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Geological Responses to Urbanization of the Naples Bay Estuarine System, Southwestern Florida, USA
Journal article

Geological Responses to Urbanization of the Naples Bay Estuarine System, Southwestern Florida, USA

Bryan R. Fielder, Timothy M. Dellapenna, Michael Savarese and Christian J. Noll
Abstracts with programs - Geological Society of America, Vol.40(6), p.225
Geological Society of America, 2008 annual meeting
10-2008

Abstract

acoustical methods Bay of Naples canals channels characterization Collier County Florida cores Dollar Bay dredging estuarine environment Florida geophysical methods Gulf Coastal Plain human activity mangrove swamps mires Naples Florida samples Sedimentary petrology sediments shore features shorelines side-scanning methods southwestern Florida spatial distribution substrates swamps urban environment Hydrology United States Watersheds
The Naples Bay Estuarine System, situated in southwest Florida, has undergone extensive modifications caused directly and indirectly by anthropogenic influences. These alterations include the substitution of mangrove-forested shorelines with concrete bulkheads, canalization of the bay shoreline and within the watershed, and navigational channel dredging. The system consists of northern Naples Bay, southern Naples Bay, and Dollar Bay, whose shorelines range from highly developed to undeveloped, respectively. This project investigates the natural geological response of the system to these alterations; using data from side scan sonar, sediment grab samples, and vibracores. In the highly urbanized northern Naples Bay, substrates consist primarily of muddy sands, with few oyster reefs. Southern Naples Bay and Dollar Bay, however, consist of coarser sediment, and are characterized by extensive mangrove shorelines and numerous oyster reefs. The impact of anthropogenic alterations has significantly shifted sediment distributions in northern Naples Bay from a coarser to finer grained substrate, to a lesser degree in southern Naples Bay, and Dollar Bay has not made this transition, due to the relative lack of anthropogenic modifications made to this part of the system.

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