East Central Texas forests

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East Central Texas forests
Road in Northern Post Oak Savanna, Gus Engeling Wildlife Management Area, Anderson County, Texas, USA (15 April 2017).jpg
Northern Post Oak savanna, Gus Engeling Wildlife Management Area
Texas ecoregions.gif
East Central Texas forests (33)
Ecology
Realm Nearctic
Biome Temperate broadleaf and mixed forests
Geography
Area52,600 km2 (20,300 sq mi)
CountryUnited States
States
  • Oklahoma
  • Texas
Climate type Humid subtropical (Cfa)
Conservation
Conservation status Critical/endangered
Habitat loss75%
Map of the East Central Texas forests 33 and adjacent ecoregions. Sub-ecoregions include:
Northern Post Oak Savanna 33a
Southern Post Oak Savanna 33b
San Antonio Prairie 33c
Northern Prairie Outliers 33d
Bastrop Lost Pines 33e
Floodplains and Low Terraces 33f East Central Texas Ecoregions.gif
Map of the East Central Texas forests 33 and adjacent ecoregions. Sub-ecoregions include:
Northern Post Oak Savanna 33a
Southern Post Oak Savanna 33b
San Antonio Prairie 33c
Northern Prairie Outliers 33d
Bastrop Lost Pines 33e
Floodplains and Low Terraces 33f

The East Central Texas forests or East Central Texas Plains (33) is a small temperate broadleaf and mixed forests ecoregion almost entirely within the state of Texas, United States. [1] The northern forests perimeter is partially within the southeast Oklahoma border.

Contents

Description

East Central Texas forests are distinguished from the adjacent Texas blackland prairies and Western Gulf coastal grasslands by their greater tree density. On the other hand, they are more open and have a greater concentration of hardwoods than the forests of the Piney Woods. [1] The climate is hot and humid. [2]

Subregions

Northern Post Oak Savanna

The landscapes of this ecoregion are generally more level and gently rolling compared to the more dissected and irregular topography of much of Southern Post Oak Savanna. It is underlain by mostly Eocene and Paleocene-age formations with some Cretaceous rocks to the north. The deciduous forest or woodland is composed mostly of post oak, blackjack oak, eastern red cedar, and black hickory. Prairie openings contained little bluestem and other grasses and forbs. The land cover currently has more improved pasture and less post oak woods and forest than the Southern Post Oak Savanna. Some coniferous trees occur, especially on the transitional boundary with the Tertiary Uplands ecoregion. Loblolly pine has been planted in several areas. Typical wildlife species include white-tailed deer, eastern wild turkey, northern bobwhite, eastern fox squirrel, and eastern gray squirrel. [3]

Southern Post Oak Savanna

This ecoregion has more woods and forest than the adjacent prairie ecoregions, and consists of mostly hardwoods compared to the pines to the east in the South Central Plains. Historically a post oak savanna, current land cover is a mix of post oak woods, improved pasture, and rangeland, with some invasive mesquite to the south. A thick understory of yaupon and eastern redcedar occurs in some parts. The ecoregion is underlain by Miocene, Oligocene, Eocene, and Paleocene sediments. Sand exposures within these Tertiary deposits have a distinctive sandyland flora, and in a few areas unique bogs occur. The endangered Houston Toad is associated with the deep sandy soils of this ecoregion [3]

San Antonio Prairie

This ecoregion is a narrow, 100-mile long region occurring primarily on the Eocene Cook Mountain Formation. Upland Alfisol prairies were dominated by little bluestem and yellow indiangrass and contained a different mix of grasses and forbs than the dark, clayey, more calcareous soils of the Northern Texas blackland prairies. Since the 1830s, settlement clustered along the Old San Antonio Road (Texas State Highway 21 in the south, Old San Antonio Road in the north) within this narrow belt of prairie land. Currently, land cover is a mosaic of woodland, improved pasture, rangeland, and some cropland. [3]

Northern Prairie Outliers

The small, disjunct areas of this ecoregion have a blend of characteristics from the Texas blackland prairies and the East Central Texas forests. The northern two outliers, north of the Sulphur River, occur on Cretaceous sediments, while south of the river, Paleocene and Eocene formations predominate. A mosaic of forest and prairie occurred historically in this and adjacent regions. Burning was important in maintaining grassy openings, and woody invasions have taken place in the absence of fire. The tallgrass prairies included little bluestem, big bluestem, yellow indiangrass, and tall dropseed. Current land cover is mostly pasture, with some cropland. [3]

Bastrop Lost Pines

The Houston Toad (Anaxyrus houstonensis) is an endangered species occurring in the East Central Texas forests. Endangered Houston toad (Bufo houstonensis)1.jpg
The Houston Toad ( Anaxyrus houstonensis ) is an endangered species occurring in the East Central Texas forests.

