Mike,
Lithaqua is not a coral, but rather a green algae, that has been calcified. We bring it in from Belgium through Bacta-Pur Europe. Lithaqua comes from a tropical benthic genus of green algae called Halimeda. It was first discovered in the 1950's when large numbers of deep bore holes were drilled into Pacific atolls. Geologists found that the dominant element of the carbonate structure was not stony coral, but rather a "lithified" sand made up of the lobes of Halimeda.
The members of this genus rank as one of the most important calcifiers of the biosphere; it is likely that their CaCO3 production over all of the tropical seas is considerably greater than that of stony corals.
Anatomically, members of this genus are constructed of tubules, with very few cross walls. Thus, individual cells are extremely long and narrow. At the surface of the discs or lobes, the surface expression of these tubules (called utricles) is slightly swollen to form a continuous surface as kind of a cellular pavement. Just below the surface of the lobe, there are considerable spaces between the utricles. The calcification, mostly of aragonite needles (CaCO3), occurs alost entirely in these interutricular spaces. Thus, through the anatomy of their utricles, these algae have provided one of the basic requirements for biomineralization, confined spaces in which critical supersaturation can occur.
When a halimeda disc is sectioned, it is possible to see under a dissecting microscope that the chlorplasts are crowded into the outer parts of the utricles. Most of the cellular remander of the lobes and joints is colorless or nearly so. Thus, when photosynthesis is proceeding rapidly, C02 diffuses from the water immediately exterior to the plant and, particularly because this is the largest surface of each utricle, from the interutricular spaces. This stongly raises the pH and the concentration of the carbonate ion in the interutricular spaces. As long as calcium is available to diffuse through the porous cell wall from the exterior, calcium carbonate becomes highly supersaturated in the largely enclosed spaces.
The production of calcium in corals is different and even more long winded, but, a basic summary is; calcification occurs in the basal disc of each polyp and the biomineralization zone is well removed from the photosynthetic region. Therefore, it makes it highly unlikely that carbon dioxide removal and pH elevation is a direct driving force in coral calcification. In fact, for every molecule of CO2 taken up and calcium carbonate laid down, two ions of bicarbonate are used and two molecules of C02 are produced. These acidic conditions and excess carbon dioxide actually slow down calcification.
Have you had enough yet, I have?
Russ