The researchers used the new chronology to investigate the climate and environmental changes at a timescale equivalent to a human generation, or approximately 50 years, which is rare for terrestrial paleoclimate archives of this time period from the southwestern U.S.

"The White Sands sediments are unique in that they allow us to reconstruct environmental conditions during the last ice age at a very high temporal resolution, so that we can see fluctuations that were relevant for the humans present at that time," said co-author Jessica Tierney, a professor at the U of A Department of Geosciences.