This ecoregion is an outlier of relict loblolly pine-post oak upland forest occurring on some dissected hills. It is the westernmost tract of southern pine in the United States. The pines mostly occur on gravelly soils that formed in Pleistocene high gravel, fluvial terrace deposits associated with the ancestral Colorado River, and sandy soils that formed in Eocene sandstones (such as the Weches Formation). The Lost Pines are about 100 miles (160 km) west of the Texas pine belt of the South Central Plains and occur in a drier environment with 36 inches (910 mm) of average annual precipitation. In this area, the deep, acidic, sandy soils and the additional moisture provided by the Colorado River contribute to the occurrence of pines, which are thought to be a relict population predating the last glacial period. The largest population of the Houston Toad occurs in this ecoregion [3]

Floodplains and Low Terraces

This ecoregion contains floodplain and low terrace deposits downstream from the Texas blackland prairies and upstream from the Texas coastal plains. It includes only the wider floodplains of major streams, such as the Sulphur, Trinity, Brazos, and Colorado rivers. In addition, it covers primarily Holocene deposits and not Pleistocene deposits on older, high terraces. The bottomland forests contain water oak, post oak, elms, green ash, pecan, willow oak and bald cypress to the east, and to the west some hackberry and eastern cottonwoods. The northern floodplains tend to have more forested land cover, while in the south the Brazos and Colorado River floodplains are characterized by more cropland and pasture. [3]

Fauna

The forests are home to a rich wildlife including Virginia opossums (Didelphis virginiana), North American least shrews (Cryptotis parva), North American beavers (Castor canadensis) and many species of butterflies and reptiles. Larger mammals that once lived here, including jaguar (Panthera onca) and Plains bison (Bison bison bison), have now disappeared from the region. [1] Endangered fauna found in this ecoregion include the Houston toad (Bufo houstonensis) and Attwater's prairie chickens (Tympanuchus cupido attwateri). [2]

Conservation

This environment has been heavily altered by cattle ranching and clearance for farmland with only a quarter of the original habitats remaining, in fragmented patches and not in large blocks. There are no national forests in the region.

See also

Related Research Articles

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Prairies are ecosystems considered part of the temperate grasslands, savannas, and shrublands biome by ecologists, based on similar temperate climates, moderate rainfall, and a composition of grasses, herbs, and shrubs, rather than trees, as the dominant vegetation type. Temperate grassland regions include the Pampas of Argentina, Brazil and Uruguay, and the steppe of Ukraine, Russia and Kazakhstan. Lands typically referred to as "prairie" tend to be in North America. The term encompasses the area referred to as the Interior Lowlands of Canada, the United States, and Mexico, which includes all of the Great Plains as well as the wetter, hillier land to the east.

<span class="mw-page-title-main">Edwards Plateau</span> Geographic and ecological region of Texas, United States

The Edwards Plateau is a geographic region forming the crossroads of Central, South and West Texas, United States. It is named in honor of Haden Edwards. It is bounded by the Balcones Fault to the south and east; the Llano Uplift and the Llano Estacado to the north; and the Pecos River and Chihuahuan Desert to the west. San Angelo, Austin, San Antonio and Del Rio roughly outline the area. The plateau, especially its southeast portion, is also known as the Texas Hill Country.

<span class="mw-page-title-main">Piney Woods</span> Temperate coniferous forests ecoregion of the United States

The Piney Woods is a temperate coniferous forest terrestrial ecoregion in the Southern United States covering 54,400 square miles (141,000 km2) of East Texas, southern Arkansas, western Louisiana, and southeastern Oklahoma. These coniferous forests are dominated by several species of pine as well as hardwoods including hickory and oak. Historically the most dense part of this forest region was the Big Thicket though the lumber industry dramatically reduced the forest concentration in this area and throughout the Piney Woods during the 19th and 20th centuries. The World Wide Fund for Nature considers the Piney Woods to be one of the critically endangered ecoregions of the United States. The United States Environmental Protection Agency (EPA) defines most of this ecoregion as the South Central Plains.

