Due to modern developments Raman spectroscopy has evolved into a fast vibrational technique. Detailed fingerprints in combination with non-destructivity and minimal sample preparation has allowed the construction of reference libraries in a variety of research fields. Long-term stability and comparability are important characteristics when developing reference libraries. In addition, small shifts in highly similar spectra of different samples may limit the full potential of Raman spectroscopy. Since libraries often contain a large number of different and/or highly similar spectra, it is important that each data point in all the spectra corresponds to the exact Raman wavenumber. This is often not the case, due to shifts in optical pathway and/or shifts in laser wavelength. This paper describes a complete calibration protocol (wavelength and intensity) and evaluates the procedure for both short and long term stability, by means of 60 randomly selected measurement sessions spread over a period of nine months. A two-step standardization procedure is proposed to deal with spectral shifts.

Confocal micro-Raman spectroscopy requires a minimum of sample handling and no reagents and allows fast identification of microorganisms. Since it reflects the overall molecular composition of the cells, it provides much more information than classical, microbial analyses. However, since the molecular makeup of a cell depends on culture conditions, it can be argued that this will affect the reproducibility and discrimination ability of Raman spectroscopy. We used Bacillus cereus, Bacillus pumilus, and Bacillus licheniformis, which are known to be clearly distinct from each other and each displaying important phenotypic heterogeneity, in a wide variety of culture conditions to analyze this. It is illustrated that the influence of culture conditions on the identification accuracy and taxonomic resolution of Raman spectroscopy is important though the effect on the final identification is limited within the set of stains studied. Furthermore, some conditions even allow for better discrimination than others. From a practical point of view, it is especially important that differences in culturing time (and culturing temperature) can be accommodated.

Coesite inclusions occur in a wide range of lithologies and coesite is therefore a powerful ultrahigh-pressure (UHP) indicator. The transformation of coesite to quartz is evidenced by three optically well identifiable characteristics (e.g. palisade textures, radial crack patterns, polycrystalline quartz pseudomorphs). Under overpressure monomineralic coesite (on an optical basis), lacking the above transformation characteristics may survive. Raman micro-spectroscopy was applied on monomineralic coesite inclusions in garnet porphyroblasts from diamond-bearing garnet-clinozoisite-biotite gneisses of the Barchi-Kol area (Kokchetav Massif, Northern Kazakhstan). These coesite inclusions are euhedral and display a characteristic anisotropic hallo. However, Raman maps and separate spectra of these inclusions display shifted bands for coesite and quartz. Microscopically undetectable, quartz shows on the Raman map as a thin shell around coesite inclusion. Shift of the main coesite band allows to estimate their overpressure: coesite inclusions record 0-2.4 GPa in garnet and zircon. The quartz shell remains under lower pressure 0-1.6 GPa. The possible application of coesite and quartz Raman geobarometers for UHP metamorphic rocks is discussed.

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