Maupiti in Society Islands: Revising Darwin's sinking-island theory

A satellite image of Maupiti, one of the Society Islands, which is on its way to becoming an atoll. Submerged reef appears in pale blue. 

Credit: NASA EARTH OBSERVATORY

The three different formations of South Pacific coral-reef islands have long fascinated geologists.

Tahiti's coral forms a "fringing" reef, a shelf growing close to the island's shore.

The "barrier" reefs of Bora Bora are separated from the main island by a calm lagoon.

Finally, an "atoll," such as Manuae, appears as a ring of coral enclosing a lagoon with no island at its center.

The question of how reefs develop into these shapes over evolutionary time produced an enduring conflict between two hypotheses, one from British naturalist Charles Darwin and the other from Canadian geologist Reginald Daly.

In a paper (see PDF) recently published in the journal Geology, researchers at MIT and Woods Hole Oceanographic Institution (WHOI) use modern measurements and computer modeling to resolve this old conundrum.

Charles Darwin

Darwin proposed that fringing reefs, barrier reefs and atolls reflect different stages in a dramatic process that occurs as an island sinks into the ocean floor—the ultimate fate of all of the world's volcanic ocean islands.

As young volcanic rock cools and is carried away from a volcanic "hot spot" by the movement of tectonic plates, an island sinks as much as a few millimeters per year.

As the island sinks, resident coral reefs on the island flanks grow upward toward the sea surface. The living coral organisms up top, and their symbiotic algae, get enough sunlight to keep pace with the sinking of the island.

As the coral grows upward and the island sinks down, a fringing reef progresses to a barrier reef, and eventually to a signature atoll.

Michael Toomey

However, Darwin's reef theory can't explain the trajectories of all volcanic ocean-island systems, as MIT/WHOI graduate student Michael Toomey and collaborators Taylor Perron, the Cecil and Ida Green Assistant Professor of Geology at MIT, and Andrew Ashton, a coastal geomorphologist at WHOI, discovered.

The Hawaiian Islands, they realized, show a different kind of progression: For example, the researchers found fringing reef where they expected to find no reef development and drowned barrier reefs where they expected living barrier reefs.

"Those islands are just not sinking into atolls like the Society Islands," Toomey says, "so we wanted to develop a model to explain these differences."

More information: "Profiles of ocean island coral reefs controlled by sea-level history and carbonate accumulation rates" geology.gsapubs.org/content/early/2013/05/09/G34109.1.full.pdf+html

NASA: MODIS snap Cyclone Oli circling over Tahiti

Cyclone Oli was a Category 4 storm on February 4, 2010, when the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite captured this true-color image.

The powerful storm was moving southeast across the South Pacific over the French Polynesian Islands.

Tahiti, the most populous of the islands, is under the outer edge of the storm in the upper right.

According to the Joint Typhoon Warning Center, Oli had winds of 213 kilometers per hour (132 miles per hour or 115 knots) at 1:40 p.m., local time, when this image was acquired. Forecasters expected the storm to weaken as it continued to move south over cooler waters.

At least 3,400 people were evacuated from Tahiti and nearby islands as Oli approached, reported BBC News. The storm’s strong winds damaged homes and power lines. One person died and several others were injured in the storm, said BBC News.

The highest resolution version of the image is provided above. The image is available in additional resolutions from the MODIS Rapid Response System.