VU Research Portal

Total Page:16

File Type:pdf, Size:1020Kb

VU Research Portal VU Research Portal A 13,000-year record of climate- and human-impact-induced flooding in the Lower Meuse Peng, F. 2020 document version Publisher's PDF, also known as Version of record Link to publication in VU Research Portal citation for published version (APA) Peng, F. (2020). A 13,000-year record of climate- and human-impact-induced flooding in the Lower Meuse. General rights 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 ? 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. E-mail address: [email protected] Download date: 07. Oct. 2021 VRIJE UNIVERSITEIT A 13,000-year record of climate- and human-impact-induced flooding in the Lower Meuse ACADEMISCH PROEFSCHRIFT ter verkrijging van de graad Doctor of Philosophy aan de Vrije Universiteit Amsterdam, op gezag van de rector magnificus prof.dr. V. Subramaniam, in het openbaar te verdedigen ten overstaan van de promotiecommissie van de Faculteit der Bètawetenschappen op dinsdag 20 oktober 2020 om 9.45 uur in de aula van de universiteit, De Boelelaan 1105 door Fei Peng geboren te Henan, China promotor: prof.dr. R.T. van Balen copromotoren: dr. M.A. Prins dr. C. Kasse Reading committee: prof.dr. Mark Macklin prof.dr. Hans Middelkoop prof.dr. Philip Ward prof.dr. Klaudia Kuiper dr. Joep Storms Contents Summary ................................................................................................................................................ 1 1. Introduction ....................................................................................................................................... 5 1.1. Background .................................................................................................................................. 5 1.2. The research area ......................................................................................................................... 6 1.3. Outline.......................................................................................................................................... 7 2. An improved method for paleoflood reconstruction and flooding phase identification, applied to the Meuse River in the Netherlands ................................................................................................ 9 2.1. Introduction .................................................................................................................................. 9 2.2. Setting ........................................................................................................................................ 11 2.3. Material and methods ................................................................................................................. 12 2.3.1. Coring and scanning ........................................................................................................... 12 2.3.2. Grain-size analysis and end-member modelling ................................................................. 13 2.3.3. Thermo gravimetric analysis ............................................................................................... 14 2.3.4. Geochronology .................................................................................................................... 15 2.4. Results ........................................................................................................................................ 17 2.4.1. Description of the sedimentary units .................................................................................. 17 2.4.2. Age-depth model ................................................................................................................. 21 2.4.3. End-member modelling analysis ......................................................................................... 21 2.5. A new method for paleoflood reconstruction, the Flood Energy Index (FEI) ........................... 24 2.6. Discussion .................................................................................................................................. 25 2.6.1. The Holocene floodplain evolution ..................................................................................... 25 2.6.2. Evaluation of FEI ................................................................................................................ 27 2.6.3. Holocene paleoflooding phases .......................................................................................... 28 2.7. Conclusion ................................................................................................................................. 31 2.8. Supplementary ........................................................................................................................... 33 2.8.1. Correlation of cores WA11 and WA16 ............................................................................... 33 2.8.2. X-ray fluorescence (XRF) analysis ..................................................................................... 33 2.8.3. Analyses of Fe-Mn concretions and grain-size tests ........................................................... 33 2.8.4. Tuned age-depth model for the clastic sequence ................................................................ 34 2.8.5. Pollen assemblage and cultural periods subdivision ........................................................... 35 3. Paleoflooding reconstruction from Holocene levee deposits in the Lower Meuse valley, the Netherlands .......................................................................................................................................... 43 3.1. Introduction ................................................................................................................................ 43 3.2. Research area ............................................................................................................................. 45 3.3. Material and methods ................................................................................................................. 47 3.3.1. Location selection, archeological investigations and sampling .......................................... 