Understanding impacts of global warming on phytoplankton-the foundation of marine ecosystems-is critical to predicting changes in future biodiversity, ocean productivity, and ultimately fisheries production. Using phytoplankton community abundance and environmental data that span ∼90 years (1931-2019) from a long-term Pacific Ocean coastal station off Sydney, Australia, we examined the response of the phytoplankton community to long-term ocean warming using the Community Temperature Index (CTI), an index of the preferred temperature of a community. With warming of ∼1.8 • C at the site since 1931, we found a significant increase in the CTI from 1931-1932 to 2009-2019, suggesting that the relative proportion of warm-water to cold-water species has increased. The CTI also showed a clear seasonal cycle, with highest values at the end of austral summer (February/March) and lowest at the end of winter (August/September), a pattern well supported by other studies at this location. The shift in CTI was a consequence of the decline in the relative abundance of the cool-affinity (optimal temperature = 18.7 • C), chain-forming diatom Asterionellopsis glacialis (40% in 1931-1932 to 13% in 2009 onward), and a substantial increase in the warm-affinity (21.5 • C), also chain-forming diatom Leptocylindrus danicus (20% in 1931-1932 to 57% in 2009 onward). L. danicus reproduces rapidly, forms resting spores under nutrient depletion, and displays a wide thermal range. Species such as L. danicus may provide a glimpse of the functional traits necessary to be a "winner" under climate change.