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4) To fur<strong>the</strong>r develop Optically Stimulated Luminescence (OSL) dating <strong>of</strong> quartz grains, a<br />

relatively new technique that has recently been used to directly date s<strong>and</strong>y coastal<br />

features.<br />

Potential Significance<br />

The study <strong>of</strong> relict str<strong>and</strong>plains <strong>and</strong> <strong>the</strong>ir stratigraphic context has <strong>the</strong> potential to provide<br />

high-resolution records that can be used to reconstruct <strong>the</strong> <strong>evolution</strong> <strong>of</strong> a coast (Zenkovitch,<br />

1967). With <strong>the</strong> exception <strong>of</strong> <strong>the</strong> recent studies by Morton et al. (2000) <strong>and</strong> Blum et al. (2002),<br />

this is a research area that is only recently being explored in <strong>the</strong> United States. The anticipated<br />

outcome <strong>of</strong> this work is a detailed history that is expected to emerge from <strong>the</strong> geochronologic<br />

<strong>and</strong> sedimentologic analyses <strong>of</strong> <strong>the</strong> dozen beach ridge sets on St. Vincent Isl<strong>and</strong>. Coastal<br />

geomorphologic features, especially coastal barriers, are highly sensitive to sea-level change.<br />

The dozen sets <strong>of</strong> beach ridges preserved on St. Vincent Isl<strong>and</strong> hold an unusually complete <strong>and</strong><br />

well-preserved record <strong>of</strong> <strong>the</strong> isl<strong>and</strong>’s response to this history <strong>of</strong> sea-level change during <strong>the</strong> late<br />

Quaternary. The Quaternary period has been a time <strong>of</strong> major global change. Much <strong>of</strong> that<br />

change, particularly sea-level change, has been geologically abrupt as can be seen in <strong>the</strong> Gulf <strong>of</strong><br />

Mexico sea level curve compiled by Balsillie <strong>and</strong> Donoghue (2004). An accurate determination<br />

<strong>of</strong> how abrupt changes in sea level over <strong>the</strong> past few millennia have affected coastal l<strong>and</strong>forms<br />

may be critically important to our underst<strong>and</strong>ing <strong>of</strong> <strong>the</strong> nature <strong>and</strong> potential effects <strong>of</strong> global<br />

change in <strong>the</strong> near future. The anticipated outcome <strong>of</strong> this project was a better underst<strong>and</strong>ing <strong>of</strong><br />

<strong>the</strong> response <strong>of</strong> coastal geologic environments to abrupt environmental change. Given that <strong>the</strong><br />

nor<strong>the</strong>astern Gulf <strong>of</strong> Mexico is a stable margin <strong>and</strong> reflects global eustatic change, this project<br />

will also have several broader impacts. It will answer some fundamental questions concerning<br />

<strong>the</strong> impact <strong>of</strong> global change, in <strong>the</strong> form <strong>of</strong> abrupt sea-level change, on coastal environments.<br />

An improved underst<strong>and</strong>ing <strong>of</strong> <strong>the</strong> history <strong>and</strong> timing <strong>of</strong> late Holocene climate-related events,<br />

<strong>and</strong> <strong>of</strong> <strong>the</strong> response <strong>of</strong> coastal environments to those events, is an essential component in <strong>the</strong><br />

development <strong>of</strong> global change predictions over <strong>the</strong> next few centuries.<br />

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