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300 Pages·2015·28.2 MB·English
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PHYSICAL, METABOLIC, AND ENERGETIC INVESTIGATIONS OF METHANE-METABOLIZING MICROBIAL COMMUNITIES Thesis by Jeffrey Marlow In Partial Fulfillment of the Requirements for the degree of Doctor of Philosophy CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California 2016 (Defended June 5th, 2015) ii © 2015 Jeffrey Marlow All Rights Reserved iii ACKNOWLEDGEMENTS Whatever information of consequence that may be encompassed by this compilation is a testament to the generous network of support I have enjoyed during its completion. Most fundamentally, my family and dear friends, scattered across time zones, have provided critical grounding that has bolstered my faith in both the importance and limits of my scientific pursuits. Administration, staff members, and other researchers across the Caltech campus have helped in ways both seen and unseen to enable a frictionless scientific experience. I greatly appreciate the personal encouragement and scientific insight of all members of the Orphan Lab past and present – especially Jan Haskell, Stephanie Connon, Shana Goffredi, Joshua Steele, Greg Wanger, Connor Skennerton, Anne Dekas, Jennifer Glass, David Case, Derek Smith, Shawn McGlynn, Alexis Pasulka, and Roland Hatzenpichler – as well as other colleagues, most notably Joel Scheingross, Megan Newcombe, James Hemp, Sebastian Kopf, Ryan Hunter, Ajay Limaye, Doug LaRowe, Bethany Ehlmann, and Andrew Thurber. I am very grateful for the logistical, financial, and scientific support of John Grotzinger, Wiebke Ziebis, Lisa Levin, Peter Girguis, and Michael Roukes. Jan Amend has witnessed and shepherded my development as a scientist, from a dishwashing freshman at Washington University to a continuing collaborator in the study of microbial ecosystems. Countless scientific conversations with all of the remarkable colleagues above have shaped my scientific identity and set the groundwork for my future investigations. Financial support from the National Science Foundation’s Graduate Student Fellowship Program, Caltech’s Center for Environmental Microbial Interactions, and the National Research Council have made this work and its dissemination possible. My thesis advisory committee – Doug Rees, Woodward Fischer, Tori Hoehler, Dianne Newman, and Victoria Orphan – has provided generous guidance, overcoming busy schedules to discuss results and prioritize ballooning investigatory ambitions. In particular, Dianne Newman kindled my scientific drive through insightful interrogation and encouraged me to follow empirically testable questions with a focused tenacity. Victoria Orphan led and taught by the most effective means possible, through the quiet stimulation of wonder and awe rather than a fear of insufficiency or unworthiness. Her appreciation that, in its purest form, the curiosity that constitutes the most essential seed of a scientist’s soul knows no bounds, allowed me to cultivate a wide range of interests that has – inevitably – enabled unforeseen scientific opportunities and broadened their ultimate impact. This list is a poor approximation of my indebtedness, but the deep support and prodding intellectual stimulation I have received from the vivacious scientific community in which I find myself inspires a brimless excitement for future questions we will engage and answers we will chase, together. iv v ABSTRACT Understanding the roles of microorganisms in environmental settings by linking phylogenetic identity to metabolic function is a key challenge in delineating their broad-scale impact and functional diversity throughout the biosphere. This work addresses and extends such questions in the context of marine methane seeps, which represent globally relevant conduits for an important greenhouse gas. Through the application and development of a range of culture-independent tools, novel habitats for methanotrophic microbial communities were identified, established settings were characterized in new ways, and potential past conditions amenable to methane-based metabolism were proposed. Biomass abundance and metabolic activity measures – both catabolic and anabolic –demonstrated that authigenic carbonates associated with seep environments retain methanotrophic activity, not only within high-flow seep settings but also in adjacent locations exhibiting no visual evidence of chemosynthetic communities. Across this newly extended habitat, microbial diversity surveys revealed archaeal assemblages that were shaped primarily by seepage activity level and bacterial assemblages influenced more substantially by physical substrate type. In order to reliably measure methane consumption rates in these and other methanotrophic settings, a novel method was developed that traces deuterium atoms from the methane substrate into aqueous medium and uses empirically established scaling factors linked to radiotracer rate techniques to arrive at absolute methane consumption values. Stable isotope probing metaproteomic investigations exposed an array of functional diversity both within and beyond methane oxidation- and sulfate reduction- linked metabolisms, identifying components of each proposed enzyme in both pathways. A core set of commonly occurring unannotated protein products was identified as promising targets for future biochemical investigation. Physicochemical and energetic principles governing anaerobic methane oxidation were incorporated into a reaction transport model that was applied to putative settings on ancient Mars. Many conditions enabled exergonic model reactions, marking the metabolism and its attendant biomarkers as potentially promising targets for future astrobiological investigations. This set of inter-related investigations targeting methane metabolism extends the known and potential habitat of methanotrophic microbial communities and provides a more detailed understanding of their activity and functional diversity. vi TABLE OF CONTENTS Acknowledgements ....................................................................................................... iii Abstract ............................................................................................................................ v Table of Contents ........................................................................................................... vi Introduction ..................................................................................................................... 1 Chapter 1: Carbonate Hosted Methanotrophy Represents an Unrecognized Methane Sink in the Deep Sea Case Study ............................................. 6 Introduction ............................................................................................................... 