Abstract
The unexpected finding that certain major marine photosynthetic microorganisms can serve as a source of CO2 rather than a sink emerged during measurements of inorganic carbon fluxes associated with the CO2-concentrating mechanism. During steady-state photosynthesis, CO2 was evolved at sustained rates up to 5-fold that of photosynthesis; the steady-state external CO2 concentration reached was significantly higher than that at CO2-HCO3- equilibrium. The evolved CO2 originated from HCO3- taken up and intracellularly converted to CO2 in a light-dependent process. Our results bear implications for carbon cycling in the marine environment; the use of naturally-observed stable carbon isotope fractionations as paleobarometer and productivity probe; and for intracellular energy balance and pH regulation.
| Original language | English |
|---|---|
| Pages (from-to) | 949-953 |
| Number of pages | 5 |
| Journal | Canadian Journal of Botany |
| Volume | 76 |
| Issue number | 6 |
| DOIs | |
| State | Published - Jun 1998 |
Keywords
- CO evolution
- Carbonic anhydrase
- Cyanobacteria
- Photosynthesis
- Synechococcus