100 Million Years of Antarctic Climate Evolution: Evidence from Fossil Plants 19 J

Total Page:16

File Type:pdf, Size:1020Kb

100 Million Years of Antarctic Climate Evolution: Evidence from Fossil Plants 19 J Antarctica: A Keystone in a Changing World Proceedings of the 10th International Symposium on Antarctic Earth Sciences, Santa Barbara, California, August 26 to September 1, 2007, Alan K. Cooper, Peter Barrett, Howard Stagg, Bryan Storey, Edmund Stump, Woody Wise, and the 10th ISAES editorial team, Polar Research Board, National Research Council, U.S. Geological Survey ISBN: 0-309-11855-7, 164 pages, 8 1/2 x 11, (2008) This free PDF was downloaded from: http://www.nap.edu/catalog/12168.html Visit the National Academies Press online, the authoritative source for all books from the National Academy of Sciences, the National Academy of Engineering, the Institute of Medicine, and the National Research Council: • Download hundreds of free books in PDF • Read thousands of books online, free • Sign up to be notified when new books are published • Purchase printed books • Purchase PDFs • Explore with our innovative research tools Thank you for downloading this free PDF. If you have comments, questions or just want more information about the books published by the National Academies Press, you may contact our customer service department toll-free at 888-624-8373, visit us online, or send an email to [email protected]. This free book plus thousands more books are available at http://www.nap.edu. Copyright © National Academy of Sciences. Permission is granted for this material to be shared for noncommercial, educational purposes, provided that this notice appears on the reproduced materials, the Web address of the online, full authoritative version is retained, and copies are not altered. To disseminate otherwise or to republish requires written permission from the National Academies Press. Antarctica: A Keystone in a Changing World http://www.nap.edu/catalog/12168.html Proceedings of the 10th International Symposium on Antarctic Earth Sciences Santa Barbara, California August 26 to September 1, 2007 Editors: Alan K. Cooper, Peter Barrett, Howard Stagg, Bryan Storey, Edmund Stump, Woody Wise, and the 10th ISAES editorial team *John Anderson Dieter Futterer Timothy Naish John Barron John Gamble Sandra Passchier Philip Bart John Goodge Stephen Pekar Donald Blankenship William Hammer Carol Raymond Frederick Davey Patricia Helton Carlo Alberto Ricci Michael Diggles Erik Ivins Michael Studinger Carol Finn Philip Kyle David Sugden Paul Fitzgerald Wesley LeMasurier Vanessa Thorn Fabio Florindo Paul Mayewski Terry Wilson Jane Francis This special International Polar Year volume is a joint effort of the Polar Research Board of the National Academies and the U.S. Geological Survey. The Polar Research Board is the U.S. National Committee to the Scientific Committee on Antarctic Research, which is the official sponsor of the 10th ISAES. Publication of printed papers is by the National Academies Press and publication of electronic media is by the U.S. Geological Survey. Copyright © National Academy of Sciences. All rights reserved. Antarctica: A Keystone in a Changing World http://www.nap.edu/catalog/12168.html THE NATIONAL ACADEMIES PRESS 500 FIFTH STREET, N.W. WASHINGTON, DC 20001 Note: This publication was overseen by two members of the Polar Research Board (PRB) who served as members of the 10th ISAES local organizing committee: Robin Bell, chair- person of the 10th ISAES Local Organizing Committee and Mahon C. Kennicutt II, U.S. delegate to the Scientific Committee on Antarctic Research (SCAR) and a vice president of SCAR. Funding support for this collaborative project was provided by the U.S. National Science Foundation’s Office of Polar Programs, the U.S. Geological Survey and SCAR. This book is a companion to the Online Proceedings of the 10th ISAES hosted by the USGS at http://pubs.usgs.gov/of/2007/1047/. International Standard Book Number-13: 978-0-309-11854-5 International Standard Book Number-10: 0-309-11854-9 Additional copies of this book are available from the National Academies Press, 500 Fifth Street, N.W., Washington, DC 20055; (800) 624-6242 or (202) 334-3313 (in the Washington metropolitan area); Internet, http://www.nap.edu. Copyright 2008 by the National Academy of Sciences. All rights reserved. Printed in the United States of America Front cover: Depicting change from greenhouse to icehouse times in Antarctica. Upper: Snowstorm on Seymour Island, Antarctic Peninsula. Image provided by Jane