

Coral Skeleton Growth Stony coral skeletons form through two main growth zones, rapid accretion deposits (RADs) and thickening deposits (TDs), that emerge in the earliest life stages. Ocean acidification alters their growth, increasing TD density via a shift toward more crystalline calcium carbonate phases, and reducing RADs development. The result is a denser yet structurally weaker skeleton, redefining coral resilience under future ocean scenarios. More detiails can be found in the Research Article by Federica Scucchia, Paul Zaslansky, and co‐workers (DOI: 10.1002/advs.202508585). Coral Skeleton Growth Stony coral skeletons form through two main growth zones, rapid accretion deposits (RADs) and thickening deposits (TDs), that emerge in the earliest life stages. Ocean acidification alters their growth, increasing TD density via a shift toward more crystalline calcium carbonate phases, and reducing RADs development. The result is a denser yet structurally weaker skeleton, redefining coral resilience under future ocean scenarios. More detiails can be found in the Research Article by Federica Scucchia, Paul Zaslansky, and co-workers (DOI: 10.1002/advs.202508585 ). Advanced Science, Volume 12, Issue 48, December 29, 2025.
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