Document Type
Dissertation
Degree
Doctor of Philosophy (PhD)
Major/Program
Biology
First Advisor's Name
Evelyn Gaiser
First Advisor's Committee Title
Committe Chair
Second Advisor's Name
James Heffernan
Second Advisor's Committee Title
Committee Member
Third Advisor's Name
Jennifer Richards
Third Advisor's Committee Title
Committee Member
Fourth Advisor's Name
Colin Saunders
Fourth Advisor's Committee Title
Committee Member
Fifth Advisor's Name
Hugh Willoughby
Fifth Advisor's Committee Title
Committee Member
Keywords
diatoms, climate, paleoecology, tropical cyclones, estuaries
Date of Defense
11-13-2014
Abstract
Estuaries are dynamic on many spatial and temporal scales. Distinguishing effects of unpredictable events from cyclical patterns can be challenging but important to predict the influence of press and pulse drivers in the face of climate change. Diatom assemblages respond rapidly to changing environmental conditions and characterize change on multiple time scales. The goals of this research were to 1) characterize diatom assemblages in the Charlotte Harbor watershed, their relationships with water quality parameters, and how they change in response to climate; and 2) use assemblages in sediment cores to interpret past climate changes and tropical cyclone activity.
Diatom assemblages had strong relationships with salinity and nutrient concentrations, and a quantitative tool was developed to reconstruct past values of these parameters. Assemblages were stable between the wet and dry seasons, and were more similar to each other than to assemblages found following a tropical cyclone. Diatom assemblages following the storm showed a decrease in dispersion among sites, a pattern that was consistent on different spatial scales but may depend on hydrological management regimes.
Analysis of sediment cores from two southwest Florida estuaries showed that locally-developed diatom inference models can be applied with caution on regional scales. Large-scale climate changes were suggested by environmental reconstructions in both estuaries, but with slightly different temporal pacing. Estimates of salinity and nutrient concentrations suggested that major hydrological patterns changed at approximately 5.5 and 3 kyrs BP. A highly temporally-resolved sediment core from Charlotte Harbor provided evidence for past changes that correspond with known climate records. Diatom assemblages had significant relationships with the three-year average index values of the Atlantic Multidecadal Oscillation and the El Niño Southern Oscillation. Assemblages that predicted low salinity and high total phosphorus also had the lowest dispersion and corresponded with some major storms in the known record, which together may provide a proxy for evidence of severe storms in the paleoecological record.
Identifier
FI14110752
Recommended Citation
Nodine, Emily R., "Evidence of Climate Variability and Tropical Cyclone Activity from Diatom Assemblage Dynamics in Coastal Southwest Florida" (2014). FIU Electronic Theses and Dissertations. 1657.
https://digitalcommons.fiu.edu/etd/1657
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