Temperature and nutrient supply interactively control phytoplankton growth and productivity,
yet the role of these drivers together still has not been determined experimentally over large
spatial scales in the oligotrophic ocean. We conducted four microcosm experiments in the
tropical and subtropical Atlantic (29°N-27°S) in which surface plankton assemblages were
exposed to all combinations of three temperatures (in situ, 3 °C warming and 3 °C cooling)
and two nutrient treatments (unamended and enrichment with nitrogen and phosphorus).
We found that chlorophyll a concentration and the biomass of picophytoplankton consistently increase in response to nutrient addition, whereas changes in temperature have a
smaller and more variable effect. Nutrient enrichment leads to increased picoeukaryote
abundance, depressed Prochlorococcus abundance, and increased contribution of small
nanophytoplankton to total biomass. Warming and nutrient addition synergistically stimulate
light-harvesting capacity, and accordingly the largest biomass response is observed in the
warmed, nutrient-enriched treatment at the warmest and least oligotrophic location (12.7°N).
While moderate nutrient increases have a much larger impact than varying temperature upon
the growth and community structure of tropical phytoplankton, ocean warming may increase
their ability to exploit events of enhanced nutrient availabilit