Diurnal variation in the coupling of photosynthetic electron transport and carbon fixation in iron-limited phytoplankton in the NE subarctic Pacific

• Main Authors: N. Schuback, M. Flecken, M. T. Maldonado, P. D. Tortell
• Format: Article
• Language: English
• Published: Copernicus Publications 2016-02-01
• Series: Biogeosciences
• Online Access: http://www.biogeosciences.net/13/1019/2016/bg-13-1019-2016.pdf
• ISSN: 1726-4170; 1726-4189

Active chlorophyll <i>a</i> fluorescence approaches, including fast repetition rate fluorometry (FRRF), have the potential to provide estimates of phytoplankton primary productivity at an unprecedented spatial and temporal resolution. FRRF-derived productivity rates are based on estimates of charge separation in reaction center II (ETR_RCII), which must be converted into ecologically relevant units of carbon fixation. Understanding sources of variability in the coupling of ETR_RCII and carbon fixation provides physiological insight into phytoplankton photosynthesis and is critical for the application of FRRF as a primary productivity measurement tool. In the present study, we simultaneously measured phytoplankton carbon fixation and ETR_RCII in the iron-limited NE subarctic Pacific over the course of a diurnal cycle. We show that rates of ETR_RCII are closely tied to the diurnal cycle in light availability, whereas rates of carbon fixation appear to be influenced by endogenous changes in metabolic energy allocation under iron-limited conditions. Unsynchronized diurnal oscillations of the two rates led to 3.5-fold changes in the conversion factor between ETR_RCII and carbon fixation (<i>K</i>_c / <i>n</i>_PSII). Consequently, diurnal variability in phytoplankton carbon fixation cannot be adequately captured with FRRF approaches if a constant conversion factor is applied. Utilizing several auxiliary photophysiological measurements, we observed that a high conversion factor is associated with conditions of excess light and correlates with the increased expression of non-photochemical quenching (NPQ) in the pigment antenna, as derived from FRRF measurements. The observed correlation between NPQ and <i>K</i>_c / <i>n</i>_PSII requires further validation but has the potential to improve estimates of phytoplankton carbon fixation rates from FRRF measurements alone.</p>