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

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128 INTRODUCTION/RED RIVER AREA<br />

are placed too far to the east and that there has been significant recession of the<br />

Pineywoods due to human impact beginning as early as 1815 (e.g., Jonesboro in Red River<br />

County, the site of the earliest Anglo settlement in Texas).<br />

In northern Lamar County, the aspect of the vegetation is definitely similar to the<br />

mixed deciduous or deciduous-pine forests typical of some regions of the Pineywoods. Tall<br />

stands of Quercus falcata (southern red oak), abundant Liquidambar styraciflua (sweetgum),<br />

Pinus taeda (loblolly pine), P. echinata (shortleaf pine), Quercus alba (white oak), Acer<br />

rubrum (red maple), Betula nigra (river birch), Carpinus caroliniana (American hornbeam),<br />

Crataegus marshallii (parsley hawthorn), bottomland brakes of Arundinaria gigantea (giant<br />

cane), Calycocarpum lyonii (cupseed), Trachelospermum difforme (climbing dogbane), and<br />

herbs such as Lysimachia lanceolata (lance-leaf loosestrife), Monotropa hypopithys (American<br />

pinesap), Osmunda cinnamomea (cinnamon fern), Polygala sanguinea (blood milkwort),<br />

Porteranthus stipulatus (Indian-physic), Saccharum contortum (bent-awn plume grass),<br />

Sacciolepis striata (American cupscale), Saururus cernuus (lizard’s-tail), Stachys tenuifolia<br />

(slender-leaf betony), and Veronicastrum virginicum (Culver’s-physic) are just a few examples<br />

of eastern plants found in Lamar County. Even farther west, in Fannin County, there are<br />

still isolated pockets of eastern Texas vegetation (e.g., Talbot property). Species reaching to<br />

or near their western limits there include Quercus falcata (southern red oak), Q. nigra (water<br />

oak), Q. phellos (willow oak), Nyssa sylvatica (black-gum), Sassafras albidum (sassafras),<br />

Chasmanthium sessiliflorum (narrow-leaf wood-oats), Erechtites hieraciifolia (American burnweed),<br />

Luzula bulbosa (bulb woodrush), Monotropa uniflora (Indian-pipe), Pedicularis<br />

canadensis (common lousewort), Pycnanthemum albescens (white-leaf mountain-mint),<br />

Sorghastrum elliottii (slender Indian grass), and Woodwardia areolata (narrow-leaved chain fern).<br />

Grayson County, the next county to the west, does not have areas dominated by eastern Texas<br />

plants as do Lamar and Fannin counties, but there is a significant eastern Texas component<br />

to the vegetation. Numerous plant species reach their western limits in Grayson County,<br />

including Agrimonia rostellata (woodland groovebur), Asimina triloba (common pawpaw),<br />

Cinna arundinacea (stout wood reed), Desmodium glutinosum (tick-clover), Impatiens capensis<br />

(spotted touch-me-not), Liatris aspera (tall gayfeather), Monarda lindheimeri (Lindheimer’s<br />

beebalm), Podophyllum peltatum (may-apple), Polygonatum biflorum (Solomon’s-seal),<br />

Quercus velutina (black oak), Thalictrum arkansanum (meadowrue), Triosteum angustifolium<br />

(yellow-flowered horse-gentian), and Vaccinium arboreum (farkleberry). A few typically<br />

eastern plants extend even farther west into Cooke and Montague counties and beyond.<br />

More typically western plants also extend eastward in the Red River Basin, though not<br />

as commonly as eastern plants range westward. One example of such a western species is<br />

Heliotropium convolvulaceum (bindweed heliotrope), known in Texas primarily from the<br />

Panhandle and Trans-Pecos but extending east in extremely dry sandy habitats along the<br />

Red River to Grayson and Lamar counties. Two other examples of species extending east in<br />

the same sandy habitats to Grayson County are Croton texensis (Texas croton) and<br />

Euphorbia hexagona (green spurge). Yet another example is Dalea lanata (woolly dalea),<br />

confined in Texas largely to the Panhandle but extending east along the Red River to Cooke<br />

and Grayson counties.<br />

The area adjacent to the Red River in Grayson County is further complicated by the<br />

presence of the Preston Anticline, a post-Cretaceous (Bradfield 1957) fold in the sedimentary<br />

strata that brought deeper layers to the surface (Bullard 1931). In places the river<br />

valley is two hundred feet below the surrounding area and creeks have cut deep canyonlike<br />

valleys. The overall topography near the Red River is thus very rugged (Bullard 1931).<br />

Parker (1856) in an early account described the Texas shore of the Red River as “very bold,<br />

presenting a stratification of red clay and white sand, giving a striking and very peculiar

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