Carbonates and Evaporites

, 18:89 | Cite as

A pragmatic test of the early origin and fixation of gamma-ray spectrometric (U, Th) and magneto-susceptibility (Fe) patterns related to sedimentary cycle boundaries in pure platform limestones

  • Jindrich Hladil
  • Pavel Bosak
  • Ladislav Slavik
  • James L. Carew
  • John E. Mylroie
  • Milan Gersl


In a pragmatic test conducted on vertical stratigraphic sections in Quaternary platform limestones of San Salvador Island, The Bahamas, gamma-ray spectrometric (GRS) and magnetosusceptibility (κ) data confirmed that characteristic geophysical patterns are coupled with depositional cycle boundaries. These geophysical patterns appear to develop in the early stages of diagenesis and are long lasting, because similar patterns are found both in the very young Bahamian limestones and in very old Devonian (Givetian-Frasnian) platform limestones of Moravia, Czech Republic. Because the Devonian limestones retain gamma ray and magnetic signatures similar to those seen in the Bahamian rocks, these signals are apparently resistant to changes that occur in later diagenetic alteration, including deep-burial diagenesis and 380 million years of rock-fluid interactions. Each sedimentary cycle on the Bahamian carbonate platform is marked by a terra rossa paleosol horizon that represents a lowstand emergent surface. The paleosol is typically characterized by a GRS-spike related to increased Th concentration. There is only a subtle downward infiltration of that GRS signal, but the Th signal may diffuse upward via sediment recycling. Two U-related GRS maxima are regularly developed within short distances below and above the cycle boundary. The lower anomaly reflects U enrichment in the sub-soil cementation zone, whereas the upper anomaly is related to increased U-content in the flooding beds of the next cycle. Such a combination of one Th-spike between two U-anomalies forms a distinctive tripartite GRS pattern.

The κ-anomalies form a bimodal signal that consists of a narrow but extraordinarily strong positive κ-anomaly that is coincident with the Th-spike, and another spike that is developed in the sub-soil cementation zone. In cases where a buried cycle boundary forms the truncated floor of a horizontal cave that is filled with carbonate sediment, both U and Th GRS peaks are broadened. The κ-curves also display elevated but strongly oscillating values across the cave fill. The spikes are arranged asymmetrically downward and the strongest spike corresponds to infiltration/cementation of the cave floor. The evidence from the Quaternary limestones suggests that these two patterns (the tripartite Th and U pattern of the standard cycle boundary, and the broadened pattern related to filled caves) have an early origin. In spite of large inhomogeneities on cycle-boundary surfaces, the above geophysical patterns appear to be distinctive, differ from the normal GRS-and κ-backgrounds of platform carbonates, and appear stabile over the long term. This test indicates that these two patterns may be useful for recognition of exposure surfaces/cycle boundaries via routine pattern searches in GR, GRS and κ well-logs from platform limestone sequences of a wide range of ages and paleoenvironments.


