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terrestrial pollen records are abundant and widely distributed, making them an excellent proxy for past vegetation dynamics. age-depth models relate pollen samples from sediment cores to a depositional age based on the relationship between sample depth and available chronological controls. Large-scale synthesis of pollen data benefit from consistent treatment of age uncertainties. Generating new age models helps to reduce potential artifacts from legacy age models that used outdated techniques.doi:10.2475/ajs.s5-28.166.304 fatcat:d3aq5z3jufabfje2uqp4w4ecny