<span class="mw-page-title-main">Tallgrass prairie</span> Ecosystem native to central North America

The tallgrass prairie is an ecosystem native to central North America. Historically, natural and anthropogenic fire, as well as grazing by large mammals provided periodic disturbances to these ecosystems, limiting the encroachment of trees, recycling soil nutrients, and facilitating seed dispersal and germination. Prior to widespread use of the steel plow, which enabled large scale conversion to agricultural land use, tallgrass prairies extended throughout the American Midwest and smaller portions of southern central Canada, from the transitional ecotones out of eastern North American forests, west to a climatic threshold based on precipitation and soils, to the southern reaches of the Flint Hills in Oklahoma, to a transition into forest in Manitoba.

<span class="mw-page-title-main">Oak savanna</span> Lightly forested grassland where oak trees are dominant

An oak savanna is a type of savanna—or lightly forested grassland—where oaks are the dominant trees. The terms "oakery" or "woodlands" are also used commonly, though the former is more prevalent when referencing the Mediterranean area. These savannas were maintained historically through wildfires set by lightning, humans, grazing, low precipitation, and/or poor soil.

<span class="mw-page-title-main">Big Thicket</span> Heavily-forested area of Southeast Texas in the United States

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<span class="mw-page-title-main">Texas Blackland Prairies</span> Temperate grassland region of Texas, US

The Texas Blackland Prairies are a temperate grassland ecoregion located in Texas that runs roughly 300 miles (480 km) from the Red River in North Texas to San Antonio in the south. The prairie was named after its rich, dark soil. Less than 1% of the original Blackland prairie vegetation remains, scattered across Texas in parcels.

<span class="mw-page-title-main">Western Gulf coastal grasslands</span> Subtropical grassland ecoregion of Mexico and the United States

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<span class="mw-page-title-main">Osage Plains</span> Physiographic section extending through five U.S. states

The Osage Plains are a physiographic section of the larger Central Lowland province, which in turn is part of the larger Interior Plains physiographic division. The area is sometimes called the Lower Plains, North Central Plains,or Rolling Plains. The Osage Plains, covering west-central Missouri, the southeastern third of Kansas, most of central Oklahoma, and extending into north-central Texas, is the southernmost of three tallgrass prairie physiographic areas. It grades into savanna and woodland to the east and south, and into shorter, mixed-grass prairie to the west. The Osage Plains consist of three subregions. The Osage Plains proper occupy the northeast segment. Although sharply demarcated from the Ozark uplift, the plains are nonetheless a transitional area across which the boundary between prairie and woodland has shifted over time. In the central portion of the physiographic area lies the second subregion, the Flint Hills, commonly called "the Osage" in Oklahoma. This large remnant core of native tallgrass prairie is a rocky rolling terrain that runs from north to south across Kansas and extends into Oklahoma. To the west and south of these hills are the Blackland Prairies and Cross Timbers. This vegetatively complex region of intermixed prairie and scrubby juniper-mesquite woodland extends into north-central Texas. Bluestem prairies and oak-dominated savannas and woodlands characterize the natural vegetation in the Cross Timbers. Much of the area has been converted to agriculture, although expanses of oak forest and woodland are still scattered throughout the eastern portion of the subregion.

<span class="mw-page-title-main">Willamette Valley (ecoregion)</span> Temperate broadleaf and mixed forests ecoregion of the United States

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References

  1. 1 2 3 "East Central Texas forests". Terrestrial Ecoregions. World Wildlife Fund. Retrieved 2010-10-20.
  2. 1 2 World Wildlife Fund, ed. (2001). "East Central Texas forests". WildWorld Ecoregion Profile. National Geographic Society. Archived from the original on 2010-03-08. Retrieved 2010-10-20.
  3. 1 2 3 4 5 6 PD-icon.svg This article incorporates public domain material from Ecoregions of Texas poster, back (PDF). United States Geological Survey . Retrieved 2016-02-06.