Phytoliths are microscopic silica structures produced in plant tissue, and palms (family Arecaceae) are prolific producers of them. The stability of these structures contributes to the abundance of palms within the fossil record, as these structures can fossilize in sediments where leaves cannot, providing a wider range of evidence of the past palm geographic distribution. Palms generally grow in warmer and wetter environments, but certain species can live in more extreme climates (i.e., cold, dry). However, because 90% of palms are currently distributed around the equator and tropical rainforests, they are often used as an indicator of warmer environments in the fossil record. The current understanding of the taxonomic groups below the family level is limited, and it is unclear whether palm phytolith shape can be used to identify different palm groups in the fossil record. The Palm Project hopes to address this gap by testing phytolith classification using a morphometric approach. Over 100 species of known modern Arecaceae (~30 images/species) phytoliths have been imaged with a confocal microscope, and a semi-automated script in ImageJ quantifies the overall shape (globular or hat), density, and size of the phytolith ornamentations. Next, multivariate analysis on the morphometric data attempts to distinguish the phytoliths of various modern subfamilies based on distinct morphological traits, forming a quantitative baseline to describe and classify phytoliths. When combined with the collected ecological data, this could potentially identify signals between the environment of modern palm species and the phytoliths they form. Once the morphological differences between groups of modern palms are quantified, the same analysis can be applied to fossil phytoliths of unknown origins. This could reveal which taxonomic and ecological groups they belong to based on the most similar modern phytolith, giving insight into the phylogeny of Arecaceae and the paleoenvironment the fossils came from.