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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. -
Pathways and Mechanisms of Late Ordovician (Katian) Faunal Migrations of Laurentia and Baltica
Estonian Journal of Earth Sciences, 2015, 64, 1, 62–67 doi: 10.3176/earth.2015.11 Pathways and mechanisms of Late Ordovician (Katian) faunal migrations of Laurentia and Baltica Adriane R. Lama and Alycia L. Stigalla,b a Department of Geological Sciences, Ohio University, Athens 45701-2979, Ohio, U.S.A. b OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Laboratories, Athens 45701-2979, Ohio, U.S.A.; [email protected], [email protected] Received 2 July 2014, accepted 9 October 2014 Abstract. Late Ordovician strata within the Cincinnati Basin record a mass faunal migration event during the C4 and C5 depositional sequences. The geographic source region for the invaders and the paleoceanographic conditions that facilitated dispersal into the Cincinnati Basin has previously been poorly understood. Using Parsimony Analysis of Endemicity, biogeographic relationships among Laurentian and Baltic basins were analyzed for each of the C1–C5 depositional sequences to identify dispersal paths. The results support multiple dispersal pathways, including three separate dispersal events between Baltica and Laurentia. Within Laurentia, results support dispersal pathways between areas north of the Transcontinental Arch into the western Midcontinent, between the Upper Mississippi Valley into the Cincinnati Basin, and between the peri-cratonic Scoto-Appalachian Basin and the Cincinnati Basin. These results support the hypothesis that invasive taxa entered the Cincinnati Basin via multiple dispersal pathways and that the equatorial Iapetus current facilitated dispersal of organisms from Baltica to Laurentia. Within Laurentia, surface currents and large storms moving from northeast to southwest likely influenced the dispersal of organisms. Larval states were characterized for the Richmondian invaders, and most invaders were found to have had planktotrophic planktic larvae. -
Assembling Laurentia—Integrated Theme Sessions on Tectonic Turning Points
Assembling Laurentia—Integrated Theme Sessions on Tectonic Turning Points Michael L. Williams, Dept. of Geosciences, University of Massachusetts, Amherst, Massachusetts 01003, USA, [email protected]; Dawn A. Kellett, Geological Survey of Canada–Atlantic Division, Natural Resources Canada/Government of Canada, 1 Challenger Drive, Dartmouth, Nova Scotia B2Y 4A2, Canada, [email protected]; Basil Tikoff*, Dept. of Geoscience, University of Wisconsin– Madison, 1215 W. Dayton Street, Madison, Wisconsin 53706, USA, [email protected]; Steven J. Whitmeyer, Dept. of Geology and Environmental Science, James Madison University, 801 Carrier Drive, MSC 6903, Harrisonburg, Virginia 22807, USA, [email protected] The North American continent records the headlined by a Pardee Symposium, which and the broader implications of, these changes, evolution of tectonic processes and tectonic will provide an overview of the tectonic evo- and to widen the scope of investigation environments from the earliest Archean to lution of Laurentia and an introduction to the beyond a particular boundary or regional geo- modern times. The continent hosts a rich concept of key “Turning Points.” Seven logical event to the scale of Laurentia itself. Archean (and possibly Hadean) record, at related topical sessions, under the general The time slices for the topical sessions are as least three great Proterozoic orogenic belts, heading “Assembling Laurentia,” will span follows (with brief explanations from each and a wide range of Phanerozoic tectonic, the GSA meeting. -
The East Asian Jigsaw Puzzle Pangaea at Risk? from Neville Haile
192 Nature Vol. 293 17 September 1981 ment with the known seismic refraction (Business and Technological Systems, Inc.) pretation of long-wavelength crustal fields and heat flow data. His group believes that magnetization model for the United States, in terms of a geological/geophysical the region is the site of a late Precambrian derived from Magsat scalar data, had much model, promises to contribute significantly rift which was reactivated in the Mesozoic better resolution than that using POGO to our understanding of the Earth's crust. to form an aulacogen and its model data. In the older disciplines of main-field involves thinning of the upper crust and an Although preliminary, the results dis modelling and studies of external fields, increase in density in the lower crust. The cussed at the meeting indicate that sep there are significant new developments in magnetic low is accounted for by either an aration of the measured field into its core, both analytical techniques and in our isotherm upwarp or, less likely, a litho crustal and external 'components' is being understanding of the physics of the field logical variation in the crust. Mayhew's achieved. The newest discipline, inter- sources. 