1996
DOI: 10.1080/00357529.1996.11761532
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Fluorescent Minerals

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Cited by 8 publications
(8 citation statements)
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“…Having assumed that snail uses physical-and cellular-based processes [87][88][89][90] in shell regeneration, we aimed to analyze the polymorphs of the crystals structures obtained by biomineralization ex vivo. Additional analysis of the obtained deposits carried out by fluorescence microscopy indicated similarity between calcite standard [92,93] and microgranular phase formed after biomineralization ex vivo using C. aspersum hemolymph with respect to the red auto-fluorescence (see Fig. 11).…”
Section: Resultsmentioning
confidence: 88%
“…Having assumed that snail uses physical-and cellular-based processes [87][88][89][90] in shell regeneration, we aimed to analyze the polymorphs of the crystals structures obtained by biomineralization ex vivo. Additional analysis of the obtained deposits carried out by fluorescence microscopy indicated similarity between calcite standard [92,93] and microgranular phase formed after biomineralization ex vivo using C. aspersum hemolymph with respect to the red auto-fluorescence (see Fig. 11).…”
Section: Resultsmentioning
confidence: 88%
“…We assumed that calcite was likely to be the biomineral formed ex vivo by hemocytes on the surface of 3D chitinous scaffolds ( Figure 9C,D), and so we carried out the initial analysis of deposits, using fluorescence microscopy. The results obtained ( Figure 10) clearly show a high similarity of red auto-fluorescence between calcite standard [114,115] and microgranular deposits formed after biomineralization ex vivo, using C. aspersum hemolymph. To analyze the obtained biomineral with respect to calcite composition, we used traditional analytical techniques, such as X-ray diffraction analysis (XRD) (Figure 11), FTIR ( Figure 12) and Raman (Figure 13) spectroscopy.…”
Section: Figurementioning
confidence: 76%
“…A previous study using remote laser-induced fluorescence to investigate various soils and rocks up to ~100,000 years old found that fluorescence in rocks such as the matrix around a fossil could be largely attributed to residual organic material 27 . It is also known that minerals can also fluoresce, especially if they contain impurities in their crystal structure, which could be an additional source of fluorescence from the fossil matrix 28 , 29 . Figure 1 illustrates that the emission spectra within certain regions of the leaf exhibit a partial overlap with the spectrum observed in the matrix region.…”
Section: Resultsmentioning
confidence: 99%