Exposing oocytes to a solution containing CO2/HCO3 causes the familiar fall in intracellular pH (pHi) and a rise in surface pH (pHS) followed by a decay. Musa‐Aziz et al (ASN, 2005) examined the effects of carbonic anhydrases (CAs) on pH transients caused by CO2 influx. They found that injecting CAII into oocytes or expressing CAIV on the oocyte surface accelerates the initial rate of pHi acidification (dpHi/dt) and amplifies the height of the pHS spike (ΔpHS). They proposed that both enzymes enhance CO2 influx by maximizing CO2 gradients across the plasma membrane. We use a mathematical model of a Xenopus oocyte—which accounts for CO2, carbonic acid (H2CO3), HCO3, protons, and a multitude of non‐HCO3 buffer pairs—to investigate the above findings. We simulate the experimental protocol in which the CO2/HCO3 solution is delivered from the bulk to the oocyte surface by raising exponentially the concentrations of CO2, H2CO3 and HCO3 in the bulk and assuming that initially no CO2, H2CO3 and HCO3 are present in the extracellular unconvected fluid. We use the experimental data for 1.5% CO2/10mM HCO3 (pHo=7.5) to find parameter values that simultaneously match ΔpHS, the time that it takes for pHS to reach its peak (tP), dpHi/dt, and the time delay in the pHi decay. We validate the model against data collected when exposing oocytes to 5% CO2/33mM HCO3 and to 10% CO2/66mM HCO3. The model confirms that CAII and CAIV enhance CO2 influx.
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