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Improved Constraints on Sedimentary Environments of Palygorskite Deposits of the Hawthorne Formation, Southern Georgia, from a Detailed Study of a Core

Published online by Cambridge University Press:  01 January 2024

Mark P. S. Krekeler*
Affiliation:
Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois 60607, USA
*
*E-mail address of corresponding author: rhodochrosite@email.msn.com

Abstract

The sedimentology and mineralogy of a 2.5 m core from a palygorskite deposit of the Miocene Hawthorne Formation, southern Georgia is described. The lithology involves laminated clay-rich sediment composed of ∼90% clay and 10% sand, with six clay-pebble layers present. Sand to pebble-size clasts of phosphate material are common throughout the core. The sand laminations are probably flood-related and the clay-pebble layers are storm deposits, with the pebbles being derived locally from subaerial environments. Phosphate clasts are reworked bone material.

The sands are quartz-rich and are subarkosic in composition with average quartz counts of 86.50% and average total feldspar counts of 11.50%. Heavy minerals observed include orthopyroxene, clinopyroxene, amphibole, zircon, rutile, garnet, tourmaline, kyanite, muscovite, biotite, spinels and opaques. Palygorskite fibers dominate the clay-size fraction of the samples and comprise ∼80–90% of sample material with smectite comprising the remainder. Hydroxylapatite comprises ∼3% of sediment volume and occurs as individual euhedral hexagonal crystals and as clusters of crystals.

Investigation of this core suggests that the palygorskite deposit represents a dynamic system with regular flooding and storm deposition being common. Mineral composition of sands may be useful for stratigraphic correlation of palygorskite deposits in the Apalachicola Embayment. This study supports the general environmental interpretations of previous workers for the palygorskite deposits of southern Georgia, but provides greater detail.

