.W., p. 134- 11. Benton, M.J. and Trewin, N.H., 1978, Discussion and comments on Nicholson's 1872 manuscript "contributions to the study of errant annelides of the older palaeozoic rocks. Publ. Dept. Geol. Min. Univ. Aberdeen, vol. 1, p. 1-16. Bentz, A., 1929, Rossile Rohrenbauten im Unterneokom des Isterberes bei Bentheim: Preuss. Geol. Landesanst. , Jahrb., vol. 49, pt. 2 (1928), p. 1173-1183, pi. 1. Billings, E., 1862, New species of fossils from different parts of the Lower, Middle and Upper Silurian rocks of Canada. In. Paleozoic fossils. Geol. Surv. Can., vol. 1, p. 96-168. Bjerstedt, T.W., 1987, Latest Devonian-Earliest Mississipian nearshore trace fossil assemblages from West Virginia, Pennsylvania and Maryland. Jour. Paleont., vol. 61, no. 5, p. 865-889. ., 1988, Trace fossils from the Early Mississipian Price Delta, southeast West Virginia. Jour. Paleont., vol. 62, no. 4, p. 506-519, figs. 10. Birkenmajer, K., 1971, Some trilobite resting and crawling traces: Lethaia, vol. 4, p. 303-319, 14 text-fig. Blanckenhorn, M., 1917, Organische reste im mittlern buntsandstein hessens s-ber. Ges. Beford, Ges. Naturwiss (1916), Marburg (1917). s., p. 21-45. Bogachev [Bogatschew], V.V., 1908, Problematicheskaya vodorosly Taonurus v Russkom Paleogen: Ezhegodnik po Geologii i Mineralogii, vol. 10, no. 7-8, p. 221-223, text-fig. 1-3 (Ger. text p. 224-226). [The problematic alga Taonurus from the Russian Paleogene.] Bowman, H.N., Stroud, W.J., Sherwin, L. and Rays, H.N., 1986, Sydney Basin stratigraphy: In. L. Sherwin & G.G. Holmes (eds.) , Geology of the Wollongong and Port Hacking, 1:100,000 sheets 9029, 9129. Geol. Surv. N.S.W. Bown, T.M. , 1982, Ichnofossils and rhizoliths of the near shore fluvial Jebel Qatrani Formation (Oligocene), Fayum Province, 598 Egypt. Palaeogeo. Palaeoclim. Palaeoeco., 40: 255-309. Bown, T.M. and Kraus, M.J., 1983, Ichnofossils of the alluvial Willwood Formation (Lower Eocene), Bighorn basin, northwest Wyoming, U.S.A. Palaeogeo. Palaeoclim. Palaeoeco., 43: 95- 128. Boyd, D.W., 1966, Lamination deformed by burrowers in Flathead Sandstone (Middle Cambrian) of Central Wyoming. Cont., 5: 45-54. Boyd, D.W., 1975, False or misleading traces. In. R.W. Frey (ed.), The Study of Trace Fossils. Springer-Verlag, New York, p. 65-83. Bracken, B. and Pickard, M.D., 1984, Trace fossils from cretaceous. Tertiary North Horn Formation in Central Utah. Jour. Paleont., vol. 58, no. 2, p. 477-489, 13 figs. Bradley, G.M., Yoo, E.K., Moloney, J., Beckett, J. and Richardson, S.J., 1985, Petroleum data package, Sydney Basin, New South Wales. Geol. Surv. N.S.W., Report GS 1985/004. Bradley, J., 1981, Zoophycos and Umbellula (Pennatulacea) : their synthesis and identity. Palaeogeog. Palaeoclimatol. Palaeoeco., vol. 13, no. 2, p. 103-128. Bradshaw, M.A., 1981, Palaeoenvironmental interpretation and systematics of Devonian trace fossils from Tayer Group (Lower Beacon Super Group), Antarctica. New Zealand, Jour. Geol. Geophys., vol. 24, p. 615-652. Braithwaite, C.J.R. and Talbot, M.R., 1972, Crustacean burrows in the Seychelles, Indian Ocean. Palaeogeo. Palaeoclim. Palaeoeco., 11:265-285. Branagan, D. , Herbert, C. and Langford-Smith, T., 1966, Notes on the Narrabeen Group (Triassic) coastal section north of Long Reef, Sydney