searching for silicate bioweathering on earth and mars martin fisk, oregon state university michael...
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![Page 1: Searching for Silicate Bioweathering on Earth and Mars Martin Fisk, Oregon State University Michael Storrie-Lombardi, Kinohi Institute contributors Radu](https://reader035.vdocument.in/reader035/viewer/2022062409/5697bfe21a28abf838cb476c/html5/thumbnails/1.jpg)
Searching for Silicate Bioweathering
on Earth and MarsMartin Fisk, Oregon State
University
Michael Storrie-Lombardi, Kinohi Institute
contributors
Radu Popa, Portland State University
Olivia Mason, Oregon State University
Ed Vicenzi, Smithsonian Institution
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Pillow Lavas
PhotoJonathan Kaye,
UW
PhotoBill Chadwick,
NOAA
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Probabilistic Classification of Biotic Alteration in Basalts
Elemental Abundance Signatures for Abiotic & Biotic Alteration of Ocean Basalts
[Na, Mg, Al, Si, P, Cl, K, Ca, Ti, Mn, & Fe]
Storrie-Lombardi, M. C. and Fisk, M. R. (2004) Elemental abundances in sub-ocean basalt glass and secondary minerals: evidence of biotic and abiotic alteration Geochem., Geophys., and Geosys. 5 (10), doi:10.1029/2004GC000755.
Abiotic
Glass
Biotic
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Biotic [oxide]
Abiotic [oxide]
Una
ltere
d [o
xide
]
PCA
ANN
(Sans Expert)
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Hawaiian HSDP Archaea
QuickTime™ and aTIFF (LZW) decompressor
are needed to see this picture.
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Oregon Dunite withmicrobial galleries and DNA fluorescence
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Fisk, M.R, Popa, R., Mason, O.U., Storrie-Lombardi, M.C., and Vicenzi, E.2006, Iron-Magnesium Silicate Bioweathering on Earth (and Mars?), Astrobiology, 6 (1), p. 48-68.
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Nakhla
Nakhla
Observations in a Martian Meteorite
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Why Choose an Ancient Igneous Rock Site?
1. Provides information on earliest volcanism on the planet.
2. Provides a record to test the hypothesis of early aqueous alteration.
3. Igneous rocks preserve evidence of life for billions of years.
4. Biosignature in igneous rocks can incorporate but do not depend on the
presence of classical organic constituents [ H, C, O, N, P].
5. Biosignatures in igneous rocks are amenable to automated pattern
recognition techniques.
6. Igneous rock sites are dry and comply with planetary protection
constraints.
7. Multiple sites exist (many already well-surveyed) exhibiting low
altitude, low latitude, minimal slope, and minimal wind characteristics.
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Ideal Igneous Site
Mandatory• Exposed Noachian igneous rocks.
Excellent if• Prolonged exposure to water• Dry ever since for preservation.
Ideally• “Go to” availability of sulfates and layered terrain
And of course• Surveyed by MOC, MOLA, TES, THEMIS, HSRC,
and OMEGA and targeted by MRO/CRISM.• Optimize engineering constraints for wind, altitude,
latitude, and slope.
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Site Location Altitude Proponent(km)
NE Syrtis Major 10oN 70oE 0.5-1.5 Harvey
Nili Fossae 22oN 75oE -0.6 Mustard
Marwth Vallis 22.3oN 343.5oE -2 Bibring
Eos Chasma 10.9oS 321.7oE -4.1 Hamilton
What Site?
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