Coral atolls record slowly sinking seafloor
Reef-building corals can only live in shallow, sunlit water, yet reefs rise from great depths. Darwin argued that a fringing reef around a volcanic island keeps growing upward while the island slowly subsides. The reef becomes a barrier reef separated from land by a lagoon, then an atoll once the peak disappears, so the shape of a reef records movement of the ocean floor that no one can see directly.