Francis. Lower: Middle Cretaceous forest on Antarctica; painting by Robert Nicholls, with per- mission for use by the artist and by the British Antarctic Survey who commissioned the painting and have it on display there. Back cover: Upper: Estimates skin-depth temperatures derived from the thermal IR channel of historical AVHRR data. Image is from NASA website: http://svs.gsfc.nasa. gov/vis/a000000/a003100/a003188/index.html. Lower: Predictions of ice-sheet volume changes and the effect of these changes on global sea levels. Models are from the paper by Miller et al. in this book, and are in turn based on work of Deconto and Pollard (Nature 421:245-249, 2003). Suggested citation: Cooper, A. K., P. J. Barrett, H. Stagg, B. Storey, E. Stump, W. Wise, and the 10th ISAES editorial team, eds. (2008). Antarctica: A Keystone in a Changing World. Proceedings of the 10th International Symposium on Antarctic Earth Sciences. Washington, DC: The National Academies Press. Copyright © National Academy of Sciences. All rights reserved. Antarctica: A Keystone in a Changing World http://www.nap.edu/catalog/12168.html The National Academy of Sciences is a private, nonprofit, self-perpetuating society of distinguished scholars engaged in scientific and engineering research, dedicated to the furtherance of science and technology and to their use for the general welfare. Upon the authority of the charter granted to it by the Congress in 1863, the Academy has a mandate that requires it to advise the federal government on scientific and technical matters. Dr. Ralph J. Cicerone is president of the National Academy of Sciences. The National Academy of Engineering was established in 1964, under the charter of the National Academy of Sciences, as a parallel organization of outstanding engineers. It is autonomous in its administration and in the selection of its members, sharing with the National Academy of Sciences the responsibility for advising the federal government. The National Academy of Engineering also sponsors engineering programs aimed at meeting national needs, encourages education and research, and recognizes the superior achievements of engineers. Dr. Charles M. Vest is president of the National Academy of Engineering. The Institute of Medicine was established in 1970 by the National Academy of Sciences to secure the services of eminent members of appropriate professions in the examination of policy matters pertaining to the health of the public. The Institute acts under the responsibility given to the National Academy of Sciences by its congressional charter to be an adviser to the federal government and, upon its own initiative, to identify issues of medical care, research, and education. Dr. Harvey V. Fineberg is president of the Institute of Medicine. The National Research Council was organized by the National Academy of Sciences in 1916 to associate the broad community of science and technology with the Academy’s purposes of furthering knowledge and advising the federal government. Functioning in accordance with general policies determined by the Academy, the Council has become the principal operating agency of both the National Academy of Sciences and the National Academy of Engineering in providing services to the government, the public, and the scientific and engineering communities. The Council is administered jointly by both Academies and the Institute of Medicine. Dr. Ralph J. Cicerone and Dr. Charles M. Vest are chair and vice chair, respectively, of the National Research Council. www.national-academies.org Copyright © National Academy of Sciences. All rights reserved. Antarctica: A Keystone in a Changing World http://www.nap.edu/catalog/12168.html Copyright © National Academy of Sciences. All rights reserved. Antarctica: A Keystone in a Changing World http://www.nap.edu/catalog/12168.html 10TH ISAES EDITORIAL TEAM John Anderson, Department of Earth Sciences, Rice University, Houston, Texas 77251 USA, [email protected] Peter Barrett, Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand, [email protected] John Barron, U.S. Geological Survey, 345 Middlefield Rd., Menlo Park, California 94025 USA, [email protected] Philip Bart, Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803 USA, [email protected] Donald Blankenship, Institute for Geophysics, The University of Texas at Austin, 10100 Burnet Road, Austin, Texas 78758 USA, [email protected] Alan Cooper, Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305 USA, [email protected] AND Emeritus scientist, U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025 USA, [email protected] Frederick Davey, GNS-Science, 1 Fairway Drive, Lower Hutt, New Zealand, [email protected] AND Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/c, 34010 Sgonico, Trieste, Italy Michael Diggles, U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025 USA, [email protected] Carol Finn, U.S. Geological Survey, Denver Federal Center, Denver, Colorado 80225 USA, cfi[email protected] Paul Fitzgerald, Department of Earth Sciences, Syracuse
