To overcome the limiting supply of CO2, organisms like coral
concentrate bicarbonate ions in compartments into which they pump H + ions and lower the pH. As seen in Figure 2, at pH 5 or lower, 90 % of the DIC converts to CO2.
Not exact matches
With a higher internal pH,
bicarbonate sheds an H + and converts into carbonate
ions and when
concentrated in the presence of
concentrated Ca + +, calcium carbonate minerals readily form.
Instead, as with photosynthesis, calcifiers actively uptake the more abundant
bicarbonate ions and
concentrate them in compartments.
The majority of marine algae have carbon
concentrating mechanisms (CCMs) that facilitate the active influx of CO2 and / or
bicarbonate ions -LRB--RRB- and elevate C concentrations at the site of C fixation (i.e. Rubisco), with few algae being CO2 - only users [22,23].