0 The East Asian jigsaw puzzle Pangaea at risk? from Neville Haile UNTIL fairly recently, reconstructions of the world palaeogeography followed Wegener in showing Eurasia, excluding the Indian subcontinent, as a single block, with the Malay Peninsula and part or all of the Indonesian Archipelago depending from it and looking rather vulnerablel ,2. Other world palaeogeo graphical maps simply omit South-east Asia and most of China (see the figure)3,4. -
ORDOVICIAN FISH from the ARABIAN PENINSULA by IVAN J
[Palaeontology, Vol. 52, Part 2, 2009, pp. 337–342] ORDOVICIAN FISH FROM THE ARABIAN PENINSULA by IVAN J. SANSOM*, C. GILES MILLER , ALAN HEWARDà,–, NEIL S. DAVIES*,**, GRAHAM A. BOOTHà, RICHARD A. FORTEY and FLORENTIN PARIS§ *Earth Sciences, University of Birmingham, Birmingham B15 2TT, UK; e-mail: [email protected] Department of Palaeontology, The Natural History Museum, London SW7 5BD, UK; e-mails: [email protected] and [email protected] àPetroleum Development Oman, Muscat, Oman; e-mail: [email protected] §Ge´osciences, Universite´ de Rennes, 35042 Rennes, France; e-mail: fl[email protected] –Present address: Petrogas E&P, Muscat, Oman; e-mail: [email protected] **Present address: Earth Sciences, Dalhousie University, Halifax, Nova Scotia B3H 3J5, Canada; e-mail: [email protected] Typescript received 25 February 2008; accepted in revised form 19 May 2008 Abstract: Over the past three decades Ordovician pteras- morphs from the Arabian margin of Gondwana. These are pidomorphs (armoured jawless fish) have been recorded among the oldest arandaspids known, and greatly extend from the fringes of the Gondwana palaeocontinent, in par- the palaeogeographical distribution of the clade around the ticular Australia and South America. These occurrences are periGondwanan margin. Their occurrence within a very dominated by arandaspid agnathans, the oldest known narrow, nearshore ecological niche suggests that similar group of vertebrates with extensive biomineralisation of Middle Ordovician palaeoenvironmental settings should be the dermoskeleton. Here we describe specimens of arandas- targeted for further sampling. pid agnathans, referable to the genus Sacabambaspis Gagnier, Blieck and Rodrigo, from the Ordovician of Key words: Ordovician, pteraspidomorphs, Gondwana pal- Oman, which represent the earliest record of pteraspido- aeocontinent, Sacabambaspis, Oman. -
The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A. -
Geology in 2000 and Beyond by John C
THE EPOCH No. 32 Spring 1998 - January 2000 A Newsletter for Alumni and Students Department of Geology Website: http://www.geology.buffalo.edu The State University of New York at Buffalo E-mail: [email protected] 876 Natural Sciences Complex Telephone: (716) 645-6800, Ext. 6100 Buffalo, New York 14260-3050 Fax: (716) 645-3999 HIGHLIGHTS Geology in 2000 and Beyond By John C. Fountain, Professor & Chairman Departmental News The Fall of 1999 marked a major turning point for the Geology A Review of the Department, not because that is when I began my term as department chair but because, for the first time in five years, the department is fully staffed Last Decade . 2 again – and thus for the first time ever, our programmatic model begun under Field Camp Truck Mike Sheridan can fully be implemented. Replacement Fund . 3 When the department expanded after the formation of the SUNY system, there was one faculty member in each major area (mineralogy, petrology, Meet the NEW Faculty .. 4 structure etc.). The advantages of this model include excellent undergraduate education and a broad range of research interests. The disadvantage of this Duttweiler Geological approach is that each faculty member worked essentially alone, which is a Field Station . 7 significant disadvantage in competing for sponsored research funds. When Mike Sheridan was selected to replace Chet Langway as Chair in 1990, he began a reorganization of the department into concentrated Research News research programs. This resulted in the formation of two major programs: Paoha Island environmental geology and volcanology. While not all of our research falls How did it emerge? . -
