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Assembly, Configuration, and Break-Up History of Rodinia
Author's personal copy Available online at www.sciencedirect.com Precambrian Research 160 (2008) 179–210 Assembly, configuration, and break-up history of Rodinia: A synthesis Z.X. Li a,g,∗, S.V. Bogdanova b, A.S. Collins c, A. Davidson d, B. De Waele a, R.E. Ernst e,f, I.C.W. Fitzsimons g, R.A. Fuck h, D.P. Gladkochub i, J. Jacobs j, K.E. Karlstrom k, S. Lu l, L.M. Natapov m, V. Pease n, S.A. Pisarevsky a, K. Thrane o, V. Vernikovsky p a Tectonics Special Research Centre, School of Earth and Geographical Sciences, The University of Western Australia, Crawley, WA 6009, Australia b Department of Geology, Lund University, Solvegatan 12, 223 62 Lund, Sweden c Continental Evolution Research Group, School of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia d Geological Survey of Canada (retired), 601 Booth Street, Ottawa, Canada K1A 0E8 e Ernst Geosciences, 43 Margrave Avenue, Ottawa, Canada K1T 3Y2 f Department of Earth Sciences, Carleton U., Ottawa, Canada K1S 5B6 g Tectonics Special Research Centre, Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia h Universidade de Bras´ılia, 70910-000 Bras´ılia, Brazil i Institute of the Earth’s Crust SB RAS, Lermontova Street, 128, 664033 Irkutsk, Russia j Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway k Department of Earth and Planetary Sciences, Northrop Hall University of New Mexico, Albuquerque, NM 87131, USA l Tianjin Institute of Geology and Mineral Resources, CGS, No. -
Mesozoic Central Atlantic and Ligurian Tethys1
42. RIFTING AND EARLY DRIFTING: MESOZOIC CENTRAL ATLANTIC AND LIGURIAN TETHYS1 Marcel Lemoine, Institut Dolomieu, 38031 Grenoble Cedex, France ABSTRACT The Leg 76 discovery of Callovian sediments lying above the oldest Atlantic oceanic crust allows us to more closely compare the Central Atlantic with the Mesozoic Ligurian Tethys. As a matter of fact, during the Late Jurassic and Ear- ly Cretaceous, both the young Central Atlantic Ocean and the Ligurian Tethys were segments of the Mesozoic Tethys Ocean lying between Laurasia and Gondwana and linked by the Gibraltar-Maghreb-Sicilia transform zone. If we as- sume that the Apulian-Adriatic continental bloc (or Adria) was then a northern promontory of Africa, then the predrift and early drift evolutions of both these oceanic segments must have been roughly the same: their kinematic evolution was governed by the east-west left-lateral motion of Gondwana (including Africa and Adria) relative to Laurasia (in- cluding North America, Iberia, and Europe), at least before the middle Cretaceous (=100 Ma). By the middle Cretaceous, opening of the North Atlantic Ocean led to a drastic change of the relative motions between Africa-Adria and Europe-Iberia. From this time on, closure of the Ligurian segment of the Tethys began, whereas the Central Atlan- tic went on spreading. In fact, field data from the Alps, Corsica, and the Apennines show evidence of a Triassic-Jurassic-Early Cretaceous paleotectonic evolution rather comparable with that of the Central Atlantic. Rifting may have been started during the Triassic (at least the late Triassic) but reached its climax in the Liassic. -
Helicobacter Pylori's Historical Journey Through Siberia and the Americas
Helicobacter pylori’s historical journey through Siberia and the Americas Yoshan Moodleya,1,2, Andrea Brunellib,1, Silvia Ghirottoc,1, Andrey Klyubind, Ayas S. Maadye, William Tynef, Zilia Y. Muñoz-Ramirezg, Zhemin Zhouf, Andrea Manicah, Bodo Linzi, and Mark Achtmanf aDepartment of Zoology, University of Venda, Thohoyandou 0950, Republic of South Africa; bDepartment of Life Sciences and Biotechnology, University of Ferrara, 44121 Ferrara, Italy; cDepartment of Mathematics and Computer Science, University of Ferrara, 44121 Ferrara, Italy; dDepartment of Molecular Biology and Genetics, Research Institute for Physical-Chemical Medicine, 119435 Moscow, Russia; eDepartment of Diagnostic and Operative Endoscopy, Pirogov National Medical and Surgical Center, 105203 Moscow, Russia; fWarwick Medical School, University of Warwick, Coventry CV4 7AL, United Kingdom; gLaboratorio de Bioinformática y Biotecnología Genómica, Escuela Nacional de Ciencias Biológicas, Unidad Profesional Lázaro Cárdenas, Instituto Politécnico Nacional, 11340 Mexico City, Mexico; hDepartment of Zoology, University of Cambridge, Cambridge CB2 3EJ, United Kingdom; and iDepartment of Biology, Division of Microbiology, Friedrich Alexander University Erlangen-Nuremberg, 91058 Erlangen, Germany Edited by Daniel Falush, University of Bath, Bath, United Kingdom, and accepted by Editorial Board Member W. F. Doolittle April 30, 2021 (received for review July 22, 2020) The gastric bacterium Helicobacter pylori shares a coevolutionary speakers). However, H. pylori’s presence, diversity, and structure history with humans that predates the out-of-Africa diaspora, and in northern Eurasia are still unknown. This vast region, hereafter the geographical specificities of H. pylori populations reflect mul- Siberia, extends from the Ural Mountains in the west to the tiple well-known human migrations. We extensively sampled H. -
