By Ilya Gershevitch

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Acknowledgements. The experimental work was financially supported by the Deutsche Forschungsgemeinschaft. References Bell LS (1990) Palaeopathology and diagenesis: an SEM evaluation of structural changes using backscattered electron imaging. J Arch Sci 17:85-102 Cook M, Malta E, Anderson C (1989) Fluorochrome labelling in Roman period skeletons from Dakleh Oasis, Egypt. Am J Phys Anthropol 80: 137-143 Duff RB, Webley OM & Scott RO (1963) Solubilization of minerals and related materials by 2-ketogluconic acid-producing bacteria.

For practical purposes, a summarized historical survey of vertebrate palaeohistological publications may be divided into distinct areas of research subject: 1. The dermal skeleton, especially among "lower" (non-tetrapod) vertebrates, which contain bony and dental tissues combined; 2. The endoskeleton among "non tetrapod" vertebrates; 42 3. Dermal bones and flat bones of tetrapods; 4. Compact bone of tetrapods, mainly studied on shaft cross-section; 5. Long bone growth and endochondral ossification; 6.

Similar tissue phenotypes will be found in them, irrespective of phylogeny. These data provide the rationale from which any attempt at a significant use of comparative bone histology for taxonomic purposes, and especially systematic determination of fossil bone samples of unknown pedigree, can be performed (Enlow 1966). 2 Some Speculations on the Relationships Between Bone Tissue Phenotypes and Genomes As summarized in the previous section, comparative histological and ontogenetic data suggest that bone tissue phenotype diversity is the result of a complex and multifactorial determinism (see de Ricqh~s 1975-78, 1980).

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