Temperature, resources, and phytoplankton size structure in the ocean

By Emilio Marañón, P. Cermeño, M. Latasa, R. Tadonléké. 2012

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Dissolved organic matter (DOM) release by phytoplankton in the contemporary and future ocean (2014, background): “Similarly, resource availability is key to explaining the success of different algal size classes at different temperatures in the contemporary ocean (Marañón et al., 2012).”
Modelling spatial and temporal patterns in size-structured marine plankton communities: top -down and bottom -up controls (2014, background): “Approximately half the data come from a global compilation of size-fractionated chlorophyll a measurements, including Atlantic Meridional Transect (AMT) cruises 2 and 3 (Marañón et al., 2012), with the remainder taken from AMT cruises 6, 8, 10 and 11.”
Thoughts on the evolution and ecological niche of diatoms (2021, background): “The presence of a large vacuole has also been repeatedly linked in the literature to diatom success for another reason: luxury nutrient uptake (Stolte and Riegman 1996, Maranón et al. 2012, 2015).”