Oh man NIkki your making me good deep again, lol. your close on the concept but the outside sources such as refugium, and depressing PH doesnt really apply as you noted, but a good conclution. Hmm how do I explain this one with out sounding like an expert, lol
Ok the respiratory carbon dioxide (CO2) is turned into carbonic acid (H2CO3), which is in turn converted into bicarbonate (HCO3-) and carbonate (CO3--) ions. The enzyme responsible for the addition of water to carbon dioxide to form carbonic acid is carbonic anhydrase, which is present in high concentrations in corals. The cells also have special pumps that exchange one calcium ion (Ca2+), kicking it out of the cell for 2H+ ions, which it brings into the cell. Next, one of the two CO2 molecules we made earlier is going to diffuse out of the cell, where all the calcium is being moved to. Since all the protons are being removed from where the Ca2+ is moving to, the pH goes up. The area right next to the cell gets super saturated with Ca2+ that the cell keeps pumping out, and one Ca++ combines with that one CO2 molecule that diffused out. the result is the formation of the skeliton. the left over product is 2H+, which is taken back up by the cell to start the process all over again.
So a quick overview would be that the calcium is a product that the coral is trying to get rid of. with the use of carbonates the coral has figured out a method of doing so fairly easy, and the whole process helps the coral and its zoox get the extra co2 it needs for respiration. So having to much calcium causes the coral to use to much of its energy budjet to get rid of it, will you get better growth?? not much at all, but what you will do is stress the coral out.
Sorry if that one seems difficult, its a real tough one to explain, and I need a heck of alot more coffie now
Mike