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Holocene aridity and storm phases, Gulf and Atlantic coasts, USA

Published online by Cambridge University Press:  20 January 2017

Ervin G. Otvos
Ervin G. Otvos*
Affiliation:
Department of Coastal Sciences and Gulf Coast Research Laboratory, University of Southern Mississippi, PO Box 7000, Ocean Springs, MS 39566-7000, USA
*
E-mail address: http://ervin.otvos@usm.edu.
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Abstract

A bottomland flora that prevailed between ∼9900 and 6000 cal yr B.P. in a North Carolina stream valley may not reflect a regionally much wetter Atlantic climate, coeval with record drought in the Great Plains region and assumed dry Gulf coastal conditions. Such conditions were inferred for 6000 ± 1000 yr ago when the Bermuda High may have consistently occupied summer positions far to the NE. Arid episodes coeval with the Little River local wet interval are known from eolian sediments and pollen spectra in the Atlantic and the Gulf coastal plain. For multiple reasons, the regional extent, intensity, and duration of coastal aridity and alternating wet phases and the Bermuda High positions are not yet adequately constrained. The climate and edaphic causes for the steadily growing predominance of southern pines over hardwoods, achieved between ∼8900 and 4200 cal yr B.P. at different sites at different times are similarly still unresolved. New data from Shelby Lake, AL, reconfirms that no credible field or other proxy evidence exists for a previously postulated “catastrophic Gulf hurricane phase” in the late Holocene.

Keywords

Drought and wet phasesBermuda HighPine or hardwood dominanceHurricane proxiesClimate indicators“Storm quiescence”Mid–late Holocene transgression
Type
Scientific Communication
Information
Quaternary Research , Volume 63 , Issue 3 , May 2005 , pp. 368 - 373
Copyright
University of Washington

