Expansion of Phragmites australis into tidal wetlands of North America

• Published in: Aquatic botany Vol. 64; no. 3; pp. 261 - 273
• Main Authors: Chambers, Randolph M., Meyerson, Laura A., Saltonstall, Kristin
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-09-1999
• Subjects: Brackish; Brackish marsh; Canada; Common reed; Disturbance; Freshwater; Genetic variation; Invasion; North America; Phragmites australis; USA; ANW, North America; ASW, North America; Common reed; Brackish marsh; Phragmites australis; Genetic variation; Invasion; Disturbance
• ISSN: 0304-3770; 1879-1522
• DOI: 10.1016/S0304-3770(99)00055-8

Phragmites expansion into tidal wetlands of North America is most extensive along the northern and middle Atlantic coasts, but over 80% of the US coastal wetland area occurs along the Gulf of Mexico and southern Atlantic coasts and may be susceptible to ongoing expansion. Rapid spread of
Phragmites has been documented in freshwater (<0.5
ppt), oligohaline (0.5–5
ppt) and mesohaline (5–18
ppt) tidal wetlands. The advance of
Phragmites into tidal wetlands of North America may have been facilitated by widespread coastal changes since European settlement, including disturbance of hydrologic cycles and nutrient regimes; the presence of
Phragmites has become a signature of tidal wetland alteration. Although ploidy levels from 2
n
=
36 to 72 have been documented for
Phragmites throughout the continent, no genetics research to date has tested whether recent introduction of aggressive clones could account for
Phragmites expansion. A fundamental concern regarding
Phragmites expansion, particularly into tidal freshwater wetlands, is the observed reduction in biodiversity as many native species of plants are replaced by a more cosmopolitan species. Commensurate with a shift in habitat type is a reduction in insect, avian and other animal assemblages. Ecosystem services, including support of higher trophic levels, enhancement of water quality and sediment stabilization, however, are not diminished when a tidal wetland becomes dominated by
Phragmites, provided that tidal flooding is retained.