WGBH/NOVA #4220 Making North America: Origins KIRK JOHNSON
WGBH/NOVA #4220 Making North America: Origins KIRK JOHNSON (Sant Director, Smithsonian National Museum of Natural History): North America, the land that we love: it looks pretty familiar, don’t you think? Well, think again! The ground that we walk on is full of surprises, if you know where to look. 00:25 As a geologist, the Grand Canyon is perhaps the best place in the world. Every single one of these layers tells its own story about what North America was like when that layer was deposited. So, are you ready for a little time-travelling? 00:38 I’m Kirk Johnson, the director of the Smithsonian National Museum of Natural History, and I’m taking off on the fieldtrip of a lifetime,… 00:50 Look at that rock there. That is crazy! …to find out, “How did our amazing continent get to be the way it is?” EMILY WOLIN (Geophysicist): Underneath Lake Superior, that’s about 30 miles of volcanic rock. KIRK JOHNSON: Thirty miles of volcanic rock? How did the landscape shape the creatures that lived and died here? Fourteen-foot-long fish, in Kansas. That’s what I’m telling you! 01:14 And how did we turn the rocks of our homeland… Ho-ho. Oh, man! …into riches? This thing is phenomenal. In this episode, we hunt down the clues to our continent’s epic past. 01:26 You can see new land being formed, right in front of your eyes. Why does this golf course hold the secret to the rise and fall of the Rockies? What forces nearly cracked North America in half? And is it possible that the New York City skyline… I’ve always wanted to do this. -
Justin V. Strauss Department of Earth Sciences Dartmouth College HB6105 Fairchild Hall Hanover, NH 03755 (603) 646–6954 [email protected]
Justin V. Strauss Department of Earth Sciences Dartmouth College HB6105 Fairchild Hall Hanover, NH 03755 (603) 646–6954 [email protected] Education Harvard University, Cambridge, MA PhD, Department of Earth and Planetary Sciences May 2015 MA, Department of Earth and Planetary Sciences May 2014 The Colorado College, Colorado Springs, CO BA, Department of Geology Aug. 2006 Teaching and Work Experience Dartmouth College, Department of Earth Sciences, Hanover, NH Assistant Professor Jan. 2016–present Stanford University, Department of Geological Sciences, Stanford, CA Agouron Institute Geobiology Postdoctoral Scholar July 2015 - Dec. 2015 Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA Field Assistant – Dr. Francis Macdonald July 2009 - Aug. 2009 Field Assistant – Dr. Francis Macdonald May 2008 Princeton University, Department of Geosciences, Princeton, NJ Lab Technician – Dr. Adam Maloof Aug. 2007 - Dec. 2007 Field Assistant – Dr. Adam Maloof June 2007 - Aug. 2007 The Colorado College, Department of Geology, Colorado Springs, CO Paraprofessional Sept. 2006 - June 2007 Honors and Awards 2018 National Geographic Explorer 2018 American Chemical Society Doctoral New Investigator Award 2015 Agouron Institute Geobiology Postdoctoral Fellowship 2015 Geological Society of America Student Research Grant 2014 Geological Society of America Student Research Grant 2013 Star Family Prize for Excellence in Undergraduate Advising Nominee – Harvard University 2013 Bok Center Distinction in Teaching Award – Harvard University 2012 Bok Center Distinction in Teaching Award – Harvard University 2012 GACMAC 2012 Jerome Remick III Poster Award 2012 National Science Foundation Graduate Research Fellowship Recipient 2011 National Science Foundation GRFP Honorable Mention 2006 William A. Fischer Special Recognition Geosciences Award 2005 Patricia J. Buster Scholarship for Undergraduate Research 2004 Patricia J. -
Buenellus Chilhoweensis N. Sp. from the Murray Shale (Lower Cambrian Chilhowee Group) of Tennessee, the Oldest Known Trilobite from the Iapetan Margin of Laurentia
