Digital Cover

Total Page:16

File Type:pdf, Size:1020Kb

Digital Cover The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate variability Yu, Shiyong 2003 Link to publication Citation for published version (APA): Yu, S. (2003). The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate variability. Deaprtment of Geology. Total number of authors: 1 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 The Littorina transgression in L southeastern Sweden and its relation to mid-Holocene U climate variability N D Q Shi-Yong Yu U LUNDQUA Thesis 51 Quaternary Sciences A Department of Geology GeoBiosphere Science Centre Lund University T Lund 2003 H E S I S LUNDQUA Thesis 51 The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate variability Shi-Yong Yu Avhandling att med tillstånd från Naturvetenskapliga Fakulteten vid Lunds Universitet för avläggandet av filosofie doktorsexamen, offentligen försvaras i Geologiska institutionens föreläsningssal Pangea, Sölvegatan 12, Lund, fredagen den 14 november kl. 13.15. Lund 2003 Lund University, Department of Geology, Quaternary Sciences Coring the shallow sea bed of the Smygen Bay, SE Sweden. Photo courtesy of B. E. Berglund (2001). The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate variability By Shi-Yong Yu GeoBiosphere Science Centre, Department of Geology/Quaternary Sciences, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden This thesis is based on the work carried out while I Appendix III: Yu, S.-Y., Berglund, B.E., Andrén, was a Ph. D. student at the Department of Geol- E., and Sandgren, P.: Mid-Holocene Baltic Sea ogy, GeoBiosphere Science Centre, Lund Univer- transgression along the coast of Blekinge, SE Swe- sity, between September 1999 and November 2003. den — ancient lagoons correlated with beach ridges. The results of this work have been presented in six Manuscript submitted to GFF. separate papers listed below as appendices (I–VI) and are hereafter referred to by their Roman nu- Appendix IV: Yu, S.-Y. 2003: Centennial-scale merals. The papers have been submitted to peer- cycles in middle Holocene sea level along the south- reviewed international journals. Three of them will eastern Swedish Baltic coast. Geological Society appear soon and the other three are still under con- of America Bulletin 115 (in press). sideration. Appendix V: Yu, S.-Y., and Sandgren, P.: Mid-Ho- Appendix I: Yu, S.-Y., Andrén, E., Barnekow, L., locene changes in North Atlantic Oscillation pat- Berglund, B.E., and Sandgren, P. 2003: Holocene terns and Baltic nearshore hydrography at centen- palaeoecology and shoreline displacement on the nial time scales. Manuscript submitted to Journal Biskopsmåla Peninsula, southeastern Sweden. of Quaternary Science. Boreas 32 (in press). Appendix VI: Yu, S.-Y, Berglund, B.E., and Appendix II: Yu, S.-Y., Berglund, B.E., Sandgren, Sandgren, P.: Acceleration of Baltic sea-level rise P., and Fritz, S.C. 2004: Holocene palaeoecology suggests a global meltwater pulse 8000 years ago. and shoreline displacement along the Blekinge coast, Manuscript submitted to Science. SE Sweden and implications for climate and sea- level changes. The Holocene 14 (in press). Contents PREFACE ................................................................................................................................... 1 INTRODUCTION ...........................................................................................................2 LATE QUATERNARY HISTORY OF THE BALTIC SEA................................................... 3 STAGE 1 – BALTIC ICE LAKE....................................................................................................................... 3 STAGE 2 – YOLDIA SEA............................................................................................................................... 3 STAGE 3 – ANCYLUS LAKE ......................................................................................................................... 3 STAGE 4 – LITTORINA SEA.......................................................................................................................... 4 POSTGLACIAL SHORELINE DISPLACEMENT IN SOUTHEASTERN SWEDEN ......4 STUDY AREA............................................................................................................................. 4 SITE DESCRIPTIONS .............................................................................................................. 5 SMYGEN BAY .............................................................................................................................................. 5 HUNNEMARA ANCIENT LAKE...................................................................................................................... 5 LAKE RYSSJÖN............................................................................................................................................ 5 LAKE FÄRSKSJÖN........................................................................................................................................ 6 OTHER SITES DISCUSSED............................................................................................................................. 6 METHODS................................................................................................................................... 7 FIELDWORK ................................................................................................................................................ 