“…The cellular patterns are of different sizes and scales: cells 20 m in diameter, larger cells 200 m in diameter, and the largest (on Selakan Bank) about 1 km in diameter [12,13]. These reef patterns may occur (1) on fringing reefs, notably in the Arabian Gulf, in the Red sea [14,15], and in Madagascar [16], (2) on barrier reefs in New Georgia [17], in Belize [18], on the Great Barrier Reef [19][20][21], and in Mayotte [16], and (3) on atolls in Hawaii (Maro reef, [22]), in Fiji, in French Polynesia [23,24], and in Kiribati (Caroline/Millennium, [25]). According to Montaggioni [23] and Purkis and Riegl [15], the reticulated shape of the mesh reef could mimic a preexisting karst topography, inherited from an episode of lower sea level.…”