47 3.3.2. Magnetic susceptibility (MS) .............................................................................................. 47 3.3.3. Thermogravimetric analysis (TGA) .................................................................................... 48 3.3.4. Grain size analysis and end-member modelling ................................................................. 48 3.3.5. Chronology ......................................................................................................................... 48 3.4. Results ........................................................................................................................................ 49 3.4.1. Geomorphological analysis ................................................................................................. 49 3.4.2. Stratigraphic descriptions and sedimentary results ............................................................. 49 3.4.3. Chrono-stratigraphic framework and age-model ................................................................ 56 3.4.4. Flood energy reconstruction based on decomposed levee grain size records ..................... 58 3.5. Discussion .................................................................................................................................. 60 3.5.1. Longitudinal differential levee sedimentation .................................................................... 60 3.5.2. The influence of flooding phases and human activity on levee sedimentation ................... 61 3.5.3. Applicability of Ooijen levee sediments in paleoflood reconstruction ............................... 65 3.6. Conclusion ................................................................................................................................. 66 4. Rapid flood intensification and environmental response of the Lower Meuse during the Allerød-Younger Dryas climate oscillation ....................................................................................... 68 4.1. Introduction ................................................................................................................................ 68 4.2. Geological setting and Lateglacial river evolution .................................................................... 69 4.3. Material and methods ................................................................................................................. 72 4.3.1. Coring description and sampling ........................................................................................ 72 4.3.2. Grain size analysis and end-member modelling ................................................................. 72 4.3.3. Thermogravimetric analysis (TGA) ...................................................................................
Recommended publications
  • MAY 21 to 25, 2018
    Abstracts Volume MAY 21 to 25, 2018 7th international OLOT - CATALONIA - SPAIN DL GI 743-2018 ISBN 978-84-09-01627-3 Cover Photo: ACGAX. Servei d’Imatges. Fons Ajuntament d’Olot. Autor: Eduard Masdeu Authors: Xavier Bolós and Joan Martí Abstracts Volume MAY 21 to 25, 2018 Scientific Committee Members IN ALPHABETICAL ORDER Patrick BACHÈLERY Károly NÉMETH Observatoire de Physique du Globe de Clermont-Ferrand Massey University (New Zealand) and Laboratoire Magmas et Volcans (France) Oriol OMS Pierre BOIVIN Universitat Autònoma de Barcelona (Spain) Laboratoire Magmas et Volcans (France) Michael ORT Xavier BOLÓS Northern Arizona University (USA) Univesidad Nacional Autónoma de México (Mexico) Pierre-Simon ROSS Gerardo CARRASCO Institut National de la Recherche Scientifique (Canada) Universidad Nacional Autónoma de México (Mexico) Dmitri ROUWET Shane CRONIN Istituto Nazionale di Geofisica e Vulcanologia (Italy) The University of Auckland (New Zealand) Claus SIEBE Gabor KERESZTURI Universidad Nacional Autónoma de México (Mexico) Massey University (New Zealand) Ian SMITH Jiaqi LIU The University of Auckland (New Zealand) Chinese Academy of Sciences (China) Giovanni SOSA Didier LAPORTE Universidad Nacional Autónoma de México (Mexico) Laboratoire Magmas et Volcans (France) Gregg VALENTINE Volker LORENZ University at Buffalo (USA) University of Wuerzburg (Germany) Benjamin VAN WYK DE VRIES José Luís MACÍAS Observatoire de Physique de Globe de Clermont- Ferrand Universidad Nacional Autónoma de México (Mexico) and Laboratoire Magmas et Volcans (France)
    [Show full text]
  • Geomorphology 372 (2021) 107469
    Geomorphology 372 (2021) 107469 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Rapid flood intensification and environmental response of the Lower Meuse during the Allerød-Younger Dryas climate transition Fei Peng a,⁎, Ronald van Balen a,b, Christiaan Beets a, Cornelis Kasse a, Maarten Prins a, Nathalie Van der Putten a, Simon Troelstra a, Hessel Woolderink a, John Van der Woude a a Department of Earth Sciences, Vrije Universiteit Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, the Netherlands b TNO - Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB Utrecht, the Netherlands article info abstract Article history: Lateglacial climatic oscillations exerted profound impacts on the Meuse fluvial system. In the Lower Meuse Received 7 April 2020 (southern Netherlands), geomorphological studies in the last decades mainly centred on Lateglacial vegetation Received in revised form 5 September 2020 evolution, channel pattern changes and river terrace formation. Little information has been reported about the Accepted 6 October 2020 paleohydrology and its relation with the regional climate conditions. This study investigates a sediment core Available online 9 October 2020 that contains flood sediments deposited from the early Allerød up to the middle Holocene. We conducted grain size analysis, thermogravimetric analysis (organic matter and calcium carbonate content), pollen and mac- Keywords: Grain-size distribution rofossil analysis, and determined the oxygen and carbon stable isotope ratios of biogenic carbonate (opercula of 14 End-member modelling the freshwater gastropod Bithynia tentaculata). The chronology of the core is based on AMS Cdatingandpollen Lateglacial biostratigraphical correlation. The pollen and macrofossil studies reveal that the core site was a lake environment Lower Meuse flood during the Allerød and Younger Dryas periods.