7 CORE LOGGING AND MAGNETIC-SUSCEPTIBILITY SCANNING..................................................................... 8 CORE SPLICING AND SUBSAMPLING............................................................................................................ 8 ORGANIC CONTENT, ORGANIC CARBON AND MINERAL MAGNETISM ......................................................... 8 POLLEN AND DINOFLAGELLATES................................................................................................................ 8 DIATOMS..................................................................................................................................................... 8 MACROFOSSILS........................................................................................................................................... 9 RADIOCARBON DATING .............................................................................................................................. 9 RESULTS — SUMMARIES OF PAPERS............................................................................. 9 PAPER I ....................................................................................................................................................... 9 PAPER II .................................................................................................................................................... 10 PAPER III ................................................................................................................................................... 10 PAPER IV ................................................................................................................................................... 11 PAPER V .................................................................................................................................................... 12 PAPER VI ................................................................................................................................................... 12 DISCUSSION............................................................................................................................ 13 TIMING AND PATTERN OF THE LITTORINA TRANSGRESSION..................................................................... 13 IRREGULAR ISOSTASY OR VARIABLE ICE VOLUME? ................................................................................. 13 ATMOSPHERIC FORCING VERSUS TIDAL ACTIONS..................................................................................... 15 CONCLUSIONS....................................................................................................................... 15 ACKNOWLEDGEMENTS ...................................................................................................... 16 SVENSK SAMMANFATTNING............................................................................................. 17 REFERENCES ........................................................................................................................
Recommended publications
  • Paleoenvironmental Reconstructions in the Baltic Sea and Iberian Margin
    Paleoenvironmental reconstructions in the Baltic Sea and Iberian Margin Assessment of GDGTs and long-chain alkenones in Holocene sedimentary records Lisa Alexandra Warden Photography: Cover photos: Dietmar Rüß Inside photos: Dietmar Rüß, René Heistermann and Claudia Zell Printed by: Ridderprint, Ridderkerk Paleoenvironmental reconstructions in the Baltic Sea and Iberian Margin Assessment of GDGTs and long-chain alkenones in Holocene sedimentary records Het gebruik van GDGTs en alkenonen in Holocene sedimentaire archieven van de Baltische Zee en kustzeeën van het Iberisch schiereiland voor paleomilieureconstructie (met een samenvatting in het Nederlands) Proefschrift ter verkrijging van de graad van doctor aan de Universiteit Utrecht op gezag van de rector magnificus, prof. dr. G.J. van der Zwaan, ingevolge het besluit van het college voor promoties in het openbaar te verdedigen op vrijdag 31 maart 2017 des middags te 12.45 uur door Lisa Alexandra Warden geboren op 24 januari 1982 te Philadelphia, Verenigde Staten van Amerika Promotor: Prof. dr. ir. J.S. Sinninghe Damsté This work has been financially supported by the European Research Council (ERC) and the NIOZ Royal Netherlands Institute for Sea Research. “We are the first generation to feel the impact of climate change and the last generation that can do something about it.” -President Obama For Lauchlan, who was with me the whole time as I wrote this thesis. Photo by Dietmar Rüß Contents Chapter 1 – Introduction 9 Chapter 2 - Climate forced human demographic and cultural change in
    [Show full text]
  • Post-Glacial History of Sea-Level and Environmental Change in the Southern Baltic Sea
    Post-Glacial History of Sea-Level and Environmental Change in the Southern Baltic Sea Kortekaas, Marloes 2007 Link to publication Citation for published version (APA): Kortekaas, M. (2007). Post-Glacial History of Sea-Level and Environmental Change in the Southern Baltic Sea. Department of Geology, Lund University. Total number of authors: 1 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 Post-glacial history of sea-level and environmental change in the southern Baltic Sea Marloes Kortekaas Quaternary Sciences, Department of Geology, GeoBiosphere Science Centre, Lund University, Sölvegatan 12, SE-22362 Lund, Sweden This thesis is based on four papers listed below as Appendices I-IV.
