Appalachian mixed mesophytic forests

Appalachian mixed mesophytic forests

Hanson's Point in the Red River Gorge, Kentucky
Ecology
Biome Temperate broadleaf and mixed forest
Borders
Bird species 200[1]
Mammal species 73[1]
Geography
Area 192,200 km2 (74,200 sq mi)
Country United States
States
Conservation
Habitat loss 14.8%[1]
Protected 8.37%[1]

The Appalachian mixed mesophytic forests is an ecoregion of the Temperate broadleaf and mixed forests Biome, as defined by the World Wildlife Fund. It consists of mesophytic plants west of the Appalachian Mountains in the Southeastern United States.

This ecoregion consists of the following EPA level III ecoregions:

Setting

This ecoregion is located in the plains and hill country west of the Appalachians in northwest Alabama and east central Tennessee, eastern Kentucky, western North Carolina and Virginia, most of West Virginia, western Maryland, southeastern Ohio and western Pennsylvania. These forests are known for their rich diversity of plants and animals, which is due to several contributing factors, especially that the area was an unglaciated refugium for many species. It shares species with the high elevation Appalachian-Blue Ridge forests to the east, the hardwood forests to the west, and the mixed hardwood/conifer forests to the south.

Climate

The climate varies from humid continental in the north to humid subtropical in the south.

Flora

They are one of the most biologically diverse temperate forest regions on earth. It has an unusually diverse tree flora, with as many as 30 tree species at a single site including many relics of the ancient forest that once covered North America more widely. Along with the forest there is a rich undergowth of ferns, fungi, herbaceous plants, shrubs and small trees as well as areas of glade, heath, shale, peat bog and cranberry bog.

Mesophytic forests

Mesophytic forests are found on deep and enriched soils in sheltered topography such as coves and low-elevation slopes. They are often found near small streams. The herb layer is very rich and, in undisturbed areas, the trees can grow very large. Typical trees include sugar maple (Acer saccharum), beech (Fagus grandifolia), tuliptree (Liriodendron tulipifera), basswood (Tilia americana), northern red oak (Quercus rubra), cucumber tree (Magnolia acuminata), and black walnut (Juglans nigra). Other trees found here are eastern hemlock (Tsuga canadensis), white ash (Fraxinus americana), sweetgum (Liquidambar styraciflua), and yellow buckeye (Aesculus flava).[2]

Dry calcareous forests

The southern Ridge and Valley/Cumberland dry calcareous forests occur on dry to dry-mesic calcareous habitats on low escarpments of the Cumberland Plateau. They are often found on deep soils in a variety landscapes within their range. Trees are mainly oaks and hickories, with other species less abundant. Oaks include white oak (Quercus alba), northern red oak (Quercus rubra), post oak (Quercus stellata), chinkapin oak (Quercus muehlenbergii), and Shumard oak (Quercus shumardii). Hickories include shagbark hickory (Carya ovata). Other trees can be sugar maple (Acer saccharum), eastern red-cedar (Juniperus virginiana), or pines.[3]

Appalachian cove forests

Appalachian cove forests are found in sheltered concave slopes with a moist environment. Characteristic tree include yellow buckeye (Aesculus flava), sugar maple (Acer saccharum), white ash (Fraxinus americana), basswood (Tilia americana), tuliptree (Liriodendron tulipifera), Carolina silverbell (Halesia tetraptera), eastern hemlock (Tsuga canadensis), beech (Fagus grandifolia), cucumber tree (Magnolia acuminata), and Fraser magnolia (Magnolia fraseri).[4]

Dry-mesic oak forests

Dry-mesic oak forests cover large areas at lower and middle elevations on flat to gently rolling terrain. Mature stands have a variety of oak and hickory species adapted to dry-mesic conditions. Oaks include northern red oak (Quercus rubra), white oak (Quercus alba), black oak (Quercus velutina), and scarlet oak (Quercus coccinea); hickories include mockernut hickory (Carya tomentosa), shagbark hickory (Carya ovata), red hickory (Carya ovalis), and pignut hickory (Carya glabra). In addition, red maple (Acer rubrum), sweet birch (Betula lenta), and yellow birch (Betula alleghaniensis) are common; sugar maple (Acer saccharum) is occasional. In areas that have been recently disturbed, white pine (Pinus strobus), Virginia pine (Pinus virginiana), or tulip tree (Liriodendron tulipifera) can be abundant. Areas of impeded drainage sometimes harbor small wetlands, including non-forested seeps or forested wetlands with red maple (Acer rubrum), swamp white oak (Quercus bicolor), or black tupelo (Nyssa sylvatica).[5]

Dry oak forests and woodlands

The Allegheny-Cumberland dry oak forest and woodland forest system is found on acidic soils on the Allegheny and Cumberland plateaus, and ridges in the southern Ridge and Valley. The forests are typically dominated by white oak (Quercus alba), southern red oak (Quercus falcata), chestnut oak (Quercus prinus), scarlet oak (Quercus coccinea), with lesser amounts of red maple (Acer rubrum), pignut hickory (Carya glabra), and mockernut hickory (Carya tomentosa). A few shortleaf pines (Pinus echinata) or Virginia pines (Pinus virginiana) may occur, particularly adjacent to escarpments or following fire. Sprouts of chestnut (Castanea dentata) can often be found where it was formerly a common tree.[6]

