John A. Baross | |
---|---|
Born | August 27, 1940 |
Nationality | American |
Alma mater | University of Washington, San Francisco State University |
Spouse | Jody Deming |
Awards | Fellow of the American Academy of Microbiology, 2021 NASA Exceptional Scientific Achievement Medal |
Scientific career | |
Doctoral advisor | John Liston |
Doctoral students | Julie Huber, Matthew O. Schrenk |
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]
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 one of the first to show that thermophilic microbes grow in deep-sea hydrothermal vents, work that involved incubating samples on the research vessel's engine block. [3] [4] [5] His research group has studied microorganisms at Axial Seamount, [6] North Gorda Ridge, [7] and the CoAxial Segment in the Northeast Pacific Ocean, [8] and Lost City Hydrothermal Field. [9]
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]
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]
Baross is a Fellow of the American Academy of Microbiology, [22] chair of the Steering Committee of the International Census of Marine Microbes, [23] and involved in the collection of the hydrothermal vent sulfide chimneys on display at the American Museum of Natural History. [24] He was the 2021 recipient of the NASA Exceptional Scientific Achievement Medal and was the featured scientist for December 2021 in the 2021 NASA Science Calendar. [25]
An extremophile is an organism that is able to live in extreme environments, i.e., environments with conditions approaching or stretching the limits of what known life can adapt to, such as extreme temperature, pressure, radiation, salinity, or pH level.
Hydrothermal vents are fissures on the seabed from which geothermally heated water discharges. They are commonly found near volcanically active places, areas where tectonic plates are moving apart at mid-ocean ridges, ocean basins, and hotspots. The dispersal of hydrothermal fluids throughout the global ocean at active vent sites creates hydrothermal plumes. Hydrothermal deposits are rocks and mineral ore deposits formed by the action of hydrothermal vents.
Karl Otto Stetter is a German microbiologist and authority on astrobiology. Stetter is an expert on microbial life at high temperatures.
Geobiology is a field of scientific research that explores the interactions between the physical Earth and the biosphere. It is a relatively young field, and its borders are fluid. There is considerable overlap with the fields of ecology, evolutionary biology, microbiology, paleontology, and particularly soil science and biogeochemistry. Geobiology applies the principles and methods of biology, geology, and soil science to the study of the ancient history of the co-evolution of life and Earth as well as the role of life in the modern world. Geobiologic studies tend to be focused on microorganisms, and on the role that life plays in altering the chemical and physical environment of the pedosphere, which exists at the intersection of the lithosphere, atmosphere, hydrosphere and/or cryosphere. It differs from biogeochemistry in that the focus is on processes and organisms over space and time rather than on global chemical cycles.
The hydrogen cycle consists of hydrogen exchanges between biotic (living) and abiotic (non-living) sources and sinks of hydrogen-containing compounds.
Abiogenesis is the natural process by which life arises from non-living matter, such as simple organic compounds. The prevailing scientific hypothesis is that the transition from non-living to living entities on Earth was not a single event, but a process of increasing complexity involving the formation of a habitable planet, the prebiotic synthesis of organic molecules, molecular self-replication, self-assembly, autocatalysis, and the emergence of cell membranes. The transition from non-life to life has never been observed experimentally, but many proposals have been made for different stages of the process.
The Endeavour Hydrothermal Vents are a group of hydrothermal vents in the north-eastern Pacific Ocean, located 260 kilometres (160 mi) southwest of Vancouver Island, British Columbia, Canada. The vent field lies 2,250 metres (7,380 ft) below sea level on the northern Endeavour segment of the Juan de Fuca Ridge. In 1982, dredged sulfide samples were recovered from the area covered in small tube worms and prompted a return to the vent field in August 1984, where the active vent field was confirmed by HOV Alvin on leg 10 of cruise AII-112.
Dr. Mary A. Voytek is the director of the National Aeronautics and Space Administration (NASA) Astrobiology Program at NASA Headquarters in Washington, D.C. In 2015, Voytek formed Nexus for Exoplanet System Science (NExSS), a systems science initiative by NASA, to search for life on exoplanets. Voytek came to NASA from the U.S. Geological Survey in Reston, VA, where she headed the USGS Microbiology and Molecular Ecology Laboratory from 1998 to 2009.
