In more acidic conditions, bicarbonate ions tend to convert into carbonic acid and release hydrogen ions (H+). This reduces the availability of bicarbonate ions for the organisms to use in the formation of their shells.
The solubility of calcium carbonate increases with decreasing pH. This means that the formed shells may become more prone to dissolution in more acidic conditions. The acidification of the water can lead to the breakdown of the calcium carbonate structure, potentially impacting the structural integrity of the shells.
Some organisms may also experience direct physiological effects due to the changes in pH. For example, the acidification of the water can affect metabolic processes, enzyme activities, and other physiological functions in these organisms.