Thermokarst and Wildfire
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University of Vermont ScholarWorks @ UVM Graduate College Dissertations and Theses Dissertations and Theses 2015 Thermokarst And Wildfire: Effects Of Disturbances Related To Climate Change On The Ecological Characteristics And Functions Of Arctic Headwater Streams Julia Rose Larouche University of Vermont Follow this and additional works at: https://scholarworks.uvm.edu/graddis Part of the Ecology and Evolutionary Biology Commons Recommended Citation Larouche, Julia Rose, "Thermokarst And Wildfire: Effects Of Disturbances Related To Climate Change On The cE ological Characteristics And Functions Of Arctic Headwater Streams" (2015). Graduate College Dissertations and Theses. 520. https://scholarworks.uvm.edu/graddis/520 This Dissertation is brought to you for free and open access by the Dissertations and Theses at ScholarWorks @ UVM. It has been accepted for inclusion in Graduate College Dissertations and Theses by an authorized administrator of ScholarWorks @ UVM. For more information, please contact [email protected]. THERMOKARST AND WILDFIRE: EFFECTS OF DISTURBANCES RELATED TO CLIMATE CHANGE ON THE ECOLOGICAL CHARACTERISTICS AND FUNCTIONS OF ARCTIC HEADWATER STREAMS A Dissertation Presented by Julia R. Larouche to The Faculty of the Graduate College of The University of Vermont In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Specializing in Natural Resources May, 2015 Defense Date: March 16, 2015 Dissertation Examination Committee: William B. Bowden, Ph.D., Advisor Shelly A. Rayback, Ph.D., Chairperson Beverley C. Wemple, Ph.D. Paul R. Bierman, Ph.D. Benjamin T. Crosby, Ph.D. Cynthia J. Forehand, Ph.D., Dean of the Graduate College ABSTRACT The Arctic is warming rapidly as a result of global climate change. Permafrost – permanently frozen ground – plays a critical role in shaping arctic ecosystems and stores nearly one half of the global soil organic matter. Therefore, disturbance of permafrost will likely impact the carbon and related biogeochemical processes on local and global scales. In the Alaskan Arctic, fire and thermokarst (permafrost thaw) have become more common and have been hypothesized to accelerate the hydrological export of inorganic nutrients and sediment, as well as biodegradable dissolved organic carbon (BDOC), which may alter ecosystem processes of impacted streams. The biogeochemical characteristics of two tundra streams were quantified several years after the development of gully thermokarst features. The observed responses in sediment and nutrient loading four years after gully formation were more subtle than expected, likely due to the stabilization of the features and the dynamics controlling the hydrologic connectivity between the gully and the stream. The response of impacted streams may depend on the presence of water tracks, particularly their location in reference to the thermokarst and downslope aquatic ecosystem. We found evidence of altered ecosystem structure (benthic standing stocks, algal biomass, and macroinvertebrate composition) and function (stream metabolism and nutrient uptake), which may be attributable to the previous years’ allochthonous gully inputs. The patterns between the reference and impacted reaches were different for both stream sites. Rates of ecosystem production and respiration and benthic chlorophyll-a in the impacted reaches of the alluvial and peat-lined streams were significantly lower and greater, respectively, compared to the reference reaches, even though minimal differences in sediment and nutrient loading were detected. Rates of ammonium and soluble reactive phosphorus uptake were consistently lower in the impacted reach at the alluvial site. The observed differences in metabolism, nutrient uptake and macroinvertebrate community composition suggest that even though the geochemical signal diminished, gully features may have long-lasting impacts on the biological aspects of downstream ecosystem function. In a separate study, a suite of streams impacted by thermokarst and fire were sampled seasonally and spatially. Regional differences in water chemistry and BDOC were more significant than the influences of fire or thermokarst, likely due to differences in glacial age and elevation of the landscape. The streams of the older (>700 ka), lower elevation landscape contained higher concentrations of dissolved nitrogen and phosphorus and DOC and lower BDOC compared to the streams of the younger (50-200 ka) landscapes that had lower dissolved nutrient and DOC quantity of higher biodegradability. The findings in this dissertation indicate that arctic stream ecosystems are more resilient than we expected to small-scale, rapidly stabilizing gully