, Volume 13, Issue 6, pp 813–827

Hydrologic Modification and the Loss of Self-organized Patterning in the Ridge–Slough Mosaic of the Everglades

  • Danielle L. Watts
  • Matthew J. Cohen
  • James B. Heffernan
  • Todd Z. Osborne

DOI: 10.1007/s10021-010-9356-z

Cite this article as:
Watts, D.L., Cohen, M.J., Heffernan, J.B. et al. Ecosystems (2010) 13: 813. doi:10.1007/s10021-010-9356-z


The ridge–slough landscape of the Everglades (Florida, USA), is characterized by elevated ridges dominated by sawgrass (Cladium jamaicense) interspersed among deeper sloughs dominated by floating, submerged and emergent macrophytes and calcareous periphyton. Interactions among hydrologic conditions (water depth, hydroperiod), plant composition and production, and respiration are hypothesized to create alternative peat accretion equilibria at the point scale, while spatial interactions among patches create regular pattern at the landscape scale. Despite significant research on these interactions, few studies have examined the hypothesis that the ridge–slough landscape consists of spatially coupled alternative stable patch states, and none has used diagnostic indicators thereof to assess landscape resilience to hydrologic change. Dense random sampling of water depths (a proxy for soil elevation) along a gradient of hydrologic impairment of drained to relatively natural to impounded conditions was used to evaluate four predictions related to this hypothesis: (1) bimodal soil elevation distributions show strong fidelity to community type; (2) positive autocorrelation at short distances with negative values at longer distances; (3) strong anisotropy (diagnostic of flow orientation), and spatial structure (diagnostic of the strength of landscape self-organization); and (4) loss of these features with hydrologic modification. Our results support the hypothesis that soil elevations are strongly bimodal and anisotropic in areas with minimal hydrologic impact, and spatial autocorrelation patterns indicate the operation of scale-dependent feedbacks. These metrics change markedly with hydrologic modification, although with differences between drainage and impoundment. Moreover, changes in landform precede associated changes in vegetation, suggesting their utility as diagnostic indicators of landscape degradation and recovery.


biogeomorphology bi-modality scale-dependent feedbacks alternative stable states peat accretion patterned landscape 

Copyright information

© Springer Science+Business Media, LLC 2010

Authors and Affiliations

  • Danielle L. Watts
    • 1
  • Matthew J. Cohen
    • 2
  • James B. Heffernan
    • 3
  • Todd Z. Osborne
    • 4
  1. 1.School of Natural Resources and EnvironmentUniversity of FloridaGainesvilleUSA
  2. 2.School of Forest Resources and ConservationUniversity of FloridaGainesvilleUSA
  3. 3.Department of Biological SciencesFlorida International UniversityMiamiUSA
  4. 4.Soil and Water Science DepartmentsUniversity of FloridaGainesvilleUSA

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