bution of miliacin (olean-18-en-3β-ol methyl ether) and related compounds in broomcorn millet (Panicum miliaceum) and other reputed sources: Implications for the use of sedimentary miliacin as a tracer of millet. Organic Geochemistry, Elsevier, 2013Elsevier, , 63, pp.48-55. <10.1016Elsevier, /j.orggeochem.2013 Miliacin biosynthesis has been proposed for other Panicum species, Setaria italica (Italian or foxtail millet), Pennisetum sp., and Chaetomium olivaceum (an olive green mold). We found miliacin concentrations in seeds of different varieties of P. miliaceum to be similarly high (with trace amounts of β-and α-amyrin methyl ethers). It was absent from hulls and roots, and nominally present in leaves and stems. The transfer of miliacin from plant to sediments is therefore mostly from seeds. Miliacin was abundant (often with larger amounts of β-and α-amyrin methyl ethers) in all other Panicum species studied but only in some species of the genus Pennisetum and absent in * Corresponding author e-mail address: jeremy.jacob@univ-orleans.fr 2 Setaria italica. Neither C. olivaceum nor its growth medium (rice) showed any trace of miliacin.Our results of no miliacin from S. italica and C. olivaceum , high miliacin concentrations in seed of P. miliaceum relative to other PTMEs and to other grasses, and considering the high biomass that cultivated broomcorn millet has relative to other potential plant sources, support the use of sedimentary records of miliacin in some contexts, to track past millet agricultural dynamics.