Recommended publications
  • Heterogenous Thinning and Subglacial Lake Activity on Thwaites Glacier, West Antarctica Andrew O
    https://doi.org/10.5194/tc-2020-80 Preprint. Discussion started: 9 April 2020 c Author(s) 2020. CC BY 4.0 License. Brief Communication: Heterogenous thinning and subglacial lake activity on Thwaites Glacier, West Antarctica Andrew O. Hoffman1, Knut Christianson1, Daniel Shapero2, Benjamin E. Smith2, Ian Joughin2 1Department of Earth and Space Sciences, University of Washington, Seattle, 98115, United States of America 5 2Applied Physics Laboratory, University of Washington, 98115, United States of America Correspondence to: Andrew O. Hoffman ([email protected]) Abstract. A system of subglacial laKes drained on Thwaites Glacier from 2012-2014. To improve coverage for subsequent drainage events, we extended the elevation and ice velocity time series on Thwaites Glacier through austral winter 2019. These new observations document a second drainage cycle and identified two new laKe systems located in the western tributaries of 10 Thwaites and Haynes Glaciers. In situ and satellite velocity observations show temporary < 3% speed fluctuations associated with laKe drainages. In agreement with previous studies, these observations suggest that active subglacial hydrology has little influence on Thwaites Glacier thinning and retreat on decadal to centennial timescales. 1 Introduction Although subglacial laKes beneath the Antarctic Ice Sheet were first discovered more than 50 years ago (Robin et al., 1969; 15 Oswald and Robin, 1973), they remain one of the most enigmatic components of the subglacial hydrology system. Initially identified in ice-penetrating radar data as flat, bright specular reflectors (Oswald and Robin, 1973; Carter et al., 2007) subglacial laKes were thought to be relatively steady-state features of the basal hydrology system with little impact on the dynamics of the overlying ice on multi-year timescales.
    [Show full text]
  • 2006-2007 Science Planning Summaries
    Project Indexes Find information about projects approved for the 2006-2007 USAP field season using the available indexes. Project Web Sites Find more information about 2006-2007 USAP projects by viewing project web sites. More Information Additional information pertaining to the 2006-2007 Field Season. Home Page Station Schedules Air Operations Staffed Field Camps Event Numbering System 2006-2007 USAP Field Season Project Indexes Project Indexes Find information about projects approved for the 2006-2007 USAP field season using the USAP Program Indexes available indexes. Aeronomy and Astrophysics Dr. Bernard Lettau, Program Director (acting) Project Web Sites Biology and Medicine Dr. Roberta Marinelli, Program Director Find more information about 2006-2007 USAP projects by Geology and Geophysics viewing project web sites. Dr. Thomas Wagner, Program Director Glaciology Dr. Julie Palais, Program Director More Information Ocean and Climate Systems Additional information pertaining Dr. Bernhard Lettau, Program Director to the 2006-2007 Field Season. Artists and Writers Home Page Ms. Kim Silverman, Program Director Station Schedules USAP Station and Vessel Indexes Air Operations Staffed Field Camps Amundsen-Scott South Pole Station Event Numbering System McMurdo Station Palmer Station RVIB Nathaniel B. Palmer ARSV Laurence M. Gould Special Projects Principal Investigator Index Deploying Team Members Index Institution Index Event Number Index Technical Event Index Project Web Sites 2006-2007 USAP Field Season Project Indexes Project Indexes Find information about projects approved for the 2006-2007 USAP field season using the Project Web Sites available indexes. Principal Investigator/Link Event No. Project Title Aghion, Anne W-218-M Works and days: An antarctic Project Web Sites chronicle Find more information about 2006-2007 USAP projects by Ainley, David B-031-M Adélie penguin response to viewing project web sites.
    [Show full text]
  • Data Structure
    Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference.
