This story was provided by NOAA's Atlantic Oceanographic and Meteorological Laboratory. For the AOML story go online to AOML's website.
Scientists studying coral reefs in volcanically acidified water of the southwestern Pacific Ocean measured a net loss of coral reef skeletons due to increased bio-erosion by worms and other organisms, according to new research by NOAA, the Cooperative Institute for Marine and Atmospheric Studies (CIMAS) and Australian scientists.
Inside look at coral
Coral skeleton sample from the study, and its 3D reconstructions showing the external surface in gray, and CT-scan analysis of new coral structure added on the outside (colored green) and boreholes from worms showing structure loss on the inside (in blue).
The study, published in the
Proceedings of the Royal Society B, measured changes in the reef framework in several naturally high-carbon dioxide settings near Papua New Guinea. For the first time, scientists found increased activity of worms and other organisms that bore into the reef structure resulting in a net loss of the framework that is the foundation of coral reef ecosystems.
This two-year study used cutting edge technology to analyze the combined influences of organisms that add to and break down reef framework. Micro-CT scans and specialized software allowed scientists to peer inside the coral skeletons to see the bore holes left by worms. They created three-dimensional digital models to precisely measure the net difference between new coral material added by calcifying organisms and coral material lost through bio-erosion by worms and other organisms.
“This is the first study to piece together all of the coral reef ocean acidification processes, simultaneously looking at the different organisms that grow and erode reef habitats, and their net effects on one another over time,” said Ian Enochs, a coral ecologist at CIMAS and NOAA’s Atlantic Oceanographic and Meteorological Laboratory and lead author of the study. “This demonstrates that ocean acidification is a two-front assault on coral reefs, simultaneously slowing the growth of skeleton, and speeding up the rate at which old reef habitats are eroded.”
This research was funded by NOAA’s Ocean Acidification Program and Coral Reef Conservation Program, as well as the Great Barrier Reef Foundation’s “Resilient Coral Reefs Successfully Adaption to Climate Change” research and development program in collaboration with the Australian Institute of Marine Science.
Please go online to read the the new research in Proceedings of Royal Society B.
Go online to view an animation of a coral CT scan showing erosion by worms and other organisms and accretion or growth of new coral structure in naturally acidified waters.
For more information contact Monica Allen, director of public affairs for NOAA Research, at 301-734-1123 or by email at monica.allen@noaa.gov