Photosynthesis in marine diatoms is a vital fraction of global primary production empowered by CO 2 -concentrating mechanisms.
Acquisition of HCO 3− from seawater is a critical primary step of the CO 2 -concentrating mechanism, allowing marine photoautotrophic eukaryotes to overcome CO 2 limitation in alkaline high-salinity water. However, little is known about molecular mechanisms governing this process. Here, we show the importance of a plasma membrane-type HCO 3 − transporter for CO 2 acquisition in a marine diatom. Ten putative solute carrier (SLC) family HCO 3 − transporter genes were found in the genome of the marine pennate diatom Phaeodactylum tricornutum. Homologs also exist in marine centric species, Thalassiosira pseudonana, suggesting a general occurrence of SLC transporters in marine diatoms. Seven genes were found to encode putative mammalian-type SLC4 family transporters in P. tricornutum, and three of seven genes were specifically transcribed under low CO 2 conditions. One of these gene products, PtSLC4-2, was localized at the plasmalemma and significantly stimulated both dissolved inorganic carbon (DIC) uptake and photosynthesis in P. tricornutum. DIC uptake by PtSLC4-2 was efficiently inhibited by an anion-exchanger inhibitor, 4,4′-diisothiocyanostilbene-2,2′-disulfonic acid, in a concentration-dependent manner and highly dependent on Na + ions at concentrations over 100 mM. These results show that DIC influx into marine diatoms is directly driven at the plasmalemma by a specific HCO 3 − transporter with a significant halophilic nature.bicarbonate transporter | chromista | marine environment | sodium-dependent I norganic carbon entry into algal cells is the primary limiting factor for photosynthesis and requires specific transporters (1). The problem is exacerbated especially in marine environment. Specifically, dissolved CO 2 concentrations are low, and the rate of spontaneous CO 2 formation from HCO 3 − is much slower in the ocean relative to freshwater because of the high alkalinity and salinity of seawater (2). Marine diatoms are responsible for one-fifth of global primary productivity and play a key role in global cycles of carbon and other elements (3, 4). The concentration of dissolved CO 2 in seawater under the present atmospheric pCO 2 (below 15 μM at 20°C) is much lower than the K m [CO 2 ] of ribulose-1,5-bisphosphate carboxylase/oxygenase in diatom species (5). Marine diatoms are, thus, believed to rely directly or indirectly on the use of abundant levels of seawater HCO 3 − to support their primary production. The CO 2 -concentrating mechanism (CCM) has been studied extensively in cyanobacteria, and molecular characterizations have revealed a set of CCM components that completely account for the strategy of cyanobacterial tolerance of CO 2 limitation. Freshwater β-cyanobacteria possess three plasma membrane HCO 3