Abstract
Factors related to depth have the potential to provide an analogue for future changes in the skeletal mineralogy of calcifying marine organisms and communities, given that oceanic pH decreases with depth, with a minimum pH of
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Figuerola, B., Kuklinski, P., & Taylor, P. D. (2015). Depth patterns in Antarctic bryozoan skeletal Mg-calcite: Can they provide an analogue for future environmental changes? Marine Ecology Progress Series, 540, 109–120. https://doi.org/10.3354/meps11515
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