Iron-mediated changes in phytoplankton photosynthetic competence during SOIREE
By Philip W. Boyd, E. Abraham. 2001
171 citations recorded by the source corpus.
Subfields: Environmental Chemistry, Oceanography
View Paper: https://www.semanticscholar.org/paper/54687d5de2b9aa3e120c751d9bd86340b243e397
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In Environmental Chemistry
In Oceanography
Citations in the corpus
- The impact of in situ Fe fertilisation on the microbial food web in the Southern Ocean (2001, methodology): “For the picophytoplankton this suggests that the stimulation of the population (Boyd and Abraham, 2001) was quickly controlled as suggested by Morel et al.”
- ENVIRONMENTAL FACTORS CONTROLLING PHYTOPLANKTON PROCESSES IN THE SOUTHERN OCEAN1 (2002, background): “…trace elements such as iron (Sunda and Huntsman 1997), there is evidence that smaller cells are also slightly iron limited, with iron-mediated increases in Fv/Fm for cells less than 5 and less than 2 m during shipboard (Olson et al. 2000) and in situ iron enrichments (Boyd and Abraham 2001).”
- The effect of in situ iron addition on the sinking rates and export flux of Southern Ocean diatoms (2001, background): “The decrease in sinking rates over time after iron addition mirrors the physiological reduction in Fe-stress as observed in other physiological proxies such as Fv/Fm (Boyd and Abraham, 2001).”
- Interpretation of fast repetition rate (FRR) fluorescence: signatures of phytoplankton community structure versus physiological state (2009, methodology): “Published data by Steglich et al. (2001) and Bruyant et al. (2005) both demonstrate that Prochlorococcus marinus is characterized by relatively high values of Fv/Fm (ca. 0.55 to 0.65) and low values of σPSII (478) (ca. 300 to 600), suggesting that they fall along the eukaryote rather than the…”
- Direct estimation of functional PSII reaction center concentration and PSII electron flux on a volume basis: a new approach to the analysis of Fast Repetition Rate fluorometry (FRRf) data (2012, background): “For example, a number of studies in large, ironlimited ocean regions have indicated a doubling in the value of this parameter when iron was supplied; typically, from a value of around 0.3 to 0.6 (Behrenfeld et al. 1996; Boyd and Abraham 2001; Behrenfeld et al. 2004; Moore et al. 2007).”
- The evolution and termination of an iron‐induced mesoscale bloom in the northeast subarctic Pacific (2005, methodology): “Discrete samples from a range of depths in the mixed layer were analyzed for photosynthetic competence (Fv/Fm) of the phytoplankton community following procedures outlined in Boyd and Abraham (2001).”