“…Mineralized tissues (a) can grow and be replaced over time, (b) can form and be added to over time [recording structures (Klevezal, 1996)] or (c) can be periodically shed and totally replaced. Considering the calcium phosphate and calcium carbonate mineralized tissues, examples of (a) include bone and its remodeling (Kenkre & Bassett, 2018), rodent incisors (Pugach & Gibson, 2014) and sea urchin teeth (Ma ¨rkel et al, 1977); of (b) fish otoliths (Campana & Neilson, 1985), tooth cementum (Naji et al, 2022) and shark vertebrae (Natanson et al, 2018); of (c) deer antlers (Kierdorf et al, 2022) and stomatopod dactyl clubs (Christensen et al, 2023). These three classes provide different windows into biomineralization and dactyl clubs, and their non-equilibrium mineral constituents are the topic discussed in a paper by Christensen et al in this issue of IUCrJ.…”