Phytoplankton in a changing world: cell size and elemental stoichiometry

By Z. Finkel, John Beardall, Kevin J. Flynn, Antonietta Quigg, T. Rees, J. Raven. 2010

1,137 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/e8235d6be6d7ac73bf9f325f1880020b585e8664

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In Oceanography

Citations in the corpus

Dissolved organic matter (DOM) release by phytoplankton in the contemporary and future ocean (2014, background): “Moreover, conditions of increased stratification and nutrient limitation would be expected to favour small-celled taxa (Finkel et al., 2010) with relatively large surface area to volume ratios and therefore greater potential for DOM loss via leakage.”
Dimensions of marine phytoplankton diversity (2019, background): “This unimodal distribution has been observed (e.g. Raven, 1994; Bec et al., 2008; Finkel et al., 2010; Marañón et al., 2013; Sommer et al., 2017) and explained as a trade-off between replenishing cell quotas versus synthesizing new biomass (Verdy et al.”
Ocean acidification enhances the growth rate of larger diatoms (2014, background): “Increasing CO2 and other greenhouse gases are significantly altering atmospheric and ocean circulation and chemistry and are expected to affect phytoplankton primary production and community structure (Finkel et al. 2010).”
The Haber Bosch–harmful algal bloom (HB–HAB) link (2014, background): “However, P limitation in lakes is not universal (Lewis and Wurtsbaugh 2008) as some regions are either naturally (Finlay et al 2010) or culturally enriched (Bennett et al 2001) in P relative to N, and excess N loading is changing the nutrient stoichiometry and limiting element in some coastal areas…”
Temperature, resources, and phytoplankton size structure in the ocean (2012, background): “…determines the trophic organization of pelagic ecosystems and thus the efficiency with which organic matter produced by photosynthesis is channeled towards upper trophic levels or exported to the ocean’s interior (Legendre and Rassoulzadegan 1996; Falkowski and Oliver 2007; Finkel et al. 2010).”
Phytoplankton niches estimated from field data (2012, background): “Changes in climate will affect the distribution and productivity of phytoplankton in the ocean (Behrenfeld et al. 2006; Finkel et al. 2010).”
The biological pump in a high CO 2 world (2012, background): “Nevertheless, indications of preferential remineralization of nitrogen during sedimentation are observed (see overview in Boyd & Trull 2007) and oceanic nutrient ratios are found to be dynamic on decadal to geological scales (Finkel et al. 2010, Deutsch & Weber 2012).”
Global biogeochemical impacts of phytoplankton: a trait‐based perspective (2015, background): “Changes in the stoichiometry of individual species can be of similar magnitude to effects driven by turnover between species (Behrenfeld et al. 2006; Finkel et al. 2009).”
Does warming enhance the effect of microzooplankton grazing on marine phytoplankton in the ocean? (2012, background): “Similarly, temperature–growth relationships for phytoplankton can differ for individual species and mixed communities because of temperature covariance of growth-relevant factors like light, nutrients, and cell size (Lopez-Urrutia et al. 2006; Chen and Liu 2010; Finkel et al. 2010).”