Servizio Comunitario di Informazione in materia di Ricerca e Sviluppo - CORDIS

Serendipitous discovery that high-latitude surface waters may soon become corrosive to CaCO3 minerals such as aragonite

Today's surface ocean is saturated with respect to calcium carbonate, but increasing atmospheric carbon dioxide concentrations are reducing ocean pH and carbonate ion concentrations, and thus the level of calcium carbonate saturation. Experimental evidence suggests that if these trends continue, key marine organisms-such as corals and some plankton-will have difficulty maintaining their external calcium carbonate skeletons. For this result we used 13 models of the ocean-carbon cycle to assess calcium carbonate saturation under the IS92a -business-as-usual- scenario for future emissions of anthropogenic carbon dioxide. In our projections, Southern Ocean surface waters will begin to become under-saturated with respect to aragonite, a metastable form of calcium carbonate, by the year 2050.

By 2100, this under-saturation could extend throughout the entire Southern Ocean and into the sub-arctic Pacific Ocean. When live pteropods were exposed to our predicted level of under-saturation during a two-day shipboard experiment, their aragonite shells showed notable dissolution. Our findings indicate that conditions detrimental to high-latitude ecosystems could develop within decades, not centuries as suggested previously. This work is described in an article published in "Nature" in 2005: Orr et al. [2005] Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms, Nature, 437, doi:10.1038/nature04095, 681-686.

Informazioni correlate

Reported by

Marine Environment Laboratories (MEL-IAEA)
4, Quai Antonie 1er
98000 MONACO
See on map