作者：K. Muenzner, E. S. Lindstrom and T. Rohrlack

Boreal lakes are generally seen as sources of carbon dioxide (CO₂) to the atmosphere, even though a part of them are periodically undersaturated with CO₂ and have the potential to be net-autotrophic. This undersaturation is the result of photosynthetic activity by phytoplankton, especially flagellated species like Gonyostomum semen, which form high-biomass blooms in brown water lakes. We hypothesized that CO₂ reduction by G. semen is common across boreal lakes, and that those reductions vary with dissolved organic carbon (DOC) concentrations across lakes. In our field study, we explored how G. semen abundance affected the partial pressure of CO₂ (p CO₂) in the water column and the estimated carbon flux to the atmosphere in four lakes in Sweden and Norway in summer 2021. We found that lake p CO₂ and carbon flux to the atmosphere decreased with increasing G. semen abundances, though all lakes still emitted CO₂ to the atmosphere. High DOC concentrations acted as a limiting factor for G. semen growth, indicating that G. semen's potential to reduce p CO₂ and carbon flux to the atmosphere weakens with increasing DOC concentrations. Still, G. semen's impact on p CO₂ and carbon flux to the atmosphere is relevant in a wider spatial context, because G. semen and other motile flagellated species are expected to increase in range and bloom frequency in boreal lakes. Thus, we propose that CO₂ fixation via photosynthesis is an underestimated factor in controlling CO₂ dynamics in boreal lakes, and that it should be included in large-scale CO₂ budget calculations.

（来源：Limnology and Oceanography 2025   DOI: 10.1002/lno.70081）