, Volume 152, Issue 4, pp 607–616 | Cite as

Seasonal plant water uptake patterns in the saline southeast Everglades ecotone

  • Sharon M. L. Ewe
  • Leonel da S. L. Sternberg
  • Daniel L. Childers


The purpose of this study was to determine the seasonal water use patterns of dominant macrophytes coexisting in the coastal Everglades ecotone. We measured the stable isotope signatures in plant xylem water of Rhizophora mangle, Cladium jamaicense, and Sesuvium portulacastrum during the dry (DS) and wet (WS) seasons in the estuarine ecotone along Taylor River in Everglades National Park, FL, USA. Shallow soilwater and deeper groundwater salinity was also measured to extrapolate the salinity encountered by plants at their rooting zone. Average soil water oxygen isotope ratios (δ 18O) was enriched (4.8 ± 0.2‰) in the DS relative to the WS (0.0 ± 0.1‰), but groundwater δ 18O remained constant between seasons (DS: 2.2 ± 0.4‰; WS: 2.1 ± 0.1‰). There was an inversion in interstitial salinity patterns across the soil profile between seasons. In the DS, shallow water was euhaline [i.e., 43 practical salinity units (PSU)] while groundwater was less saline (18 PSU). In the WS, however, shallow water was fresh (i.e., 0 PSU) but groundwater remained brackish (14 PSU). All plants utilized 100% (shallow) freshwater during the WS, but in the DS R. mangle switched to a soil–groundwater mix (δ 55% groundwater) while C. jamaicense and S. portulacastrum continued to use euhaline shallow water. In the DS, based on δ 18O data, the roots of R. mangle roots were exposed to salinities of 25.4 ± 1.4 PSU, less saline than either C. jamaicense (39.1 ± 2.2 PSU) or S. portulacastrum (38.6 ± 2.5 PSU). Although the salinity tolerance of C. jamaicense is not known, it is unlikely that long-term exposure to high salinity is conducive to the persistence of this freshwater marsh sedge. This study increases our ecological understanding of how water uptake patterns of individual plants can contribute to ecosystem levels changes, not only in the southeast saline Everglades, but also in estuaries in general in response to global sea level rise and human-induced changes in freshwater flows.


Seasonal water uptake Mangrove ecotone Plant water use 



We thank G. Losada, T. Grahl, and G. Koch for field assistance, Greg Juszli, and the Wetland Ecosystems Ecology Laboratory for helpful comments on an earlier draft. We also thank the two anonymous reviewers for their helpful comments and Dr. Carlos Coronado (South Florida Water Management District) for kindly allowing the use of his aerial picture of the field site. This material is based on work supported by the National Science Foundation through FIU’s Florida Coastal Everglades LTER program (Grant #9910514) and the University of Miami’s Biocomplexity Grant #0322051. This manuscript is a Southeast Environmental Research Center Contribution No. 344.


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Copyright information

© Springer-Verlag 2007

Authors and Affiliations

  • Sharon M. L. Ewe
    • 1
  • Leonel da S. L. Sternberg
    • 2
  • Daniel L. Childers
    • 3
    • 4
  1. 1.Ecology and Environment, Inc.West Palm BeachUSA
  2. 2.University of MiamiCoral GablesUSA
  3. 3.Southeast Environmental Research CenterFlorida International UniversityMiamiUSA
  4. 4.Department of BiologyFlorida International UniversityMiamiUSA

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