Hyn. Holman et al., SURFACE-ENHANCED INFRARED ABSORPTION-REFLECTANCE (SEIRA) MICROSPECTROSCOPY FOR BACTERIA LOCALIZATION ON GEOLOGIC MATERIAL-SURFACES, Journal of microbiological methods, 34(1), 1998, pp. 59-71
Surface-enhanced infrared absorption-reflectance (SEIRA) microspectros
copy is potentially a useful chemical/biological probe to provide insi
ghts into the localization of living endolithic bacteria on the surfac
es of geologic materials. This hypothesis was tested by validating and
demonstrating the use of SEIRA with a metal-overlayer configuration t
i, identify qualitatively on vesicular basalt surfaces the highly loca
lized differences in the chemical composition and in the structure of
clusters of endolithic bacteria, vesicles, and minerals. The metal-ove
rlayer configuration was achieved by evaporating a thin gold-film on b
asalt specimen surfaces. Fourier-transform SEIRA microspectra of the s
pecimen surfaces were recorded in the 650-4000 cm(-1) infrared region
at a resolution of 4 cm(-1) on a Fourier-transform infrared spectromet
er coupled to an infrared microscope. All bacteria-inhabiting surfaces
exhibited infrared absorption bands indicative of bacterial cells, ba
nds that became ideal biomarkers by which to detect the presence of ba
cteria. All basalt surfaces exhibited infrared absorption bands indica
tive of silicates, bands that became ideal mineral markers by which to
detect the presence of silicate-containing minerals and locations of
vesicles (gas-bubble cavities). Comparative analysis of space-resolved
microspectra suggested that bacteria in the vesicular basalt lived no
t only on the vesicle surface but that they also penetrated and lived
beneath the vesicle surface. The penetration terminated when calcic-pl
agioclase feldspar became the dominant constituent mineral in the vesi
cular basalt. With this experimental effort, the practical aspects and
the usefulness of SEIRA as a promising tool to complement existing te
chniques for studying the in-situ localization of living bacteria in g
eologic materials have been demonstrated. (C) 1998 Elsevier Science B.
V. All rights reserved.