Roger Everett Summons | |
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Born | [1] Sydney, New South Wales, Australia | 11 June 1946
Alma mater | University of New South Wales |
Scientific career | |
Fields | |
Institutions | |
Thesis | The alkaloids of some Australian and New Guinea plants (1971) |
Doctoral advisors | Emery Gellert J. Ellis |
Website | summons |
Roger Everett Summons FAA FRS (born 11 June 1946) is the Schlumberger Professor of Geobiology at the Massachusetts Institute of Technology and Professor of Geobiology in the Department of Earth, Atmospheric and Planetary Sciences. [2]
Summons’ research spans biogeochemistry, geobiology, and astrobiology. His work employs organic geochemical methods to examine the lipid chemistry of modern and ancient microbes, the isotopic signatures of climate change, and the evolution and origins of life.
Summons was elected a member of the National Academy of Sciences in 2020. [3]
Roger Summons was born on 11 June 1946 in Sydney, Australia, [1] and attended Lithgow High School. He earned his B.Sc. (Honours Class I) in 1968 [4] and Ph.D. in 1971 in organic chemistry from the Wollongong University College of the University of New South Wales. [5] [6] This institution is now the University of Wollongong. [7] Summons' doctoral supervisors were professors Emery Gellert and J. Ellis. [5] Following graduation, Summons completed a two-year fellowship in the genetics department, Stanford University, from 1972 to 1973 before starting postdoctoral and research fellowships in the Research School of Chemistry at the Australian National University. At Stanford, Summons worked under the direction of Alan Duffield and Joshua Lederberg. [8]
Before joining MIT as a professor of geobiology in 2001, he held appointments at the Australian National University’s Research School of Biological Sciences from 1977 to 1983, and at Geoscience Australia, Canberra from 1983 to 2001, where he led a research team that focused on the characterization of the biogeochemical carbon cycle and the nature and habitat of Australian petroleum. [9]
Summons is particularly known for the application of organic geochemical techniques to sediments of Precambrian age and modern microbes in order to increase the understanding of the early evolution of life on Earth. Summons is a member of the editorial boards of the peer-reviewed scientific journals Astrobiology, Geobiology, and Palaeoworld since their inception. He also served as associate editor of the peer-reviewed scientific journal Geochimica et Cosmochimica Acta from 1995 to 2006.
From 2003 to 2007, Summons served on three committees of the US National Research Council including the Committee on Origin and Evolution of Life, the Committee on Limits of Life, and the Committee on Mars Astrobiology. Summons served as NASA co-chair of the organic contamination panel for the Mars 2020 Rover, [10] and was a member of the NASA Astrobiology Institute Executive Council from 2008 to 2017. During that time, he led the Foundations of Complex Life, the MIT NASA Astrobiology Institute team which interrogated the environmental, ecological, and genetic factors that lead to the evolution of complex life. [11] [12]
In addition to actively teaching both graduate and undergraduate courses at MIT, Summons is engaged as a collaborator with the search for organics on Mars as a member of the SAM Team of NASA's Mars Science Laboratory mission. He is also an investigator in the Simons Collaboration on the Origins of Life (SCOL). [13]
Astrobiology is a scientific field within the life and environmental sciences that studies the origins, early evolution, distribution, and future of life in the universe by investigating its deterministic conditions and contingent events. As a discipline, astrobiology is founded on the premise that life may exist beyond Earth.
Allan Hills 84001 (ALH84001) is a fragment of a Martian meteorite that was found in the Allan Hills in Antarctica on December 27, 1984, by a team of American meteorite hunters from the ANSMET project. Like other members of the shergottite–nakhlite–chassignite (SNC) group of meteorites, ALH84001 is thought to have originated on Mars. However, it does not fit into any of the previously discovered SNC groups. Its mass upon discovery was 1.93 kilograms (4.3 lb).
The possibility of life on Mars is a subject of interest in astrobiology due to the planet's proximity and similarities to Earth. To date, no proof of past or present life has been found on Mars. Cumulative evidence suggests that during the ancient Noachian time period, the surface environment of Mars had liquid water and may have been habitable for microorganisms, but habitable conditions do not necessarily indicate life.
A biosignature is any substance – such as an element, isotope, or molecule – or phenomenon that provides scientific evidence of past or present life. Measurable attributes of life include its complex physical or chemical structures and its use of free energy and the production of biomass and wastes. A biosignature can provide evidence for living organisms outside the Earth and can be directly or indirectly detected by searching for their unique byproducts.
In 1976 two identical Viking program landers each carried four types of biological experiments to the surface of Mars. The first successful Mars landers, Viking 1 and Viking 2, then carried out experiments to look for biosignatures of microbial life on Mars. The landers each used a robotic arm to pick up and place soil samples into sealed test containers on the craft.
The NASA Astrobiology Institute (NAI) was established in 1998 by the National Aeronautics and Space Administration (NASA) "to develop the field of astrobiology and provide a scientific framework for flight missions." In December 2019 the institute's activities were suspended.
