Basin-scale variability of phytoplankton bio-optical characteristics in relation to bloom state and community structure in the Northeast Atlantic
By CM Moore, M. Lucas, R. Sanders, R. Davidson. 2005
108 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/d35fbe8222b7f7df880aa066273c8a6231ed7585
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In Ecology
- David John Suggett
- R. Geider
- CM Moore
- S. Hennige
- Mark E. Warner
- Anna Hickman
- David C. Smith
- Kathleen Emma McDougall
In Oceanography
- David John Suggett
- R. Geider
- CM Moore
- Mark E. Warner
- S. Hennige
- Anna Hickman
- David C. Smith
- Kathleen Emma McDougall
Citations in the corpus
- Major contribution of diatom resting spores to vertical flux in the sub-polar North Atlantic (2013, background): “The species composition at the surface was typical of phytoplankton communities during the spring bloom in this region (Moore et al., 2005; Sieracki et al., 1993); phytoplankton chlorophyll and carbon concentrations in surface waters were average for the peak of the North Atlantic spring bloom…”
- Investigation and sensitivity analysis of a mechanistic phytoplankton model implemented in a new modular numerical tool (Eco3M) dedicated to biogeochemical modelling (2006, background): “Natural phytoplanktonic populations 401–798 Moore et al. (2005) Culture (Chlorella pyrenoidosa) 282–350 Kolber et al. (1998) Culture 101–1000 Olson et al. (1996) Individual algal cells 300–581 Gorbunov et al. (1999)”
- Photobiology of Symbiodinium revisited: bio-physical and bio-optical signatures (2009, methodology): “Since PI and cell size influence absorption (Laurion et al. 2004; Moore et al. 2005), algal pigments were expressed relative to chlorophyll a to enable cross comparison between types.”
- Phytoplankton photoacclimation and photoadaptation in response to environmental gradients in a shelf sea (2006, background): “As previously noted (Moore et al. 2005), such covariability is expected at 478 nm, i.”
- Interpretation of fast repetition rate (FRR) fluorescence: signatures of phytoplankton community structure versus physiological state (2009, methodology): “6D), >50% of the variance in σPSII (478) across the Atlantic Ocean from ~50° N to 40°S could be explained by Hex/ΣDP + But/ΣDP (Fig.”