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R. J. PANKHURST (CHIEF EDITOR) P. DOYLE E J. GREGORY J. S. GRIFFITHS A. J. HARTLEY R. E. HOLDSWORTH A. C. MORTON N. S. ROBINS M. S. STOKER J. P. TURNER Special Publication reviewing procedures The Society makes every effort to ensure that the scientific and production quality of its books matches that of its journals. Since 1997, all book proposals have been refereed by specialist reviewers as well as by the Society's Books Editorial Committee. If the referees identify weaknesses in the proposal, these must be addressed before the proposal is accepted. Once the book is accepted, the Society has a team of Book Editors (listed above) who ensure that the volume editors follow strict guidelines on refereeing and quality control. We insist that individual papers can only be accepted after satis- factory review by two independent referees. The questions on the review forms are similar to those for Journal of the Geological Society. The referees' forms and comments must be available to the Society's Book Editors on request. Although many of the books result from meetings, the editors are expected to commission papers that were not pre- sented at the meeting to ensure that the book provides a balanced coverage of the subject. Being accepted for presentation at the meeting does not guarantee inclusion in the book. Geological Society Special Publications are included in the ISI Science Citation Index, but they do not have an impact factor, the latter being applicable only to journals. -
Balkatach Hypothesis: a New Model for the Evolution of the Pacific, Tethyan, and Paleo-Asian Oceanic Domains
Research Paper GEOSPHERE Balkatach hypothesis: A new model for the evolution of the Pacific, Tethyan, and Paleo-Asian oceanic domains 1,2 2 GEOSPHERE, v. 13, no. 5 Andrew V. Zuza and An Yin 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, California 90095-1567, USA doi:10.1130/GES01463.1 18 figures; 2 tables; 1 supplemental file ABSTRACT suturing. (5) The closure of the Paleo-Asian Ocean in the early Permian was accompanied by a widespread magmatic flare up, which may have been CORRESPONDENCE: avz5818@gmail .com; The Phanerozoic history of the Paleo-Asian, Tethyan, and Pacific oceanic related to the avalanche of the subducted oceanic slabs of the Paleo-Asian azuza@unr .edu domains is important for unraveling the tectonic evolution of the Eurasian Ocean across the 660 km phase boundary in the mantle. (6) The closure of the and Laurentian continents. The validity of existing models that account for Paleo-Tethys against the southern margin of Balkatach proceeded diachro- CITATION: Zuza, A.V., and Yin, A., 2017, Balkatach hypothesis: A new model for the evolution of the the development and closure of the Paleo-Asian and Tethyan Oceans criti- nously, from west to east, in the Triassic–Jurassic. Pacific, Tethyan, and Paleo-Asian oceanic domains: cally depends on the assumed initial configuration and relative positions of Geosphere, v. 13, no. 5, p. 1664–1712, doi:10.1130 the Precambrian cratons that separate the two oceanic domains, including /GES01463.1. the North China, Tarim, Karakum, Turan, and southern Baltica cratons. -
African Families in a Global Context
RR13X.book Page 1 Monday, November 14, 2005 2:20 PM RESEARCH REPORT NO. 131 AFRICAN FAMILIES IN A GLOBAL CONTEXT Edited by Göran Therborn Nordiska Afrikainstitutet, Uppsala 2006 RR13X.book Page 2 Monday, November 14, 2005 2:20 PM Indexing terms Demographic change Family Family structure Gender roles Social problems Africa Ghana Nigeria South Africa African Families in a Global Context Second edition © the authors and Nordiska Afrikainstitutet, 2004 Language checking: Elaine Almén ISSN 1104-8425 ISBN 91-7106-561-X (print) 91-7106-562-8 (electronic) Printed in Sweden by Elanders Infologistics Väst AB, Göteborg 2006 RR13X.book Page 3 Monday, November 14, 2005 2:20 PM Contents Preface . 5 Author presentations . 7 Introduction Globalization, Africa, and African Family Pattern . 9 Göran Therborn 1. African Families in a Global Context. 