Low-elevation pine forests

Southern Appalachian low-elevation pine forests occur on a variety of topographic and landscape positions, including ridgetops, upper- and mid-slopes, and in lower elevations (generally below 2,300 feet (700 m)) such as mountain valleys. These forests dominated by shortleaf pine (Pinus echinata) and Virginia pine (Pinus virginiana).Pitch pine (Pinus rigida) may sometimes be present. Hardwoods are sometimes abundant, especially dry-site oaks such as southern red oak (Quercus falcata), chestnut oak (Quercus prinus), and scarlet oak (Quercus coccinea), but also pignut hickory (Carya glabra), red maple (Acer rubrum), and others. The shrub layer may be well-developed, with hillside blueberry (Vaccinium pallidum), black huckleberry (Gaylussacia baccata), or other acid-tolerant species most characteristic. Herbs are usually sparse but may include narrowleaf silkgrass (Pityopsis graminifolia) and Goat-rue (Tephrosia virginiana).[7]

Montane oak forests

Montane oak forests occur on exposed ridges and on south- to west-facing slopes at middle elevations. Soils are thin and nutrient-poor and trees are often stunted and wind-flagged. Northern red oak (Quercus rubra) and white oak (Quercus alba) are common, as are sprouts of American chestnut (Castanea dentata). Winterberry (Ilex montana), flame azalea (Rhododendron calendulaceum), catawba rhododendron (Rhododendron catawbiense), and great rhododendron (Rhododendron maximum) are common shrubs.[8]

Hemlock-northern hardwood forests

Hemlock-northern hardwood forests are found at higher elevations. They include yellow birch (Betula alleghaniensis), mountain maple (Acer spicatum), sugar maple (Acer saccharum), beech (Fagus grandifolia), and eastern hemlock (Tsuga canadensis). Mountain laurel (Kalmia latifolia) and rhododendron (Rhododendron spp.) are found in the understory.[9]

Spruce-fir forests

Spruce-fir forests occur at the highest elevations, above 3,200 feet (980 m). Their environment is cool and wet, with frequent fog and precipitation. Red spruce (Picea rubens) and Fraser fir (Abies fraseri) dominate the forest canopy.[10]

Bogs

Cranberry bogs harbor species typical of ecoregions found to the north. These species include cranberry and blueberry (Vaccinium spp.), bog rosemary (Andromeda glaucophylla), and buckbean (Menyanthes trifoliata). These bogs are relicts that have survived since the last glacial period.

Other habitats

More unique, restricted habitats within these forests include glades, heath barrens, shale barrens, and sphagnum bogs. These often support endemic plants and land snails.

Prehistoric period

During the Last Glacial Maximum about 18,000 years ago, the influence of Arctic air masses and boreal vegetation extended to about 33° N. latitude, the approximate latitude of Birmingham and Atlanta. Forests of the glacial period were dominated by various spruces (Picea spp.) and jack pine; fir (Abies spp.) was abundant in some locations. With the exception of the absence of certain prairie elements, the understories of these forests were generally typical of modern spruce-fir forests within and near Canada. Temperate deciduous forests dominated from about 33° to 30° N. latitude, including most of the glacial Gulf Coast from about 84° W. longitude. Regional climate was similar to or slightly drier than modern conditions. Oak, hickory, chestnut, and southern pine species were abundant. Walnuts, beech, sweetgum, alder, birch, tulip poplar, elms, hornbeams (Carpinus spp.), basswoods, and others that are generally common in modern southern deciduous forests were also common then. Grasses, sedges, and sunflowers were also common.

Fauna

The woodlands of the area are rich in wildlife. In particular they are important habitat for migrating birds including wood warblers, vireos, and thrushes. The rivers of the ecoregion have the highest species richness of any freshwater ecosystem. In particular, there are a large number of endemic fish and shellfish species.

Threats

This ecoregion is considered critically endangered with 95% of the habitat degraded or converted to commercial forest. Large areas have been destroyed and fragmented through surface mining, including mountaintop removal. Large areas have also been logged and then converted to plantations of fast-growing tree species, such as Loblolly Pine (Pinus taeda) which are then used to produce wood pulp, which is particularly a problem in the Cumberland Plateau of Tennessee. Another threat to habitats come from growing numbers of deer. Major rivers in the ecoregion, such as the Tennessee River, have been dammed. This has resulted in the threatened or endangered status of many species of native fish, amphibians, and shellfish.

Natural areas

The remaining forest is mostly found in protected areas.

See also

References

  1. 1 2 3 4 Hoekstra, J. M.; Molnar, J. L.; Jennings, M.; Revenga, C.; et al. (2010). Molnar, J. L., ed. The Atlas of Global Conservation: Changes, Challenges, and Opportunities to Make a Difference. University of California Press. ISBN 978-0-520-26256-0.
  2. "South-Central Interior Mesophytic Forest". NatureServe Explorer. Retrieved 8 October 2012.
  3. "Southern Ridge and Valley / Cumberland Dry Calcareous Forest". NatureServe Explorer. Retrieved 2 November 2012.
  4. "Southern and Central Appalachian Cove Forest". NatureServe Explorer. Retrieved 8 October 2012.
  5. "Northeastern Interior Dry-Mesic Oak Forest". NatureServe Explorer. Retrieved 8 October 2012.
  6. "Allegheny-Cumberland Dry Oak Forest and Woodland". NatureServe Explorer. Retrieved 11 October 2012.
  7. "Southern Appalachian Low-Elevation Pine Forest". NatureServe Explorer. Retrieved 11 October 2012.
  8. "Central and Southern Appalachian Montane Oak Forest". NatureServe Explorer. Retrieved 10 October 2012.
  9. "Appalachian (Hemlock)-Northern Hardwood". NatureServe Explorer. Retrieved 8 October 2012.
  10. "Central and Southern Appalachian Spruce-Fir Forest". NatureServe Explorer. Retrieved 8 October 2012.

Bibliography

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