    [Show full text]
  • Stratigraphy of Upper Carboniferous and Permian Rocks Exposed Between the Byrd and Nimrod Glaciers JOHN L
    Boulder, here. The project was supported by National Science Founda- belts along the Panthalassan margin of Gondwanaland. Colorado: Geological Society of America. tion grants OPP 89-17348 and OPP 89-15429. Elliot, D.H. 1992. Jurassic magmatism and tectonism associated with Gondwanaland break-up: An antarctic perspective. In B.C. Alabaster and R.J. Pankhurst (Eds.), Magmatism and the causes of References continental break-up (Special Publication No. 68). London: Geo- logical Society of London. Barrett, P.J., D.H. Elliot, and J.F. Lindsay. 1986. The Beacon Super- Elliot, D.H., and D. Larsen. 1993. Mesozoic volcanism in the central group (Devonian-Triassic) and Ferrar Group (Jurassic) in the Transantarctic Mountains, Antarctica: Depositional environment Beardmore Glacier area, Antarctica. In M.D. Turner and J.F. and tectonic setting. In R.H. Findlay, R. Unrug, M.R. Banks, and J.J. Gondwana Eight: Assembly, evolution and Splettstoesser (Eds.), Geology of the central Transantarctic Moun- Veevers, (Eds.), tains (Antarctic Research Series, Vol. 36). Washington, D.C.: Ameri- dispersal. Rotterdam: Balkema. can Geophysical Union. Larsen, D. 1988. The petrology and geochemistry of the volcaniclastic Collinson, J.W., J.L. Isbell, D.H. Elliot, M.F. Miller, and J.W.G. Miller. In upper part of the Falla Formation and Prebble Formation, Beard- press. Permian-Triassic Transantarctic basin. In J.J. Veevers and C. more Glacier area, Antarctica. (Unpublished master of science the- McA. Powell (Eds.), Permian-Triassic Pangaean basins and fold- sis, Ohio State University, Columbus, Ohio.) Stratigraphy of Upper Carboniferous and Permian rocks exposed between the Byrd and Nimrod Glaciers JOHN L.
    [Show full text]
  • Chapter 4 Tectonic Reconstructions of the Southernmost Andes and the Scotia Sea During the Opening of the Drake Passage
    123 Chapter 4 Tectonic reconstructions of the Southernmost Andes and the Scotia Sea during the opening of the Drake Passage Graeme Eagles Alfred Wegener Institute, Helmholtz Centre for Marine and Polar Research, Bre- merhaven, Germany e-mail: [email protected] Abstract Study of the tectonic development of the Scotia Sea region started with basic lithological and structural studies of outcrop geology in Tierra del Fuego and the Antarctic Peninsula. To 19th and early 20th cen- tury geologists, the results of these studies suggested the presence of a submerged orocline running around the margins of the Scotia Sea. Subse- quent increases in detailed knowledge about the fragmentary outcrop ge- ology from islands distributed around the margins of the Scotia Sea, and later their interpretation in light of the plate tectonic paradigm, led to large modifications in the hypothesis such that by the present day the concept of oroclinal bending in the region persists only in vestigial form. Of the early comparative lithostratigraphic work in the region, only the likenesses be- tween Jurassic—Cretaceous basin floor and fill sequences in South Geor- gia and Tierra del Fuego are regarded as strong enough to be useful in plate kinematic reconstruction by permitting the interpretation of those re- gions’ contiguity in mid-Mesozoic times. Marine and satellite geophysical data sets reveal features of the remaining, submerged, 98% of the Scotia 124 Sea region between the outcrops. These data enable a more detailed and quantitative approach to the region’s plate kinematics. In contrast to long- used interpretations of the outcrop geology, these data do not prescribe the proximity of South Georgia to Tierra del Fuego in any past period.
