Late Triassic through Early Cretaceous detrital zircon separated from Lower Cretaceous sedimentary strata provides a record of arc magmatism that is not obscured by products of the mid- to Late Cretaceous surge, which dominate the exposed Sierra Nevada batholith. Matching U-Pb age-probability maxima to U-Pb dates of exposed arc plutonic rocks provides confirmation that the detrital zircon was sourced in the erupting and eroding Sierra Nevada arc. These data suggest that magmatic productivity in the southwestern arc increased steadily through the Middle Jurassic, from an Early Jurassic lull through the Late Jurassic. The detrital-zircon record documents an original footprint of the Early Cretaceous arc extending from its current exposure in the western Sierra Nevada foothills northwestward into the eastern Sacramento Valley, where its relatively mafic roots are presumably buried beneath younger sedimentary strata infilling the Great Valley. The sparse record of Late Triassic magmatism preserved in the analyzed intra-arc and forearc deposits likely reflects greater separations in both time and space between the Early Cretaceous basins and the Triassic arc. Analysis of an atypically dense sample set from the Goldstein Peak Formation intra-arc basin deposits, in conjunction with new data from the Lower Cretaceous Gravelly Flat Formation and published data from other Lower Cretaceous forearc strata of the Great Valley Group, suggests that an even greater density and broader geographic distribution of detrital-zircon samples are needed to more completely reconstruct the record of arc magmatism.