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Evidence of biological activity in Hawaiian subsurface basalts

ScholarsArchive at Oregon State University

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Title Evidence of biological activity in Hawaiian subsurface basalts
Names Fisk, Martin R. (creator)
Storrie-Lombardi, M. C. (creator)
Douglas, S. (creator)
Popa, R. (creator)
McDonald, G. (creator)
Di Meo-Savoie, C. (creator)
Date Issued 2003-12-11 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract The Hawaii Scientific Drilling Program (HSDP) cored and recovered igneous rock from the surface to a
depth of 3109 m near Hilo, Hawaii. Much of the deeper parts of the hole is composed of hyaloclastite
(fractured basalt glass that has been cemented in situ with secondary minerals). Some hyaloclastite units
have been altered in a manner attributed to microorganisms in volcanic rocks. Samples from one such unit
(1336 m to 1404 m below sea level) were examined to test the hypothesis that the alteration was associated
with microorganisms. Deep ultraviolet native fluorescence and resonance Raman spectroscopy indicate
that nucleic acids and aromatic amino acids are present in clay inside spherical cavities (vesicles) within
basalt glass. Chemical mapping shows that phosphorus and carbon were enriched at the boundary between
the clay and volcanic glass of the vesicles. Environmental scanning electron microscopy (ESEM) reveals
two to three micrometer coccoid structures in these same boundaries. ESEM-linked energy dispersive
spectroscopy demonstrated carbon, phosphorous, chloride, and magnesium in these bodies significantly
differing from unoccupied neighboring regions of basalt. These observations taken together indicate the
presence of microorganisms at the boundary between primary volcanic glass and secondary clays. Amino
acids and nucleic acids were extracted from bulk samples of the hyaloclastite unit. Amino acid abundance
was low, and if the amino acids are derived from microorganisms in the rock, then there are less than
100,000 cells per gram of rock. Most nucleic acid sequences extracted from the unit were closely related to
sequences of Crenarchaeota collected from the subsurface of the ocean floor.
Genre Article
Topic Hawaiian deep drilling
Identifier Fisk, M. R., M. C. Storrie-Lombardi, S. Douglas, R. Popa, G. McDonald, and C. Di Meo-Savoie, Evidence of biological activity in Hawaiian subsurface basalts, Geochem. Geophys. Geosyst., 4(12), 1103, 2003.

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