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

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REFERENCES Aitken, M.J., 1991, Thermoluminescence dating: p.121-140 in Goksu, H.Y. et al (eds), Scientific Dating Methods: Dordrecht Kluwer Publ. Aitken, M. J., 1998, An Introduction to Optical Dating: The Dating of Quaternary Sediments by the use of Photon-Stimulated Luminescence: New York, Oxford University Press. Alvarez, L.F., 1984, Los Guarixes, Isla del Carmen, Camp., su climatologia, cambios de nivel de mar y patron de asenta miento: Professional thesis, School of Anthropology, University of Veracruz, Jalapa, Veracruz, Mexico, 83 p. Alvarez, L.F., 1985, El sitio arqueologico Los Guarixes. Los Talleres Tipograficos del Gobierno Municipal de Ciudad del Carmen, Campeche. Balsillie, J.H., 1995, William F. Tanner on Environmental Clastic Granulometry. Special Publication 40: Tallahassee, Florida Geological Survey. 145 p. Balsillie, J.H., Donoghue, J.F., Butler, K.M., and Koch, J.L., 2002, Plotting equation for Gaussian percentiles and a spreadsheet program for generating probability plots: Journal of Sedimentary Research, v. 72, p. 929-933. Balsillie, J.H. and Donoghue, J.F., 2004, High resolution sea-level history for the Gulf of Mexico since the last glacial maximum: Florida Geological Survey Report of Investigations #103. Tallahassee, FL, Florida Geological Survey, 31 p. Ballarini, M., Wallinga, J., Murray, A.S., Van Heteren, S., Oost, A.P., Bos, A.J.J. and van Eijk, C.W.E., 2003, Optical dating of young coastal dunes on a decadal time scale: Quaternary Science Reviews, v.22 (10-13), p.1011-1017. Bard, E., Hamelin, B., Fairbanks, R.G. and Zindler, A., 1990, Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals: Nature, v.345, p.405-410. Bard, E., 1997, Nuclide production by cosmic rays during the last ice age: Science, v.277, p.532- 533. Bard, E., 1998, Geochemical and geophysical implications of the radiocarbon calibration: Geochimica et Cosmochimica Acta., v.62 (12), p.2025-2038. Bard, E., Arnold, M., Hamelin, B., Tisnerat-Laborak, N. and Labioch, G., 1998, Radiocarbon calibration by means of mass spectrometric 230 Th/ 234 U and 14 C ages of corals: an updated database including samples from Barbados, Mururoa and Tahiti: Radiocarbon, v.40, p.1085- 1092. 257
Berger, G., 1988, Dating quaternary events by luminescence: Geological Society of America Special Paper, v. 227, p.13-50. Berger, G., 1995, Progress in luminescence dating methods for quaternary sediments: In N.W. Ritter and N.R. Catto (eds). Dating Methods for Quaternary Deposits. Newfoundland: Geological Association of Canada, p. 81-104. Best, J.L., Ashworth, P.J., Bristow, C.S. and Roden, J., 2003, Three-dimensional sedimentary architecture of a large mid-channel sand braid bar, Jamuna River, Bangladesh: Journal of Sedimentary Research, v.73, p.516-530. Bloom, A.L., ed., 1977, Atlas of Sea-level curves: final report, International Geological Correlation Program, Project 61, 92 p. Blum, M. D., Carter, A. E., Zayac, T., and Goble, R. J., 2002, Middle Holocene Sea-Level and Evolution of the Gulf of Mexico Coast (USA): Journal of Coastal Research. Special Issue 36, p. 65-80. Boggs, S., 1995, Principles of Sedimentology and Stratigraphy, 3 rd edition, New Jersey: Prentice- Hall Inc. p. 343-356. Braley, C. O., 1982, Archaeological testing and evaluation of the Paradise Point Site (8Fr71), St. Vincent National Wildlife Refuge, Franklin County, Florida: Report to Interagency Archaeological Services Division, National Parks Service. Bristow, C.S., Chroston, P.N. and Bailey, S.D., 2000, The structure and development of foredunes on a locally prograding coast: insights from ground-penetrating radar surveys, Norfolk, UK: Sedimentology, v.47, p.923-944. Bristow, C.S. and Pucillo, K., 2006, Quantifying rates of coastal progradation from sediment volume using GPR and OSL: the Holocene fill of Guichen Bay, south-east South Australia: Sedimentology, v.53, p.769-788. Campbell, K. M., 1986, St. Vincent Island (St. Vincent National Wildlife Refuge), Florida: in Neathery, T., ed., Geological Society of America Centennial Field Guide, Southeastern Section, DNAG, p. 351-353. Carter, R.W.G., 1986, The morphodynamics of beach ridge formation: Magilligan, Northern Ireland. Marine Geology, v.73, p.191-214. Curray, J.R., 1960, Sediments and history of the Holocene transgression, continental shelf, Northwest Gulf of Mexico: in Sherard, F.P., Phleger, F.B. and VanAndel, T.H. eds., Recent Sediments, Northwest Gulf of Mexico: American Association of Petroleum Geologists, Tulsa, p.221-266. 258
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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 279 and 280: Douglas, B., Kearney, M. and Leathe
Page 281 and 282: Jol, H.M., Peterson, C.D., Vanderbu
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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