    [Show full text]
  • Ume 10, -U Ser
    Volume 10, -u ser . - 1968 Editors EDWARD S. DEEVEY a-- RICHARD FOSTER FLINT J. GORDON OGDEN, III _ IRVINg ROUSE Managing Editor RENEE S. KRA YALE UNIVERSITY NEW HAVEN, CONNECT.IC U l"ii)fl h d IiV r E AT\As g'LyyEi.. R C N, / r..? i.NA .3 8. ComIlient, usually corn ; fOg the date with other relevant dates, for each ,Ttdterial, silil"iiliari ing t e signitic.ance ant Sillpllilt 3't(i"r ing t., t t e radiocarbon t was i' itl ii73kinz 'P;.5 lit;re, i'; till teelmital :i"it.' i°_i , e.g. the iral lthout subscribers at $50.0( * Suggestions to authors of the reprints o the United Suites Geological Survey, 5th ed., Vashington, D. C., 1958 jc.=oscrxwxcn.t Panting ()ihce, $1.75). Volume 10, Number 1 - 1968 RADIOCARBON Published by THE AMERICAN JOURNAL OF SCIENCE Editors EDWARD S. DEEVEY- RICHARD FOSTER FLINT J. GORDON OGDEN, III - IRVING ROUSE Managing Editor RENEE S. KRA YALE UNIVERSITY NEW HAVEN, CONNECTICUT VOL. 1 10, No. Radiocarbon 1965 CONTENTS Il1I Barker and John lackey British Museum Natural Radiocarbon Measurements V 1 BONN H. IV. Scharpenseel, F. Pietig, and M. A. Tawcrs Bonn Radiocarbon Measurements I ............................................... IRPA Anne Nicole Schreurs Institut Royal du Patrimoine Artistirlue Radiocarbon Dates I ........ 9 Lu Soren Hkkansson University of Lund Radiocarbon Dates I Lv F. Gilot Louvain Natural Radiocarbon Measurements VI ..................... 55 1I H. R. Crane and J. B. Griffin University of Michigan. Radiocarbon Dates NII 61 N PL IV. J. Callow and G. I. Hassall National Physical Laboratory Radiocarbon Measurements V ..........
    [Show full text]
  • CHANGES in SEA LEVEL, POSTGLACIAL UPLIFT, and MOBILITY of the EARTH’S INTERIOR by BENO GUTENBERG CONTENTS Abstract
    BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 52, PP. 721-772, S FIGS. M AY!, 1941 CHANGES IN SEA LEVEL, POSTGLACIAL UPLIFT, AND MOBILITY OF THE EARTH’S INTERIOR BY BENO GUTENBERG CONTENTS Abstract.................................................................................................................................. 721 Introduction........................................................................................................................... 722 Material.................................................................................................................................. 722 Causes for slow variations of tide-gauge readings.......................................................... 722 Method of calculation........................................................................................................ 726 Eustatic changes................................................................................................................... 728 Postglacial uplift in Fennoscandia..................................................................................... 733 Postglacial uplift in North America.................................................................................. 739 Postglacial uplift, summary................................................................................................ 750 Viscosity and strength of the earth.................................................................................... 751 Conclusions...........................................................................................................................
    [Show full text]
  • 20020011.Pdf
    Color profile: Generic CMYK printer profile Composite Default screen 1144 PERSPECTIVE Geological and evolutionary underpinnings for the success of Ponto-Caspian species invasions in the Baltic Sea and North American Great Lakes David F. Reid and Marina I. Orlova1 Abstract: Between 1985 and 2000, ~70% of new species that invaded the North American Great Lakes were endemic to the Ponto-Caspian (Caspian, Azov, and Black seas) basins of eastern Europe. Sixteen Ponto-Caspian species were also established in the Baltic Sea as of 2000. Many Ponto-Caspian endemic species are characterized by wide environmental tolerances and high phenotypic variability. Ponto-Caspian fauna evolved over millions of years in a series of large lakes and seas with widely varying salinities and water levels and alternating periods of isolation and open connections between the Caspian Sea and Black Sea depressions and between these basins and the Mediterranean Basin and the World Ocean. These conditions probably resulted in selection of Ponto-Caspian endemic species for the broad environmental tolerances and euryhalinity many exhibit. Both the Baltic Sea and the Great Lakes are geologi- cally young and present much lower levels of endemism. The high tolerance of Ponto-Caspian fauna to varying environmental conditions, their ability to survive exposure to a range of salinities, and the similarity in environmental conditions available in the Baltic Sea and Great Lakes probably contribute to the invasion success of these species. Human activities have dramatically increased the opportunities for transport and introduction and have played a cata- lytic role. Résumé : Entre 1985 et 2000, environ 70 % des espèces qui ont envahi pour la première fois les Grands-Lacs d’Amérique du Nord étaient endémiques aux bassins versants de la région pontocaspienne de l’Europe de l’Est, soit ceux de la mer Caspienne, de la mer d’Azov et de la mer Noire.