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References

Baker, R.G., Bettis, E.A. III, Denniston, R.F., Gonzalez, L.A., (2001). Plant remains, alluvial chronology, and cave speleothem isotopes indicate abrupt Holocene climatic change at 6 ka in Midwestern USA. Global and Planetary Change 28, 285–291.CrossRefGoogle Scholar
F.Z., Brook, (1996). A late Quaternary pollen record from the middle Ogeechee River Valley, southeastern coastal plain, Georgia.Masters Thesis,University of Georgia, , 110 p.Google Scholar
Clark, J.S., Grimm, E.M., Donovan, J.J., Fritz, S.C., Engstrom, D.R., Almendinger, J.E., (2002). Drought cycles and landscape responses to past aridity on prairies of the northern Great Plains. Ecology 83, 595–601.Google Scholar
Delcourt, P.A., (1980). Goshen Springs: late Quaternary vegetation record for southern Alabama. Ecology 61, 371–386.Google Scholar
Delcourt, P.A., Delcourt, H.R., (1996). Quaternary paleoecology of the Lower Mississippi Valley. Engineering Geology 45, 219–242.CrossRefGoogle Scholar
Delcourt, P.A., Delcourt, H.R., Brister, R.C., Lackey, L.E., (1980). Quaternary vegetation history of the Mississippi Embayment. Quaternary Research 13, 111–132.Google Scholar
Delcourt, H.R., Delcourt, P.A., Spiker, E.C., (1983). A 12,000-year record of forest history from Cahaba Pond, St. Clair County, Alabama. Ecology 64, 874–887.Google Scholar
Delcourt, P., Delcourt, H.R., Morse, D.F., Morse, P.A., (1993). History, evolution, and organization of vegetation and human culture. Martin, Wm.H., Boyce, S.G., Echternacht, A.C., Biodiversity of the southeastern United States. Lowland terrestrial communities John Wiley Publishers, 47–79.502 p.Google Scholar
Eden, D.N., Page, M.J., (1998). Paleoclimatic implications of a storm erosion record from late Holocene lake sediments, North Island, New Zealand. Palaeogeography, Palaeoclimatology, Palaeoecology 139, 37–58.Google Scholar
Fletcher, Ch.H. III, van Pelt, J.E., Brush, G.S., Sherman, J., (1993). Tidal wetland record of Holocene sea-level movements and climate history. Palaeogeography, Palaeoclimatology, Palaeoecology 102, 177–213.Google Scholar
Forman, S.L., Oglesby, R., Markgraf, V., Stafford, T., (1995). Paleoclimatic significance of late Quaternary eolian deposition on the Piedmont and High Plains, central United States. Global and Planetary Change 11, 35–55.Google Scholar
Forman, S.L., Oglesby, R., Webb, R.S., (2001). Temporal and spatial patterns of Holocene dune activity on the Great Plains of North America: megadroughts and climate links. Global and Planetary Change 29, 1–29.Google Scholar
Givens, C.R., Givens, F.M., (1983). Age and significance of fossil white spruce (Picea glauca), Tunica Hills, Louisiana–Mississippi. Quaternary Research 27, 283–296.Google Scholar
Goman, M., Leigh, D.S., (2004). Wet early to middle Holocene conditions on the upper coastal plain of North Carolina. Quaternary Research 61, 256–264.Google Scholar
Ivester, A.H., Leigh, D.S., Godfrey-Smith, D.I., (2001). Chronology of inland eolian dunes on the coastal plain of Georgia, USA. Quaternary Research 55, 293–302.Google Scholar
Kutzbach, J.E., (1987). Model simulations of the climatic patterns during the deglaciation of North America. Shane, L.C.K., Cushing, E.J., Ruddiman, W.F., Wright, H.E. Jr., North American and adjacent oceans during the last glaciations The Geology of North America vol. K-3, 425–446.Google Scholar
Lambert, W.J., Aharon, P., Rodriguez, A.B., (2003). An assessment of the late Holocene record of severe storm impact from Lake Shelby, Alabama. Transactions-Gulf Coast Association of Geological Societies 53, 443–452.Google Scholar
H.J.K., Lamoreaux,(1999). Human–environmental relationships in the Coastal Plain of Georgia based on high-resolution paleoenvironmental records from three peat deposits.Ph.D. dissertation,Univ. of Georgia, , Athens., .Google Scholar
Leigh, D.S., Feeney, T.P., (1995). Paleochannels indicating wet climate and lack of response to lower sea levels, southeast Georgia. Geology 23, 687–690.Google Scholar
Liu, K.-b., Fearn, M.L., (1993). Lake-sediment record of late Holocene hurricane activities from coastal Alabama. Geology 21, 793–796.Google Scholar
Liu, K.-b., Fearn, M.L., (2000). Reconstruction of prehistoric landfall frequencies of catastrophic hurricanes. Quaternary Research 54, 238–245.Google Scholar
Otvos, E.G., (1999). Quaternary coastal history, basin geometry and assumed evidence of hurricane activity, northeastern Gulf of Mexico coastal plain. Journal of Coastal Research 15, 438–443.Google Scholar
Otvos, E.G., (2002). Discussion of “Prehistoric landfall frequencies of catastrophic hurricanes” (Liu and Fearn, 2000). Quaternary Research 57, 425–428.Google Scholar
Otvos, E.G., (2004a). Prospects for interregional correlations using Wisconsin and Holocene aridity episodes, northern Gulf of Mexico coastal plain. Quaternary Research 61, 105–118.CrossRefGoogle Scholar
Otvos, E.G., (2004b). Holocene Gulf levels: recognition issues and an updated sea-level curve. Journal of Coastal Research 20, 680–699.Google Scholar
C.A., Seielstad, (1994). Holocene environmental history of Chatterton Springs on the southern Coastal Plain of Georgia.M. A.Thesis,Univ. of Georgia, , Athens., .Google Scholar
U.S. Department of Commerce, NOAA, , (1948–2003). Climatological data (precipitation). Annual data sheets for Mississippi.Google Scholar
U.S. Army Corps of Engineers, Mobile District, , (1981). Hurricane frederic post-disaster report. 30 August–14 September, 1979, 242 p with 61 plates.Google Scholar
Watts, W.A., (1971). Postglacial and interglacial vegetation history of southern Georgia and central Florida. Ecology 52, 676–690.Google Scholar
Watts, W.A., (1980). Late-Quaternary vegetation history at White Pond on the Inner Coastal Plain of South Carolina. Quaternary Research 13, 187–199.Google Scholar
Watts, W.A., Hansen, B.S., (1994). Pre-Holocene and Holocene pollen records of vegetation history from the Florida Peninsula and their climatic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 109, 163–176.Google Scholar
Watts, W.A., Grimm, E.C., Hussey, T.C., (1996). Mid-Holocene forest history of Florida and the coastal plain of Georgia. Sassaman, K.E., Anderson, D.G., Archaeology of the Mid-Holocene Southeast University Press of Florida, Gainesville., 28–38.387 p.Google Scholar
Whitehead, D.R., (1972). Development and environmental history of the Dismal Swamp. Ecological Monographs 42, 301–315.Google Scholar
Whitehead, D.R., (1981). Late-Pleistocene vegetation changes in northeastern North Carolina. Ecological Monographs 51, 451–471.CrossRefGoogle Scholar
Wright, H.E. Jr., (1992). Patterns of Holocene change in the Midwest US. Quaternary Research 38, 129–134.Google Scholar