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ILLUSTRATED FLORA OF EAST TEXAS - Brit - Botanical Research ...

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RED RIVER AREA<br />

AREA ADJACENT TO THE RED RIVER<br />

RED RIVER AREA/INTRODUCTION 127<br />

There is a narrow band of vegetation, found on the primarily sandy soils adjacent to the<br />

Red River (Fig. 74) in the northernmost portion of East Texas, specifically in the northern<br />

parts of Bowie, Red River, Lamar, Fannin, and Grayson counties, that we are referring to<br />

as the Red River Area. The specialized habitats associated with the Red River have afforded<br />

plants sites where they could survive long-term changes in climate and have also provided<br />

a two-way migration corridor allowing plant species to extend their ranges westward from<br />

the forested areas to the east—and also eastward from the drier habitats to the west (Elisens<br />

et al. 2004). This region is in various ways quite different from the vegetational areas with<br />

which it has sometimes been included (see Fig. 3; Correll & Johnston 1970; Hatch et al.<br />

1990). The westernmost part of this band, in Grayson County, has typically been classified<br />

as part of the Cross Timbers and Prairies (vegetational area 5), and indeed it closely resembles<br />

and grades into the East Cross Timbers. The eastern part of the band has often been<br />

classified as part of vegetational area 3 (Post Oak Savannah) (Correll & Johnston 1970;<br />

Hatch et al. 1990). Such a classification is justified, since portions of the vegetation do<br />

resemble the post oak-dominated savannahs/woodlands typical of vegetational area 3.<br />

However, significant components of the vegetation more typically associated with eastern<br />

or southeastern Texas (vegetational area 1—Pineywoods) extend west along the Red River<br />

in microhabitats with special soil or moisture conditions. In fact, many areas of northern<br />

Lamar, Bowie, and Red River counties are clearly tied vegetationally to the Pineywoods—<br />

a number are even dominated by pines. A specific example is the Pinus echinata-Quercus<br />

alba forest documented for Lamar County by Wilson and Hacker (1986). This forest is<br />

somewhat similar to the Dry-Mesic Mixed Pine-Hardwood Uplands described for the<br />

Pineywoods by Van Kley (page 95). Based on such vegetational patterns, Wilson (1990)<br />

has argued that the generally accepted boundaries of the Pineywoods in northeastern Texas<br />

FIG.74/ PHOTOGRAPH <strong>OF</strong> THE RED RIVER FROM CARPENTER’S BLUFF BRIDGE IN NORTH<strong>EAST</strong>ERN GRAYSON CO.(PHOTO BY GMD).

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