John A. Baross (born August 27, 1940) is an American marine microbiologist and professor of oceanography and astrobiology at the University of Washington who has made significant discoveries in the field of the microbial ecology of hydrothermal vents and the physiology of thermophilic bacteria and archaea.[1]
Education and academic career
Baross earned Bachelor of Science degrees in Microbiology and Chemistry from San Francisco State University in 1965. He earned an MS and Ph.D. in Microbiology from the University of Washington in 1973. At Oregon State University, he was a postdoctoral researcher (1973-1977), an assistant professor (1977-1983), and an associate professor (1983-1985). He moved to the University of Washington in 1985 and has been a full professor there since 1995. He was one of the founding members of the University of Washington Astrobiology program.[2]
Baross was among the first microbiologists to sample Mt. St. Helens after it erupted in 1980;[10] this research revealed the succession of anaerobic microorganisms in volcanic lakes after the eruption and the importance of the nitrogen cycle in the restoration of the lakes to their former states.[11][12]
Astrobiology
Baross' research focuses on extreme environments, particularly volcanic environments, and implications for the origin of life.[1][13] He was among the first to propose hydrothermal vents as a site for the origin of life.[14][15][16] He has coined the term ‘ribofilm’ – a proto-biofilm that may have acted as the first living organism.[17] Baross advocates the idea that key metabolic pathways, in particular those involving metalloenzymes, are rooted in geochemical reactions on mineral surfaces. He is therefore a major proponent for the exploration of icy moons like Enceladus which was discovered to be geochemically active and may favor the production of essential biomolecules.[18] His recent contributions stress the importance of an environmentally diverse planetary surface with active hydrological and geological cycles as an ideal setting for prebiotic reaction networks.[19]
Baross chaired two National Academy of Sciences task groups on origins of life topics: the Committee on the Origins and Evolution of Life (2000-2004) and the Group on the Limits of Organic Life in the Universe (2004-2007). These groups explored the possibility of a "weird life" based on alternative substrates.[20] He has served on six national and international planetary protection committees. He is the co-author of the textbook "Planets and Life: The Emerging Science of Astrobiology."[21]
^Cone, Joseph (1991). Fire Under the Sea: The Discovery of the Most Extraordinary Environment on Earth--volcanic Hot Springs on the Ocean Floor. Morrow. pp. 196–197. ISBN0688098347.
^Baross, John A.; Hoffman, Sarah E. (1985). "Submarine hydrothermal vents and associated gradient environments as sites for the origin and evolution of life". Origins of Life and Evolution of the Biosphere. 15 (4): 327–345. Bibcode:1985OrLi...15..327B. doi:10.1007/BF01808177. ISSN1573-0875. S2CID4613918.
^Helmreich, Stefan (2009). Alien Ocean: Anthropological Voyages in Microbial Seas. University of California Press. pp. 79–80. ISBN9780520942608.
^Planets and life : the emerging science of astrobiology. Sullivan, Woodruff Turner., Baross, John A. Cambridge: Cambridge University Press. 2007. ISBN978-0-521-82421-7. OCLC144222457.{{cite book}}: CS1 maint: others (link)
^"John Baross". College of the Environment. Retrieved 2021-07-22.