    [Show full text]
  • The U-Pb Detrital Zircon Signature of West Antarctic Ice Stream Tills in The
    Antarctic Science 26(6), 687–697 (2014) © Antarctic Science Ltd 2014. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/3.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. doi:10.1017/S0954102014000315 The U-Pb detrital zircon signature of West Antarctic ice stream tills in the Ross embayment, with implications for Last Glacial Maximum ice flow reconstructions KATHY J. LICHT, ANDREA J. HENNESSY and BETHANY M. WELKE Indiana University-Purdue University Indianapolis, Department of Earth Sciences, 723 West Michigan Street, Indianapolis, IN 46202, USA [email protected] Abstract: Glacial till samples collected from beneath the Bindschadler and Kamb ice streams have a distinct U-Pb detrital zircon signature that allows them to be identified in Ross Sea tills. These two sites contain a population of Cretaceous grains 100–110 Ma that have not been found in East Antarctic tills. Additionally, Bindschadler and Kamb ice streams have an abundance of Ordovician grains (450–475 Ma) and a cluster of ages 330–370 Ma, which are much less common in the remainder of the sample set. These tracers of a West Antarctic provenance are also found east of 180° longitude in eastern Ross Sea tills deposited during the last glacial maximum (LGM). Whillans Ice Stream (WIS), considered part of the West Antarctic Ice Sheet but partially originating in East Antarctica, lacks these distinctive signatures. Its U-Pb zircon age population is dominated by grains 500–550 Ma indicating derivation from Granite Harbour Intrusive rocks common along the Transantarctic Mountains, making it indistinguishable from East Antarctic tills.
    [Show full text]
  • The Eastern Margin of the Ross Sea Rift in Western Marie Byrd Land
    Characterization Geochemistry 3 Volume 4, Number 10 Geophysics 29 October 2003 1090, doi:10.1029/2002GC000462 GeosystemsG G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Eastern margin of the Ross Sea Rift in western Marie Byrd Land, Antarctica: Crustal structure and tectonic development Bruce P. Luyendyk Department of Geological Sciences and Institute for Crustal Studies, University of California, Santa Barbara, California 93106, USA ([email protected]) Douglas S. Wilson Department of Geological Sciences, Marine Science Institute, Institute for Crustal Studies, University of California, Santa Barbara, California 93106, USA Also at Marine Science Institute, University of California, Santa Barbara, California 93106, USA Christine S. Siddoway Department of Geology, Colorado College, Colorado Springs, Colorado 80903, USA [1] The basement rock and structures of the Ross Sea rift are exposed in coastal western Marie Byrd Land (wMBL), West Antarctica. Thinned, extended continental crust forms wMBL and the eastern Ross Sea continental shelf, where faults control the regional basin-and range-type topography at 20 km spacing. Onshore in the Ford Ranges and Rockefeller Mountains of wMBL, basement rocks consist of Early Paleozoic metagreywacke and migmatized equivalents, intruded by Devonian-Carboniferous and Cretaceous granitoids. Marine geophysical profiles suggest that these geological formations continue offshore to the west beneath the eastern Ross Sea, and are covered by glacial and glacial marine sediments. Airborne gravity and radar soundings over wMBL indicate a thicker crust and smoother basement inland to the north and east of the northern Ford Ranges. A migmatite complex near this transition, exhumed from mid crustal depths between 100–94 Ma, suggests a profound crustal discontinuity near the inboard limit of extended crust, 300 km northeast of the eastern Ross Sea margin.
    [Show full text]
  • Evidence for Extending Anomalous Miocene Volcanism at the Edge of The
    1 Evidence for Extending Anomalous Miocene Volcanism at the Edge of the 2 East Antarctic Craton 3 4 K. J. Licht1, T. Groth1, J. P. Townsend2, A. J. Hennessy1, S. R. Hemming3, T. P. Flood4, and M. 5 Studinger5 6 1Department of Earth Sciences, Indiana University-Purdue University Indianapolis, Indianapolis, IN, 7 USA, 2HEDP Theory Department, Sandia National Laboratories, Albuquerque, NM, USA, 3Department of 8 Earth and Environmental Sciences, Columbia University, Lamont-Doherty Earth Observatory, Palisades, 9 NY, USA, 4Geology Department, St. Norbert College, DePere, WI, USA, 5NASA Goddard Space Flight 10 Center, Greenbelt, MD, USA 11 12 Corresponding author: Kathy Licht ([email protected]) 13 14 Key Points: 15 x Olivine basalt, hyaloclastite erratics and detrital zircon at Earth’s southernmost moraine 16 (Mt. Howe) indicate magmatic activity 17- 25 Ma. 17 x The source, indicated by a magnetic anomaly (-740 nT) ~400 km inland from the West 18 Antarctic Rift margin, expands extent of Miocene lavas. 19 x Data corroborate lithospheric foundering beneath southern Transantarctic Mountains based 20 on location of volcanism (duration < 5 my). 21 22 Abstract 23 Using field observations followed by petrological, geochemical, geochronological, and 24 geophysical data we infer the presence of a previously unknown Miocene subglacial volcanic 25 center ~230 km from the South Pole. Evidence of volcanism is from boulders of olivine-bearing 26 amygdaloidal/vesicular basalt and hyaloclastite deposited in a moraine in the southern 27 Transantarctic Mountains. 40Ar/39Ar ages from five specimens plus U-Pb ages of detrital zircon 28 from glacial till indicate igneous activity 25-17 Ma.