    [Show full text]
  • Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993
    CIRC. 1119 U.S. GEOLOGICAL SURVEY CIRCULAR 1119 Proceedings of the Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993 Proceedings of the Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993 Edited by Larry V. Benson U.S. GEOLOGICAL SURVEY CIRCULAR· 1119 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government U.S. GOVERNMENT PRINTING OFFICE: 1996 Free on application to the U.S. Geological Survey Information Services Box 25286 Federal Center Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin" (1993: Reno, Nev.) Proceedings of the Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993/ edited by Larry V. Benson. p. em.- (U.S. Geological Survey circular; 1119) Includes index. 1. Paleoclimatology-Great Basin-congresses. 2. Great Basin-climate-Congresses. I. Benson, Larry V. II. Title. Ill. Series QC884.W67 1993 96-29329 551.6979-dc20 CIP PREFACE The workshop "'Ongoing Paleoclimatic Studies in the Northern Great Basin" was jointly sponsored by the U.S. Geological Smvey (USGS), the University ofNevada-Reno (UNR), and the Quaternary Sciences Center (QSC) of the Desert Research Institute, Reno, Nevada. W. Berry Lyons, chairman of the Hydrology Program (UNR), and Dale Ritter, head of the QSC, chaired the presentations. On May 16, Joseph Smoot, of the USGS, led a field trip along the Truckee River Canyon downstream from Wadsworth, Nevada.
    [Show full text]
  • Nature-Directed Approach to Hydrology and Hydraulics of Extreme Floods and Megafloods
    Nature-Directed Approach to Hydrology and Hydraulics of Extreme Floods and Megafloods Item Type text; Electronic Dissertation Authors Liu, Tao Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction, presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 01/10/2021 17:03:45 Link to Item http://hdl.handle.net/10150/632582 NATURE-DIRECTED APPROACH TO HYDROLOGY AND HYDRAULICS OF EXTREME FLOODS AND MEGAFLOODS by Tao Liu __________________________ Copyright © Tao Liu 2019 A Dissertation Submitted to the Faculty of the DEPARTMENT OF HYDROLOGY AND ATMOSPHERIC SCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY WITH A MAJOR IN HYDROLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 2019 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE Tao Liu, Nature-Directed Approach to Hydrology and Hydraulics of As members of the Dissertation Committee, we certify that we have read the dissertation Extreme Floods and Megajloods prepared by titled and recommend that it be accepted as fulfilling the dissertation requirement fo ec of Doctor of Philosophy. a� (04/08/2019) Date: (04/08/2019) Date: (04/08/2019) Date: (04/08/2019) Date: Final approva"-- �-�-�--��� of the final co 3 ACKNOWLEDGEMENT It is the time to say “thank you” to all people who have made a great contribution to this work and my time in the hydrology program. Dr. Vic Baker is the most important person for me to pursue the “Ph.