    [Show full text]
  • Relative Sea Level Changes, Glacio-Isostatic Rebound and Shoreline Displacement in the Southern Baltic
    SZYMON UŒCINOWICZ RELATIVE SEA LEVEL CHANGES, GLACIO-ISOSTATIC REBOUND AND SHORELINE DISPLACEMENT IN THE SOUTHERN BALTIC Polish Geological Institute Special Papers,10 WARSZAWA 2003 CONTENTS Introduction ..................................................................6 Area, objective and scope of study ......................................................7 Area of study ...............................................................7 Objective and scope of the work .....................................................8 Analysed materials ............................................................9 Geological setting of the Southern Baltic: an outline .............................................9 Pre-Quaternary ..............................................................9 Quaternary................................................................10 Relative sea level changes ..........................................................11 The problem and methods for its solution ...............................................11 Late Pleistocene and Early Holocene ..................................................18 The turn of Early and Middle Holocene, Middle Holocene ......................................31 Late Holocene ..............................................................35 Vertical crust movements ..........................................................37 Glacio-isostatic rebound: an outline of the problem ..........................................37 Glacio-isostatic movements in the Southern Baltic ...........................................38
    [Show full text]
  • Littorina Sea Since Ca 8700 Cal Yr BP Relative Sea Level Curves
    EOLO L G OG O IA O I IK N L S T Ü I T U U T U R T A T M 1820 E O N E T LL E ET MA Global sea level rise and changing erosion: examples from the Baltic Sea Basin Alar Rosentau University of Tartu, Estonia Jan Harff, Szczecin University, Poland; IOW Warnemünde, Germany Birgit Hünicke, Helmholtz-Zentrum Geesthacht, Germany Ice sheet extension during LGM Svendsen, J.I. et al. 2004.Late Quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews 23, 1229–1271 Ice sheet extension during LGM Svendsen, J.I. et al. 2004.Late Quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews 23, 1229–1271 Tide-gauge measurements data by Ekman, 1996 Vertical crustal movements data by Lidberg et al., 2007 Eustatic sea level Black: Global eustatic sea level curve of Waelbroeck et al. (2002) Red: Barbados eustatic curve using ICE-5G(VM2) model Purple “step-discontinuous” curve, the “ice equivalent” eustatic sea level history of the ICE-5G model of global deglaciation m bsl Peltier 2007 History of the Baltic Sea Baltic Ice Lake ca 15 000- 11 700 cal yr BP History of the Baltic Sea Yoldia Sea ca 11 700- 10 800 cal yr BP History of the Baltic Sea Ancylus Lake ca 10 800- 8 700 cal yr BP History of the Baltic Sea Littorina Sea Since ca 8700 cal yr BP Relative sea level curves Rosentau, A., Meyer, M., Harff, J, Dietrich, R, Richter, A. 2007 RSL change model for Littorina Sea Changes in volume and area Rosentau, A et al.
