The transport properties of liquid iron alloys at high pressure (P) and temperature (T) are essential for understanding the formation, composition, and evolution of planetary cores.Light alloying elements (e.g., Si, O, S, C, N, H) in liquid iron are particularly relevant due to the density deficit of Earth's core, yet high P-T experimental diffusion studies involving such alloys remain scarce with large uncertainties on the P and T dependence required for extrapolation to core conditions. In this study, we measured the chemical diffusion rates of carbon in liquid iron over a P-T range of 3-15 GPa and 1700-2450 K using a multi-anvil apparatus. Diffusion couples consisting of pure Fe and Fe-2.5wt.%C cylinders were placed end-to-end in an MgO capsule in a vertical orientation. Carbon concentration profiles were measured by electron microprobe and modeled numerically to correct for non-isothermal diffusion that occurred prior to reaching the peak temperature. Carbon diffusion coefficients range from 6 × 10 −9 m 2 •s −1 to 2 × 10 −8 m 2 •s −1 , with global Arrhenian fit parameters D 0 = 1.4 ± 0.5 × 10 −7 m 2 •s −1 , ΔE = 43 ± 6 kJ•mol −1 , and ΔV = −0.06 ± 0.19 cm 3 •mol −1 . A negligible P effect is consistent with previous studies of oxygen diffusion in liquid iron and high-T This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.