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LIST OF FIGURES<br />

1.1 Location map <strong>of</strong> St. Vincent Isl<strong>and</strong> on <strong>the</strong> nor<strong>the</strong>astern Gulf <strong>of</strong> Mexico<br />

coast, Florida, sou<strong>the</strong>astern U.S.A. Inset map shows <strong>the</strong> chain <strong>of</strong> barrier<br />

isl<strong>and</strong>s <strong>and</strong> spits <strong>of</strong> which St. Vincent is a part........................................................................15<br />

1.2 Beach ridge sets on St. Vincent Isl<strong>and</strong>. See Figure 1.1 for location<br />

(Source: Stapor, 1973) .............................................................................................................16<br />

1.3 The Florida Platform. The edge <strong>of</strong> <strong>the</strong> platform is marked by <strong>the</strong> west<br />

Florida shelf <strong>and</strong> slope, which drop into <strong>the</strong> deep Gulf <strong>of</strong> Mexico. Note<br />

that Florida occupies approximately half <strong>of</strong> <strong>the</strong> carbonate platform.<br />

(Source: USGS, 2001) .............................................................................................................17<br />

1.4 Pleistocene glacial advances <strong>and</strong> retreats, as recorded in benthic<br />

oxygen isotope records. The record shows <strong>the</strong> predicted sea level (solid<br />

18<br />

line) <strong>and</strong> mean ocean O (dashed line), derived from ice volume<br />

histories. (Source: Raymo et al., 2006)...................................................................................18<br />

1.5 Composite sea level curves for <strong>the</strong> nor<strong>the</strong>rn Gulf <strong>of</strong> Mexico. The solid<br />

line adapted from Balsillie <strong>and</strong> Donoghue (2004) is a comprehensive<br />

compilation <strong>of</strong> radiocarbon dated sea-level indicators for <strong>the</strong> nor<strong>the</strong>rn Gulf<br />

<strong>of</strong> Mexico. The dashed curve is <strong>the</strong> global “eustatic” sea-level history<br />

from Red Sea benthic foraminifera data <strong>of</strong> Siddall et al (2003). .............................................19<br />

1.6 The Apalachicola River drainage basin, northwest Florida. The<br />

boundaries <strong>of</strong> <strong>the</strong> basin are shown by <strong>the</strong> solid black line. (Source:<br />

Northwest Water Management District, 1996). St. Vincent Isl<strong>and</strong> is<br />

located in <strong>the</strong> lower left center <strong>of</strong> <strong>the</strong> map...............................................................................20<br />

1.7 Model <strong>of</strong> beach ridge formation. (Source: Tanner, 1989) .................................................21<br />

1.8 Global sea-level history from 400,000 years to present, based on dated<br />

shoreline indicators from Barbados <strong>and</strong> New Guinea (symbols) <strong>and</strong><br />

oxygen isotope data from marine sediments (solid line). (Source: Lea et al,<br />

2002) ........................................................................................................................................22<br />

2.1 Infrared orthophoto <strong>of</strong> St. Vincent Isl<strong>and</strong> showing <strong>the</strong> beach ridge<br />

plain that covers <strong>the</strong> surface <strong>of</strong> <strong>the</strong> isl<strong>and</strong> (USGS imagery). Location is<br />

shown in Figure 1.1..................................................................................................................28<br />

2.2 Sediment transport rates in <strong>the</strong> Apalachicola barrier isl<strong>and</strong> chain. The<br />

arrows indicate <strong>the</strong> direction <strong>of</strong> transport <strong>and</strong> <strong>the</strong> numbers represent <strong>the</strong><br />

volume (in 10 3 m 3 /yr) <strong>of</strong> material deposited <strong>and</strong> eroded. (Source: Stapor,<br />

1973) ........................................................................................................................................29<br />

vii

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