thermokarst features and disturbance caused by fire. Scaling the results of these types of studies should consider the size of thermokarst features in relation to the size of impacted rivers and streams. It remains to be determined how general permafrost thaw will affect the structure and function of arctic streams in the future. CITATIONS Material from this dissertation has been submitted for publication to Journal of Geophysical Research Letters Biogeosciences on September 9, 2014 in the following form: Larouche, J.R., Bowden, W.B., Flinn, M.B., Kampman, J.R. Impacts of a thermo- erosional gully on ecosystem structure and function of an arctic alluvial tundra stream, North Slope, Alaska. Journal of Geophysical Research Letters Biogeosciences. Material from this dissertation has been submitted for publication to Journal of Biogeosciences on January 24, 2015 in the following form: Larouche, J.R., Abbott, B.W., Bowden, W.B., Jones, J.B. The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams. Journal of Biogeosciences. ii DEDICATION For Ted and Michael Leaf, each equally my love and joy. iii ACKNOWLEDGEMENTS Throughout this endeavor I have received support and encouragement from a great number of individuals. I would like to express my deep appreciation and gratitude to my advisor, Dr. William ‘Breck’ Bowden, for the mentorship and encouragement he provided me from my first trip to Alaska a decade ago, through to completion of this degree. His guidance has made this a thought-provoking and rewarding journey; his love for science and the field of arctic ecology is truly an inspiration to many. I would like to thank my committee members, Drs. Shelly Rayback, Beverley Wemple, Paul Bierman, and Benjamin Crosby, for their friendly guidance and valuable suggestions that each of them offered to me over the years. Dr. Michael Flinn provided much needed encouragement, statistical advice, not to mention the help he gave me wrangling a colossal salmon on a gravel bar of the Kelly River. I am indebted to my field assistants, Colin Penn and Pat Tobin, who were dedicated, industrious, comical, thoughtful individuals. Other wonderful people and colleagues who have helped in the field and in the laboratory: Josh Benes, Malcolm Herstand, Alan Howard, Lauren Koenig, Alea Tuttle, Elissa Schuett, Lisle Snyder, Joel Tilley, and Genna Waldvogel. I am truly fortunate to have worked with such a talented group of professors and graduate students with the ARCSS/TK team – Ben Abbott, Andrew Balser, Andres Baron, Sarah Godsey, and Jeff Kampman are now friends and colleagues. I thank the BWRL group, particularly Joe Bartlett and Joel Nipper, for the hydrological correspondence during and after my time in Vermont. Jason Stuckey, Randy Fulweber, and Jorge Noguera have provided valuable GIS analyses and mapping. I would iv like to acknowledge my funding source, the National Science Foundation, and the staff of the Toolik Field Station and National Park Service for logistical support. To my fellow academic goddesses: Courtney, Becky, Pooja, Morgan, and Val, and to the Ghouls and my Wombs, thank you for your love, perspectives, reassurance and friendships during and beyond this journey. Ashlie Dyer, an amazing individual who cared for my son in the early months of his life while I finished up writing. Lynne and Skip Auch were integral with their love and support in this last year. I would be remiss if I didn’t acknowledge those who reside in my heart day in and day out. I thank my parents, Michael Larouche and Martha Sullivan, and sister, Renée D’Agata, for the constant love and for supporting my pursuits in life. Finally, to my husband, Ted Auch, whose endless love, devotion, nourishment, friendship and editing made it possible for me to complete this dissertation and to my little Michael Leaf, I look forward to our visit to the tundra together. v TABLE OF CONTENTS Page CITATIONS .................................................................................................................. ii DEDICATION .............................................................................................................. iii ACKNOWLEDGEMENTS ........................................................................................... iv LIST OF TABLES ...................................................................................................... viii LIST OF FIGURES ........................................................................................................ x CHAPTER 1: BACKGROUND .................................................................................... 1 1.1 Introduction ........................................................................................................ 1 1.2 Disturbance in