
Roger Buick
· Professor, Earth & Space SciencesUniversity of Washington · Earth and Space Sciences
Active 1972–2026
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About
Professor Roger Buick is a faculty member in the Department of Earth & Space Sciences at the University of Washington, specializing in astrobiology with a focus on the origin and earliest evolution of life on Earth. His research techniques intersect geology, biology, and chemistry, examining the oldest and best-preserved rocks from various locations including the Australian outback, Greenland ice-cap, South African veld, and Canadian woods. His work aims to understand when the main forms of microbial metabolism first arose, how early atmospheric conditions were modulated, and how these factors influenced environmental change in Earth's history. Professor Buick's research encompasses multiple projects such as studying the early evolution of bacterial metabolism through paleontology and stable isotope geochemistry, investigating early atmospheric composition and pressure via mineral and sediment analysis, and analyzing secular trends in marine nutrient fluxes to understand ecosystem evolution. He also explores the early evolution of continental crust through geochemical analysis, and searches for molecular fossils in Precambrian rocks to uncover organic biomarkers that inform the phylogenetic history of microbial ecosystems. His contributions have advanced understanding of Earth's early atmosphere, biosphere, and tectonic development, providing insights into the conditions that fostered the emergence of life and its evolution over billions of years.
Research topics
- Earth science
- Geology
- Geochemistry
- Astrobiology
- Paleontology
- Meteorology
- Physics
- Atmospheric sciences
- Environmental science
- Environmental chemistry
Selected publications
Pervasive aerobic nitrogen cycling in the surface ocean across the Paleoproterozoic Era
Earth and Planetary Science Letters · 2018-08-17 · 106 citations
articleSenior authorTransient surface ocean oxygenation recorded in the ∼2.66-Ga Jeerinah Formation, Australia
Proceedings of the National Academy of Sciences · 2018-07-09 · 78 citations
articleOpen accessSignificance Understanding how and when Earth’s surface became oxygenated is essential for understanding its biogeochemical evolution. Incipient oxygenation of Earth’s surface environments before the Great Oxidation Event (GOE; ∼2.4 Ga) has been well-documented, but the nature of these redox changes, whether protracted or transient, is poorly understood. We present nitrogen isotope ratios, selenium abundances, and selenium isotope ratios from the Jeerinah Formation (∼2.66 Ga; Fortescue Group, We…
Proceedings of the National Academy of Sciences · 2021 · 55 citations
Senior authorCorrespondingsinks, followed by enhanced nutrient supply to the ocean from weathering of volcanic rocks causing increased biological productivity.
Atmospheric CO <sub>2</sub> levels from 2.7 billion years ago inferred from micrometeorite oxidation
Science Advances · 2020 · 34 citations
level indicated by our model result would help resolve how the Late Archean Earth remained warm when the young Sun was ~20% fainter.
Geochimica et Cosmochimica Acta · 2019-12-23 · 27 citations
articleOpen accessSenior author
Recent grants
COLLABORATIVE RESEARCH: Presaging Paleoproterozoic Global Change: Geobiology of the Late Archean Eon
NSF · $80k · 2004–2008
Selenium biogeochemistry as a deep-time redox proxy and biosignature
NSF · $300k · 2009–2014
Frequent coauthors
- 159 shared
Eva E. Stüeken
University of St Andrews
- 88 shared
Michael A. Kipp
- 81 shared
Ariel D. Anbar
University of Louisiana at Lafayette
- 73 shared
Alan J. Kaufman
- 69 shared
Timothy W. Lyons
- 68 shared
Jessica Garvin
- 68 shared
Gail Lee Arnold
The University of Texas at El Paso
- 65 shared
David C. Catling
Earth and Space Research
Labs
Education
- 2000
Ph.D., Astrobiology
University of Washington
- 1994
M.S., Astronomy
University of Washington
- 1991
B.A., Physics
University of California, San Diego
Awards & honors
- Fellow of the Geological Society of America (2019)
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