Enrichment of oxygen heavy isotopes during photosynthesis in phytoplankton

Some of the oxygen produced during oxygenic photosynthesis is consumed but little is known about the extent of the processes involved. We measured the ¹⁷O/¹⁶O and ¹⁸O/¹⁶O ratios in O₂ produced by certain marine and freshwater phytoplankton representing important groups of primary producers. When the cells were performing photosynthesis under very low dissolved oxygen concentrations (<3 μ M), we observed significant enrichment in both ¹⁸O and ¹⁷O with respect to the substrate water. The difference in δ¹⁸O between O₂ and water was about 4.5, 3, 5.5, and 7‰ in the diatom Phaeodactylum tricornutum, Nannochloropsis sp. (Eustigmatophyceae), the coccolithophore Emiliania huxleyi and the green alga Chlamydomonas reinhardtii, respectively. The difference in δ¹⁷O was about 0.52 that of δ¹⁸O. As explained, the observed enrichments most probably stem from considerable oxygen consumption during photosynthesis even when major O₂-consuming reactions such as photorespiration were minimized. These enrichments increased linearly with rising O₂ levels but with different δ¹⁷O/δ¹⁸O slopes for the various organisms, suggesting engagements of different O₂-consuming reactions with rising O₂ levels. Consumption of O₂ may be important for energy dissipation during photosynthesis. The isotope enrichment observed here, not accounted for in earlier assessments, closes an important gap in our understanding of the difference between the isotopic compositions of atmospheric oxygen and that of seawater, i.e., the Dole effect.