Series Data from Flathead Lake Montana: Implications for Late Pleistocene and Holocene Paleoclimate
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University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2006 Acquisition and evaluation of sedimentologic paleomagnetic and geochemical time -series data from Flathead Lake Montana: Implications for late Pleistocene and Holocene paleoclimate Michael Sperazza The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Sperazza, Michael, "Acquisition and evaluation of sedimentologic paleomagnetic and geochemical time -series data from Flathead Lake Montana: Implications for late Pleistocene and Holocene paleoclimate" (2006). Graduate Student Theses, Dissertations, & Professional Papers. 9599. https://scholarworks.umt.edu/etd/9599 This Dissertation is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. Maureen and Mike MANSFIELD LIBRARY The University of Montana Permission is granted by the author to reproduce this material in its entirety, provided that this material is used for scholarly purposes and is properly cited in published works and reports. **Please check "Yes" or "No" and provide signature Yes, I grant permission No, I do not grant permission Author's Signature: Date: Any copying for commercial purposes or financial gain may be undertaken only with the author's explicit consent. 8/98 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ACQUISITION AND EVALUATION OF SEDIMENTOLOGIC, PALEOMAGNETIC, AND GEOCHEMICAL TIME-SERIES DATA FROM FLATHEAD LAKE, MONTANA: IMPLICATIONS FOR LATE PLEISTOCENE AND HOLOCENE PALEOCLIMATE by Michael Sperazza B. S., University of Colorado, Boulder, Colorado 1980 M. A., University of Montana, Missoula, Montana 2000 Presented in partial fulfillment of the requirements for the degree of Doctor of Philosophy The University of Montana May 2006 Approved by: /fc- S. Chairperson Dean, Graduate School S- 2Ss> -QL Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 3231692 INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. ® UMI UMI Microform 3231692 Copyright 2006 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, Ml 48106-1346 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Sperazza, Michael, Ph.D., May 2006 Geology Acquisition and Evaluation of Sedimentologic, Paleomagnetic, and Geochemical Time- Series Data from Flathead Lake, Montana: Implications for Late Pleistocene and Holocene Paleoclimate. Chairperson: Dr. Marc S. Hendrix The main objective of this research was to examine a suite of time-series proxy data for potential use in the reconstruction of post Last Glacial Maximum climate history for the northern US Rocky Mountain region. I sought to test the hypothesis that data derived from sediments within a very large watershed (>18,000 km2) could provide centennial scale resolution when applied to a basin with multiple climate environs. In this study, I utilized naturally occurring lacustrine sediments from Flathead Lake, Montana to evaluate paleoclimate implications, using a variety of physical, mineralogical, and geochemical data with calculated uncertainty. The results of this research include: 1) development and testing of a methodology for utilizing laser diffraction to determine size fractions of very fine-grained naturally occurring sediments; 2) quantification of methodological uncertainty for paleomagnetic secular variation when used as a chronostratigraphic tool in lacustrine settings; 3) establishment of methodological uncertainty for grain size, mineralogical, and certain geochemical time-series data sets; and 4) evaluation of grain size, mineralogical, carbon/nitrogen, and various elemental analyses and their respective uncertainties for use in paleoclimate reconstructions. ii Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PREFACE FORWARD Lake sediment records have long been exploited as a source of time-series data for elucidating past climate changes, because lakes respond quickly to environmental change and may be characterized by long periods of uninterrupted sedimentation. Interpreting ancient climates from lacustrine sediments is achieved by the development of time-series data sets for variable parameters, called proxies, within natural records. A proxy data set is utilized as a substitute for one or more climatic, environmental, or physical condition that existed in the past, but cannot be measured directly. Proxies are presumed to vary predictably with changing climate and so commonly are inferred to represent a record of climate change. Accurate calibration and discernment of these data is essential before they can be used to understand and predict modern and ancient climate variability. In this dissertation, I collected time-series data from sediment cores recovered in Flathead Lake, Montana. My focus was to quantify the limitations and resolution of the data and to examine proxy variations and uncertainty that can potentially be utilized in paleoclimate reconstructions. Chapter 1, entitled “High-Resolution Particle Size Analysis of Naturally Occurring Very Fine-Grained Sediment through Laser Diffractometry” has been published in the Journal of Sedimentary Research. This paper covers the establishment and testing of operational methods for determining grain size using laser diffraction techniques. The chapter iii Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. quantifies uncertainty and the variability of sampling preparation, operational settings and optical properties. Chapter 2, entitled “Assessment of Paleomagnetic Secular Variation Correlation and Establishment of a Chronostratigraphic Model for Late Pleistocene and Holocene Lacustrine Sediments of Core 9P from Flathead Lake, Montana” evaluates chronological methods applied to core FL-00-9P. A detailed assessment of paleomagnetic secular variation is presented that constrains procedural variations and quantifies uncertainty. A shortened version of this chapter is in preparation for publication. Chapter 3, entitled “Examination of Potential Paleoclimate Proxies for Large Open Lacustrine Systems: Late Pleistocene and Holocene Sedimentary Record, Flathead Lake, Montana” is an analyses of grain size, mineralogy, and carbon / nitrogen as paleoclimate proxies. The chapter tests proxy resolution and reviews the connection of each to climate change. Potential limitations of each proxy are considered, including uncertainty and external forcing, such as topography, watershed, and sediment redistribution. The chapter concludes with a brief interpretation of climate change, considering uncertainty, for the proxies acquired from Flathead Lake. Various portions of this chapter will be published, including an expanded analysis comparing proxies from other high latitude oligotrophic lakes. iv Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ACKNOWLEDGEMENTS A project so broad scoped, such as this research, would not be successful without the assistance of a number of individuals and institutions that were instrumental in assisting me with my data collection and the completion of this project. I would like to start by thanking Dr. Marc Hendrix my Committee Chair for his inspiration, motivation, and patient review of my data and articles. I have a special appreciation to Committee member Dr. Johnnie Moore for his challenging perspectives, knowledgeable comments, and laboratory assistance. I give my thanks and gratitude to Dr. Joel Harper, Dr. Jim Sears, and Dr. Randell Skelton, the rest of my Committee, for their reviews of my dissertation and serving on my committee, and Dr. Gray Thompson and Dr. Thomas Foor for their reviews of my documents and comprehensive exams. The data analyses could not be preformed without material to process and I greatly appreciate the assistance of the University of Minnesota, Limnological Research Center (LRC) for the coring barge and equipment, and for the use of their state of the art facilities to initially process and photograph the recovered cores. I would like to give a personal thanks to Dr. Emi Ito for allowing my use of the facility and Dr. Doug Schnurrenberger, Amy Myrbo, Chad Wittkop, Anders Noren, and Paul Wagner (now University of