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4. Falk H (1997) Fossilien (in press). It should be mentioned that for the following fossils the occurence of fringelites could be established using the method described in Ref. [5]:Millericrinus munsterianus (ORBIGNY), Upper Jurassic/Oxford, Liesberg, Baselland, CH;Solenopora jurassica (BROWN), Upper Jurassic/Oxford, Novion-Porcien, D�p. Ardennes, F; non determined stromatolite, Lower Triassic/Buntsandstein, Huy, NW of Halberstadt, Harzvorland/Sachsen-Anhalt, D;Encrinus robustus (ASSMANN) oracculeatus (MEYER), Triassic/Muschelkalk, Deuna/Worbis, Th�ringer Becken, D; Encrinus cf. brahli (OVERWEG), Triassic/Unterer Muschelkalk, Wei�enborn/G�ttingen, D;Chelocrinus carnalli (Beyrich), Triassic/Muschelkalk, Elvese/G�ttingen, D;Encrinus liliiformis (LAMARCK), Triassic/Muschelkalk, Alverdissen, D;Bacterocrinus fusiformis (ROEMER), middle Devonian/Eifel-Givet, Loogh layer, Weinberg/Kerpen, Eifel, D;Cupressocrinites oprassus (GOLDFUSS), middle Devonian/Eifel-Givet, Loogh layer, Meerb�sch, Hillesheimer Mulde, Eifel, D;Eucalyptocrinites sp., middle Devonian/Eifel-Givet, Loogh layer, Meerb�sch, Hillesheimer Mulde, Eifel, D;Spinocyrtia ostiolata (SCHLOTHEIM), middle Devonian/Eifel, Junkerberg layer, Gondelsheim, Pr�mer Mulde, Eifel, D. It should also be mentioned that ocurrence of fringelite containing fossils seems to be limited to non-Alpine sites of Europe. Obviously, the more quiet sediments of these areas allowed for the preservation of these chemofossils, whereas the higher temperatures associated with the formation of the Alps destroyed them (a screening of Alpine fossils of Devon to Paleocene age from Austria provided hitheroto no indication of the occurrence of fringelites).
5. Falk H, Mayr E, Richter A (1994) Microchim Acta117:1