ENVIRONMENTAL FACTORS CONTROLLING PHYTOPLANKTON PROCESSES IN THE SOUTHERN OCEAN1

By Philip W. Boyd. 2002

312 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

Iron‐light interactions differ in Southern Ocean phytoplankton (2012, background): “Although iron limitation plays a major role in maintaining high-nitrate, low-chlorophyll (HNLC) conditions across much of the S. Ocean, other environmental factors also contribute to this HNLC condition (Boyd 2002).”
The fate of biogenic iron during a phytoplankton bloom induced by natural fertilisation: Impact of copepod grazing (2008, methodology): “Our estimation of Fe supply and regeneration allowed us to estimate a fe ratio as defined by Boyd et al. (2005). During KEOPS, the fe ratio equalled 0.”
PHOTOSYNTHESIS AND COLD ACCLIMATION: MOLECULAR EVIDENCE FROM A POLAR DIATOM 1 (2004, background): “RNA helicases catalyze the unwinding of RNA duplexes and secondary structures in an ATPdependent manner (De la Cruz et al. 1999).”
Spinning the “Ferrous Wheel”: The importance of the microbial community in an iron budget during the FeCycle experiment (2005, background): “ccus are not present in the polar Southern Ocean, presumably due to low temperature [Boyd, 2002].”
Regional scale characteristics of the seasonal cycle of chlorophyll in the Southern Ocean (2011, background): “…it is largely accepted that the key factors exerting bottom up control of phytoplankton production in this, the largest “high nitrate-low chlorophyll (HNLC)” region in the world ocean (Minas and Minas, 1992) is the availability of light, iron (Fe) and silicic acid (Boyd, 2002; Arrigo et al., 2008).”