We examined the vegetation of the Southeast Saline Everglades (SESE), where
water management and sea level rise have been important ecological forces
during the last 50 years. Marshes within the SESE were arranged in well-def
ined compositional zones parallel to the coast, with mangrove-dominated shr
ub communities near the coast giving way to graminoid-mangrove mixtures, an
d then Cladium marsh. The compositional gradient was accompanied by an inte
riorward decrease in total aboveground biomass, and increases in leaf area
index and periphyton biomass. Since the mid-1940s, the boundary of the mixe
d graminoid-mangrove and Cladium communities shifted inland by 3.3 km. The
interior boundary of a low-productivity zone appearing white on both black-
and-white and CIR photos moved inland by 1.5 km on average. A smaller shift
in this 'white zone' was observed in an area receiving fresh water overflo
w through gaps in one of the SESE canals, while greater change occurred in
areas cut off from upstream water sources by roads or levees. These large-s
cale vegetation dynamics are apparently the combined result of sea level ri
se - ca. 10 cm since 1940 - and water management practices in the SESE.