Document Type
Dissertation
Degree
Doctor of Philosophy (PhD)
Major/Program
Biology
First Advisor's Name
John Kominoski
First Advisor's Committee Title
Committee chair
Second Advisor's Name
Steven Pennings
Second Advisor's Committee Title
Committee Member
Third Advisor's Name
Steven Oberbauer
Third Advisor's Committee Title
Committee Member
Fourth Advisor's Name
Michael Ross
Fourth Advisor's Committee Title
Committee Member
Fifth Advisor's Name
Tiffany Troxler
Fifth Advisor's Committee Title
Committee Member
Keywords
coastal wetlands, sea-level rise, saltwater intrusion, carbon storage, ecosystem vulnerability, Florida Everglades, Texas coast, resilience
Date of Defense
6-27-2018
Abstract
Coastal wetlands protect coastlines through efficient storage of organic carbon (OC) that decreases wetland vulnerability to sea level rise (SLR). Accelerated SLR is driving saltwater intrusion and altering vegetation communities and biogeochemical conditions in coastal wetlands with uncertain implications. We quantified changes in OC stocks and fluxes driven by 1) saltwater and phosphorous intrusion on freshwater and brackish marshes, 2) vegetation along an experimental saltmarsh to mangrove gradient, 3) saltwater intrusion and vegetation change across a marsh to mangrove ecotone, and 4) vegetation change and mangrove forest development along a marsh to mangrove ecotone. Increasing salinity in freshwater marshes decreased root biomass and soil elevation within one year. In brackish marshes, increased salinity decreased root productivity and biomass and increased root breakdown rate (k), while added salinity did not increase elevation loss. In our experimental marsh-mangrove ecotone, mangrove vegetation promoted higher organic carbon (OC) storage by increasing above and belowground biomass and reducing organic matter k. However, mangroves also increased belowground k, and decreased allochthonous marine subsidies, indicating the potential for OC storage trade-offs. In the Southeast Everglades, we identified strong interior-coastal gradients in soil stoichiometry and mangrove cover. Interior freshwater soil conditions increased k, while total soil OC stocks decreased toward the coast indicating that saltwater intrusion is driving large scale soil OC loss. In the southeast Everglades, mangrove expansion increased root biomass and root productivity, but did not mitigate the overall loss of OC stocks toward the coast. Similarly, in the southwest Everglades, saltwater intrusion drove a decrease in soil OC. However, mangrove encroachment drove a rapid recovery and increased OC stocks. Mangrove encroachment doubled aboveground biomass within the last ten years, increased it 30 times in the last 30 years, and doubled belowground biomass after 20 years. Our research shows that 1) moderate saltwater intrusion without mangrove encroachment will lead to a loss in OC stocks and potentially lead to wetland elevation loss and submergence, 2) in the absence of a change in saltwater intrusion, mangrove expansion can enhance OC storage 3) mangrove expansion can mitigate OC loss during saltwater intrusion, but this pattern depends on mangrove recruitment and ecosystem productivity.
Identifier
FIDC006842
Recommended Citation
Charles, Sean Patrick, "Saltwater Intrusion and Vegetation Shifts Drive Changes in Carbon Storage in Coastal Wetlands" (2018). FIU Electronic Theses and Dissertations. 3791.
https://digitalcommons.fiu.edu/etd/3791
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