Mass tree mortality leads to mangrove peat collapse at Bay Islands, Honduras after Hurricane Mitch

Authors

  • Donald R. Cahoon,

    Corresponding author
    1. US Geological Survey, National Wetlands Research Center, Lafayette, LA 70506, USA,
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  • Philippe Hensel,

    1. US Geological Survey, National Wetlands Research Center, Lafayette, LA 70506, USA,
    2. Johnson Controls, Inc. at USGS, National Wetlands Research Center, Lafayette, LA 70506, USA,
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  • John Rybczyk,

    1. US Geological Survey, National Wetlands Research Center, Lafayette, LA 70506, USA,
    2. Western Washington University, Huxley College of the Environment, Department of Environmental Sciences, Bellingham, WA 98225, USA, and *Johnson Controls, Inc. at USGS, National Wetlands Research Center, Lafayette, LA 70506, USA
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  • Karen L. McKee,

    1. US Geological Survey, National Wetlands Research Center, Lafayette, LA 70506, USA,
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  • C. Edward Proffitt,

    1. US Geological Survey, National Wetlands Research Center, Lafayette, LA 70506, USA,
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  • Brian C. Perez

    1. US Geological Survey, National Wetlands Research Center, Lafayette, LA 70506, USA,
    2. Johnson Controls, Inc. at USGS, National Wetlands Research Center, Lafayette, LA 70506, USA,
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Donald R. Cahoon, US Geological Survey, Patuxent Wildlife Research Center, Laurel, MD 20708, USA (tel. +1 301 497 5523; fax +1 301 497 5744; e-mail don_cahoon@usgs.gov).

Summary

  • 1We measured sediment elevation and accretion dynamics in mangrove forests on the islands of Guanaja and Roatan, Honduras, impacted by Hurricane Mitch in 1998 to determine if collapse of underlying peat was occurring as a result of mass tree mortality. Little is known about the balance between production and decomposition of soil organic matter in the maintenance of sediment elevation of mangrove forests with biogenic soils.
  • 2Sediment elevation change measured with the rod surface elevation table from 18 months to 33 months after the storm differed significantly among low, medium and high wind impact sites. Mangrove forests suffering minimal to partial mortality gained elevation at a rate (5 mm year−1) greater than vertical accretion (2 mm year−1) measured from artificial soil marker horizons, suggesting that root production contributed to sediment elevation. Basin forests that suffered mass tree mortality experienced peat collapse of about 11 mm year−1 as a result of decomposition of dead root material and sediment compaction. Low soil shear strength and lack of root growth accompanied elevation decreases.
  • 3Model simulations using the Relative Elevation Model indicate that peat collapse in the high impact basin mangrove forest would be 37 mm year−1 for the 2 years immediately after the storm, as root material decomposed. In the absence of renewed root growth, the model predicts that peat collapse will continue for at least 8 more years at a rate (7 mm year−1) similar to that measured (11 mm year−1).
  • 4Mass tree mortality caused rapid elevation loss. Few trees survived and recovery of the high impact forest will thus depend primarily on seedling recruitment. Because seedling establishment is controlled in large part by sediment elevation in relation to tide height, continued peat collapse could further impair recovery rates.

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