Microtopography is often observed and studied in plant communities where environmental conditions limit distribution, for example in desert and peatland ecosystems. Brackish marshes, relatively poorly studied despite their importance in many coastal areas, frequently display similar fine-scale variability. In these systems, limits to plant distribution derive from the combination of flooding and salinity fluctuations. We examined the relationship between spatial variability of vegetation and biogeochemical features of sediment in a brackish tidal ecosystem in 2 adjacent Spartina spp. marshes of differing hydrology and vegetation distribution. The first, a low-elevation, interior marsh, was frequently flooded and poorly drained, and it exhibited distinct hummock/hollow topography. The plant distribution was reflected in patchy sediment biogeochemical features at the same scale. The second marsh, on a well-drained, elevated streamside bank, contained homogeneous vegetation cover and relatively uniform sediment chemistry. The formation of the hummock/hollow topography in the interior marsh appeared to be controlled by the plants, as they maximized growth in a high-stress, variable environment. The plants favorably modified discrete patches of these environments to such a degree that the hummock sediment biogeochemistry was very similar to that of the higher-elevation homogeneous marsh. The microtopography of this interior brackish marsh strongly resembles that of other stress-impacted ecosystems.KEY WORDS: Hummock/ hollow topography 路 Ecosystem engineering 路 Spatial variability 路 Patchiness 路 Marsh sediment 路 Microsite heterogeneity
Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 320: [121][122][123][124][125][126][127][128][129] 2006 Such systems include peatlands (Malmer & Wallen 1999, Branfireun 2004, forested wetlands (Huenneke & Sharitz 1986), and even subtidal seagrass beds (Hebert & Morse 2003). For each of these, sediment biogeochemical variability has been shown to coincide with vegetational patterns. As with terrestrial systems, the scale of the spatial variability may also reflect that of the dominant plant species (e.g. Huenneke & Sharitz 1986).Tidal marshes exhibit both mesoscale (10 to 1000 m 2 ) and microtopographic variability. These dynamic systems display well-defined spatial variability related to age (Tyler & Zieman 1999) and to geomorphological features such as distance from tidal creeks and elevation (Bertness & Ellison 1987, Gardner et al. 1988). This mesoscale topography may develop along hydrological or salinity gradients, which largely determine soil chemical conditions. Variability at finer spatial scales in marshes is also common, often resulting from disturbance (Fischer et al. 2000). Fire, grazing, wrack deposition, treefall, and flooding may all generate discrete patches in wetlands (e.g. Bertness & Ellison 1987, White & Howes 1994, Berg et al. 1997, Stoeckel & Miller-Goodman 2001, McLaren & Jefferies 2004. On longer time sc...