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Signs of Life: Sulfur Deposits at Borup Fiord Pass, Canadian Arctic
This page contains archived content and is no longer being updated. At the time of publication, it represented the best available science. However, more recent observations and studies may have rendered some content obsolete.
High in the Canadian Arctic is a glacier-carved valley that is like none other on Earth. Borup Fiord Pass on Ellesmere Island, shown in the top image, is the only known place where sulfur from a natural spring is deposited over ice. The sulfur leaves a pale yellow stain that almost seems to glow in the lower image, a photo taken from a helicopter in July 2006.
The top image is a natural-color satellite view of the spring, acquired by the Advanced Land Imager (ALI) on NASA’s EO-1 satellite on July 6, 2006. Though the sulfur stain is not visible at this scale in photo-like images, another sensor on the satellite, Hyperion, makes measurements in hundreds of wavelengths of light that are invisible to our eyes. Using this hyperspectral data, scientists have mapped the location of sulfur deposits on the ice surface (green outline).
The study of the Arctic sulfur spring is more than a mere curiosity; what scientists learn from it may help us find life elsewhere in the solar system. Near the top of the short list of places in our solar system that might harbor extraterrestrial life is Jupiter’s rocky moon Europa. Smaller than our moon, Europa is covered in water ice that might conceal an ocean of liquid water. Liquid water is a key ingredient for life.
If Europa has an ocean, could there be life in it? Clues could come from dark, non-ice deposits that have been detected on Europa’s icy surface. The dark deposits may be seeping up from the ocean through cracks in the ice, and observations from the Galileo spacecraft suggest that the dark deposits may contain sulfur. Are the deposits on Europa’s ice similar to the one known sulfur deposit over ice on Earth?
At the Borup Pass spring, hydrogen sulfide gas in the water is converted to stable deposits of either elemental sulfur, the most common material in the deposit, or gypsum. The process by which hydrogen sulfide becomes sulfur is complex, and most often occurs when microbes, like bacteria, are present. The very presence of elemental sulfur deposits on the ice in Borup Pass is an indicator that life is likely there. Do the deposits on Europa also contain elemental sulfur?
Scientists at NASA’s Jet Propulsion Laboratory along with colleagues from other organizations used Hyperion data to measure the abundance of elemental sulfur in Borup Pass. All matter radiates energy with a “fingerprint” unique to each chemical element. By measuring these energy fingerprints in Hyperion data, the group estimated the abundance of sulfur and other deposits at the spring.
They also measured the energy fingerprints with a more detailed detector on the ground and took samples of the deposit to analyze concentrations in the lab. Though not perfect, the three types of measurements aligned fairly well. This means that an orbiting sensor like Hyperion could be used to identify chemicals in Europa’s non-ice deposits that may be a sign of extraterrestrial microbial life.
NASA Earth Observatory image created by Jesse Allen and Robert Simmon, using EO-1 ALI data provided courtesy of the NASA EO-1 team. Aerial photograph and Hyperion detection data provided by Damhait Gleeson, NASA JPL. Caption by Holli Riebeek.
A natural-color satellite image and an aerial photograph show a unique glacial valley in the Canadian Arctic, where sulfur deposits on the ice may give scientists insights into how to search for extraterrestrial life.
Gleeson, D.F., Pappalardo, R.T., Grasby, S.E., Anderson, M.S., Beauchamp, B., Castaño, Chein, S.A., Dogget, T., Mandrake, L., and Wagstaff, K.L. (2010, June 15; published online 2010, March 6). Characterization of a sulfur-rich Arctic spring site and field analog to Europa using hyperspectral data. Remote Sensing of Environment, 114 (6), 1297-1311.
McKinnon, W.B. (2004). Europa. World Book at NASA, World Book Online Reference Center. Accessed April 23, 2010.