Basin. Aust. Jour. Sc., 29(4): 117-118. Brenchley, P.J., 1985, Str}pm influenced sandstone beds. Modern Geology, vol. 9, no. 4, p. 369-396. Bromley, R.G. and Frey, R.W., 1974, Redescription of the trace fossil Gyroli thes and taxonomic evaluation of Thalassinoides, Ophiomorpha and Spongeliomorpha. Bull. Geol. Soc. Den., 23: 311-335. ., 1975, Trace fossils at omission surfaces. In R.W. Frey (ed.). The study of trace fossils, Springer- Verlag, New York, p. 399-428. ., Curran, H.A., Frey, R.W., Gutschick, R.C. and Suttner, L.J., 1975, Problems in interpreting unusually large burrows. In. R.W. Frey (eds.) , In The study of trace fossils. Springer-Verlag, New York, U.S.A., p. 351-376. and Asgaard, U., 1979, Triassic fresh water ichnocoenoses from Carlsberg Fjord, East Greenland, Palaeogeogr. Palaeoclimatol, Palaeoecol., vol. 28, p. 39-80. and Ekdale, A.A., 1984, Chondrites: A trace fossil indicator of anoxia in sediments. Sciences, vol. 224, p. 872-874. and Ekdale, A.A., 1986, Composite ichnofabrics and tiering of burrows. Geol. Mag., vol. 123, no. 1, p. 59- 65. Brongniart, A.T., 1823, Observations sur les Fucoides: Soc. Histoire Nat. Paris, Mem., vol. 1, p. 301-320, pi. 19-21. ., 1828-38, Histoire des vegetaux fossiles ou recherches botaniques et geologiques sur les vegetaux renfermes dans les diverses couches du globe: vol.
Recommended publications
  • 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).
    [Show full text]
  • Onetouch 4.0 Scanned Documents
    / Chapter 2 THE FOSSIL RECORD OF BIRDS Storrs L. Olson Department of Vertebrate Zoology National Museum of Natural History Smithsonian Institution Washington, DC. I. Introduction 80 II. Archaeopteryx 85 III. Early Cretaceous Birds 87 IV. Hesperornithiformes 89 V. Ichthyornithiformes 91 VI. Other Mesozojc Birds 92 VII. Paleognathous Birds 96 A. The Problem of the Origins of Paleognathous Birds 96 B. The Fossil Record of Paleognathous Birds 104 VIII. The "Basal" Land Bird Assemblage 107 A. Opisthocomidae 109 B. Musophagidae 109 C. Cuculidae HO D. Falconidae HI E. Sagittariidae 112 F. Accipitridae 112 G. Pandionidae 114 H. Galliformes 114 1. Family Incertae Sedis Turnicidae 119 J. Columbiformes 119 K. Psittaciforines 120 L. Family Incertae Sedis Zygodactylidae 121 IX. The "Higher" Land Bird Assemblage 122 A. Coliiformes 124 B. Coraciiformes (Including Trogonidae and Galbulae) 124 C. Strigiformes 129 D. Caprimulgiformes 132 E. Apodiformes 134 F. Family Incertae Sedis Trochilidae 135 G. Order Incertae Sedis Bucerotiformes (Including Upupae) 136 H. Piciformes 138 I. Passeriformes 139 X. The Water Bird Assemblage 141 A. Gruiformes 142 B. Family Incertae Sedis Ardeidae 165 79 Avian Biology, Vol. Vlll ISBN 0-12-249408-3 80 STORES L. OLSON C. Family Incertae Sedis Podicipedidae 168 D. Charadriiformes 169 E. Anseriformes 186 F. Ciconiiformes 188 G. Pelecaniformes 192 H. Procellariiformes 208 I. Gaviiformes 212 J. Sphenisciformes 217 XI. Conclusion 217 References 218 I. Introduction Avian paleontology has long been a poor stepsister to its mammalian counterpart, a fact that may be attributed in some measure to an insufRcien- cy of qualified workers and to the absence in birds of heterodont teeth, on which the greater proportion of the fossil record of mammals is founded.
