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

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Curray, J.R., Emmel, F.J. and Crampton, P.J.S., 1969, Holocene history of a strandplain lagoonal coast, Nayarit, Mexico: Lagunas costeras, un simposio. Mem. Simp. Intern Lagunas Costeras. Unam Unesco, p.63-100. Curray, J.R., 1996, Origin of beach ridges: comment on Tanner, W.F., 1995. Origin of beach ridges and swales. Mar. Geol., 129: 149-161: Marine Geology, v.136, p.121-125. Davis, R.A., Fox, H.T., Hayes, M.O. and Boothroyd, J.C., 1972, Comparison of ridge-and-runnel systems in tidal and non-tidal environments: Journal of Sedimentary Petrology, v.42, p.401-412. Davis, J.L. and Annan, A.P., 1989, Ground penetrating radar for high resolution mapping of soil and rock stratigraphy: Geophysical Prospecting, v.37, p.531-555. Davis, R.A., 1997, The Evolving Coast. New York: Scientific American Library. Davis, J. H., and Mokray, M. F., 2000, Assessment of the effect of road construction and other modifications of surface-water flow at St. Vincent National Wildlife Refuge, Franklin County Florida: US Geological Survey Water Resource Investigations Report 00-4007. deBeaumont, E., 1845, Lecons de geologie pratique: P. Bertrand, Paris, p.223-252. Doeglas, D.J., 1946, Interpretation of the results of mechanical analyses: Journal of Sedimentary Petrology, v.16, p.19-40. Dominguez, J.M.L., Bittencourt, A.C.S.P. and Martin, L., 1992, Controls on Quaternary coastal evolution of the east-northeastern coast of Brazil: roles of sea-level history, trade winds and climate: In Quaternary Coastal Evolution, Sedimentary Geology, v.80, p.213-232. Donoghue, J.F. and Tanner, W.F., 1992, Quaternary terraces and shorelines of the Panhandle Florida region: In Quaternary Coasts of the United States: Marine and Lacustrine Systems, SEPM Special Pub. 48, Eds C.H. Fletcher and J.F. Wehmiller, p.233-241. Donoghue, J.F., 1993, Late Wisconsinian and Holocene depositional history, northeastern Gulf of Mexico: Marine Geology, v.112, p.185-205. Donoghue, J.F. and Tanner, W.F., 1994, Effects of Near-Term Sedimentologic Evolution of the Lifetime of Estuarine Resources. Apalachicola River and Bay National Estuarine Research Preserve: NOAA Technical Memorandum, NOS-SRD-27. 57 p. Donoghue, J. F., and White, N. M., 1995, Late Holocene sea-level change and delta migration, Apalachicola River region, northwest Florida, USA: Journal of Coastal Research, v. 11, no. 3, p. 651-653. Dorsey, R.A., 1997, Predicted sea level changes, Florida Gulf Coast over the past 21,000 years. GARI Research Series #9, 31 p. 259
Douglas, B., Kearney, M. and Leatherman, S., 2001, Sea level rise: history and consequences. International Geophysics Series, v.75, San Diego: Academic Press. Duller, G.A.T., 1991, Equivalent dose determination using single aliquots: Nuclear Tracks and Radiation Measurements, v.18, p.371-378. Duller, G.A.T., 1999, Analyst version 2.12. Luminescence Laboratory, University of Wales. Eichenholtz, M.E., Pirkle, E.C. and Pirkle, F.L., 1989, Sediment characteristics of selected beach ridges along Florida’s northeastern coast: Southeastern Geology, v.30, p.155-167. Ekman, M., 1988, The world’s longest continued series of sea-level observations: Pure Applied Geophysics, v.127, p.73-77. Fairbridge, R.W., 1961, Eustatic changes in sea level: In: Physics and Chemistry of the Earth. Eds. L.H. Ahrens, Frank Press, Kalervo Rankiama, S.K. Runcorn. v.4, p.99-185. Fernald, E.A. and Purdum, E.D., 1992, Atlas of Florida: Gainsville, Florida: University Press of Florida. 280 p. Fisher, J.J., 1968, Barrier island formation: discussion: Geological Society of American Bulletin, v.79, p.1421-1426. Fisk, H.N., 1956, Nearshore sediments of the continental shelf off Louisianna: Eighth Texas Conference on Soil Mechanics and Foundation Engineering, p.1. Folk, R.L., 1974, Petrology of Sedimentary Rocks: Austin, Hemphill Publishing Company, 182 p. Folz. E. and Mercier, N., 1999, A single-aliquot OSL protocol using bracketing regenerative doses to accurately determine equivalent doses in quartz: Radiation Measurements, v.30, p.477- 485. Forrest, B., 2003, Application of luminescence techniques to coastal studies at the St. Joseph Peninsula, Gulf County, Florida: unpublished MSc. Thesis, McMaster University, Hamilton, Ontario, 217 p. Fraser, G.S. and Hester, N.C., 1977, Sediments and sedimentary structures of a beach-ridge complex, southwestern shore of Lake Michigan: Journal of Sedimentary Petrology, v.47, p.1187-1200. Frazier, D.E., 1974, Depositional episodes: their relationship to the Quaternary stratigraphy in the northwestern portion of the Gulf basin: Austin, University of Texas, Bureau of Economic Geology, Geological Circular 74-1, 28 p. 260
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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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Page 277: Berger, G., 1988, Dating quaternary
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Page 283 and 284: Northwest Florida Water Management
Page 285 and 286: Stapor, F.W. and Tanner, W.F., 1977
Page 287 and 288: BIOGRAPHICAL SKETCH Beth Margaret F
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