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and having broader, shorter leaves rather than linear, needle-like leaves <strong>of</strong><br />
the latter. Milnerites planus differs from Saintgeorgeia jensenii by having<br />
different shaped leaves that are closer together and not as curved and<br />
by a flattened shoot.<br />
Genus Podozamites (Brongniart) Braun in Munster, 1843<br />
Discussion: Like Pagiophyllum, Podozamites is another in a series<br />
<strong>of</strong> morphogenera based on leaf characters that are used for mainly<br />
Mesozoic sterile coniferous foliage. Podozamites, as it is usually employed,<br />
is distinguished from the others by having linear, lanceolate<br />
leaves containing numerous parallel veins that converge apically. They<br />
are borne alternately or spirally on long shoots.<br />
Geologic range: Triassic throughout the Cretaceous.<br />
cf. Podozamites<br />
Figures 5A, 6C<br />
Material: SGDS.558A.<br />
Description and Discussion: Several small fragments <strong>of</strong> lamina<br />
showing narrow parallel veins apparently represent Podozamites. The<br />
size <strong>of</strong> the whole leaf is unknown, but the dimensions <strong>of</strong> the fragments<br />
indicate that it was probably rather small. These fragments are comparable<br />
to Podozamites distans (Presl) Braun and P. punctatus Harris from<br />
the Rhaetic Scoresby Sound flora <strong>of</strong> East Greenland (Harris, 1935) (Fig.<br />
5A). Although the lower part <strong>of</strong> the leaf shows elongate cells over the<br />
veins, no other epidermal cells are visible.<br />
SUMMARY<br />
419<br />
The flora from the SGDS is the first Early Jurassic flora reported<br />
from western North America. The majority <strong>of</strong> Early Jurassic floras are<br />
found in Eurasia. Early Jurassic floras are marked by an ascendance <strong>of</strong><br />
many Triassic types in Europe (Vakhrameev, 1991). Ferns were common,<br />
as were conifers and bennettitalean forms, in many floras <strong>of</strong> this<br />
age. Podozamites, Clathropteris, and Equisetum, present in the <strong>St</strong>. <strong>George</strong><br />
flora, were well represented in Early Jurassic floras in Eurasia. This flora<br />
and fragments <strong>of</strong> other plant material which occur at the SGDS suggests<br />
the flora was much more diverse when living and that more taxa will<br />
likely be uncovered with additional collecting at other sites within and<br />
adjacent to <strong>St</strong>. <strong>George</strong>.<br />
ACKNOWLEDGMENTS<br />
We are grateful to Andrew R.C. Milner (<strong>City</strong> Paleontologist, <strong>St</strong>.<br />
<strong>George</strong>, Utah) who was responsible for collecting the material described<br />
here and providing additional data, and to Dr. James I. Kirkland (<strong>St</strong>ate<br />
Paleontologist, Utah Geological Survey) for inviting us to study this<br />
flora. We acknowledge the assistance <strong>of</strong> Darcy <strong>St</strong>ewart, Paul Jensen and<br />
the late Layton Ott for allowing collection <strong>of</strong> fossils on their properties,<br />
Pr<strong>of</strong>essor M.E. Popa (University <strong>of</strong> Bucharest) for reviewing the manuscript,<br />
and to Dr. Brooks Britt (Department <strong>of</strong> Geology, Brigham Young<br />
University) for his assistance with the illustrations.<br />
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