    [Show full text]
  • United States
    DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES ISTo. 146 WASHINGTON GOVERNMENT Pit IN TING OFFICE 189C UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DI11ECTOK BIBLIOGRAPHY AND INDEX NORTH AMEEICAN GEOLOGY, PALEONTOLOGY, PETEOLOGT, AND MINERALOGY THE YEA.R 1895 FEED BOUGHTON WEEKS WASHINGTON Cr O V E U N M K N T P K 1 N T I N G OFFICE 1890 CONTENTS. Page. Letter of trail smittal...... ....................... .......................... 7 Introduction.............'................................................... 9 List of publications examined............................................... 11 Classified key to tlio index .......................................... ........ 15 Bibliography ............................................................... 21 Index....................................................................... 89 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTEEIOE, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washington, D. 0., June 23, 1896. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the year 1895, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINER­ ALOGY FOR THE YEAR 1895. By FRED BOUGHTON WEEKS. INTRODUCTION. The present work comprises a record of publications on North Ameri­ can geology, paleontology, petrology, and mineralogy for the year 1895. It is planned on the same lines as the previous bulletins (Nos. 130 and 135), excepting that abstracts appearing in regular periodicals have been omitted in this volume. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica­ tion in which the paper is printed, and a brief summary of the con­ tents, each paper being numbered for index reference.
    [Show full text]
  • Northumbria Research Link
    Northumbria Research Link Citation: Hutchinson, David K., Coxall, Helen K., Lunt, Daniel J., Steinthorsdottir, Margret, de Boer, Agatha M., Baatsen, Michiel, von der Heydt, Anna, Huber, Matthew, Kennedy- Asser, Alan T., Kunzmann, Lutz, Ladant, Jean-Baptiste, Lear, Caroline H., Moraweck, Karolin, Pearson, Paul N., Piga, Emanuela, Pound, Matthew, Salzmann, Ulrich, Scher, Howie D., Sijp, Willem P., Śliwińska, Kasia K., Wilson, Paul A. and Zhang, Zhongshi (2021) The Eocene-Oligocene transition: a review of marine and terrestrial proxy data, models and model-data comparisons. Climate of the Past, 17 (1). pp. 269-315. ISSN 1814-9324 Published by: Copernicus Publications URL: https://doi.org/10.5194/cp-17-269-2021 <https://doi.org/10.5194/cp-17-269-2021> This version was downloaded from Northumbria Research Link: http://nrl.northumbria.ac.uk/id/eprint/44997/ Northumbria University has developed Northumbria Research Link (NRL) to enable users to access the University’s research output. Copyright © and moral rights for items on NRL are retained by the individual author(s) and/or other copyright owners. Single copies of full items can be reproduced, displayed or performed, and given to third parties in any format or medium for personal research or study, educational, or not-for-profit purposes without prior permission or charge, provided the authors, title and full bibliographic details are given, as well as a hyperlink and/or URL to the original metadata page. The content must not be changed in any way. Full items must not be sold commercially in any format or medium without formal permission of the copyright holder.
