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Live specimens of the pteropod Limacina helicina antarctica were extracted from the top 200 meters of the Southern Ocean in early 2008, where aragonite saturation levels were around 1. The dataset likely contains measurements of seawater carbonate chemistry and the proportion of different shell dissolution levels, comparing specimens from aragonite-undersaturated regions with those from supersaturated ones. According to the description, eight days of incubation in aragonite saturation levels of 0.94-1.12 produced equivalent levels of dissolution observed in the natural undersaturated region.
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