    [Show full text]
  • The Late Quaternary Development of the Baltic Sea
    The late Quaternary development of the Baltic Sea Svante Björck, GeoBiosphere Science Centre, Department of Geology, Quaternary Sciences, Lund University, Sölveg. 12, SE-223 62 Lund, Sweden INTRODUCTION Since the last deglaciation of the Baltic basin, which began 15 000-17 000 cal yr BP (calibrated years Before Present) and ended 11 000-10 000 cal yr BP, the Baltic has undergone many very different phases. The nature of these phases were determined by a set of forcing factors: a gradually melting Scandinavian Ice Sheet ending up into an interglacial environment, the highly differential glacio-isostatic uplift within the basin (from 9 mm/yr to -1mm/yr; Ekman 1996), changing geographic position of the controlling sills (Fig. 1), varying depths and widths of the thresholds between the sea and the Baltic basin, and climate change. These factors have caused large variations in salinity and water exchange with the outer ocean, rapid to gradual paleographic alterations with considerable changes of the north-south depth profile with time. For example, the area north of southern Finland-Stockholm has never experienced transgressions, or land submergence, while the developmen south of that latitude has been very complex. The different controlling factors are also responsible for highly variable sedimentation rates, both in time and space, and variations of the aquatic productivity as well as faunal and floral changes. The basic ideas in this article follow the lengthy, but less up-dated version of the Baltic Sea history (Björck, 1995), a more complete reference list and, e.g., the calendar year chronology of the different Baltic phases can be found on: http://www.geol.lu.se/personal/seb/Maps%20of%20the%20Baltic.htm.
    [Show full text]
  • In the Wake of Deglaciation - Sedimentary Signatures of Ice-Sheet Decay and Sea-Level Change
    ! "# "$%&%'($$) * * +%,( - ."" %% /( 0 * 1 ./-2+ .-2/ *./3 4 .34/ 4*./5 6 .6/ 47 ( .-2/ .34 6/ 5 * * * ( 4 7 *-2 ( -2 8 ! 0(6 70-*9 * - (: ;<'$=<$( 7( 7 0-* %%><$="&$( 7(3 * 70-.?%"(&( 7/ 9 ( - *34 3 .?%%( 7/ 7 * @ (6 7 5 34 (3 * @ 7 (6 A 34(6 @ ( ! 5B 9 5 C * @ 5B @ (6 . :/ *6* (6 D: - 0(@ @ * * - 5(6 5B @ ( !" "$%& 1EE ( ( E F G 1 1 1 1%<';$> 07:;#&;%##;#%>', 07:;#&;%##;#%>,% ! *%$>;% IN THE WAKE OF DEGLACIATION - SEDIMENTARY SIGNATURES OF ICE-SHEET DECAY AND SEA-LEVEL CHANGE Henrik Swärd In the wake of deglaciation - sedimentary signatures of ice-sheet decay and sea-level change Studies from south-central Sweden and the western Arctic Ocean Henrik Swärd ©Henrik Swärd, Stockholm University 2018 ISBN print 978-91-7797-163-4 ISBN PDF 978-91-7797-164-1 Cover: Sólheimajökull, Iceland. Photo: Henrik Swärd Printed in Sweden by Universitetsservice US-AB, Stockholm 2018 Distributor: Department of Geological Sciences, Stockholm University S.D.G. Abstract Lacustrine and marine sedimentary archives help
    [Show full text]
  • Extent and Timing of the Weichselian Glaciation Southeast of the Baltic Sea
    ALTIC RIB UM PE O I R N Q P UA T ER International Field Symposium of the INQUA Peribaltic Working Group Tartu, September 13–17, 2009 EXTENT AND TIMING OF THE WEICHSELIAN GLACIATION SOUTHEAST OF THE BALTIC SEA University of Tartu, Institute of Ecology and Earth Sciences Tartu 2009 Organisers: University of Tartu, Institute of Ecology and Earth Sciences, Department of Geology. University of Latvia, Faculty of Geography and Earth Sciences. INQUA Peribaltic Working Group (INQUA TERPRO Commission). ESTQUA – Estonian National Committee of INQUA. Organising Commitee: Volli Kalm, Maris Rattas, Vitalijs Zelčs, Tiit Hang, Alar Rosentau, Kadri Sohar, Liina Laumets, Katrin Lasberg, Marko Kohv. Recommended reference to this publication: Kalm, V., Laumets, L. & Hang,T. (eds.), 2009. Extent and timing of the Weichselian Glaciation southeast of the Baltic Sea: Abstracts & Guidebook. The INQUA Peribaltic Working Group Field Symposium in southern Estonia and northern Latvia, September 13–17, 2009. Tartu Ülikooli Kirjastus, Tartu, 112 pages. Sponsored by: Institute of Ecology and Earth Sciences, University of Tartu. Latvian Peat Producers Joint Stock Company Association “Seda” Skolas laukums Bauskas iela 20, Rīga, LV - 1, Seda, Valka District, 1004, Latvia, phone: +371 LV-4728, Latvia,, phone: 7605096, fax: +371 +371 64722113, fax: 7627810, [email protected] +371 64781101 Editors: Volli Kalm, Liina Laumets & Tiit Hang. The front cover photography “Late Weichselian till on glaciofluvial deposits, Kambja endmoraine” (photo by Maris Rattas). Graphical elaboration by Katrin Lasberg. Copyright by: Institute of Ecology and Earth Sciences, University of Tartu. 2009. ISBN 978–9949–19–218–2 Tartu University Press www.tyk.ee CONTENTS ABSTRACTS AND POSTERS Leeli AMON, Atko HEINSALU, Siim VESKI LATE-GLACIAL MULTIPROXY EVIDENCE OF VEGETATION DEVELOPMENT AND CLIMATE CHANGE AT SOLOVA, SOUTHERN ESTONIA ...................................................................................
