Figure 5: Evolutionary continuity of shingle-like biomineralization pattern in Acropora lineage.

(a–d) Direct comparison of microstructural features of modern (a) and fossil (b–d) aragonite skeletons of Acropora showing evidence of continuous growth of shingles. Shown are ultra-thin transverse sections (polarized transmitted light, crossed Nicols) of: (a) extant A. muricata (ZPAL H.25/90(535B)), (b) Miocene (Burdigalian) Acropora exerata (ZPAL H.27/28(C56)), (c) Miocene (Aquitanian) Acropora sp. (ZPAL H.27/23(C54)); (d) Middle Eocene Acropora alvarezi (ZPAL H.27/18(C100)), (e) regular incremental growth lines (yellow arrows) in shingled thickening deposits in Miocene (Aquitanian) Acropora sp. (ZPAL H.27/23(C54).