    [Show full text]
  • 1 Influence of Sea Ice Anomalies on Antarctic Precipitation Using
    https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution Hailong Wang1*, Jeremy Fyke2,3, Jan Lenaerts4, Jesse Nusbaumer5,6, Hansi Singh1, David Noone7, and Philip Rasch1 (1) Pacific Northwest National Laboratory, Richland, WA 5 (2) Los Alamos National Laboratory, Los Alamos, NM (3) Associated Engineering, Vernon, British Columbia, Canada (4) Department of Atmospheric and Oceanic Sciences, University of Colorado at Boulder, Boulder, CO (5) NASA Goddard Institute for Space Studies, New York, NY (6) Center for Climate Systems Research, Columbia University, New York, NY 10 (7) Oregon State University, Corvallis, OR *Correspondence to: [email protected] 1 https://doi.org/10.5194/tc-2019-69 Preprint. Discussion started: 12 June 2019 c Author(s) 2019. CC BY 4.0 License. Abstract We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source– 5 receptor relationships for precipitation over Antarctica. Surface sensible heat fluxes, evaporation, and column-integrated water vapor are larger over Southern Ocean (SO) areas with lower SIC, but changes in Antarctic precipitation and its source attribution with SICs reflect a strong spatial variability. Among the tagged source regions, the Southern Ocean (south of 50°S) contributes the most (40%) to the Antarctic total precipitation, followed by more northerly ocean basins, most notably the S.
    [Show full text]
  • Mesozoic and Cenozoic Structural Patterns in the Transantarctic
    and J . Berg for providing powders of xenoliths from the 0 kilometers 300 McMurdo Volcanic Province and unpublished data for these samples. I Victoria Land 0 miles 200 Mc rdo Station 0 GlIB? --BGB Byrd Glacier h East Antarctic Ice Sheet + 80.S RB Ross Ice Shelf Byrd Glacier1 -7 MRB BGB References Nimrod Glacier Berg, J.H., R.A. Hank, and R.I. Kalamarides. 1985. Petrology and Marsh Glacier geochemistry of lower crustal basic granulites from the Erebus Vol- canic Province, Antarctica. 1985. Antarctic Journal of the U.S., 20(5), 22-23. Beardmore Shackleton Glacier Glacier Borg, S.C., and D.J. DePaolo. 1990. Isotopic imaging of deep conti- nental lithosphere. Systematics and applications downunder (ab- stract). 7th International Conference on Geochronology, Cosmochronology, and Isotope Geology, Canberra, Australia, Sep- IAntarcScaS Outcrop area: tember 1990. (Abstracts, Vol. 27.) Canberra: Geological Society of ______________ outh Pole Transantarctic ___________________ + Mountains Australia. Borg, S.C., and D.J. DePaolo. In press. A tectonic model of the Ant- arctic Gondwana margin with implications for southeastern Aus- Figure 3. This map of the Transantarctic Mountains in the vicinity tralia: Isotopic and geochemical evidence. Tectonopliysics. of the Ross Ice Shelf shows our working hypothesis for the dis- Borg, S.C., D.J. DePaolo, E.D. Wendlandt, and T.G. Drake. 1989. tribution of lower crustal provinces. This interpretation is based Studies of granites and metamorphic rocks, Byrd Glacier area. Ant- on the inferences from the isotopic compositions shown in figure arctic Journal of the U.S., 25(5), 19-21. 2 and on our inference from field work that the entire north side of Borg, S.C., D.J.
