Interpretation The
significance of these old clones is that the incursion of desert vegetation
into the present desert areas probably occurred earlier than indicated by
fossils from pack rat middens. The apparent discrepancy in timing of residency
of desert vegetation may be explained by the relative occurrence of old clones
and of pack rat nests. Old creosote clones tend to occur on stable, level,
sandy-gravelly surfaces or long, persistent sandy slopes, where pack rat
activity is nil. In contrast, pack rats tend to build nests, especially those
that survive thousands of years, in the shelter of rock ledges and crevices on
rocky slopes. Consequently, valley bottom populations of creosote bush would
not be sampled by rocky slope/dwelling pack rats. Therefore, the absence of
creosote bush from pack rat midens of the Chihuahuan Desert is not sufficient
to conclude the absence of creosote bush from that region. The foregoing
information leads to the interpretation that the ployploid series in creosote
bush was already well established during the last ice age. On this
interpretation, creosote bushes probably did exist in valley bottom refuges at
low elevations in all three desert areas during the late stages of the last ice
age. They probably spread very rapidly northward about 12,000 BP at a time when
drastic climatic changes were shrinking the continental ice sheets. All
photos by author |
Reference *Vasek, F. C.,
1980. Creosote bush: long-lived clones in the Mojave Desert. Amer. J. Bot. 67:
246-255. |
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