Marine Biologist: The accelerated structural degradation of the deep-water coral Lophelia pertusa in the Boreal Basin over the last twenty years is widely attributed to oceanic acidification. Proponents of this theory argue that higher acidity depletes the dissolved calcium carbonate that the corals extract from the water to build their skeletons. However, recent hydrographic surveys demonstrate that the overall concentration of dissolved calcium carbonate in the Boreal Basin has actually risen by nearly twelve percent over this exact timeframe. Clearly, the degradation of the coral's structure is not a consequence of oceanic acidification, but must stem from a different environmental stressor, such as the recently documented increase in deep-sea trawling.
Statement: If true, the fact that the recent twelve percent increase in dissolved calcium carbonate in the Boreal Basin consists entirely of aragonite—the specific crystalline form of calcium carbonate that constitutes the existing skeletons of Lophelia pertusa and which dissolves rapidly when exposed to higher acidity—weakens the marine biologist's argument.
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