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Although unexpected, statistically significant four to seven point isochrons are observed for four fossil dinosaur bone samples and one Upper Triassic tooth with MSWDs ranging from 0.083 to 4.5.
Notably, mobility of Lu alone cannot account for the observed age patterns.
By counting the visible growth bands and measuring the mean age of a single septum, the extension rate of was estimated to be between 0.1 and 3.1 mm/year.
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Likely mechanisms to account for the presence of statistically meaningful isochrons as well as for the late diagenetic exchange of both REE and Hf are diffusion, adsorption, and dissolution–reprecipitation processes.
Th not due to closed system decay within the coral lattice.