Phytoplankton photosynthetic competence, underway data of SOIREE cruise track 1999-02-08 to 1999-02-24

• Main Authors: Boyd, Philip W, Abraham, Edward R
• Format: Dataset
• Language: English
• Published: PANGAEA 2001
• Subjects: CT; DATE/TIME; DEPTH; water; Fast repetition rate fluorometry (FRRF) (Kolber & Falkowski; 1993); Fluorescence; chlorophyll; Fluorometer; Chelsea Instruments; JGOFS; Joint Global Ocean Flux Study; Photosynthetic competence; Quantum Irradiance Meter; LI-COR Inc.; Radiation; photosynthetically active; SOIREE; SOIREE-track; Southern Ocean - Australasian-Pacific Sector; Tangaroa; Underway cruise track measurements; Southern Ocean; Subarctic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.121468; https://doi.org/10.1594/PANGAEA.121468

Active fluorescence (fast repetition rate fluorometry, FRRF) was used to follow the photosynthetic response of the phytoplankton community during the 13-day Southern Ocean Iron RElease Experiment (SOIREE). This in situ iron enrichment was conducted in the polar waters of the Australasian-Pacific sector of the Southern Ocean in February 1999. Iron fertilisation of these high nitrate low chlorophyll (HNLC) waters resulted in an increase in the photosynthetic competence (Fv/Fm) of the resident cells from around 0.20 to greater than 0.60 (i.e. close to the theoretical maximum) by 10/11 days after the first enrichment. Although a significant iron-mediated response in Fv/Fm was detected as early as 24 h after the initial fertilisation, the increase in Fv/Fm to double ambient levels took 6 days. This response was five-fold slower than observed in iron enrichments (in situ and in vitro) in the HNLC waters of the subarctic and equatorial Pacific. Although little is known about the relationship between water temperature and Fv/Fm, it is likely that low water temperatures - and possibly the deep mixed layer - were responsible for this slow response time. During SOIREE, the photosynthetic competence of the resident phytoplankton in iron-enriched waters increased at dissolved iron levels above 0.2 nM, suggesting that iron limitation was alleviated at this concentration. Increases in Fv/Fm of cells within four algal size classes suggested that all taxa displayed a photosynthetic response to iron enrichment. Other physiological proxies of algal iron stress (such as flavodoxin levels in diatoms) exhibited different temporal trends to iron-enrichment than Fv/Fm during the time-course of SOIREE. The relationship between Fv/Fm, algal growth rate and such proxies in Southern Ocean waters is discussed.