17 Göran Therborn 2. Demographic Innovation and Nutritional Catastrophe: Change, Lack of Change and Difference in Ghanaian Family Systems . 49 Christine Oppong 3. Female (In)dependence and Male Dominance in Contemporary Nigerian Families . 79 Bola Udegbe 4. Globalization and Family Patterns: A View from South Africa . 98 Susan C. Ziehl RR13X.book Page 4 Monday, November 14, 2005 2:20 PM RR13X.book Page 5 Monday, November 14, 2005 2:20 PM Preface In the mid-1990s the Swedish Council for Planning and Coordination of Research (Forskningsrådsnämnden – FRN) – subsequently merged into the Council of Sci- ence (Vetenskaprådet) – established a national, interdisciplinary research committee on Global Processes. The Committee has been strongly committed to a multidi- mensional and multidisciplinary approach to globalization and global processes and to using regional perspectives. -
The Geologic Time Scale Is the Eon
Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2. -
1219421 the Opening of Neo-Tethys and the Formation of the Khuff Passive Margin
1219421 The Opening of Neo-Tethys and the Formation of the Khuff Passive Margin 1219421 The Opening of Neo-Tethys and the Formation of the Khuff Passive Margin *1 2 Bell, Andrew ; Spaak, Pieter (1) Shell Global Solutions International BV, Rijswijk, Netherlands. (2) Shell International Exporation and Production BV, The Hague, Netherlands. Any investigation of regional geology and palaeomagnetism in the Middle East will show that in the Permian, a series of terranes separated from Gondwana and drifted north, opening the Neo-Tethys Ocean in their wake. To the north of these terranes, the Palaeo-Tethys Ocean closed and was largely subducted. Eventually in a non-synchronous movement but largely in late Triassic and early Jurassic times, these terranes docked with the northern margin of the former Palaeo- Tethys during the Cimmerian Orogeny. The opening of the Neo-Tethys in Arabia does not follow the classic pattern of continental break-up resulting in oceanic crust. Classically we should expect thermal up-doming, followed by the onset of syn-rift deposition, frequently but not always associated with volcanism. The formation of en-echelon systems of rotated fault blocks are also characteristic, followed by a break-up unconformity and the formation of the first oceanic crust. What we see in Arabia as a consequence of the opening of Neo-Tethys exhibits few of these features. Distinguishing thermal up-doming from the uplift associated with the ‘Hercynian’ event in Arabia, coupled with the glacial sculpting of the Permo-Carboniferous Unayzah Formation is fraught with difficulty. Although locally volcanics of Permian age are known from Oman, they are absent over most of Arabia. -
Map of How Earth Would Have Looked If Supercontinent Gondwana Had Broken up Differently
Map of How Earth Would Have Looked if Supercontinent Gondwana Had Broken Up Differently UK EDITION FRIDAY, 14TH MARCH, 2014 News Business Economy Technology Sport Entertainment & Arts Viewpoint Video Science Map of How Earth Would Have IBTIMES TV Looked if Supercontinent Gondwana Had Broken Up Differently By Hannah Osborne March 3, 2014 10:23 GMT + Recreation of Banksy Marks 3 Years of Syrian Crisis How Earth would have looked if rift had split continent differently. Sascha Brune/Christian Heine http://www.ibtimes.co.uk/map-how-earth-would-have-looked-if-supercontinent-gondwana-had-broken-differently-1438639[14/03/2014 12:00:17 pm] Map of How Earth Would Have Looked if Supercontinent Gondwana Had Broken Up Differently A map showing what Earth would have looked like had the supercontinent Gondwana broken up differently has been created by researchers. The map looks at how the world would be completely different if the South Atlantic and West African rift had split, instead of the rift that emerged along the Equatorial Atlantic margins. Geoscientists at the University of Sydney and the GFZ German Research Centre for Geosciences used sophisticated plate tectonic and 2D numerical modelling to create the map. The Gondwana supercontinent broke up 130 million years ago leading to the creation of South America and Africa. However, for millions of years before this, the southern continents of Why advertise with us South America, Africa, Antarctica, Australia, and India were united as Gondwana. READ MORE It is still unclear why Gondwana fragmented, but it is understood if first split along the East Africa coast in a western and eastern part, before South America separated. -
Locating South China in Rodinia and Gondwana: a Fragment of Greater India Lithosphere?