    [Show full text]
  • Oblique Collision in the Northeastern Caribbean from GPS Measurements and Geological Observations
    TECTONICS, VOL. 21, NO. 6, 1057, doi:10.1029/2001TC001304, 2002 Oblique collision in the northeastern Caribbean from GPS measurements and geological observations Paul Mann,1 Eric Calais,2 Jean-Claude Ruegg,3 Charles DeMets,4 Pamela E. Jansma,5 and Glen S. Mattioli6 Received 31 May 2001; revised 16 April 2002; accepted 10 June 2002; published 11 December 2002. [1] Previous Caribbean GPS studies have shown that Tectonophysics: Continental neotectonics; 8105 Tectonophysics: the rigid interior of the Caribbean plate is moving east- Continental margins and sedimentary basins; 3025 Marine Geology northeastward (070°) at a rate of 18–20 ± 3 mm/yr and Geophysics: Marine seismics (0935); 3040 Marine Geology relative to North America. This direction implies and Geophysics: Plate tectonics (8150, 8155, 8157, 8158); 7230 maximum oblique convergence between the island of Seismology: Seismicity and seismotectonics; KEYWORDS: GPS, neotectonics, Hispaniola, Puerto Rico, Bahama Platform, Hispaniola on the Caribbean plate and the 22–27-km- earthquakes. Citation: Mann, P., E. Calais, J.-C. Ruegg, C. thick crust of the Bahama carbonate platform on the DeMets, P. E. Jansma, and G. S. Mattioli, Oblique collision in the adjacent North America plate. We present a tectonic northeastern Caribbean from GPS measurements and geological interpretation of a 15-site GPS network which spans observations, Tectonics, 21(6), 1057, doi:10.1029/2001TC001304, the Hispaniola-Bahama oblique collision zone and 2002. includes stable plate interior sites on both the North America and Caribbean plates. Measurements span the time period of 1994–1999. In a North America 1. Introduction reference frame, GPS velocities in Puerto Rico, St.
    [Show full text]
  • Annals 2/Gilmour
    Paper in: Patrick N. Wyse Jackson & Mary E. Spencer Jones (eds) (2011) Annals of Bryozoology 3: aspects of the history of research on bryozoans. International Bryozoology Association, Dublin, pp. viii+225. THE STUDY OF POST-PALEOZOIC BRYOZOANS IN RUSSIA 163 History of the study of Post-Paleozoic bryozoans in Russia (Results and Prospects) L.A. Viskova and A.V. Koromyslova A.A. Borissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia 1. Introduction 2. Triassic 3. Jurassic 4. Lower Cretaceous 5. The Upper Cretaceous-Paleogene 6. Neogene 7. Recent 8. Acknowledgements 1. Introduction Although bryozoans are widespread in the post-Paleozoic deposits of various regions of Russia and the former USSR, they have only been irregularly and insufficiently studied. The history of their studies is analyzed based on the works with more or less full information on the bryozoans that existed during different periods of geological time in the interval Triassic-Recent.1 2. Triassic The first data on the taxonomic composition and distribution of bryozoans in the Triassic of Russia date back only by the 1950s. At first they were restricted to sporadic records of species of the Paleozoic genera Dyscritella and Pseudobatostomella (Order Trepostomida). Bryozoans of the first genus come from the Norian Stage of northeastern Russia. In 1949 they were described by Vasilii Petrovich Nekhoroshev (1893–1977), professor, Doctor in Geology and Mineralogy, leading authority on Paleozoic bryozoans and founder of the St Petersburg school of paleobryozoologists (Figure 1) (Gilmour et al. 2008, Nekhorosheva 2008). The Russian Far Eastern geologists and paleontologists Buriy and Zharnikova (1961) and Lazutkina (1963) recorded species of Pseudobatostomella from the Lower Triassic of Yakutia and Southern Primorye.
    [Show full text]