Visit our keyboard shortcuts docs for details
Learn about these amazing organisms that live in some of the hottest environment on earth—including in Yellowstone's hydrothermal features.
The hydrothermal features of Yellowstone are magnificent evidence of Earth’s volcanic activity. Amazingly, they are also habitats in which microscopic organisms called thermophiles—“thermo” for heat, “phile” for lover—survive and thrive.
Grand Prismatic Spring at Midway Geyser Basin is an outstanding example of this dual characteristic. Visitors marvel at its size and brilliant colors. Along the boardwalk we cross a vast habitat for thermophiles. Nourished by energy and chemical building blocks available in the hot springs, microbes construct vividly colored communities. Living with these microscopic life forms are larger examples of life in extreme environments, such as mites, flies, spiders, and plants.
People for thousands of years likely have wondered about these extreme habitats. The color of Yellowstone’s superheated environments certainly caused geologist Walter Harvey Weed to pause and think, and even question scientists who preceded him. In 1889, he wrote:
There is good reason to believe that the existence of algae of other colors, particularly the pink, yellow and red forms so common in the Yellowstone waters, have been overlooked or mistaken for deposits of purely mineral matter.
Today, many scientists study Yellowstone’s thermophiles. Some of these microbes are similar to the first life forms capable of photosynthesis—using sunlight to convert water and carbon dioxide to oxygen, sugars, and other by-products. These life forms, called cyanobacteria, began to create an atmosphere that would eventually support human life. Cyanobacteria are found in some of the colorful mats and streamers of Yellowstone’s hot springs.
Thermophiles in the Tree of Life
In the last few decades, microbial research has led to a revised tree of life, far different from the one taught before. The new tree combines animal, plant, and fungi in one branch. The other two branches consist solely of microorganisms, including an entire branch of microorganisms not known until the 1970s—Archaea.
Dr. Carl Woese first proposed this “tree” in the 1970s. He also proposed the new branch, Archaea, which includes many microorganisms formerly considered bacteria. The red line links the earliest organisms that evolved from a common ancestor. These are all hyperthermophiles, which thrive in water above 176°F (80°C), indicating life may have arisen in hot environments on the young earth.
Relevance to Yellowstone
Among the earliest organisms to evolve on Earth were microorganisms whose descendants are found today in extreme high-temperature, and in some cases acidic, environments, such as those in Yellowstone. Their history exhibits principles of ecology and ways in which geologic processes might have influenced biological evolution.
Other life forms—the Archaea —predated cyanobacteria and other photosynthesizers. Archaea can live in the hottest, most acidic conditions in Yellowstone; their relatives are considered among the very earliest life forms on Earth.
Yellowstone’s thermophiles and their environments provide a living laboratory for scientists, who continue to explore these extraordinary organisms. They know many mysteries of Yellowstone’s extreme environments remain to be revealed.
Regardless of scientific advances, visitors and explorers in Yellowstone can still relate to something else Weed said about Yellowstone, more than a century ago:
The vegetation of the acid waters is seldom a conspicuous feature of the springs. But in the alkaline waters that characterize the geyser basins, and in the carbonated, calcareous waters of the Mammoth Hot Springs, the case is otherwise, and the red and yellow tinges of the algae combine with the weird whiteness of the sinter and the varied blue and green of the hot water to form a scene that is, without doubt, one of the most beautiful as well as one of the strangest sights in the world.
American Society for Microbiology: micronow.org
Allen, E. T., Arthur L. Day, and H.E. Merwin. 1935. Hot springs of the Yellowstone national park. [Washington]: Carnegie institution of Washington.
Brock, T.D. 1994. Life at High Temperatures. Yellowstone Association/Mammoth, WY.
Brock, Thomas D. 1995. The road to Yellowstone and beyond. Annual Review of Microbiology. 49
Dyer, B.D. 2003. A field guide to bacteria. Ithaca, NY: Cornell University Press.
Franke, M.A, et. al. 2013. Genetic Diversity in Yellowstone Lake: The Hot and Cold Spots. Yellowstone Science 21 (1): 6-22.
Fouke. B.W. 2011 . Hot-spring Systems Geobiology: abiotic and biotic influences on travertine formation at Mammoth Hot Springs, Yellowstone National Park, USA. Sedimentology. 58: 170-219.
Hamilton, T.L. et. al. 2012. Environmental constraints defining the distribution, composition, and evolution of chlorophototrophs in thermal features of Yellowstone National Park. Geobiology. (10) 3: 236-249.
Inskeep WP , et. al. 2013. The YNP metagenome project: environmental parameters responsible for microbial distribution in theYellowstone. Frontiers in Microbiology. 00067.
Klatt, C. G., et. al. 2011. Community ecology of hot spring cyanobacterial mats: predominant populations and their functional potential. ISME Journal. 5(8): 1262–1278.
Marquez, Luis et al. 2007. A virus in a fungus in a plant: 3-way symbiosis required for thermal tolerance. Science 315 (5811): 513–515.
Qin, J., C.R. Lehr, C. Yuan, X. C. Le, T. R. McDermott, and B. P. Rosen. Biotransformation of arsenic by a Yellowstone thermoacidophilic eukaryotic alga. Proceedings of the National Academy of Sciences of the United States of America. 106 (13): 5213.
Reysenbach, A.L., and Shock, E. L. 2002 . Merging Genomes with Geochemistry in Hydrothermal Ecosystems. Science. 296: 1077-1082.
Sheehan, K.B. et al. 2005. Seen and unseen: discovering the microbes of Yellowstone. Guilford, Conn: Falcon.
Snyder, J.C. et. al. 2013. Functional interplay between a virus and the ESCRT machinery in Archaea. Proceedings of the National Academy of Sciences. 110 (26) 10783-10787.
Spear, J. R. et. al. 2005. Hydrogen and bioenergetics in the Yellowstone geothermal ecosystem. Proceedings of the National Academy of Sciences. 102 (7) 2555-2560.
Steunou A.S., et. al. 2008. Regulation of nif gene expression and the energetics of N2 fixation over the diel cycle in a hot spring microbial mat. ISME Journal. (4):364-78.
Takacs-Vesbach, C., et al. 2013. Metagenome sequence analysis of filamentous microbial communities obtained from geochemically distinct geothermal channels reveals specialization of three aquificales lineages. Frontiers Research Foundation.
Thermal Biology Institute of Montana State University: http://tbi.montana.edu/
Ward, D.M., Castenholz, D.W., and Miller, S.R. 2012. Cyanobacteria in Geothermal Habitats. In Brian A. Whitton, ed. Ecology of cyanobacteria II: their diversity in space and time. Dordrecht: Springer
Last updated: December 14, 2018