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.
γ-Carotene (gamma-carotene) is a carotenoid, and is a biosynthetic intermediate for cyclized carotenoid synthesis in plants. It is formed from cyclization of lycopene by lycopene cyclase epsilon. Along with several other carotenoids, γ-carotene is a vitamer of vitamin A in herbivores and omnivores. Carotenoids with a cyclized, beta-ionone ring can be converted to vitamin A, also known as retinol, by the enzyme beta-carotene 15,15'-dioxygenase; however, the bioconversion of γ-carotene to retinol has not been well-characterized. γ-Carotene has tentatively been identified as a biomarker for green and purple sulfur bacteria in a sample from the 1.640 ± 0.003-Gyr-old Barney Creek Formation in Northern Australia which comprises marine sediments. Tentative discovery of γ-carotene in marine sediments implies a past euxinic environment, where water columns were anoxic and sulfidic. This is significant for reconstructing past oceanic conditions, but so far γ-carotene has only been potentially identified in the one measured sample.
Extraterrestrial material refers to natural objects now on Earth that originated in outer space. Such materials include cosmic dust and meteorites, as well as samples brought to Earth by sample return missions from the Moon, asteroids and comets, as well as solar wind particles.
Bruce Norman Runnegar is an Australian-born paleontologist and professor at UCLA. His research centers on using the fossil record to determine how, where, and when life originated and evolved. He has published on a wide variety of topics, including the phylogeny of molluscs, Dickinsonia fossils and oxygen levels, and molecular clock techniques.
Yamato 000593 is the second largest meteorite from Mars found on Earth. Studies suggest the Martian meteorite was formed about 1.3 billion years ago from a lava flow on Mars. An impact occurred on Mars about 11 million years ago and ejected the meteorite from the Martian surface into space. The meteorite landed on Earth in Antarctica about 50,000 years ago. The mass of the meteorite is 13.7 kg (30 lb) and has been found to contain evidence of past water alteration.
Katherine H. Freeman is the Evan Pugh University Professor of Geosciences at Pennsylvania State University and a co-editor of the peer-reviewed scientific journal, Annual Review of Earth and Planetary Sciences. Her research interests are organic geochemistry, isotopic biogeochemistry, paleoclimate and astrobiology.
John Michael Hayes was an American oceanographer. He worked at Indiana University Bloomington, and Woods Hole Oceanographic Institution in Woods Hole, Massachusetts.
Marilyn L. Fogel was an American geo-ecologist and Professor of Geo-ecology at UC Riverside in Riverside, California. She is known for her research using stable isotope mass spectrometry to study a variety of subjects including ancient climates, biogeochemical cycles, animal behavior, ecology, and astrobiology. Fogel served in many leadership roles, including Program Director at the National Science Foundation in geobiology and low-temperature geochemistry.
Dawn Yvonne Sumner is an American geologist, planetary scientist, and astrobiologist. She is a professor at the University of California, Davis. Sumner's research includes evaluating microbial communities in Antarctic lakes, exploration of Mars via the Curiosity rover, and characterization of microbial communities in the lab and from ancient geologic samples. She is an investigator on the NASA Mars Science Laboratory (MSL) and was Chair of the UC Davis Department of Earth & Planetary Sciences from 2014 to 2016. She is Fellow of the Geological Society of America.
Tanja Bosak is a Croatian-American experimental geobiologist who is currently an associate professor in the Earth, Atmosphere, and Planetary Science department at the Massachusetts Institute of Technology. Her awards include the Subaru Outstanding Woman in Science Award from the Geological Society of America (2007), the James B. Macelwane Medal from the American Geophysical Union (2011), and was elected an AGU fellow (2011). Bosak is recognized for her work understanding stromatolite genesis, in addition to her work in broader geobiology and geochemistry.
The reported presence of methane in the atmosphere of Mars is of interest to many geologists and astrobiologists, as methane may indicate the presence of microbial life on Mars, or a geochemical process such as volcanism or hydrothermal activity.
Jennifer Eigenbrode is an interdisciplinary astrobiologist who works at NASA's Goddard Space Flight Center. She specializes in organic chemistry, geology, and organic bio-geochemistry of martian and ocean-world environments.
Ruth E. Blake is an American geochemist and environmental scientist. She is a professor at Yale University in earth & planetary sciences, environmental studies, and chemical & environmental engineering. Blake's work focuses on marine biogeochemical processes, paleoclimate, astrobiology, and stable isotope geochemistry.
Susannah M. Porter is an American paleontologist and geobiologist who studies the early evolution of eukaryotes, the early Cambrian fossil record of animals, and the evolution of skeletal biomineralization. She is currently a professor at the University of California, Santa Barbara. Porter is a Fellow of the Paleontological Society. She has received national recognition awards from the Geological Society of America.
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