the florida state university college of arts and sciences evolution of ...

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McFarlan, E. Jr., 1961, Radiocarbon dating of late quaternary deposits, south Louisianna: Geological Society of American Bulletin, v.72, p.129-158. McKeown, H.A., Bart, P.J. and Anderson, J.B., 2004, High resolution stratigraphy of a sandy ramp-type margin – Apalachicola, Florida: p. 25-41 in Anderson, J. and Fillon, R., eds, Late Quaternary Stratigraphic Evolution of the Northern Gulf of Mexico Margin: Spec. Publ. 79, Society for Sedimentary Geology. Mejdahl, V. and Christiansen, H.H., 1994, Procedures used for luminescence dating of sediment: Quaternary Science Reviews, v.13, p.403-406. Miller, J.J., Griffin, J.W., Fryman, M.L., and Stapor, F.J., 1981, Archaeological and historical survey of St. Vincent National Wildlife Refuge, Florida: unpubl. Report by Cultural Resource Management, Inc. for Interagency Archaeological Services, U.S. Fish and Wildlife Service, 219 p. Missimer, T., 1973, Growth rates of beach ridges on Sanibel Island, Florida: Transactions-Gulf Coast Association of Geological Societies, v.23, p.383-388. Moore, L.J., Jol, H.M., Krose, S., Vanderburgh, S. and Kaminsky, G.M., 2004, Annual layers revealed by GPR in the subsurface of a prograding coastal barrier, southwest Washington, USA: Journal of Sedimentary Research, v.74, p.690-696. Morton, R. A., Paine, J. G., and Blum, M. D., 2000, Responses of stable bay margins and barrier island systems to Holocene sea-level changes, western Gulf of Mexico: Journal of Sedimentary Research, v.70, p. 478-490. Moslow, T.F., 1983, Depositional Models of Shelf and Shoreline Sandstones: Continuing Eduction Course Note Series #27, A continuing education course presented at the 1983 American Association of Petroleum Geologists Fall Education Conference. 102 p. Murray, A.S. and Roberts, R.G., 1998, Measurement of the equivalent dose in quartz using a regenerative-dose single-aliquot protocol: Radiation Measurements, v.29, p.503-515. Murray, A.S. and Wintle, A.G., 2000, Luminescence dating of quartz using an improved singlealiquot regenerative dose protocol: Radiation Measurements, v.32, p.57-73. Murray, A.S. and Olley, J.M., 2002, Precision and accuracy in the optically stimulated luminescence dating of sedimentary quartz: A status review: Geochronometria, v.21, p.1-16. Murray-Wallace, C.V., Banerjee, D., Bourman, R.P., Olley, J. and Brooke, B.P., 2002, Optically stimulated luminescence dating of Holocene relict foredunes, Guichen Bay, South Australia: Quaternary Science Reviews, v.21, p.1077-1086. Neal, A., Pontee, N.I., Pye, K. and Richards, J., 2002, Internal structure of mixed sand-andgravel beach deposits revealed using ground-penetrating radar: Sedimentology, v.49, p.789-804. 263
Northwest Florida Water Management District (NWFWMD), 1996, Apalachicola River and Bay System: Northwest Florida Water Management District. Available online: [http://www.nwfwmd.state.fl.us/rmd/swim/swimdesc.htm#Apalachicola] Otvos, E.G., 2000, Beach ridges—definitions and significance: Geomorphology, v.31, p.83-108. Pirazzoli, P.A., 1974, Dati storici sul medio mare a Venezia: Att Accad. Sci. Inst. Bologna, v.13, p.125-148. Pirazzoli, P.A., 1991, World atlas of Holocene sea level changes: Amsterdam, Elsevier, 300 p. Prescott, J.R. and Hutton, J.T., 1994, Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations: Radiation Measurements, v.23, p.497-500. Price, W.A., 1963, Origin of barrier chain and beach ridge, p.219 in The Geological Society of America, Abstracts With Programs: Geological Society of America Special Paper, v.73, 355 p. Psuty, N.P., 1966, The geomorphology of beach ridges in Tabasco, Mexico. Baton Rouge, LA: Louisianna State University, Coastal Studies Institute, Technical Report 30, 51 p. Randazzo, A. F., and Jones, P. S.(eds), 1997, The Geology of Florida: Gainesville, University Press of Florida, 327 p. Raney, D., Huang, I. And Urgun, H., 1985, A hydrodynamic and salinity model for Apalachicola Bay, Florida: Mississippi-Alabama Sea Grant College Program Report No. 339- 183, 84 p. Raymo, M.E., Lisiecki, L.E. and Nisancioglu, K.H., 2006, Plio-Pleistocene ice volume, Antarctic climate and the global δ 18 O record: Science, v.313, p.492-495. Reineck, H.E. and Singh, I.B., 1978, Depositional Sedimentary Environments: Springer Verlag, New York, 439 p. Reinson, G.E., 1992, Transgressive barrier island and estuarine systems, p. 179-194 in Walker, R.G. and James, N.P., eds., Facies Models: St. John’s, Newfoundland, Geological Association of Canada. p.179-194 Ritter, D.F., 1986, Process Geomorphology. Iowa: W.M.C. Brown Publishing. 579pp. Rizk, F., 1991, The Late Holocene Development of St. Joseph Spit: PhD Dissertation, Florida State University, Tallahassee, Florida, 379 p. Rohling, E.J. and Palike, H., 2005, Centennial-scale climate cooling with a sudden cold event around 8,200 years ago: Nature, v.434, p.975-980. 264
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THE FLORIDA STATE UNIVERSITY COLLEG
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ACKNOWLEDGEMENTS I would like to th
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4. RESULTS Laboratory Analyses ....
