The 23,000 year chronology for those footprints at White Sands seems to be holding up to confirmation.

This paper reports on an independent study of the chronology of a previously unrecognized stratigraphic record of paleolake Otero that is directly traceable into the track-bearing alluvium. The stratigraphic data along with 26 additional radiocarbon dates on palustrine mud determined by two labs independent of the original investigations document an aggrading lake/wetland/stream record that includes the tracks and spans >23.6 thousand years to ~17.0 thousand calibrated years before present, providing another line of evidence further supporting the validity of an LGM age for the tracks.