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CEGL003836 Arundinaria gigantea ssp. gigantea Wet Canebrake

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Giant Cane Wet Canebrake

Colloquial Name: Floodplain Canebrake

Hierarchy Level:  Association

Type Concept: This association is characterized by dense, often monospecific thickets of the bamboo shrub Arundinaria gigantea occupying large areas referred to as canebrakes. The canebrake shrubland type was historically widespread, but is now rare and occupies very little of its former acreage. It was best developed in streamside flats and alluvial floodplains on ridges and terraces where it was protected from prolonged inundation. Historically, this community covered large areas of many floodplains and streamsides in the Coastal Plain from North Carolina to Texas, Mississippi River Alluvial Plain, Interior Highlands, Interior Low Plateau, Southern Blue Ridge, Cumberland Mountains, and Western Allegheny Plateau of the southeastern United States. Stands occur on alluvial and loess soils and are often associated with bottomland hardwood forest vegetation. This association is successional and is thought to be maintained by periodic fires. It may have originated following abandonment of aboriginal agricultural fields or other natural and anthropogenic disturbances such as blow-downs and catastrophic floods. Historical accounts report cane as abundant along the Wabash and Ohio drainage systems, as well as common along larger rivers (Buffalo, White, Norfork) in the Ozarks and Ouachitas. It was also reported as common along the Red and Mississippi rivers in Louisiana, Coastal Prairie rivers in Texas, and the Black, Washita, Arkansas, Sabine, Pearl, Tombigbee, Yazoo, Savannah, and St. Mary''s rivers. Large, extant canebrakes still exist and have been documented from the Ocmulgee Basin, south of Macon, Georgia. In the Cumberland Mountains and Western Allegheny Plateau, streamside flats and bottomlands were dominated by Arundinaria, without an overstory, or with widely scattered trees.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This is a general placeholder, covering a broad geographic range, and several associations may ultimately be recognized. Dense, monospecific stands of Arundinaria gigantea were historically found in bottomland sites in the southeastern United States. Today, high-quality examples are extremely rare, if not absent. Historical accounts refer to both "pure" stands of cane without an overstory of trees (cane shrublands) and areas with variable overstory closure (woodlands or forests) but with a dense understory dominated by cane as "canebrakes."

In West Virginia, two plots from the valleys of the Ohio and Kanawha rivers are classified to this association. These stands are thought to be remnants of previously more extensive canebrakes that now persist under open tree canopies dominated by Acer negundo. Many place names in southwestern West Virginia that reference cane and remnant patches give clues to the former distribution and extent of canebrakes in the state. Historical accounts of canebrakes along the Kanawha and Ohio rivers are given by Thomas Nuttall (1821) and by George Washington in the late 1700s (Jackson and Twohig 1976).

Similar NVC Types: No Data Available
note: No Data Available

Physiognomy and Structure: No Data Available

Floristics: The vegetation is dominated by Arundinaria gigantea. Little else is known about its vegetational characteristics. However, information on its historic patterns of distribution provides some clues as to its ecology. General Land Office surveys and other historical accounts indicate that canebrakes were present in southern Illinois, southern Indiana, West Virginia, Kentucky, Missouri, Arkansas, eastern Texas (south to Wharton County), Louisiana, Tennessee, Mississippi, Alabama, Georgia, and South Carolina. Historical accounts refer to both "pure" stands of cane without an overstory of trees (cane shrublands) and areas with variable overstory closure (woodlands or forests) but with a dense understory dominated by cane as "canebrakes." Cane was abundant along the Wabash and Ohio drainage systems (B. McClain pers. comm. 2000). In Missouri, these canebrakes were also thought to be common in the Ozark Highlands, particularly in southward-draining rivers and streams with finer-textured, more developed soils on upper floodplain terraces (T. Nigh pers. comm. 2000). Stands may be found along larger rivers (Buffalo, White, Norfork) in the Arkansas Ozarks in addition to the Ouachitas. Historic accounts describe large expanses (one area was described as 75 miles long by 1-3 miles wide) of an "ocean of cane" in bottomlands of the Coastal Prairie of Texas (Smeins et al. 1992). No extant occurrences of this vegetation are known from this area today. In the Cumberland Mountains and Western Allegheny Plateau of West Virginia, numerous streamside flats and bottomlands were dominated by Arundinaria. Remnant patches persist under canopies of Acer saccharinum, Acer negundo, and Platanus occidentalis. Associated species with low cover in two West Virginia plots include Magnolia acuminata, Parthenocissus quinquefolia, Verbesina alternifolia, Hydrophyllum canadense, and species of Impatiens and Viola. Small patches of Arundinaria gigantea without a tree canopy have also been documented in disturbed areas.

Dynamics:  A canebrake is an early-successional community. It is suggested that Native Americans maintained canebrakes with the use of periodic fire to provide a ready source of cane for a myriad of uses. Canebrakes may have expanded greatly in cover following the abandonment of aboriginal agricultural lands after the collapse of Native American populations due to exotic diseases (Platt and Brantley 1997).

Environmental Description:  Stands of this association occur on alluvial and loess soils often affiliated with bottomland hardwood forest vegetation. Historically, it was best developed in streamside flats and alluvial floodplains on ridges and terraces where it was protected from prolonged inundation.

Geographic Range: This association was widespread historically but now occupies very little acreage. It may be found along rivers and streamsides in Alabama, Arkansas, Florida, Georgia, Illinois, Indiana, Kentucky, Louisiana, Mississippi, Missouri, North Carolina, Oklahoma, South Carolina, Tennessee, Texas, West Virginia, and possibly Virginia.

Nations: US

States/Provinces:  AL, AR, FL?, GA, IL, KY, LA, MO, MS, NC, OK, SC, TN, TX, VA?, WV




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: G2?

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Arundinaria gigantea ssp. gigantea Shrubland (Faber-Langendoen 2001)
> Arundinaria gigantea Floodplain Woodland [Giant Cane Woodland] (Vanderhorst 2017a)
? P5A4bIII4a. Arundinaria gigantea (Foti et al. 1994)

Concept Author(s): K.D. Patterson

Author of Description: K.D. Patterson, D. Faber-Langendoen and J. Teague

Acknowledgements: No Data Available

Version Date: 12-20-18

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