7 Results ..................................................................................................................... 12 Discussion ............................................................................................................... 21 Methods .................................................................................................................. 31 References ............................................................................................................... 42 Chapter 2: Deuterated Methane: A Novel Approach for Measuring Rates of Biological Methane Oxidation ........................................................................ 47 Introduction ............................................................................................................. 48 Methods .................................................................................................................. 50 Results and Discussion ........................................................................................... 59 Conclusion .............................................................................................................. 74 References ............................................................................................................... 75 Chapter 3: Microbial Abundance and Diversity Patterns Associated with Sediments and Carbonates from the Methane Seep Environments of Hydrate Ridge, OR ................................................................... 78 Introduction ............................................................................................................. 80 Methods .................................................................................................................. 86 Results and Discussion ........................................................................................... 92 Conclusion ............................................................................................................ 112 References ............................................................................................................. 114 Chapter 4: Stable Isotope Probing Metaproteomics Reveals Dynamic Metabolism at Marine Methane Seeps ........................................................ 121 Introduction ........................................................................................................... 122 Methods ................................................................................................................ 125 Results and Discussion ......................................................................................... 128 Conclusion ............................................................................................................ 150 References ............................................................................................................. 152 Chapter 5: The Potential for Biologically Catalyzed Anaerobic Methane Oxidation on Ancient Mars .......................................................................... 160 Introduction ........................................................................................................... 161 Data Selection and Methods ................................................................................. 165 Results ................................................................................................................... 177 Discussion ............................................................................................................. 180 Conclusion ............................................................................................................ 191 References ............................................................................................................. 192 Conclusion ................................................................................................................... 201 Appendix 1: Supplementary Information for Chapter 1 ............................................. 206 vii Appendix 2: Autoendoliths: A Distinct Type of Rock-Hosted Microbial Life .............................................................................................................. 221 Appendix 3: Supplementary Information for Chapter 3 ............................................. 233 Appendix 4: Supplementary Information for Chapter 4 ............................................. 237 Appendix 5: Supplementary Metaproteomic Study of Alternative Electron Acceptors in the Anaerobic Oxidation of Methane ..................................... 273 Appendix 6: Supplementary Information for Chapter 5 ............................................. 286 viii ix 1 I n t r o d u c t i o n Over the last several decades, as exploratory range has broadened and analytical tools have sharpened, our conception of the biosphere’s extent has expanded dramatically. Much of the newly characterized habitat is the province of microorganisms: from the deep subsurface (Whitman et al. 1998) to the upper atmosphere (Wainwright et al. 2003), microbes are increasingly viewed as a pervasive force permeating Earth’s habitable volume. These microscopic denizens are not merely passive footnotes in the saga of planetary evolution and elemental cycling; rather, microbial communities frequently drive such transformations, marshaling their metabolic versatility to produce oxygen (Farquhar et al. 2011), fix nitrogen (Burris & Roberts 1993), degrade organic matter (Middelburg et al. 1993), and access rock-bound metals (Haferburg & Kothe 2007). Researchers have developed a healthy appreciation for microbes’ range, but a wide gap between presence and functional relevance persists, and developing a more detailed understanding of the activity-based roles and relationships of these communities remains an important frontier. The most reliable methods of linking microbial identity to function, which require pure cultures of isolated species, are largely impotent when applied to environmental systems, where the vast majority of organisms are recalcitrant to culturing attempts (e.g., Rappé & Giovannoni 2003; Pace et al. 1986). What’s more, the seemingly critical role of inter-species interactions (Pham & Kim 2012; West et al. 2007) renders pure culture studies imprecise at best and dangerously misleading at worst. In response to the “culturability bottleneck,” two paths have emerged in the quest to understand microbial roles in environmental contexts: characterizing evidence of

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purest form, the curiosity that constitutes the most essential seed of a and potential past conditions amenable to methane-based metabolism .. 2007), the subseafloor sink constitutes an important bulwark against climate change . Sea were found to contain lipids indicative of ANME and SRB; it was
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