Abstract
Lakes located in the boreal region are generally supersaturated with carbon dioxide (CO(2)), which emerges from inflowing inorganic carbon from the surrounding watershed and from mineralization of allochthonous organic carbon. While these CO(2) sources gained a lot of attention, processes that reduce the amount of CO(2) have been less studied. We therefore examined the CO(2) reduction capacity during times of phytoplankton blooms. We investigated partial pressure of CO(2) (pCO(2)) in two lakes at times of blooms dominated by the cyanobacterium Gloeotrichia echinulata (Erken, Sweden) or by the nuisance alga Gonyostomum semen (Erssjön, Sweden) during two years. Our results showed that pCO(2) and phytoplankton densities remained unrelated in the two lakes even during blooms. We suggest that physical factors, such as wind-induced water column mixing and import of inorganic carbon via inflowing waters suppressed the phytoplankton signal on pCO(2). These results advance our understanding of carbon cycling in lakes and highlight the importance of detailed lake studies for more precise estimates of local, regional and global carbon budgets.