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| | Miocene macroflora of the northern Ogallala group, northern Nebraska and southern South Dakota, The Journal of ... (Site not responding. Last check: ) |
 | | REPORTS OF fossil plants from Tertiary strata of central North America are common (Stansbury, 1852; Cockerell, 1914; Berry, 1928; Elias,1932, 1942; Frye et al., 1956; Leonard,1958; Frye and Leonard, 1959; Thomasson, 1977, 1978, 1979, 1983, 1985, 1990; Thomasson et al., 1986; Leonard and Frye, 1978; Gabel, 1987; Gabel and Bich, 1988). |
 | | Geographically, plant fossils have been reported from the Great Plains Tertiary strata (and especially the Ogallala Group) from Kansas and Nebraska (MacGinitie, 1962; Thomasson, 1977, 1979, 1985) to Texas and New Mexico (Leonard, 1958; Leonard and Frye, 1978) and are found throughout the geographic range of the Ogallala Group (Figure 1). |
 | | MacGinitie (1962) demonstrated that the Valentine (Barstovian) flora had elements of deciduous hardwoods interpreted as growing on floodplains, as well as interfluves covered with pine-oak woodlands, and concluded that the grasslands of the Great Plains are a Pleistocene occurrence. |
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