In this work, it is elucidated to what degree the seagrass Zostera mar
ina L. can utilise HCO3- as an external inorganic-carbon source for ph
otosynthesis, and which of two possible systems for its acquisition is
in effect. It was found that HCO3- was used as a major source of inor
ganic carbon at the normal seawater-pH of 8.2, and that bulk CO2 contr
ibuted only marginally (less than 20%) to photosynthesis at that pH. B
y comparing photosynthetic rates at pH 8.2 and 9.0, it was deduced tha
t CO32- could not be utilised. It was further found that HCO3- could b
e acquired via extracellular dehydration to CO2, as catalysed by exter
nal/surface-bound carbonic anhydrase, prior to inorganic-carbon uptake
. Indications for active, ATPase-mediated, HCO3- transport was also fo
und, but an inhibitor of extracellular carbonic anhydrase affected pho
tosynthetic rates more than did the less specific ATPase inhibitors. T
he rationale for HCO3- dehydration versus its direct uptake is discuss
ed with regard to the photosynthetic performance of seagrasses, many o
f which are inorganic-carbon limited in their natural habitats.