Organic matter accumulation in western boreal saline wetlands: A comparison of undisturbed and oil sands wetlands

被引:26
|
作者
Trites, Marsha [1 ]
Bayley, Suzanne E. [1 ]
机构
[1] Univ Alberta, Dept Biol Sci, Edmonton, AB T6G 2E9, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Salinity; Biomass; Decomposition; Marsh; Vegetation; Oil sands mining; NAPHTHENIC ACIDS; SOIL-SALINITY; SPARTINA-ALTERNIFLORA; CARBON ACCUMULATION; ROOT DECOMPOSITION; SALT MARSHES; ALBERTA; GROWTH; VEGETATION; GRADIENT;
D O I
10.1016/j.ecoleng.2009.07.011
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Reconstructing landscapes after open pit mining of the Canadian oil sands presents enormous challenges. Freshwater peatlands dominate the pre-disturbance landscape; however, elevated salinity in the post-disturbance landscape will exclude the use of many freshwater vegetation species for reclamation. Successful reclamation will require plants to grow and accumulate peat despite elevated salinity. We evaluated the potential of salt-tolerant plants to accumulate peat by integrating plant production and decomposition rates in natural and oil sands wetlands across a salinity gradient. These wetlands were dominated by marsh-like vegetation with relatively rapid decomposition, especially of the belowground plant material. Aboveground production was high enough to compensate for rapid decomposition, resulting in mean annual organic matter accumulation of 307 g m(-2). Thus, both natural wetlands (which despite the elevated salinity had peat deposits >35 cm) and the oil sands wetlands accumulated organic matter during the study. There is potential for peat to accumulate in future oil sands wetlands, although long-term accumulation rates may be slower than in undisturbed freshwater fens and bogs. A reliable water supply and a host of other factors will be required for wetlands to accumulate organic matter, and eventually peat, in the post-mining landscape. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:1734 / 1742
页数:9
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