In this study, nine florules from the Chloropagus Formation near
Fernley, Nevada, are dated at 14.7-13.4 million years. The author
finds that dominant mixed conifer forest and sclerophyll woodland
species of the Sierra Nevada-Klamath region replaced exotic
deciduous hardwoods in the two lowest sites. He concludes that this
change reflects the loss of adequate summer rain as upwelling from
a colder ocean resulted from spreading East Antarctic ice.
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