Life Investigation For Enceladus (LIFE) was a proposed astrobiology mission concept that would capture icy particles from Saturn's moon Enceladus and return them to Earth, where they could be studied in detail for signs of life such as biomolecules.
The Tanpopo mission is an orbital astrobiology experiment investigating the potential interplanetary transfer of life, organic compounds, and possible terrestrial particles in the low Earth orbit. The purpose is to assess the panspermia hypothesis and the possibility of natural interplanetary transport of microbial life as well as prebiotic organic compounds.
Methanocaldococcussp. FS406-22 is an archaea in the genus Methanocaldococcus. It is an anaerobic, piezophilic, diazotrophic, hyperthermophilic marine archaeon. This strain is notable for fixing nitrogen at the highest known temperature of nitrogen fixers recorded to date. The 16S rRNA gene of Methanocaldococcus sp. FS406-22, is almost 100% similar to that of Methanocaldococcus jannaschii, a non-nitrogen fixer.
Mars habitability analogue environments on Earth are environments that share potentially relevant astrobiological conditions with Mars. These include sites that are analogues of potential subsurface habitats, and deep subsurface habitats.
The earliest known life forms on Earth may be as old as 4.1 billion years according to biologically fractionated graphite inside a single zircon grain in the Jack Hills range of Australia. The earliest evidence of life found in a stratigraphic unit, not just a single mineral grain, is the 3.7 Ga metasedimentary rocks containing graphite from the Isua Supracrustal Belt in Greenland. The earliest direct known life on Earth are stromatolite fossils which have been found in 3.480-billion-year-old geyserite uncovered in the Dresser Formation of the Pilbara Craton of Western Australia. Various microfossils of microorganisms have been found in 3.4 Ga rocks, including 3.465-billion-year-old Apex chert rocks from the same Australian craton region, and in 3.42 Ga hydrothermal vent precipitates from Barberton, South Africa. Much later in the geologic record, likely starting in 1.73 Ga, preserved molecular compounds of biologic origin are indicative of aerobic life. Therefore, the earliest time for the origin of life on Earth is at most 3.5 billion years ago, possibly as early as 4.1 billion years ago — not long after the oceans formed 4.5 billion years ago and after the formation of the Earth 4.54 billion years ago.
The viral shunt is a mechanism that prevents marine microbial particulate organic matter (POM) from migrating up trophic levels by recycling them into dissolved organic matter (DOM), which can be readily taken up by microorganisms. The DOM recycled by the viral shunt pathway is comparable to the amount generated by the other main sources of marine DOM.
The hydrothermal vent microbial community includes all unicellular organisms that live and reproduce in a chemically distinct area around hydrothermal vents. These include organisms in the microbial mat, free floating cells, or bacteria in an endosymbiotic relationship with animals. Chemolithoautotrophic bacteria derive nutrients and energy from the geological activity at Hydrothermal vents to fix carbon into organic forms. Viruses are also a part of the hydrothermal vent microbial community and their influence on the microbial ecology in these ecosystems is a burgeoning field of research.
The deep biosphere is the part of the biosphere that resides below the first few meters of the ocean's surface. It extends 10 kilometers below the continental surface and 21 kilometers below the sea surface, at temperatures that may reach beyond 120 °C (248 °F) which is comparable to the maximum temperature where a metabolically active organism has been found. It includes all three domains of life and the genetic diversity rivals that on the surface.
Rachel Haymon is a marine geologist known for her work linking geological and biological processes occurring at deep-sea hydrothermal vents. In 2005 she was elected a fellow of the Geological Society of America.
Everett L. Shock is an American geochemist and former experimental rock singer and songwriter. He is currently a professor with joint appointments in the School of Earth and Space Exploration and School of Molecular Sciences at Arizona State University. Shock and his research group work within a framework of chemical thermodynamics applied to field, experimental, and theoretical geochemical investigations to understand how geochemical processes provide energy to support microbial life on Earth and potentially on other ocean worlds.
Seamount microbial communities refer to microorganisms living within the surrounding environment of seamounts. Seamounts are often called the hotspot of marine life serving as a barrier that disrupts the current and flow in the ocean, which is referred to as the seamount effect.
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