Abstract
Plant fossils from the Tertiary strata of the Great Plains are relatively common and have been reported for over 100 years (Stansbury, 1852; Elias, 1942; Thomasson, 1979, 1985, 1991; Gabel, 1987). However, fossils of the family Cyperaceae are uncommon at most sites in Tertiary strata of central North America.
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