Sediment and Nutrient Deposition Associated with Hurricane Wilma in Mangroves of the Florida Coastal Everglades

The distribution of mangrove biomass and forest structure along Shark River estuary in the Florida Coastal Everglades (FCE) has been correlated with elevated total phosphorus concentration in soils thought to be associated with storm events. The passage of Hurricane Wilma across Shark River estuary...

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Veröffentlicht in:Estuaries and coasts 2010-01, Vol.33 (1), p.45-58
Hauptverfasser: Castañeda-Moya, Edward, Twilley, Robert R., Rivera-Monroy, Victor H., Zhang, Keqi, Davis, Stephen E., Ross, Michael
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container_end_page 58
container_issue 1
container_start_page 45
container_title Estuaries and coasts
container_volume 33
creator Castañeda-Moya, Edward
Twilley, Robert R.
Rivera-Monroy, Victor H.
Zhang, Keqi
Davis, Stephen E.
Ross, Michael
description The distribution of mangrove biomass and forest structure along Shark River estuary in the Florida Coastal Everglades (FCE) has been correlated with elevated total phosphorus concentration in soils thought to be associated with storm events. The passage of Hurricane Wilma across Shark River estuary in 2005 allowed us to quantify sediment deposition and nutrient inputs in FCE mangrove forests associated with this storm event and to evaluate whether these pulsing events are sufficient to regulate nutrient biogeochemistry in mangrove forests of south Florida. We sampled the spatial pattern of sediment deposits and their chemical properties in mangrove forests along FCE sites in December 2005 and October 2006. The thickness (0.5 to 4.5 cm) of hurricane sediment deposits decreased with distance inland at each site. Bulk density, organic matter content, total nitrogen (N) and phosphorus (P) concentrations, and inorganic and organic P pools of hurricane sediment deposits differed from surface (0-10 cm) mangrove soils at each site. Vertical accretion resulting from this hurricane event was eight to 17 times greater than the annual accretion rate (0.30 ± 0.03 cm year⁻¹) averaged over the last 50 years. Total P inputs from storm-derived sediments were equivalent to twice the average surface soil nutrient P density (0.19 mg cm⁻³). In contrast, total N inputs contributed 0.8 times the average soil nutrient N density (2.8 mg cm⁻³). Allochthonous mineral inputs from Hurricane Wilma represent a significant source of sediment to soil vertical accretion rates and nutrient resources in mangroves of southwestern Everglades. The gradient in total P deposition to mangrove soils from west to east direction across the FCE associated with this storm event is particularly significant to forest development due to the P-limited condition of this carbonate ecosystem. This source of P may be an important adaptation of mangrove forests in the Caribbean region to projected impacts of sea-level rise.
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The passage of Hurricane Wilma across Shark River estuary in 2005 allowed us to quantify sediment deposition and nutrient inputs in FCE mangrove forests associated with this storm event and to evaluate whether these pulsing events are sufficient to regulate nutrient biogeochemistry in mangrove forests of south Florida. We sampled the spatial pattern of sediment deposits and their chemical properties in mangrove forests along FCE sites in December 2005 and October 2006. The thickness (0.5 to 4.5 cm) of hurricane sediment deposits decreased with distance inland at each site. Bulk density, organic matter content, total nitrogen (N) and phosphorus (P) concentrations, and inorganic and organic P pools of hurricane sediment deposits differed from surface (0-10 cm) mangrove soils at each site. Vertical accretion resulting from this hurricane event was eight to 17 times greater than the annual accretion rate (0.30 ± 0.03 cm year⁻¹) averaged over the last 50 years. Total P inputs from storm-derived sediments were equivalent to twice the average surface soil nutrient P density (0.19 mg cm⁻³). In contrast, total N inputs contributed 0.8 times the average soil nutrient N density (2.8 mg cm⁻³). Allochthonous mineral inputs from Hurricane Wilma represent a significant source of sediment to soil vertical accretion rates and nutrient resources in mangroves of southwestern Everglades. The gradient in total P deposition to mangrove soils from west to east direction across the FCE associated with this storm event is particularly significant to forest development due to the P-limited condition of this carbonate ecosystem. This source of P may be an important adaptation of mangrove forests in the Caribbean region to projected impacts of sea-level rise.</abstract><cop>New York</cop><pub>Spring Science + Business Media</pub><doi>10.1007/s12237-009-9242-0</doi><tpages>14</tpages></addata></record>
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source Jstor Complete Legacy; Springer Nature - Complete Springer Journals
subjects Accretion
Animal and plant ecology
Animal, plant and microbial ecology
Biogeochemistry
Biological and medical sciences
Biomass
Brackish
Brackish water ecosystems
Chemical properties
Coastal Sciences
Earth and Environmental Science
Ecology
Environment
Environmental Management
Estuaries
Everglades
Forest soils
Freshwater
Freshwater & Marine Ecology
Fundamental and applied biological sciences. Psychology
Hurricanes
Mangrove forests
Mangrove soils
Mangroves
Marine
Organic matter
Organic phosphorus
Phosphorus
Rivers
Sediment deposition
Sedimentary soils
Sedimentation & deposition
Sediments
Sharks
Soil nutrients
Soil surfaces
Soils
Storms
Synecology
Water and Health
title Sediment and Nutrient Deposition Associated with Hurricane Wilma in Mangroves of the Florida Coastal Everglades
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