Photo: A diving buddy pair taking Reef Check Australia substrate data on the Great Barrier Reef. Copyright Steve Prutz. Sourced from Wikimedia Commons
Scientists at the Australian Institute of Marine Science in Townsville claim that coral on Australia's Great Barrier Reef reached a tipping point in 1990 with coral growth having slowed by more than 14 percent since then.
Reef corals create their hard skeletons from dissolved materials in seawater. As human induced climate change has injected growing amounts of carbon dioxide into the atmosphere, the worlds oceans have absorbed carbon dioxide making them more acidic which effectively reduces the ability of marine organisms to form skeletons. This will effect the whole food chain in the ocean.
Dr Glenn De’ath said that the severe and sudden decline in calcification was an unprecedented occurrence in the last 400 years. "The causes of this sharp decline remain unknown, but our study suggests that the combination of increasing temperature stress and ocean acidification may be diminishing the ability of GBR corals to deposit calcium carbonate," he said.
"Prior to about 1990 coral growth was fairly consistent but round about 1990 things have change and we're suggesting this is the tipping point. What's happened basically coral calcification, that's a measure of how corals grow, has decreased by about 14 per cent since then. Now we're experiencing growth which is now consistently declining. We estimate roughly, if this rate continues, which is accelerating, then the coral growth will hit zero round about 2050." Dr Glenn De’ath told Australian Broadcasting Corporation radio.
The scientists, Dr Glenn De’ath, Dr Janice Lough and Dr Katharina Fabriciu, have published their research in the international journal Science. It is the most comprehensive study to date on calcification rates for corals and include rigorous statistical analyses of annual growth bands from 328 Porites corals from 69 reefs across the length and breadth of the Great Barrier Reef, and extending back in time up to 400 years.
"It is cause for extreme concern that such changes are already evident, with the relatively modest climate changes observed to date, in the world’s best protected and managed coral reef ecosystem," said AIMS scientist and co-author Dr Janice Lough.
"Coral skeletons form the backbone of reef ecosystems. Their complexity provides the habitat for the tens of thousands of plant and animal species associated with the reef," co-author Dr Katharina Fabricius said. "Skeleton formation also offsets natural erosion and breakage. Previous laboratory experiments and models have predicted that calcification will decline in response to acidification, but here we have shown for the first time that corals are already affected in their natural environment throughout the GBR," Dr Fabricius said.
According to the scientists, oceanic pH, the measure of acidity of substances, has already dropped by 0.1 and could decrease by 0.4 by the end of this century, due to the oceans absorbing about a third of the extra carbon dioxide (the main greenhouse gas) that humans have put into the atmosphere. If the projected 0.4 decline in pH is correct, this would be "well outside the realms of anything organisms have experienced over hundreds of thousands of years," Dr Lough said. Increased ocean acidity will affect all marine life through food webs leading to precipitous changes in the biodiversity and productivity of the world's oceans, the scientists warn.
AIMS scientists Glenn De’ath, Janice Lough and Katharina Fabricius, have published their research in a paper titled "Declining coral calcification on the Great Barrier Reef", in Science magazine, 2 January 2009. The abstract is below:
Reef-building corals are under increasing physiological stress from a changing climate and ocean absorption of increasing atmospheric carbon dioxide. We investigated 328 colonies of massive Porites corals from 69 reefs of the Great Barrier Reef (GBR) in Australia. Their skeletal records show that throughout the GBR, calcification has declined by 14.2% since 1990, predominantly because extension (linear growth) has declined by 13.3%. The data suggest that such a severe and sudden decline in calcification is unprecedented in at least the past 400 years. Calcification increases linearly with increasing large-scale sea surface temperature but responds nonlinearly to annual temperature anomalies. The causes of the decline remain unknown; however, this study suggests that increasing temperature stress and a declining saturation state of seawater aragonite may be diminishing the ability of GBR corals to deposit calcium carbonate.
- Climate Change: Marine Scientists Demand Action on Greenhouse Gas Emissions - Originally published on Sydney Indymedia October 25, 2007
- Changes in Global Sea Surface Acidity Sydney Indymedia 2007 article
- Scientists say Ocean Acidity Increasing at Faster Rate -originally published Sydney Indymedia, October 18. 2007 article
- Think Not 'Global' Warming - Think 'Oceans' Warming - originally published Sydney Indymedia November 27, 2007
- Ocean warming: Ocean Heat Content Change (W - year/m2) 1993-2003 - originally published Sydney Indymedia November 27, 2007
- Australian Institute of Marine Science media release 2 January 2009 - Hard core data shows 14 per cent drop in coral growth on GBR since 1990
- ABC Radio news AM program, 2 January 2009 - Coral study finds slowest growth in 400 years