    [Show full text]
  • Background Paper on New South Wales Geology with a Focus on Basins Containing Coal Seam Gas Resources
    Background Paper on New South Wales Geology With a Focus on Basins Containing Coal Seam Gas Resources for Office of the NSW Chief Scientist and Engineer by Colin R. Ward and Bryce F.J. Kelly School of Biological, Earth and Environmental Sciences University of New South Wales Date of Issue: 28 August 2013 Our Reference: J083550 CONTENTS Page 1. AIMS OF THE BACKGROUND PAPER .............................................................. 1 1.1. SIGNIFICANCE OF AUSTRALIAN CSG RESOURCES AND PRODUCTION ................... 1 1.2. DISCLOSURE .................................................................................................... 2 2. GEOLOGY AND EVALUATION OF COAL AND COAL SEAM GAS RESOURCES ............................................................................................................. 3 2.1. NATURE AND ORIGIN OF COAL ........................................................................... 3 2.2. CHEMICAL AND PHYSICAL PROPERTIES OF COAL ................................................ 4 2.3. PETROGRAPHIC PROPERTIES OF COAL ............................................................... 4 2.4. GEOLOGICAL FEATURES OF COAL SEAMS .......................................................... 6 2.5. NATURE AND ORIGIN OF GAS IN COAL SEAMS .................................................... 8 2.6. GAS CONTENT DETERMINATION ........................................................................10 2.7. SORPTION ISOTHERMS AND GAS HOLDING CAPACITY .........................................11 2.8. METHANE SATURATION ....................................................................................12
    [Show full text]
  • The Carboniferous Evolution of Nova Scotia
    Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic.
    [Show full text]
  • Albian Ammonites from Northern Pakistan
    DE DE GRUYTER Acta Geologica Polonica, Vol. 64 (2014), No. 1, pp. 47–98 OPEN DOI: 10.2478/agp-2014-0003 G Albian ammonites from northern Pakistan WILLIAM JAMES KENNEDY1 AND ALI N. FATMI2 1Oxford University Museum of Natural History, Parks Road, Oxford OX1 3W and Department of Earth Sciences, Parks Road, Oxford OX1 3AN, United Kingdom. E-mail: [email protected] 2Formerly of the Geological Survey of Pakistan, Quetta, Pakistan (Dr Fatmi died on 27 March 2012) ABSTRACT: Kennedy, W.J. and Fatmi, A.N. 2014. Albian ammonites from northern Pakistan. Acta Geologica Polonica, 64 (1), 47–98. Warszawa. The occurrence of rich Albian ammonite faunas in what is now northern Pakistan has been known for more than 80 years, but there has been no comprehensive account of the assemblages present. A total of 36 taxa are described below. The middle part of the Lumshiwal Formation yields Upper Aptian ammonites south of the Samana Range. Elsewhere, it yields Douvilleiceras leightonense Casey, 1962, of the lower Lower Albian Leymeriella reg- ularis Zone and the Sonneratia perinflata and S. kitchini Subzones of the Sonneratia chalensis Zone of the north- west European sequence. The top one to two metres of the Lumshiwal yields an abundant fauna of rolled and phos- phatised ammonites that includes elements from much of the Albian. Of these, Prolyelliceras gevreyi (Jacob, 1907) first appears in the lower Lower Albian Leymeriella tardefurcata Zone. The commonest ammonite is Douville- iceras mammillatum (Schlotheim, 1813) sensu lato, which ranges from the perinflata Subzone of the chalensis Zone to the Otohoplites bulliensis Subzone of the O.
    [Show full text]
  • Paleontological Exploration in Africa
    Paleontological Exploration in Africa A View from the Rukwa Rift Basin of Tanzania Nancy J. Stevens, Michael D. Gottfried, Eric M. Roberts, Saidi Kapilima, Sifa Ngasala and Patrick M. O’Connor Introduction The Mesozoic – Cenozoic transition was a period of dramatic global change during which time the Earth’s continents were in the process of fragmenting from a large, relatively continuous landmass to assume a configuration similar to that seen today. The most significant tectonic activity in the southern hemisphere occurred during the Cretaceous-Paleogene interval, when the large Gondwanan sub-regions of Africa, South America, Australia, Indo- Madagascar and Antarctica became increasingly isolated from one another (Smith et al., 1994; Scotese, 2001). Continental dynamics of this scale are not only geologically significant, they also profoundly influenced the evolution of both terrestrial and marine biotas (Forster, 1999; Krause et al., 1999; Sereno, 1999; Lieberman, 2000; Upchurch et al., 2002; Humphries and Ebach, 2004). Indeed, the Cretaceous-Paleogene transition marks large-scale faunal turnover of major vertebrate and invertebrate taxa (e.g., extinction of nonavian dinosaurs, radiation of ‘‘modern’’ mammals and birds; Cracraft, 2001; Springer et al., 2003, 2004; Archibald and Fastovsky, 2004; Kielan-Jaworowska et al., 2004; Rose and Archibald, 2004; Clarke et al., 2005). Numerous hypotheses have been proposed to explain the origin, diversifica- tion, and extinction of many vertebrate groups living on, or dispersing through, Gondwana during the Cretaceous and Paleogene. For example, molecular studies have postulated a Cretaceous-Paleogene African origin for a number of higher-level amniote clades, including Placentalia (Murphy et al., 2001 and references therein), Afrotheria (Hedges et al., 1996; Springer et al., 1997, 2003, Nancy J.
