Palms are a keystone species in tropical rainforests and are thought of as a model species due to their abundance and taxonomic diversity. Because over 90% of palm species diversity is concentrated in the tropical and subtropical biomes today, palm fossils are traditionally interpreted as indicators of warm and wet climate. However, recent work suggests that, in the past, palms may have played an important role also in other biomes. Palms produce great amounts of phytoliths (hardened silica bodies precipitated in and around plant cells), which, after the plant dies, are incorporated into the soil or sediment and preserved as fossils. Importantly, phytoliths are found in many environments where leaf impressions and other macrofossil are typically absent. Palm phytoliths are therefore a valuable potential source of information to reconstruct phylogenetic relationships and interpret the ecology of fossil palms and, by inference, paleoenvironments.Unfortunately, very little work has been done to comprehensively assess how much information about palm taxonomy and ecology can be inferred by palm phytolith morphology. To remedy this, we are conducting a morphometric study of palm phytoliths across the palm phylogenetic tree. We collected leaf samples from 80 palm taxa from herbaria and botanical gardens, then extracted phytoliths using strong oxidants and acids to decompose organic materials. Through measurement of their overall shape and size, as well as the density, size, and shape of phytolith ornamentation we hope to improve overall taxonomic resolution of the palm fossil record. In addition, for each of the taxa we recorded several habitat, climate, and ecology variables to test for biogeographical and ecological signal in palm phytolith morphology.