Photoacclimation and nutrient-based model of light-saturated photosynthesis for quantifying oceanic primary production

By Michael J. Behrenfeld, Emilio Marañón, D. Siegel, S. Hooker. 2002

176 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/ecd6e7e91806224d5b007c6e965ef91fdb83dd66

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Citations in the corpus

Carbon‐based ocean productivity and phytoplankton physiology from space (2005, background): “The dependency of Chl:C on light can be modeled for a range of growth conditions as an exponential function of light [Cloern et al., 1995; Behrenfeld et al., 2002], such as Chl : C ¼ Chl : Cmin þ Chl : Cmax Chl : Cmin½ exp 3 Ig : ð1Þ [20] To more quantitatively link satellite Chl:C data with…”
Carbon‐to‐chlorophyll ratio for phytoplankton in temperate coastal waters: Seasonal patterns and relationship to nutrients (2016, methodology): “The literature data behind the parameters in Table 2 and the model study by Behrenfeld et al. (2005) suggests that C:Chl a ratios in open oceans are often considerably higher, often well above 100. A possible explanation is that at lower latitudes or in open oceanic ecosystems with more permanent nu”
Phytoplankton carbon fixation chlorophyll-biomass and diagnostic pigments in the Atlantic Ocean (2006, background): “, 2000) have previously been related to changes in the chlorophyll specific rate of carbon fixation (Marañón and Holligan, 1999; Behrenfeld et al., 2002).”
New cell-based model of photosynthesis and photo-acclimation: accumulation and mobilisation of energy reserves in phytoplankton (2009, background): “Satellite-based Chl estimates are among the few data sets to which the output from such global climate models can be compared (Morel & Berthon 1989, Behrenfeld et al. 2002).”
High variability of primary production in oligotrophic waters of the Atlantic Ocean: uncoupling from phytoplankton biomass and size structure (2003, unknown): “…between our measured values of P Bopt and P Bmax and the results of the PhotoAcc model, which reproduces the variability in Calvin cycle capacity as a function of nutrient status, which in turn is inferred from the relative positions of the nitracline and the pycnocline (Behrenfeld et al. 2002).”
Can macroalgae contribute to blue carbon? An Australian perspective (2015, background): “The oceans are by far the largest carbon sinks, estimated to hold around 37,000 Gt of inorganic carbon (Raven and Falkowski 1999), with approximately 2 Gt of additional carbon absorbed each year via physico-chemical processes (Behrenfeld et al. 2002).”