Floristic shifts in wetlands: the effects of environmental variables on the interaction between Phragmites australis (Common Reed) and Melaleuca ericifolia (Swamp Paperbark)

2008 ◽  
Vol 59 (3) ◽  
pp. 187 ◽  
Author(s):  
Kay Morris ◽  
Paul I. Boon ◽  
Elisa J. Raulings ◽  
Sean D. White

Over the past 40–50 years, the woody shrub Melaleuca ericifolia has progressively invaded large areas of Phragmites australis in Dowd Morass, a Ramsar-listed, brackish wetland in south-eastern Australia. To understand the processes underlying this shift we grew Phragmites and Melaleuca alone and together under contrasting sediment organic-matter loadings and salinities. To examine if the capacity of Phragmites to aerate the sediment influenced plant interactions, we also dissipated convective gas flow in some Phragmites plants by perforating their stems. Although Phragmites suppressed the growth of Melaleuca under all conditions, Melaleuca persisted. We did not find Phragmites ramets to be more sensitive to salinity than Melaleuca seedlings. Surprisingly Phragmites did not increase sediment redox and was more sensitive to increased organic-matter loading than Melaleuca. These results do not support the notion that colonisation by Melaleuca was facilitated by a decline in Phragmites at higher salinities or through aeration of the sediments by Phragmites. Seedlings of Melaleuca, however, were easily blown over by wind and it is likely that Phragmites stands shelter Melaleuca during establishment. Although our short-term experiment did not show that Melaleuca was a better competitor, differences in seasonal growth patterns may contribute to a shift in competitive abilities over a longer time scale.

1997 ◽  
Vol 35 (5) ◽  
pp. 287-292 ◽  
Author(s):  
Peter S. Burgoon ◽  
K. Frank Kirkbride ◽  
Mike Henderson ◽  
Evan Landon

Reed beds for dewatering biosolids have been successful throughout Europe and in the northeastern temperate United States. This paper reports on the use of reed beds in the arid Columbia Basin in the state of Washington, USA. Native stands of the common reed, Phragmites australis were propagated and planted in the reed beds. The hot, dry, windy, climate has required simple changes in standard operation of the reed beds. The reeds were stressed by the hot dry winds and lost top shoot growth when beds remained drained in the Spring Summer and Fall months. Maintenance of water levels in the cells has reduced symptoms of heat stress in the plants. These operational changes may have an effect on oxidation of organic matter and nitrogen in the filtrate. The operational changes may have effected the dewatering and decomposition of the biosolids. The dry hot summers, and freezing winters enhance the dewatering ability of the reed beds and make them an appropriate solids dewatering technology for the region.


2019 ◽  
Vol 70 (4) ◽  
pp. 469 ◽  
Author(s):  
Paul I. Boon ◽  
Doug Frood ◽  
Alison Oates ◽  
Jim Reside ◽  
Neville Rosengren

Common reed Phragmites australis is the dominant vascular plant species of the shorelines of the Gippsland Lakes, south-eastern Australia. Although substantial declines have been reported for over 50 years, with increasing salinity posited as the cause, P. australis still occurs around the Gippsland Lakes, including in environments with near-oceanic salinities. The occurrence of P. australis in highly saline environments cannot be explained in terms of either seasonal variations in surface water salinity or a freshwater subsidy provided by intrusions of non-saline groundwater into the root zone. An experimental growth trial with plants of different provenance showed that P. australis grew vigorously even at 8–16PSU (with maximum aboveground biomass at 2–4PSU). There was some evidence that specimens from saltier sites were more salt tolerant than those from fresher sites. The selection of salt-tolerant strains is the most likely explanation for the occurrence of P. australis in saline sites. However, anthropogenic salinisation is unlikely to be the only factor involved in the historical loss of reed beds, and lower and more stable water levels following the permanent opening of the Gippsland Lakes to the ocean in 1889 are probably also contributing factors.


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