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LIST OF FIGURES 1.1 Location map of
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preheating is carried out on a heat
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4.17 Site SVI 023. a) Trench. b) Sa
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4.38 Location relative to the Apala
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A.37 Granplot analysis of sample 05
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A.83 Granplot analysis of sample 05
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ABSTRACT The goal of this investiga
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4) To further develop Optically Sti
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the rate of erosion or deposition a
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esult of the buildup of offshore ba
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Recent studies of barriers using Gr
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and, therefore, sea level) (Dorsey,
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Holocene Sea Level Over 900 Holocen
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first is that sea level rose steadi
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Figure 1.2. Beach ridge sets on St.
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-100 Figure 1.4. Pleistocene glacia
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Figure 1.6. The Apalachicola River
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Figure 1.8. Global sea-level histor
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K and L have crest elevations of ap
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Geoarchaeology The earliest inhabit
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Oyster Pond Figure 2.1. Infrared or
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Figure 2.3. St. Vincent Island shor
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Pickalene Middens Paradise Point Si
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At each vibracore or trench locatio
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luminescence signal equivalent to t
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Application of OSL to Coastal Studi
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atio between the first and the fift
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Topographic Surveying Topographic s
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time elapsed between when this ener
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a) b) Figure 3.1. a) Collecting a v
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Increasing energy T CONDUCTION BAND
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Figure 3.5. Sample removed from lar
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Figure 3.7. Location of samples col
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Figure 3.9. Basis of airborne LIDAR
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Sample Sites CHAPTER 4 RESULTS A to
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SVI005 This site is located just we
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collapsed the trench. Therefore, a
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SVI025 This site is located within
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m and 3.7 m respectively. A cross s
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Vincent Island has changed little o
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(sorting). Standard deviation decre
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4,100 and 3,500 years ago. The corr
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Table 4.1 Continued Site Samples Be
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Table 4.3. Measured elevations of S
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Table 4.5. Application of Tanner’
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Table 4.7. OSL age calculations usi
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Table 4.9. Paleosealevel position e
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Figure 4.2. Example of a trench thr
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Figure 4.5. Site SVI 003. Trench ex
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a) b) 050505-01E 050505-01K 050505-
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a) b) 050505-04C 050505-04A Figure
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Figure 4.13. Site SVI 015. Vibracor
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a) b) 011006-15 011006-16 Figure 4.
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a) b) 011106-08 011106-07 011106-10
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Figure 4.21. Dutch gouge-auger core
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Figure 4.23. Line A-A’ represents
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Elevation (m) NAVD 88 5.00 4.50 4.0
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1200 +/- 100 yr 102 Figure 4.27. GP
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0.65 Set C 0.6 0.55 0.5 Set A 0.45
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6 Set B Set C Set E 5 Set A Set F S
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0.7 Set C 0.6 Set A 0.5 Set E Set F
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ENVIRONMENTS OF DEPOSITION -- SKEWN
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mean grain size (phi) 3 2.5 2 1.5 1
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SVI 015 SVI 002 SVI 003 114 SVI 004
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CHAPTER 5 DISCUSSION The beach ridg
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vibracore or trench, both of which
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Skewness can be used to identify th
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island. Another is a C-14 date of 2
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sea level. It was at this point tha
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The fourth hypothesis was that sea-
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APPENDIX A INDIVIDUAL SIEVE ANALYSI
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