RISE was part of the RITA (Rivera-Tamayo expeditions) project, which included submersible investigations (CYAMEX) at 21° N and at the Tamayo Fracture zone at the mouth of the Gulf of California. The RITA project used the French submersible CYANA on the CYAMEX expeditions. CYANA dives at 21° N occurred in 1978, one year prior to the RISE expedition.
American, French, and Mexican biologists, geologists, and geophysicists participated in both the RISE and RITA expeditions. The RISE expedition was directed by scientists at the Scripps Institution of Oceanography, part of the University of California, San Diego. Project leaders were Fred Spiess and Ken Macdonald. Woods Hole Oceanographic Institution provided the ALVIN and its support tender the catamaran Lulu. Scripps provided surface survey vessels the Melville and New Horizon. The expedition took place during March to May 1979. The RITA Project was directed by French scientists and was led by Jean Francheteau.
The discovery of biological communities at low temperature warm vents at 21°N, populated by a benthic community the same or similar to that discovered at the Galapagos spreading center, established that life forms found at the Galapagos were not unique. Further, the significance of discovering at the Galapagos site and 21°N of a chemosynthetic ecosystem that was not dependent on sunlight, existed at high pressures, and was based on chemicals emitted via volcanism, provided a model for how life could have originated on Earth.
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Martin, William; Baross, John; Kelley, Deborah; Russell, Michael J. (2008). "Hydrothermal vents and the origin of life". Nature Reviews Microbiology. 6 (11): 805–814. doi:10.1038/nrmicro1991. ISSN 1740-1526. PMID 18820700. S2CID 1709272. /wiki/Doi_(identifier)
Chemistry of seabed's hot vents could explain emergence of life. Astrobiology Magazine 27 April 2015. https://web.archive.org/web/20150905234013/http://www.astrobio.net/topic/origins/origin-and-evolution-of-life/chemistry-of-seabeds-hot-vents-could-explain-emergence-of-life/