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(SAVARESE, Michael)Tj
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(, College of Arts And Sciences, 10501 FGCU Blvd S, Fort Myers, FL )Tj
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(33965-6565, msavares@fgcu.edu, TEDESCO, Lenore, Geology, Indiana-Purdue \
Univ, )Tj
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(Indianapolis, 723 West Michigan Street, SL 118, Indianapolis, IN 46202, \
MANKIEWICZ, )Tj
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(Carol, Beloit College, 700 College St, Beloit, WI 53511-5595, LOWERY, Li\
ly, Geology, Univ )Tj
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(of the South, KITCHEN, Chris, Geology, Whitman College, and ROTH, Monica\
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(SUNY Oneonta )Tj
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(The coastal geomorphology of Southwest Florida is a unique system of ins\
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(outer islands develop upon gastropod or oyster reefs that become substra\
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(recruitment. Previous workers suggested that this system developed over \
the last 3500 years and )Tj
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(its stability is dependent upon the rate of sea-level rise relative to r\
ates of sedimentation. )Tj
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(Sediment cores taken from the Ten Thousand Islands indicate that two tra\
nsgressive/regressive )Tj
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(sediment packages occur within the Late Holocene record. These packages \
are identifiable from )Tj
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(either lithofacies shifts or faunal changes within subtidal facies. The \
initial transgression begins )Tj
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(roughly 5000 years ago and deposits subtidal sands over non-marine sedim\
ents. The system then )Tj
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(regresses through the development of intertidal oyster reefs and thin ma\
ngrove peats at ~4300 )Tj
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(years. The rate of sea level rise, however, remained too high to permit \
the regressive system to )Tj
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(persist. The second trangression places marine sediments above the peat.\
Subsequent oyster or )Tj
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(vermetiform gastropod reef development causes the coastal system to stab\
ilize or prograde. )Tj
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(Vermetiform reefs form earlier and distally relative to oyster reefs and\
may serve as the barrier )Tj
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(that ultimately predisposes Southwest Florida to its current geomorpholo\
gy. Oyster reef )Tj
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(development occurs later and more proximally and fills the inner bays. S\
lower sealevel rise rates )Tj
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(during this interval produce a thicker regressive package. Younger peats\
may overlie oyster reef )Tj
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(facies, forming inner bay islands, or may develop into thick accumulatio\
ns along the inner bay )Tj
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(margins as the coastal mangrove forest fringe stabilizes. An increase in\
sealevel rise rate should )Tj
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(disrupt this geomorphic pattern. Changes in the distribution of recent o\
yster reefs and the inner )Tj
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(bay mangrove fringe are already discernable. )Tj
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(\251 Copyright 2002 The Geological Society of America \(GSA\), all right\
s reserved. Permission is hereby )Tj
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(granted to the author\(s\) of this abstract to reproduce and distribute \
it freely, for noncommercial purposes. )Tj
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(Permission is hereby granted to any individual scientist to download a s\
ingle copy of this electronic file )Tj
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(and reproduce up to 20 paper copies for noncommercial purposes advancing\
science and education, )Tj
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