Dust and Pleistocene Ice Ages: Eolian Sediments and Climate Change at Ziegler Reservoir, Snowmass Village, Colorado
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University of Denver Digital Commons @ DU Electronic Theses and Dissertations Graduate Studies 6-1-2014 Dust and Pleistocene Ice Ages: Eolian Sediments and Climate Change at Ziegler Reservoir, Snowmass Village, Colorado Jeffrey S. Honke University of Denver Follow this and additional works at: https://digitalcommons.du.edu/etd Part of the Climate Commons, and the Geology Commons Recommended Citation Honke, Jeffrey S., "Dust and Pleistocene Ice Ages: Eolian Sediments and Climate Change at Ziegler Reservoir, Snowmass Village, Colorado" (2014). Electronic Theses and Dissertations. 293. https://digitalcommons.du.edu/etd/293 This Thesis is brought to you for free and open access by the Graduate Studies at Digital Commons @ DU. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ DU. For more information, please contact [email protected],[email protected]. DUST AND PLEISTOCENE ICE AGES: EOLIAN SEDIMENTS AND CLIMATE CHANGE AT ZIEGLER RESERVOIR, SNOWMASS VILLAGE, COLORADO __________ A Thesis Presented to the Faculty of Natural Sciences and Mathematics University of Denver __________ In Partial Fulfillment of the Requirements for the Degree Master of Arts __________ by Jeffrey S. Honke June 2014 Advisor: Dr. J. Michael Daniels ©Copyright by Jeffrey S. Honke 2014 All Rights Reserved Author: Jeffrey S. Honke Title: DUST AND PLEISTOCENE ICE AGES: EOLIAN SEDIMENTS AND CLIMATE CHANGE AT ZIEGLER RESERVOIR, SNOWMASS VILLAGE, COLORADO Advisor: Dr. J. Michael Daniels Degree Date: June 2014 Abstract The discovery of the Ziegler Reservoir fossil site near Snowmass Village, Colorado presents an opportunity to examine subalpine ecosystem response, during a relatively unknown period, in which climate conditions were similar to present. Fine- grained sediments at Ziegler Reservoir represent continuous deposition between ~140–55 ka (thousand years before present), spanning the close of the Bull Lake glacial period [marine isotope stage (MIS) 6], the Sangamon interglacial (MIS 5) and the early stages of the Pinedale (early Wisconsin) glacial period (MIS 4). Ziegler Reservoir is positioned on top of a ridge, at an elevation of 2705 m, and has a small watershed area (~14 ha), with little evidence of fluvial sediment transport. Particle size distributions, mineralogy, and geochemistry indicate eolian processes were the likely mechanism for deposition of the local, silt-rich and clay-rich sediments that ultimately filled the basin. The presence of clay-rich units (up to three-times more clay than background), is interpreted to represent glacial conditions at two distinct intervals: 1) ~140–134 ka (MIS 6) and 2) ~71–55 ka (MIS 4/3), which correspond to late Bull Lake and early Pinedale glacial periods, respectively. In addition, the absence of clay-rich sediment in the intervening sediments suggests a lack of glacial activity during sub-stages MIS 5d and 5b. In all, the Ziegler Reservoir sedimentary record provides critical information regarding environmental response of high-alpine ecosystems to climate change in the Rocky Mountains during the late Pleistocene. ii Acknowledgements A special thanks to Ansel and Evan Honke for their inspiration. I would also like to thank; Ronna Bowers, Harland Goldstein, Gary Skipp and Kenzie Turner for their assistance with drilling operations and laboratory procedures. I would also like to recognize Jeremy Havens for his assistance with layout. A thanks to fellow graduate students for their assistance in sample collections and thesis development; Nikolai Alvarado, Becky Brice, Sylvia Brady, Alicia Green, Taylor Hafley, Greg Kwoka, Sarah McCall, and Paul Quigley. A special thanks to my advisors; Jeff Pigati (USGS) and Mike Daniels (DU), for their patience and guidance. This study would not have been possible without the support of the Geosciences and Environmental Change Science Center, U.S. Geological Survey, Denver Colorado, and the Denver Museum of Nature and Science. Support for field investigations was also graciously provided through the Charles Redd Center for Western Studies. iii Table of Contents Chapter One: Introduction .................................................................................................. 1 1.1 The Snowmastodon Project ........................................................................ 2 1.2 Purpose of study and thesis questions ......................................................... 7 Chapter Two: Related Literature ...................................................................................... 10 Chapter Three: Study Area ............................................................................................... 15 3.1 Physiography............................................................................................. 15 3.2 Geologic setting ........................................................................................ 15 3.3 Glacial history ........................................................................................... 17 3.4 Current climate and vegetation ................................................................. 19 3.5 Hydrology ................................................................................................. 20 3.6 Stratigraphy ............................................................................................... 21 3.7 Chronology ............................................................................................... 23 Chapter Four: Methods ..................................................................................................... 29 4.1 Field collection.......................................................................................... 29 4.1.1 Ziegler Reservoir bulk samples ..................................................... 29 4.1.2 Ziegler Reservoir core samples ..................................................... 29 4.1.3 Impounding moraine samples ....................................................... 30 4.1.4 Modern dust samples ..................................................................... 30 4.1.5 Dust on Snow sample .................................................................... 33 4.1.6 Mancos Shale samples .................................................................. 38 4.1.7 Provenance samples ...................................................................... 38 4.2 Laboratory methods .................................................................................. 39 4.2.1 Particle size analysis...................................................................... 39 4.2.2 Grain size separations.................................................................... 40 4.2.3 Mineralogy .................................................................................... 41 4.2.4 Geochemistry ................................................................................ 42 Chapter Five: Results ........................................................................................................ 45 5.1 Particle size analysis ................................................................................. 45 5.2 Mineralogy ................................................................................................ 48 5.3 Geochemistry ............................................................................................ 52 iv Chapter Six: Discussion .................................................................................................... 55 6.1 Evidence of eolian transport ..................................................................... 55 6.1.1 Watershed and moraine morphology ............................................ 55 6.1.2 Particle size data ............................................................................ 56 6.2 Evidence of Provenance ............................................................................ 58 6.2.1 Mineralogical data ......................................................................... 61 6.2.3 Rare earth elements ....................................................................... 67 6.3 Evidence of climate change in the Ziegler Reservoir sediments .............. 68 6.3.1 Ziegler Reservoir sediments and Marine Isotope Stages .............. 68 6.3.2 Sedimentation zones and climatic interpretations ......................... 71 Chapter Seven: Conclusions ............................................................................................. 77 References ....................................................................................................................... 80 Appendicies Appendix A Sample collection data ............................................................ 87 Appendix B Particle size data ..................................................................... 91 Appendix C Silt mineralogy data ................................................................ 92 Appendix D INAA data .............................................................................. 96 v List of Figures Figure 1: Ziegler Reservoir study area .......................................................................3 Figure 2: Aerial photograph of excavation site and Locality 43 photo .....................6 Figure 3: Bull Lake glacial extent in Snowmass Creek Valley .................................18 Figure 4: Generalized cross section of Ziegler Reservoir ..........................................22 Figure 5: Composite fine-grain stratigraphy .............................................................24