As global temperatures increase, some scientists suggest that such storms will become more frequent and intense over the next few decades.
Tropical storms, with waves reaching up to 10-meters-high, can wallop coral reef islands. As global temperatures increase, some scientists suggest that such storms will become more frequent and intense over the next few decades. Additionally, potential sea level rise is perceived as a threat to the continued existence of these remote, low-lying communities.
Many coral reef islands, or atolls, are created by water moving sand and gravel, piling it up into consecutive ridged layers, "a bit like onions," says Paul Kench, earth scientist and dean of science at Simon Fraser University, Burnaby, Canada. However, new research by Kench and colleagues recently published online ahead of print for Geology uncovered a different type of island construction: storm-deposited boulders.
On Tutago island in Tuvalu's Funafuti atoll, giant coral blocks sit on top of a flat reef. Researchers noted the jumble of upended corals didn't grow there, but instead were tumbled onto the site. As storm waves hit the reefs, it's not just fist or head-sized gravel chunks that are moving—Kench says coral boulders, which can be meters in diameter, are getting plucked and hurled into piles, forming the island.
To better understand how storms shaped Tutago, the team collected radiocarbon dates on the piled coral blocks. Within these boulder deposits, they uncovered distinct clusters of ages, revealing that Tutago island formed about 750 years ago, and at least two major storm events occurred about 600 and 350 years ago.
Continue reding at The Geological Society of America
Image via NASA
