The temperature sensitivity of phytoplankton growth rates, parameterized as the activation energy (E a ) in the Boltzmann-Arrhenius equation, is critical to determining how global warming will affect marine ecosystems and the efficiency of the biological pump in the ocean. We applied both linear and nonlinear regression models to two laboratory temperature-growth experimental datasets to estimate the E a of each taxon of phytoplankton and heterotrophic protists. We found that phytoplankton E a and normalized growth rates depended strongly on community composition. Diatoms grew more rapidly and had lower E a values, whereas cyanobacteria grew more slowly and had higher E a values. The phytoplankton E a was underestimated by a single OLS regression on the pooled dataset because slowly growing cyanobacteria dominated in warm, oligotrophic ocean gyres, and rapidly growing diatoms dominated in cold, nutrient-rich waters. By contrast, the median E a values estimated from individual experiments did not differ between phytoplankton and heterotrophic protists. Our results suggest that phytoplankton community composition needs to be considered when trying to predict the effects of ocean warming on ecosystem productivity and metabolism.Temperature sensitivity of phytoplankton growth rate plays a critical role in determining the response of primary production to ocean warming in global-scale ocean models (Sarmiento et al. 2004;Taucher and Oschlies 2011) as well as the response to seasonal and other temperature changes. The Metabolic Theory of Ecology (MTE) predicts that the mean activation energy (E a ) of metabolism should be around 0.65 eV Brown et al. 2004). The E a for photosynthesis, however, is thought to be significantly lower than the value ($ 0.65 eV) for heterotrophic activities such as community respiration and zooplankton grazing . This difference has profound implications, in that rising temperature would tend to preferentially enhance heterotrophy, and with it the release of CO 2 , potentially leading to a positive feedback to climatic warming (L opez- Urrutia et al. 2006). This difference of temperature sensitivity might also be the critical factor causing low carbon export efficiency in low latitude, warm oceans compared to high latitude regions (Laws et al. 2000).In the literature, estimates of E a differ as a function of methodologies and datasets. One of the earliest and most widely used temperature coefficients (Q 10 5 1.88, corresponding to an E a of 0.41 eV) given by Eppley (1972) and later confirmed by Rose and Caron (2007) and Bissinger et al. (2008), was estimated by fitting the upper envelope of phytoplankton growth rate vs. temperature in a pooled laboratory dataset. Some studies have argued that fitting the upper envelope is inappropriate and have instead used ordinary least squares (OLS) regression to fit mean growth rates under optimal conditions, the result being a slightly lower estimate ($ 0.3 eV) of E a (Sal and L opez-Urrutia 2011). An E a of 0.3 eV is more consistent with the resu...