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Maybe a unnecessary clarification, but at least my main point here that calcification goes faster with higher dKH and pH is s not new; we quite well know how calcification works when the coral uses bicarbonate but has to expel hydrogen ions. That is a process that will be easier if the surrounding pH is higher. It also aids in the transport of hydrogenbicarbonate if the concentrationgradient is higher. I guess both mechanisms are responsible for the faster growth. It is interesting that corals do not seem to be able to fully control the speed of skeleton formation, but it is at least partial driven by concentration gradients and pH. In contrast to humans or other animals, that would be a catastrophe if you couldn't fully regulate the formation of the skeleton. Maybe that is a weakness of the coral, and that could be the reason we shouldn't push the limits too hard. But actually, what I are more interested in is the internal pH depending on the surrounding alkalinity and not the skeleton formation itself. So I'm talking about the cells from the soft tissue and how they struggle with keeping the internal pH with high surrounding bicarbonate concentration. I don't think much is written about that, but we at least know that fluctuations stress them. We will see if we can find some more data about this because it's advanced research and complicated to measure intracellular pH.
