2000 Annual Science Report
Arizona State University Reporting | JUL 1999 – JUN 2000
Exploring the Living Universe: Origin, Evolution and Distribution of Life in the Solar System
Project Progress
ASU’s commitment to establish a new, cutting edge ion probe facility on campus (Geology Dept.) was met last Fall. The new instrument contributed to the discovery of aqueous alteration processes in carbonaceous meteorites (Co-I Leshin and Post-doc Benedix), which provides an important context for understanding extraterrestrial pre-biotic chemistry. This discovery advanced our goal to determine the nature of conditions on the parent bodies of carbonaceous meteorites.
Another part of the ASU commitment to Astrobiology was met this year with the hire of geomicrobiologist Ferran Garcia-Pichel who represents an important interdisciplinary bridge between Geology, Chemistry and Biology/Microbiology.
Our goal to understand the origin and evolution of photosynthesis (Co-I Blankenship) was advanced this past year with the development of a model system for early cells constructed using an artificial reaction center and an ATP-synthase enzyme incorporated in a liposome. The model successfully carried out high rates light-driven ATP synthesis.
Our goal to understand the potential of hydrothermal environments to produce complex pre-biotic organic compounds (Co-I’s Holloway and O’Day; grad student Vogelsonger) paid off this year with the synthesis of metastable methanol under seafloor hydrothermal conditions, a process predicted by current thermodynamic models.
The Thermal Emission Spectrometer (TES), presently mapping from Mars orbit discovered several deposits of coarsely crystalline (“specular”) hematite (Fe-oxide) which only forms on Earth in the presence of abundant water and usually at elevated temperatures (Co-I Christensen, et al.). This marks an important step in defining potential landing sites for future landed missions for Astrobiology. Remote sensing analog studies for Mars were carried out in Death Valley (Co-I Farmer and Postdoc Moersch) and revealed that a spatial resolution of ~100 m/pixel is required to detect evaporite minerals (carbonates and sulfates) using mid-IR. TES maps at 3 km/pixel, indicating the need to fly higher spatial resolution instruments in the future.
-
PROJECT INVESTIGATORS:
-
PROJECT MEMBERS:
Jack Farmer
Project Investigator
Robert Blankenship
Co-Investigator
Philip Christensen
Co-Investigator
John Cronin
Co-Investigator
Thomas Dowling
Co-Investigator
James Elser
Co-Investigator
William Fagan
Co-Investigator
Ferran Garcia-Pichel
Co-Investigator
Ronald Greeley
Co-Investigator
John Holloway
Co-Investigator
L Knauth
Co-Investigator
David Kring
Co-Investigator
Laurie Leshin
Co-Investigator
David Nelson
Co-Investigator
Peggy O'Day
Co-Investigator
Thomas Sharp
Co-Investigator
Carol Tang
Co-Investigator
James Allen
Collaborator
Carl Bauer
Collaborator
Brad Bebout
Collaborator
George Cooper
Collaborator
David Des Marais
Collaborator
James Farquhar
Collaborator
Wayne Frasch
Collaborator
Peter Gogarten
Collaborator
Jeffery Moersch
Collaborator
Thomas Moore
Collaborator
John Moreau
Collaborator
Beverly Pierson
Collaborator
Sandra Pizzarello
Collaborator
Gary Plumley
Collaborator
Mark Thiemens
Collaborator
Cindy Van Dover
Collaborator
Gretchen Benedix
Postdoc
Victoria Hamilton
Postdoc
Steve Ruff
Postdoc
Alice Baldridge
Graduate Student
Marina Cosarinsky
Graduate Student
Don Crampton
Graduate Student
Darcy Gentleman
Graduate Student
Vanessa Lancaster
Graduate Student
Jason Raymond
Graduate Student
Steve Scotnicki
Graduate Student
Hebe Vanegas-Farfano
Graduate Student
Kenneth Voglesonger
Graduate Student
Teri Williams
Graduate Student
Christophor Rick
Undergraduate Student
-
RELATED OBJECTIVES:
Objective 1.0
Determine whether the atmosphere of the early Earth, hydrothermal systems or exogenous matter were significant sources of organic matter.
Objective 2.0
Develop and test plausible pathways by which ancient counterparts of membrane systems, proteins and nucleic acids were synthesized from simpler precursors and assembled into protocells.
Objective 3.0
Replicating, catalytic systems capable of evolution, and construct laboratory models of metabolism in primitive living systems.
Objective 4.0
Expand and interpret the genomic database of a select group of key microorganisms in order to reveal the history and dynamics of evolution.
Objective 5.0
Describe the sequences of causes and effects associated with the development of Earth's early biosphere and the global environment.
Objective 6.0
Define how ecophysiological processes structure microbial communities, influence their adaptation and evolution, and affect their detection on other planets.
Objective 7.0
Identify the environmental limits for life by examining biological adaptations to extremes in environmental conditions.
Objective 8.0
Search for evidence of ancient climates, extinct life and potential habitats for extant life on Mars.
Objective 9.0
Determine the presence of life's chemical precursors and potential habitats for life in the outer solar system.
Objective 12.0
Define climatological and geological effects upon the limits of habitable zones around the Sun and other stars to help define the frequency of habitable planets in the universe.