51. Seasonal and Daily‐Scale Photoacclimation Modulating the Phytoplankton Chlorophyll‐Carbon Coupling Relationship in the Mid‐Latitude Northwest Pacific.
- Author
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Xing, Xiaogang, Boss, Emmanuel, Chen, Shuangling, and Chai, Fei
- Subjects
MARINE phytoplankton ,MARINE plankton ,MARINE plants ,OCEAN temperature ,OCEANOGRAPHY - Abstract
Photoacclimation is a photo‐physiological mechanism of phytoplankton associated with the modulation of the ratio of phytoplankton chlorophyll (Chl) and carbon (C), yet little is known on how it modulates Chl dynamics and the Chl‐C coupling relationship in the mid‐latitude oceans. In this study, Chl and C estimated from optical sensors on three BGC‐Argo floats, provided a record of the biomass and physiological variability at high temporal and vertical resolutions in the mid‐latitude northwest Pacific. It is found that, despite the Chl seasonal cycle being mainly dominated by variability in biomass, Chl and C became decoupled and inversely correlated in winter, due to the dominant effect of photoacclimation. Although Chl and C co‐varied in spring and autumn, photoacclimation modulated the Chl‐C coupling relationship as well, leading to a faster increase in C and Chl, respectively, in spring and late autumn. On daily and synoptic scales, Chl dynamics were also driven by photoacclimation to a large extent. Particularly, during a typhoon event, both cloud cover and mixed‐layer dynamics introduced fast changes in mixed‐layer light level, resulting in quick photo‐physiological responses of phytoplankton in modulating the variances of Chl. Similarly, during wintertime mixing‐restratification events associated with abrupt mixed‐layer changes, photoacclimation muted the Chl response, leading to a faster increase in C than Chl. Plain Language Summary: Although chlorophyll concentration (Chl) has been widely used as a proxy for phytoplankton biomass abundance, it is co‐determined by biomass (in unit of carbon concentration, C) and photoacclimation, the physiological mechanism of phytoplankton cells which adjusts intracellular pigment density (Chl:C) in response to ambient light and nutrients. In this study, based on three BGC‐Argo floats, we investigated how biomass and photoacclimation modulated the Chl dynamics in the mid‐latitude northwest Pacific. It was found that biomass dynamics dominated Chl dynamics in spring and summer, while photoacclimation determined Chl variations in winter leading to an inverse correlation between Chl and C. Even during the biomass‐dominated seasons, photoacclimation played an important role resulting in a slower Chl accumulation than C in spring, but a faster Chl accumulation in late autumn. Remarkably, the Chl dynamics associated with short time‐scale events such as a typhoon and wintertime mixing‐restratification events were also highly affected by photoacclimation. Key Points: Phytoplankton chlorophyll and biomass dynamics were observed in the mid‐latitude northwest Pacific using BGC‐Argo floatsDuring biomass accumulation periods, pigment density was down‐regulated, associated with faster carbon increase than chlorophyllDuring late autumn, winter and typhoon events, photoacclimation, rather than biomass, dominated the mixed‐layer chlorophyll dynamics [ABSTRACT FROM AUTHOR]
- Published
- 2021
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