    [Show full text]
  • The 12Th Colloquium on Baltic Sea Marine Geology September 8 – 12, 2014 Leibniz Institute for Baltic Sea Research Warnemünde
    The 12th Colloquium on Baltic Sea Marine Geology September 8 – 12, 2014 Leibniz Institute for Baltic Sea Research Warnemünde Abstract Volume The 12th Colloquium on Baltic Sea Marine Geology, Abstract Volume 2 The 12th Colloquium on Baltic Sea Marine Geology, Abstract Volume Content Andrén, E. et al.: (Oral) Uppbaser: Understanding past and present Baltic Sea ecosystem response –background for a sustainable future .............................................................. 14 Andrén, Th. et al.: (Oral) The Baltic Sea IODP expedition 347 "Baltic Sea Paleoenvironment" – impressions from the cruise, first results and the how we got there ................................ 10 Apler, A. et al.: (Oral) Contaminated sediments (Fibre Banks) along the uplifting northern Baltic coast ............................................................................................................................. 55 Bendixen, C. et al.: (Oral) The Great Belt connection to the southern Kattegat 11.0 – 8.0 cal ka. BP – the relation to the drainage of the Ancylus Lake .......................................................... 24 Bennike, O. et al.: (Oral) First remains of submarine, non-marine, arctic plants from the Danish North Sea ...................................................................................................................... 23 Binczewska, A et al.: (Poster) Climate forcing factors for marine environmental change during the Mid and Late Holocene - a link between the eastern Atlantic and the Baltic Sea - main view of the project.
    [Show full text]
  • Integrated Ocean Drilling Program Expedition 347 Preliminary Report
    Integrated Ocean Drilling Program Expedition 347 Preliminary Report Baltic Sea Basin Paleoenvironment Paleoenvironmental evolution of the Baltic Sea Basin through the last glacial cycle Platform operations 12 September–1 November 2013 Onshore Science Party 22 January–20 February 2014 Expedition 347 Scientists Published by Integrated Ocean Drilling Program Publisher’s notes Material in this publication may be copied without restraint for library, abstract service, educational, or personal research purposes; however, this source should be appropriately acknowledged. Core samples and the wider set of data from the science program covered in this report are under moratorium and accessible only to Science Party members until 20 February 2015. Published by International Ocean Discovery Program for the Integrated Ocean Drilling Program and prepared by the European Consortium of Ocean Research Drilling (ECORD) Science Operator. Funding for the program is provided by the following agencies: National Science Foundation (NSF), United States Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan European Consortium for Ocean Research Drilling (ECORD) Ministry of Science and Technology (MOST), People’s Republic of China Korea Institute of Geoscience and Mineral Resources (KIGAM) Australian Research Council (ARC) and GNS Science (New Zealand), Australian/New Zealand Con- sortium Ministry of Earth Sciences (MoES), India Coordination for Improvement of Higher Education Personnel, Brazil Disclaimer Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the participating agencies, IODP, British Geological Survey, European Petrophysics Consortium, University of Bremen, or the authors’ institutions. Portions of this work may have been published in whole or in part in other International Ocean Discovery Program documents or publications.
    [Show full text]