The Pennsylvanian and Permian sedimentary units of the American Southwest hold valuable records of a significant major tectonic event that formed the Ancestral Rocky Mountains and associated basins, such as the Paradox and Pedregosa Basins. These mountains exposed Precambrian crystalline rocks, contributing debris into the basins, forming predominantly reddish sedimentary sequences, such as the Supai Group of Grand Canyon, and the Abo Formation and Yeso Group of New Mexico. Previous studies have indicated that components of these sedimentary sequences were derived from regions outside the Southwest, such as the Appalachian Mountains of that time.Central New Mexico contains well-exposed sequences of Pennsylvanian and Permian sedimentary units with extensively studied biostratigraphy. Tight palaeontologic age constraints from these sequences provide an opportunity to examine variations over time of the relative contribution of sediment derived from the nearby Ancestral Rocky Mountains versus sediment of more distal origins. This study utilizes the laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) approach to U-Pb dating of detrital zircons found within the Pennsylvanian and Permian sequences of central New Mexico, to evaluate changes in potential source regions and sediment transport over time, and to contribute insights to the existing tectonic and sedimentary record of the area during the Pennsylvanian and Permian periods. The findings reveal the Pennsylvanian units were dominated by locally derived sediment, characterized by zircon ages ranging from 1400 to 1800 Ma, whereas Permian units record a substantial influx of distally derived grains with zircon ages ranging from approximately ~270 Ma to 1300 Ma. This indicates that the Ancestral Rockies were the dominant sedimentary sources during the Pennsylvanian but became subdued enough in the Permian to allow the sedimentary basins to capture exotic grains derived from distant regions in North America. These findings contribute valuable insights to the tectonic and sedimentary history of central New Mexico during the Pennsylvanian and Permian periods, shedding light on the evolution of the Ancestral Rockies and the influences of distant sediment sources on the region's depositional patterns.