These microorganisms contain microcompartments named carboxysomes that encapsulate Rubisco in a protein shell and contain an enzyme, carbonic anhydrase (CA), which
converts bicarbonate ion 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.
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.
However below pH 7.0, nearly all carbonate
ions (CO3 - 2) will be
converted to
bicarbonate (HCO3 --RRB-, so that carbonate
ions no longer serve as buffering agents.
The reason for this is that
bicarbonate is
converted to carbonate in a warmer ocean, releasing a hydrogen
ion thus stabilizing the pH.
This is a normal process, and over millions of years the oceans have remained slightly alkaline, as more acidic surface water mixes with deeper water, and carbonic acid is
converted to
bicarbonate ions.