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> Has anyone else measured Ca/P > ratio variation WITHIN individual bones/teeth/conodonts? I ask because I > find significant variation within bones, as much as variation between > bones of different sites, and I wonder how this might affect other trace > element signals (as the variation in Ca/P ratios is diagenetic). I looked at the variation of Ca:P across a cuticle of a diagenetically phosphatised crustacean. The ratio increased towards the inner surface (away from the surface exposed to the phosphate-rich waters presumably) from approx 2.33-2.44 over a thickness of about 1mm. I also found that the mean Ca:P correlated with the thickness of the cuticle suggesting that the phosphate replacement was more complete in thinner cuticles. I don't know if any of this is of relevance to you as you specifically ask for vertebrate references. PS. I did some REE and trace elements in other phosphatised sediment and compared the results to the surrounding non-phosphatised sediment. Answer me off the list if you want to know more. Neil Neil Clark Curator of Palaeontology Hunterian Museum University of Glasgow email: NCLARK@museum.gla.ac.uk Mountains are found in erogenous zones. (Geological Howlers - ed. WDI Rolfe)
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