    [Show full text]
  • The First Fossil Owl (Aves, Strigiformes) from the Paleogene of Africa
    diversity Article The First Fossil Owl (Aves, Strigiformes) From the Paleogene of Africa N. Adam Smith 1,* , Thomas A. Stidham 2,3,4 and Jonathan S. Mitchell 5 1 Campbell Geology Museum, Clemson University, Clemson, SC 29634, USA 2 Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China; [email protected] 3 CAS—Center for Excellence in Life and Paleoenvironment, Beijing 100044, China 4 University of Chinese Academy of Sciences, Beijing 100049, China 5 West Virginia University Institute of Technology, Beckley, WV 25801, USA; [email protected] * Correspondence: [email protected] Received: 10 April 2020; Accepted: 21 April 2020; Published: 23 April 2020 Abstract: The relatively extensive fossil record of owls (Aves, Strigiformes) in North America and Europe stands in stark contrast to the paucity of fossil strigiformes from Africa. The first occurrence of a fossil owl from the Paleogene of Africa extends the fossil record of this clade on that continent by as much as 25 million years, and confirms the presence of large-sized owls in Oligocene continental faunas. The new fossil is tentatively referred to the Selenornithinae, a clade of large owls previously restricted to Europe. This new fossil owl was likely similar in size to the extant Eagle Owls of the genus Bubo, and suggests that the niche of large, volant, terrestrial avian predator, although relatively rare throughout avian evolutionary history, may be an ecological role that was more common among extinct owls than previously recognized. Keywords: Egypt; Fayum Depression; Jebel Qatrani Formation; Oligocene; Selenornithinae 1.
    [Show full text]
  • Body Fossils and Root-Penetration Structures
    CHAPTER 16 BODY FOSSILS AND ROOT-PENETRATION STRUCTURES 482 BODY FOSSILS AND ROOT-PENETRATION STRUCTURES RECORDED FROM THE STUDY AREA 16.1. INTRODUCTION There are three major groups of body fossils that occur in the Triassic rocks of the study area, including the Hawkesbury Sandstone. The first group comprises fossil plant remains, which are abundant and previously well studied (e.g. Helby, 1969a,b & 1973; Retallack, 1976, 1977a, b, c, & 1980), and root-penetration structures. The second group comprises fossil animal remains which are extremely rare and, except for locally abundant fossil freshwater fish in shale lenses in the Hawkesbury Sandstone and the Gosford (=Terrigal) Formation (see Reggatt, in Packham 1969, P.407; and Branagan, in Packham 1969, p.415-416), include the bones of amphibians (e.g. Warren, 1972 & 1983; and Beale, 1985) and bivalve mollusc shells of mytilid affinity (Grant-Mackie et al., 1985). Additionally, the freshwater fossil pelecypod, Unio, the branchiopod Estheria, and a variety of insects have been recorded from the Hawkesbury Sandstone (cf. Branagan, in Packham 1969, p.417). The third group comprises microfossils (microfauna and microflora) (e.g. Helby, in Packham, 1969 p.404-405 and 417; Retallack, 1980; Grant-Mackie et al., 1985). The abundance of spores, megaspores, intact spore tetrads, and abundant quantities of other microscopic organic materials including acritarchs (possibility having been reworked) have been suggested as evi­ dence that the palaeoenvironment of the Newport Formation was as marginal marine, possibly of lagoonal or estuarine character (Grant-Mackie et al., 1985). 483 16.2. TAXONOMY OF THE PLANT REMAINS AND ROOT-PENETRATION STRUCTURES 16.2.1.