    [Show full text]
  • Public Release of Subsurface Management Plan
    Oregon Caves National Monument Subsurface Management Plan 1 TABLE OF CONTENTS I. INTRODUCTION A. Purpose and Significance........................................................................................ 4 B. Legislative and Administrative Requirements......................................................... 5 II. PRESENT RESOURCE STATUS............................................................................. 7 III. DATA COLLECTION A. Cave Classification………………………………………………………………... 12 B. Inventories…………………………………………………………………………. 12 IV. RESOURCE PROTECTION A. Visitor Use 1. Carrying Capacity……………………………………….……………………….12 2. Caving Permits…………………………………………………………………. 13 B. Interpretation 1. Publications............................................................................................ 15 2. Interpretive Tours................................................................................... 16 3. Outreach Programs................................................................................ 16 4. Audio-visual.......................................................................................... 16 5. Visitor Survey....................................................................................... 16 C. Ranger Patrols.......................................................................................................... 17 D. Cave Locations.................................. E. Gates......................................................................................................................... 18 F. Cave Alteration........................................................................................................
    [Show full text]
  • Geologic Processes in the RWMC
    INEL-95/0519 Geologic Processes in the RWMC Area, Idaho National Engineering Laboratory: Implications for Long Term Stability and Soil Erosion at the Radioactive Waste Management Complex W. R. Hackett J. A. Tullis R. P. Smith S. J. Miller T. V. Dechert* P. A. McDaniel* A. L Falen* September 1995 Idaho National Engineering Laboratory Lockheed Martin Idaho Technologies Idaho Falls, Idaho 83415 and WW a Ol University of Idaho College of Agriculture Soil Science Division Moscow, Idaho 83844-2339 Prepared for the U.S. Department of Energy Assistant Secretary for Environmental Management Under DOE Idaho Operations Office Contract DE-AC07-94ID13223 DISTRIBUTION OF THIS DOCUMENT IS UMumrrm DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, make any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document.
    [Show full text]
  • Tree-Ring Investigation of Holocene Flood-Deposited Wood from the Oneida Lake Watershed, New York State
    TREE-RING RESEARCH, Vol. 71(2), 2015, pp. 83–94 DOI: http://dx.doi.org/10.3959/1536-1098-71.2.83 TREE-RING INVESTIGATION OF HOLOCENE FLOOD-DEPOSITED WOOD FROM THE ONEIDA LAKE WATERSHED, NEW YORK STATE IRINA P. PANYUSHKINA1*, STEVEN W. LEAVITT1, EUGENE W. DOMACK2,3, and ALEX C. WIEDENHOEFT4 1Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ, 85721, USA 2Department of Geosciences, Hamilton College, Clinton, NY, 13323, USA 3College of Marine Science, University of South Florida, St. Petersburg, FL, 33701, USA 4Center for Wood Anatomy Research, USDA Forest Products Laboratory, Madison, WI, 53726, USA ABSTRACT Glacial deposition and fluvial/lacustrine sedimentation interact over terrains in central New York State to preserve a history of geological and hydrological events as well as hydroclimatic transitions. The lower reach of Fish Creek draining the eastern watershed of Oneida Lake, NY, is an area with prominent wood remains. This study explores a collection of 52 logs encased in organic-rich deposits exposed by bank erosion at three locations along Fish Creek near Sylvan Beach, NY, with respect to radiocarbon ages, species, and the crossdating potential of tree rings. Radiocarbon ages and successful tree-ring crossdating document what we interpret as seven major hydrologic episodes ca.10 ka (i.e. ca. 10,000 cal yr BP), 7.4 ka, 6.8 ka, 6.4 ka, 5.5 ka, 3.1 ka and 2.2 ka cal BP, during which channel aggradation and tree burial may have been associated with abruptly increased flood frequency and/or high water tables. This pilot study establishes four floating tree-ring records: [1] early Holocene hemlock (Tsuga), mid-Holocene [2] walnut (Juglans sp.) and [3] sycamore (Platanus), and [4] late Holocene elm (Ulmus sp.), with sample sizes of 8–14 series of 55–135 years length.
    [Show full text]