Type
Research Article
Copyright
Copyright © 2004, The Clay Minerals Society

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References

Andrews, G.W. and Abbott, W.H., (1985) Miocene Diatoms from the Hawthorne Formation, Thomas County, Georgia Bulletin of American Paleontology 87 57109.Google Scholar
Arnold, D., (1971) Ethnomineralogy of Ticul Yucatan potters American Antiquity 36 2040 10.2307/278020.Google Scholar
Atakhanov, O., (1980) Silt deposits and clay pebbles in the present and ancient valleys of the Amu Darya River Problems of Desert Development 1 2934.Google Scholar
Blatt, H., (1967) Original characteristics of quartz grains Journal of Sedimentary Petrology 37 401424.Google Scholar
Blatt, H. and Totten, M.W., (1981) Detrital quartz as an indicator of distance from shore in marine mudrocks Journal of Sedimentary Petrology 51 12591266 10.2110/jsr.51.355.Google Scholar
Bradley, W.F., (1940) The structural scheme of attapulgite American Mineralogist 25 405410.Google Scholar
Dickinson, W.R. and Dickinson, W.R., (1974) Plate tectonics and sedimentation Tectonics and Sedimentation Tulsa, Oklahoma Society of Economic Paleontologists and Mineralogists 127 10.2110/pec.74.22.CrossRefGoogle Scholar
Dickinson, W.R., (1982) Composition of sandstones in the Circum-Pacific subduction complexes and fore arc basins American Association of Petroleum Geologists Bulletin 66 121137.Google Scholar
Dickinson, W.R. and Suczek, C.A., (1979) Plate tectonics and sandstone composition American Association of Petroleum Geologists Bulletin 63 21642182.Google Scholar
Dickinson, W.R. Beard, L.S. Brakenridge, G.R. Erjavec, J.L. Ferguson, R.C. Inman, K.F. Knepp, R.A. Lindeberg, F.A. and Ryberg, P.T., (1983) Provenance of North American phanerozoic sandstones in relation to tectonic setting Geological Society of America Bulletin 94 222235 10.1130/0016-7606(1983)94<222:PONAPS>2.0.CO;2.Google Scholar
Galán, E., (1996) Properties and applications of palygorskite-sepiolite clays Clay Minerals 31 443453 10.1180/claymin.1996.031.4.01.Google Scholar
Gremillion, L.R., (1965) The origin of attapulgite in the Miocene strata of Florida and Georgia Tallahasse, Florida Florida State University PhD dissertation.Google Scholar
Isphording, W.C., Singer, A. and Galán, E., (1984) The clays of the Yucatan, Mexico. A contrast in genesis Palygorskite-Sepiolite: Occurrences, Genesis, and Uses New York Elsevier 5973.Google Scholar
Jones, B. Galán, E. and Bailey, S.W., (1988) Sepiolite and palygorskite Hydrous Phyllosillicates Washington, D.C Mineralogical Society of America 631674 10.1515/9781501508998-021.Google Scholar
Krekeler, M.P.S. Guggenheim, S. and Rakovan, J., (2004) A microtexture study of palygorskite-rich sediments from the Hawthorne Formation, southern Georgia by transmission electron microscopy and atomic force microscopy Clays and Clay Minerals 52 263274 10.1346/CCMN.2004.0520302.Google Scholar
Liu, K.B. and Fearn, M.L., (2000) Reconstruction of prehistoric landfall frequencies of catastrophic hurricanes in northwestern Florida from lake sediment records Quaternary Research 54 238245 10.1006/qres.2000.2166.Google Scholar
Merkl, R.S., (1989) A sedimentological, mineralogical, and geochemical study of the fuller’s earth deposits of the Miocene Hawthorne group of south Georgia-north Florida Bloomington, Indiana Indiana University PhD dissertation.Google Scholar
Nossin, J.J., (1961) Occurrence and origin of clay pebbles on the east coast of Johore, Malaya Journal of Sedimentary Petrology 31 437447 10.1306/74D70B91-2B21-11D7-8648000102C1865D.CrossRefGoogle Scholar
Ovcharenko, F.D. Kukovsky, G., Singer, A. and Galán, E., (1984) Palygorskite and sepiolite deposits in the USSR Palygorskite-Sepiolite: Occurrences, Genesis, and Uses New York Elsevier 233241.Google Scholar
Patterson, S.H. (1974) Fuller’s earth and industrial mineral resources of the Meigs-Attapulgus-Quincy district, Georgia and Florida. US Geological Survey Professional Paper, P0828, 45 pp.Google Scholar
Scotese, C.R., (2001) Atlas of Earth History, Volume 1, Paleogeography Arlington, Texas, USA PALEOMAP project 52 pp.Google Scholar
Solomon, D.H., (1968) Clay minerals as electron acceptors and/or electron donors in organic reactions Clays and Clay Minerals 16 3139 10.1346/CCMN.1968.0160105.Google Scholar
Solomon, D.H. and Rosser, M.J., (1965) Reactions catalyzed by minerals, Part I Journal of Applied Polymer Science 9 1261 10.1002/app.1965.070090407.Google Scholar
Tanner, W.F., (1961) Clay and Peat boulders Journal of Sedimentary Petrology 31 634636 10.1306/74D70C2C-2B21-11D7-8648000102C1865D.CrossRefGoogle Scholar
Theng, B.K.G., (1974) The Chemistry of Clay-Organic Reactions New York John Wiley & Sons 343 pp.Google Scholar
Tillman, R., (1996) Estuarine tidal-accretion bar subfacies recognition and geometries American Association of Petroleum Geologists Annual Meeting, Abstracts 5 140.Google Scholar
Van Olphen, H., (1966) Maya blue: clay organic pigment Science 154 645646 10.1126/science.154.3749.645.Google Scholar
Vaughan, T.W. (1902) Fuller’s earth of southwestern Georgia and western Florida. US Geological Survey, Mineral Resources of the United States, Calender Year 1901, 922934.Google Scholar
Weaver, C.E., Singer, A. and Galán, E., (1984) Origin and geologic implications of the palygorskite deposits of the S.E. United States Palygorskite-Sepiolite: Occurrences, Genesis, and Uses New York Elsevier 3958.Google Scholar
Weaver, C.E. and Beck, K.C., (1972) Vertical variability in the attapulgite mining area Proceedings of Seventh Forum on Geology of Industrial Minerals 17 5190.Google Scholar
Weaver, C.E. and Beck, K.C., (1977) Miocene of the S.E. United States: a model for chemical sedimentation in a perimarine environment New York Elsevier 234 pp.Google Scholar
Winchell, N.H., (1894) Pebbles of clay in stratified gravel and sand Glacialists’ Magazine 1 171.Google Scholar