Uranium Devonian Thorium Frasnian Uranium Concentration 
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  1. BAIN, R.J., 1991, Distribution of Pleistocene lithofacies in the interior of San Salvador Island, Bahamas, and possible genetic models,in R.J. Bain, ed., Proceedings of the 5th Symposium on the Geology of the Bahamas 1990. Bahamian Field Station, San Salvador, Bahamas, p. 11–21.Google Scholar
  2. CAREW, J.L. and MYLROIE, J.E., 1995, Depositional model and stratigraphy for the Quaternary geology of the Bahama islands,in H.A. Curran and B. White, eds., Terrestrial and Shallow Marine Geology of the Bahamas and Bermuda: Geological Society of America Special Paper 300, p. 5–32.Google Scholar
  3. CAREW, J.L. and MYLROIE, J.E., 1997, The Bahamas (Chapter 3A),in H.L. Vacher and T. Quinn, eds., Geology and Hydrogeology of Carbonate Islands, Developments in Sedimentology, v. 54. Elsevier Publishing Company, New York, p. 91–139.Google Scholar
  4. CHEN, J.H., CURRAN, H.A., WHITE, B., and WASSERBURG, G.J., 1991, Precise chronology of the last interglacial period:234U−230Th data from fossil coral reefs in the Bahamas:Geological Society of America Bulletin, v. 103, p. 82–97.CrossRefGoogle Scholar
  5. COX, J.E., RAILSBACK, L.B., and GORDON, E.A., 2001, Evidence from Catskill pedognic carbonates for a rapid Late Devonian decrease in atmospheric carbon dioxide concentrations:Northeastern Geology and Environmental Sciences, v. 23, p. 91–102.Google Scholar
  6. ELWOOD, B.B., CRICK, R.E., and ELHASSANI, A., 1999, The magneto-susceptibility event and cyclostratigraphy (MSEC) method used in geological correlation of Devonian rocks from Anti-Atlas Morocco:American Association of Petroleum Geologists Bulletin, v. 83, p. 1119–1134.Google Scholar
  7. ELLWOOD, B.B, HARROLD, F.B., BENOIST, S.L., STRAUS, L.G., MORALES, M.G., PETRUSO, K., BICHO, N.F., ZILHAO, J., and SOLER, N., 2001, Paleoclimate and intersite correlations from late Pleistocene/Holocene cave sites: Results from southern Europe:Geoarcheology — An International Journal, v. 16, p.433–463.CrossRefGoogle Scholar
  8. HLADIL, J., 1994, Moravian Middle and Late Devonian Buildups: evolution in time and space with respect to Laurussian shelf:Courier Forschungsinstitut Senckenberg, v. 172, p. 111–125, 4 tabs in appendix.Google Scholar
  9. HLADIL, J., 2002, Geophysical records of dispersed weathering products on the Frasnian carbonate platform and early Famennian ramps in Moravia, Czech Republic: proxies for eustasy and palaeoclimate:Palaeogeography, Palaeoclimatology, Palaeoecology, v. 181, p. 213–250.CrossRefGoogle Scholar
  10. MYLROIE, J.E., 1983, Karst geology and Pleistocene history of San Salvador Island, Bahamas,in D.T. Gerace, ed., Proceedings of the First Symposium on the Geology of the Bahamas (March 22–25, 1982). CCFL Bahamian Field Station, Ft. Lauderdale, Florida, p. 6–11.Google Scholar
  11. NORTH AMERICAN COMMISSION ON STRATIGRAPHIC NOMENCLATURE, 1983, North American Stratigraphic Code:American Association of Petroleum Geologists Bulletin, v. 67, p. 841–875.Google Scholar
  12. PANUSKA, B.C., MYLROIE, J.E., and CAREW, J.L., 1997, Stratigraphic tests of the utility of paleomagnetic secular variation for correlation of paleosols, San Salvador Island, Bahamas,in J.L. Carew, ed., Proceedings of the 8th Symposium on the Geology of the Bahamas and Other Carbonate Regions 1996. Bahamian Field Station, San Salvador, Bahamas, p. 148–157.Google Scholar
  13. RUFFELL, A. and WORDEN, R., 2000, Palaeoclimate analysis using spectral gamma-ray data from the Aptian (Cretaceous) of southern England and southern France:Palaeogeography, Palaeoclimatology, Palaeoecology, v. 155, p. 265–283.CrossRefGoogle Scholar
  14. SCHWABE, S.J., CAREW, J.L., and MYLROIE, J.E., 1993, Petrology of Bahamian Pleistocene eolianites and flank margin caves: Implications for Late Quaternary island development,in B. White, ed., Proceedings of the 6th Symposium on the Geology of the Bahamas 1992. Bahamian Field Station, San Salvador, Bahamas, p. 149–164.Google Scholar
  15. STREEL, M., CAPUTO, M.V., LOBOZIAK, S., and MELO, J.H.G., 2000, Late Frasnian-Famennian climates based on palynomorph analyses and the question of the Late Devonian glaciations:Earth-Science Reviews, v. 52, p. 121–173.CrossRefGoogle Scholar

Copyright information

© Springer 2003

Authors and Affiliations

  • Jindrich Hladil
    • 1
  • Pavel Bosak
    • 1
  • Ladislav Slavik
    • 1
  • James L. Carew
    • 2
  • John E. Mylroie
    • 3
  • Milan Gersl
    • 4
  1. 1.Institute of GeologyAcademy of Sciences CRPraha 6Czech Republic
  2. 2.Department of Geology and Environmental GeosciencesCollege of CharlestonCharleston
  3. 3.Department of GeosciencesMississippi State UniversityMississippi State
  4. 4.Department of Geology and PaleontologyMasaryk UniversityBrnoCzech Republic

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