Very nice tank!
Photosynthesis isn't consuming alkalinity (where would it go?) but either coralline algae or abiotic precipitation of calcium carbonate (or rising nitrate, but that seems unlikely in this case) will deplete alkalinity.
I´m with you if it is CO
2 that is consumed in a direct way. The C that will be lost from the carbonate system (into biomass) will be replaced by C from the airs CO
2 that will be forced down into the water because of the pH rise the uptake of waters CO
2 will cause. The interface air/water will make it to zero-sum game.
On the other end - if they should use CO
3 and convert that into CO
2 we should - IMO - have a acidification process in the water and production of oxygen radicals and/or oxygen gas. The acidification because the it will need one HCO
3 ion to be converted into a CO
3 ion for each CO
3 ion the process use. The acidification will lead to the CO
2 level increase in the water and you will lose this C either to the photosynthesis or the air/water interface (depending on the actual pH and air content) IMO - if such a process exist ( all sources I have say no - it not exist) it should be consuming C from the carbonate systems in both ends of the system - still IMO - very much IMO. Compare the nitrification process that use CO
3 as first step in production of organic C. That process is consuming alkalinity.
What´s happen with if they use HCO
3 as main source (it has been shown that high alkalinity both freshwater and marine plants/algae has an ability to do that) The HCO
3 has to be converted to one CO
2 molecule, one H ion and one O atom. Either external or/and internal, either enzymatic or/and through pH shift between different cell layers. Interesting is what happens with the lose H ions and O radicals. If all of them form OH ions/radicals - I´m with you - this process is alkalinity neutral as the use of pure CO
2. But if not all O radicals will find a H ion and either do its job as an O radical (oxidise something else) or find another O and become O
2 gas - the C balance in the carbonate buffering system will not be even. the photosynthesis process will consume C from the carbonate buffering system
I have no evidences at all to what I´m suggesting more than two things I have seen / heard regarding photosynthesis in water with high alkalinity and organisms with known ability to use HCO
3 as a starting point for photosynthesis.
1. The pH swing in these system is not as high as it is in water with low/no alkalinity at all. Some of these effects can be is related to the buffering ability - but can all?
2. I have seen and heard of other with marine or high alkalinity fresh water plants that there is a consumption of alkalinity in such systems equal with what Andy Macro report
Sincerely Lasse