The ubiquity of the whewellite-rich crust in the Lower Pecos shelters suggests that the lichen flourished in the past. Since A. calcarea is a desert species, the virulence of the organism likely peaked during xeric climate episodes then waned during mesic periods.
Thus, radiocarbon ages of whewellite would correspond to dry climate periods experienced in the region, while periods with few or no C data would indicate wet climate episodes. A preliminary paleoclimate reconstruction based on fourteen AMS C dates indicates the Lower Pecos experienced dry to wet climate fluctuations during the late Holocene.
This reconstruction generally agrees with other models established for Texas.
This research was made possible through Grant MT0424-5-NC-18 from the National Center for Preservation Technology and Training (NCPTT).