TY - JOUR
T1 - Cyanobacteria-Dominated Phytoplankton in the Oligotrophic South China Sea Maintain Photosynthetic Potential Despite Diurnal Photoinactivation of PSII
AU - Yi, Xiangqi
AU - Zhang, Di
AU - Sun, Jiazhen
AU - Beardall, John
AU - Gao, Kunshan
N1 - Funding Information:
The authors would like to thank the laboratory engineers Xianglan Zeng and Wenyan Zhao for their logistic and technical supports.
Publisher Copyright:
© Copyright © 2021 Yi, Zhang, Sun, Beardall and Gao.
PY - 2021/10/29
Y1 - 2021/10/29
N2 - In the warm, oligotrophic oceans, phytoplankton frequently experience high light exposure and must compete for a potentially limited nutrient supply. Additionally, the light regimes are dynamic in view of the diel solar cycle, weather conditions, and depth. Dealing with these challenges is critical to their survival. Here, we explored, using active chlorophyll a fluorescence, the photophysiological responses of cyanobacteria-dominated phytoplankton assemblages to intra-day variations in the light regime in the oligotrophic South China Sea (SCS). Experiments were conducted at three stations (SEATS, DC2, and DC6) where phytoplankton communities were dominated by Prochlorococcus and Synechococcus, and environmental conditions were similar except for daytime light conditions. We found that, at each station, the maximum quantum yield of PSII (Fv/Fm) at dawn was as high as ∼0.5, although concentrations of both dissolved inorganic nitrogen and soluble reactive phosphate were below the detection limits. Subsequently, diurnal patterns of Fv/Fm diverged between stations. At stations DC2 and DC6, we observed significant drops (25–48%) of Fv/Fm around midday, coinciding with the incident solar photosynthetically active radiation (PAR) reaching over 2,000 μmol quanta m–2 s–1, but Fv/Fm was nearly stable at SEATS where the daily maximal PAR was less than 1,000 μmol quanta m–2 s–1. Further analysis suggests that the midday drops in Fv/Fm at DC2 and DC6 were a consequence of high light-induced PSII photoinactivation. On the other hand, we found that the patterns of diurnal variation in maximum relative electron transport rate (rETRmax) presented as being unimodal with a peak around midday at all three stations. Furthermore, we found that the diurnal pattern of rETRmax was mainly controlled by the extent of photochemical quenching (qP) which reflects the redox status of electron carriers downstream of PSII. In conclusion, our results indicate that, in the oligotrophic SCS, through increasing the activity of the electron-consuming mechanisms (high qP), the phytoplankton communities are able to maintain their midday photosynthetic potential (high rETRmax) even with a degree of PSII photoinactivation (low Fv/Fm).
AB - In the warm, oligotrophic oceans, phytoplankton frequently experience high light exposure and must compete for a potentially limited nutrient supply. Additionally, the light regimes are dynamic in view of the diel solar cycle, weather conditions, and depth. Dealing with these challenges is critical to their survival. Here, we explored, using active chlorophyll a fluorescence, the photophysiological responses of cyanobacteria-dominated phytoplankton assemblages to intra-day variations in the light regime in the oligotrophic South China Sea (SCS). Experiments were conducted at three stations (SEATS, DC2, and DC6) where phytoplankton communities were dominated by Prochlorococcus and Synechococcus, and environmental conditions were similar except for daytime light conditions. We found that, at each station, the maximum quantum yield of PSII (Fv/Fm) at dawn was as high as ∼0.5, although concentrations of both dissolved inorganic nitrogen and soluble reactive phosphate were below the detection limits. Subsequently, diurnal patterns of Fv/Fm diverged between stations. At stations DC2 and DC6, we observed significant drops (25–48%) of Fv/Fm around midday, coinciding with the incident solar photosynthetically active radiation (PAR) reaching over 2,000 μmol quanta m–2 s–1, but Fv/Fm was nearly stable at SEATS where the daily maximal PAR was less than 1,000 μmol quanta m–2 s–1. Further analysis suggests that the midday drops in Fv/Fm at DC2 and DC6 were a consequence of high light-induced PSII photoinactivation. On the other hand, we found that the patterns of diurnal variation in maximum relative electron transport rate (rETRmax) presented as being unimodal with a peak around midday at all three stations. Furthermore, we found that the diurnal pattern of rETRmax was mainly controlled by the extent of photochemical quenching (qP) which reflects the redox status of electron carriers downstream of PSII. In conclusion, our results indicate that, in the oligotrophic SCS, through increasing the activity of the electron-consuming mechanisms (high qP), the phytoplankton communities are able to maintain their midday photosynthetic potential (high rETRmax) even with a degree of PSII photoinactivation (low Fv/Fm).
KW - active Chl a fluorescence
KW - diurnal variation
KW - photoinactivation
KW - phytoplankton
KW - South China Sea
UR - http://www.scopus.com/inward/record.url?scp=85119058433&partnerID=8YFLogxK
U2 - 10.3389/fmars.2021.736586
DO - 10.3389/fmars.2021.736586
M3 - Article
AN - SCOPUS:85119058433
SN - 2296-7745
VL - 8
JO - Frontiers in Marine Science
JF - Frontiers in Marine Science
M1 - 736586
ER -