    [Show full text]
  • Ammonite Faunal Dynamics Across Bio−Events During the Mid− and Late Cretaceous Along the Russian Pacific Coast
    Ammonite faunal dynamics across bio−events during the mid− and Late Cretaceous along the Russian Pacific coast ELENA A. JAGT−YAZYKOVA Jagt−Yazykova, E.A. 2012. Ammonite faunal dynamics across bio−events during the mid− and Late Cretaceous along the Russian Pacific coast. Acta Palaeontologica Polonica 57 (4): 737–748. The present paper focuses on the evolutionary dynamics of ammonites from sections along the Russian Pacific coast dur− ing the mid− and Late Cretaceous. Changes in ammonite diversity (i.e., disappearance [extinction or emigration], appear− ance [origination or immigration], and total number of species present) constitute the basis for the identification of the main bio−events. The regional diversity curve reflects all global mass extinctions, faunal turnovers, and radiations. In the case of the Pacific coastal regions, such bio−events (which are comparatively easily recognised and have been described in detail), rather than first or last appearance datums of index species, should be used for global correlation. This is because of the high degree of endemism and provinciality of Cretaceous macrofaunas from the Pacific region in general and of ammonites in particular. Key words: Ammonoidea, evolution, bio−events, Cretaceous, Far East Russia, Pacific. Elena A. Jagt−Yazykova [[email protected]], Zakład Paleobiologii, Katedra Biosystematyki, Uniwersytet Opolski, ul. Oleska 22, PL−45−052 Opole, Poland. Received 9 July 2011, accepted 6 March 2012, available online 8 March 2012. Copyright © 2012 E.A. Jagt−Yazykova. This is an open−access article distributed under the terms of the Creative Com− mons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
    [Show full text]
  • Terra Nostra 2018, 1; Mte13
    IMPRINT TERRA NOSTRA – Schriften der GeoUnion Alfred-Wegener-Stiftung Publisher Verlag GeoUnion Alfred-Wegener-Stiftung c/o Universität Potsdam, Institut für Erd- und Umweltwissenschaften Karl-Liebknecht-Str. 24-25, Haus 27, 14476 Potsdam, Germany Tel.: +49 (0)331-977-5789, Fax: +49 (0)331-977-5700 E-Mail: [email protected] Editorial office Dr. Christof Ellger Schriftleitung GeoUnion Alfred-Wegener-Stiftung c/o Universität Potsdam, Institut für Erd- und Umweltwissenschaften Karl-Liebknecht-Str. 24-25, Haus 27, 14476 Potsdam, Germany Tel.: +49 (0)331-977-5789, Fax: +49 (0)331-977-5700 E-Mail: [email protected] Vol. 2018/1 13th Symposium on Mesozoic Terrestrial Ecosystems and Biota (MTE13) Heft 2018/1 Abstracts Editors Thomas Martin, Rico Schellhorn & Julia A. Schultz Herausgeber Steinmann-Institut für Geologie, Mineralogie und Paläontologie Rheinische Friedrich-Wilhelms-Universität Bonn Nussallee 8, 53115 Bonn, Germany Editorial staff Rico Schellhorn & Julia A. Schultz Redaktion Steinmann-Institut für Geologie, Mineralogie und Paläontologie Rheinische Friedrich-Wilhelms-Universität Bonn Nussallee 8, 53115 Bonn, Germany Printed by www.viaprinto.de Druck Copyright and responsibility for the scientific content of the contributions lie with the authors. Copyright und Verantwortung für den wissenschaftlichen Inhalt der Beiträge liegen bei den Autoren. ISSN 0946-8978 GeoUnion Alfred-Wegener-Stiftung – Potsdam, Juni 2018 MTE13 13th Symposium on Mesozoic Terrestrial Ecosystems and Biota Rheinische Friedrich-Wilhelms-Universität Bonn,
    [Show full text]