Iron requirements of the pennate diatom Pseudo‐nitzschia: Comparison of oceanic (high‐nitrate, low‐chlorophyll waters) and coastal species

By A. Marchetti, M. T. Maldonado, Erin S. Lane, P. Harrison. 2006

111 citations recorded by the source corpus.

Subfields: Biomaterials, Oceanography

View Paper: https://www.semanticscholar.org/paper/8a6274f28aba48e173e8682bee877ebb99559b80

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In Biomaterials

1. Stephen Bates
2. W. Cochlan
3. V. Trainer
4. Anne E. Thessen
5. H. Hégaret
6. A. Lelong
7. P. Soudant
8. P. Harrison

In Oceanography

1. Stephen Bates
2. V. Trainer
3. W. Cochlan
4. Philip W. Boyd
5. H. Hégaret
6. P. Soudant
7. A. Lelong
8. P. Harrison

Citations in the corpus

• Pseudo-nitzschia physiological ecology, phylogeny, toxicity, monitoring and impacts on ecosystem health (2012, background): “1 ) (Marchetti et al., 2004, 2006, 2008), the mesoscale iron-fertiliza-tion experiments (cf. reviews by de Baar et al., 2005; Boyd et al., 2007), starting in the 1990s, have provided some opportunist information on both Pseudo-nitzschia competition and DA production.”
• Pseudo-nitzschia (Bacillariophyceae) species, domoic acid and amnesic shellfish poisoning: revisiting previous paradigms (2012, background): “Furthermore, such seed populations are capable of responding rapidly to periodic inputs of iron from aeolian deposition or intermittent upwelling and mixing (Marchetti et al. 2006b; Silver et al. 2010).”
• Iron‐light interactions differ in Southern Ocean phytoplankton (2012, background): “Since phytoplankton have considerable variation in their maximum and minimum cellular iron content (Marchetti et al. 2006), and the ability to store iron in excess of cellular iron requirements when iron supply exceeds demand, we cannot reliably infer how cellular iron requirements change with…”
• Regional impacts of iron-light colimitation in a global biogeochemical model (2009, methodology): “…limitation is expressed by the term Deffe as described below.20 In calculating DefFe we represent the fact that, in contrast to nitrogen and carbon, Fe is taken up by phytoplankton in a highly variable ratio to phosphorus (e.g. Sunda and Huntsman, 1997; Marchetti et al., 2006b; Boyd et al., 2007).”
• Effects of iron limitation on intracellular cadmium of cultured phytoplankton: Implications for surface dissolved cadmium to phosphate ratios (2009, background): “Maldonado and Price, 1996; Marchetti et al., 2006 ).”