Journal of Paleontology, 92(3), 2018, p. 442–458 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/18/0088-0906 doi: 10.1017/jpa.2017.155 Buenellus chilhoweensis n. sp. from the Murray Shale (lower Cambrian Chilhowee Group) of Tennessee, the oldest known trilobite from the Iapetan margin of Laurentia Mark Webster,1 and Steven J. Hageman2 1Department of the Geophysical Sciences, University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637 〈[email protected]〉 2Department of Geology, Appalachian State University, Boone, North Carolina 28608, USA 〈[email protected]〉 Abstract.—The Ediacaran to lower Cambrian Chilhowee Group of the southern and central Appalachians records the rift-to-drift transition of the newly formed Iapetan margin of Laurentia. Body fossils are rare within the Chilhowee Group, and correlations are based almost exclusively on lithological similarities. A critical review of previous work highlights the relatively weak biostratigraphic and radiometric age constraints on the various units within the succession. Herein, we document a newly discovered fossil-bearing locality within the Murray Shale (upper Chilhowee Group) on Chilhowee Mountain, eastern Tennessee, and formally describe a nevadioid trilobite, Buenellus chilhoweensis n. sp., from that site. This trilobite indicates that the Murray Shale is of Montezuman age (provisional Cambrian Stage 3), which is older than the Dyeran (provisional late Stage 3 to early Stage 4) age suggested by the historical (mis)identification of “Olenellus sp.” from within the unit as reported by workers more than a century ago. -
(India) and Yangtze Block (South China): Paleogeographic Implications
Neoproterozoic stratigraphic comparison of the Lesser Himalaya (India) and Yangtze block (south China): Paleogeographic implications Ganqing Jiang* Department of Earth Sciences, University of California, Riverside, California 92521, USA Linda E. Sohl Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory of Nicholas Christie-Blick Columbia University, Palisades, New York 10964-8000, USA ABSTRACT terpreted to correspond with a level within the Recent studies of terminal Neoproterozoic rocks (ca. 590±543 Ma) in the Lesser Him- glaciogenic interval (Fig. 2). A passive- alaya of northwestern India and the Yangtze block (south China) reveal remarkably sim- margin setting is inferred with con®dence for ilar facies assemblages and carbonate platform architecture, with distinctive karstic un- postglacial carbonate rocks on the basis of conformities at comparable stratigraphic levels. These similarities suggest that south platform scale, comparatively simple physical China may have been located close to northwestern India during late Neoproterozoic time, stratigraphic and facies architecture, and the an interpretation permitted by the available, yet sparse paleomagnetic data. Additional thickness of successions, with no evidence for parallels in older rocks of both blocksÐsimilar rift-related siliciclastic-volcanic successions either syndepositional tectonism or igneous overlying metamorphic basement, and comparable glaciogenic intervals of possibly Stur- activity. Figure 2 summarizes pertinent litho- tian and Marinoan -
North China Craton: the Conjugate Margin for Northwestern Laurentia in Rodinia Jikai Ding1,2, Shihong Zhang1,3*, David A.D
https://doi.org/10.1130/G48483.1 Manuscript received 7 October 2020 Revised manuscript received 27 December 2020 Manuscript accepted 12 January 2021 © 2021 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 22 March 2021 North China craton: The conjugate margin for northwestern Laurentia in Rodinia Jikai Ding1,2, Shihong Zhang1,3*, David A.D. Evans2, Tianshui Yang1, Haiyan Li1, Huaichun Wu1 and Jianping Chen3 1 State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China 2 Department of Earth and Planetary Sciences, Yale University, New Haven, Connecticut 06520, USA 3 School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China ABSTRACT ern NCC and northwestern Laurentia (present In the Rodinia supercontinent, Laurentia is placed at the center because it was flanked coordinates) was proposed (Fu et al., 2015; by late Neoproterozoic rifted margins; however, the conjugate margin for western Laurentia Zhao et al., 2020) but required rigorous testing is still enigmatic. In this study, new paleomagnetic results have been obtained from 15 ca. by coeval pairs of high-quality poles with pre- 775 Ma mafic dikes in eastern Hebei Province, North China craton (NCC). Stepwise thermal cise age constraints. In this study, we report a demagnetization revealed a high-temperature component, directed northeast or southwest new high-quality paleomagnetic pole obtained with shallow inclinations, with unblocking temperatures of as high as 580 °C. Rock magne- from ca. 775 Ma mafic dikes in the eastern He- tism suggests the component is carried by single-domain and pseudo-single-domain magnetite bei Province, NCC.