Locating South China in Rodinia and Gondwana: A fragment of greater India lithosphere? Peter A. Cawood1, 2, Yuejun Wang3, Yajun Xu4, and Guochun Zhao5 1Department of Earth Sciences, University of St Andrews, North Street, St Andrews KY16 9AL, UK 2Centre for Exploration Targeting, School of Earth and Environment, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia 3State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China 4State Key Laboratory of Biogeology and Environmental Geology, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China 5Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong, China ABSTRACT metamorphosed Neoproterozoic strata and From the formation of Rodinia at the end of the Mesoproterozoic to the commencement unmetamorphosed Sinian cover (Fig. 1; Zhao of Pangea breakup at the end of the Paleozoic, the South China craton fi rst formed and then and Cawood, 2012). The Cathaysia block is com- occupied a position adjacent to Western Australia and northern India. Early Neoproterozoic posed predominantly of Neoproterozoic meta- suprasubduction zone magmatic arc-backarc assemblages in the craton range in age from ca. morphic rocks, with minor Paleoproterozoic and 1000 Ma to 820 Ma and display a sequential northwest decrease in age. These relations sug- Mesoproterozoic lithologies. Archean basement gest formation and closure of arc systems through southeast-directed subduction, resulting is poorly exposed and largely inferred from the in progressive northwestward accretion onto the periphery of an already assembled Rodinia. presence of minor inherited and/or xenocrys- Siliciclastic units within an early Paleozoic succession that transgresses across the craton were tic zircons in younger rocks (Fig. -
Paleozoic 3: Alabama in the Paleozoic
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Paleozoic 3: Alabama in the Paleozoic Instructor: Dr. Douglas W. Haywick Last Time The Paleozoic Part 2 1) Back to Newfoundland 2) Eastern Laurentian Orogenies (Appalachians) 3) Other Laurentian Orogenies (Antler, Ouachita) (web notes 25) Laurentia (Paleozoic North America) Even though this coastline of Laurentia was a passive continental margin, a plate tectonic boundary was rapidly approaching… A B A B Laurentia (Paleozoic North America) The resulting Taconic Orogeny first depressed the seafloor Laurentia (localized transgression) and A Island arc then pushed previously deposited passive continental B margin sediments up into thrust fault mountains. Baltica There was only minimal metamorphism and igneous A intrusions. B Middle Ordovician Laurentia (Paleozoic North America) Laurentia Baltica Middle Ordovician Laurentia (Paleozoic North America) Laurentia Baltica Middle Ordovician Laurentia (Paleozoic North America) The next tectonic event (the Acadian Orogeny) was caused Laurentia by the approach of Baltica A B Baltica A B Baltica Baltica Late Ordovician Laurentia (Paleozoic North America) The Acadian Orogeny was more extensive and more intense (metamorphism and A lots of igneous intrusions) B A B Early Devonian Laurentia (Paleozoic North America) The Acadian Orogeny was more extensive and more intense (metamorphism and lots of igneous intrusions) Early Devonian Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. A B B A B Mississippian Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. A B B A B Pennsylvannian Suture zone Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. -
Destruction of the North China Craton
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/257684968 Destruction of the North China Craton Article in Science China Earth Science · October 2012 Impact Factor: 1.49 · DOI: 10.1007/s11430-012-4516-y CITATIONS READS 69 65 6 authors, including: Rixiang Zhu Yi-Gang Xu Chinese Academy of Sciences Chinese Academy of Sciences 264 PUBLICATIONS 8,148 CITATIONS 209 PUBLICATIONS 7,351 CITATIONS SEE PROFILE SEE PROFILE Tianyu Zheng Chinese Academy of Sciences 62 PUBLICATIONS 1,589 CITATIONS SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: Yi-Gang Xu letting you access and read them immediately. Retrieved on: 26 May 2016 SCIENCE CHINA Earth Sciences Progress of Projects Supported by NSFC October 2012 Vol.55 No.10: 1565–1587 • REVIEW • doi: 10.1007/s11430-012-4516-y Destruction of the North China Craton ZHU RiXiang1*, XU YiGang2, ZHU Guang3, ZHANG HongFu1, XIA QunKe4 & ZHENG TianYu1 1 State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2 State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 3 School of Resource and Environmental Engineering, Hefei University of Technology, Hefei 230009, China; 4 School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China Received March 27, 2012; accepted June 18, 2012 A National Science Foundation of China (NSFC) major research project, Destruction of the North China Craton (NCC), has been carried out in the past few years by Chinese scientists through an in-depth and systematic observations, experiments and theoretical analyses, with an emphasis on the spatio-temporal distribution of the NCC destruction, the structure of deep earth and shallow geological records of the craton evolution, the mechanism and dynamics of the craton destruction.