3.8 Article

Differential salinity response between two Mississippi River subdeltas: Implications for changes in plant composition

Journal

ESTUARIES
Volume 24, Issue 1, Pages 78-89

Publisher

ESTUARINE RESEARCH FEDERATION
DOI: 10.2307/1352815

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Many studies have determined the physical dynamics of salt-water movement into riverine systems, but few studies have elucidated the role of periodic salinity incursions in affecting primary succession in active deltaic wetlands. The emergence of the neighboring Atchafalaya and Wax Lake Deltas, since a record Mississippi River flood in 1973, has created a unique area of land building and primary succession within the deteriorating wetland landscape of Louisiana. The vegetation in these deltas experiences the extremes of allogenic (riverine and tidal flooding, sedimentation, storm disturbance) and autogenic (herbivory, plant competition) forces. The rapid decline of the dominant vegetation, Sagittaria latifolia Willd. (Broadleaf Arrowhead), in the Atchafalaya Delta, and the continued dominance of this species in the Wax Lake Delta prompted us to investigate whether periodic salinity incursions were an additional stress on this species. The objectives of our study were to determine if salinity differences occurred between these deltas, describe the forces that controlled salinity incursions, and the level of salt exposure that adversely affected the growth of S. latifolia. Continuous measurements of salinity and water level at six sites, revealed that salinity pulses (up to 7.0 parts per thousand) were common in the Atchafalaya Delta; the Wax Lake Delta was not prone to elevated salinities. Salinity incursions in the Atchafalaya Delta were related to water level set-up, which was forced by strong (> 10 m s(-1)) easterly and southerly winds prior to cold front passages. The movement of distant tropical storms in the Gulf of Mexico produced salinity incursions of longer duration than cold fronts. In a greenhouse experiment, the growth of S. latifolia was impaired by salinity concentrations of 6.0 parts per thousand within 13 d; flooding treatments (20 cm) compounded the loss of aboveground tissue by the end of the experiment. Results from the field and greenhouse studies, compared with historic evidence of elevated salinities in the Atchafalaya delta, indicate that periodic salinity incursions, combined with additional stresses such as flooding and vertebrate herbivory, influence the distribution or presence of S. latifolia in the Atchafalaya Delta.

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