Download “1996-03” 1996-03.pdf – Downloaded 108 times – 3 MB

SEM and optical photomicrographs reveal similarities between whewellite microstructures and the lichen Aspicilia calcarea. This desert lichen is known to produce calcium oxalate, and has been found in several sites in the region.

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.

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Download “The Nature of a Whewellite-Rich Rock Crust Associated with Pictographs in Southwestern Texas (1996-03a)” 1996-03a.pdf – Downloaded 84 times – 2 MB

Download “A paleoclimate reconstruction of southwestern Texas using oxalate residue from lichen as a paleoclimate proxy (1996-03b)” 1996-03b.pdf – Downloaded 73 times – 342 kB

Download “Rock Art of the Chihuahuan Desert Borderlands (1996-03c)” 1996-03c.pdf – Downloaded 92 times – 4 MB

Download “A Paleoclimate Reconstruction Based on a Biogenic Oxalate Rock Crust (1996-03d)” 1996-03d.pdf – Downloaded 80 times – 4 MB

Download “Fourier Transform Raman spectroscopic Study of Prehistoric Rock Paintings from the Big Bend Region, Texas (1996-03e)” 1996-03e.pdf – Downloaded 79 times – 1 MB

This research was made possible through Grant MT0424-5-NC-18 from the National Center for Preservation Technology and Training (NCPTT).

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