Hostname: page-component-6d856f89d9-76ns8 Total loading time: 0 Render date: 2024-07-16T09:02:48.521Z Has data issue: false hasContentIssue false
  • English
  • Français

Holocene Sea-Level History: Case Study of the Statistical Evaluation of 14C Dates

Published online by Cambridge University Press:  18 July 2016

Mebus A Geyh
Mebus A Geyh*
Affiliation:
Niedersächsisches Landesamt für Bodenforschung, D3000 Hannover, Germany
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The limits of the statistical evaluation of 14C dates by histograms are discussed. The method of the attempt to establish a global chronology of the short-term eustatic sea-level changes during the Holocene is examined as well as its correlation with the precisely determined Suess wiggles.

Type
Quaternary
Information
Radiocarbon , Volume 22 , Issue 3: Heidelberg , 1980 , pp. 695 - 704
Copyright
Copyright © The American Journal of Science

References

Andrews, J T, Mears, A, Miller, G H, and Pleasant, D R, 1972, Holocene Late Glacial maximum and marine transgressions in the eastern Canadian Arctic: Nature, Phys Sci, v 239, p 147–149.Google Scholar
Bruns, Michael, Münnich, K O, and Becker, Bernd, 1980, Natural radiocarbon variations from ad 200 to 800, in Stuiver, Minze and Kra, Renee, eds, Internatl radiocarbon conf, 10th, Proc: Radiocarbon, v 22, no. 2, p 273–278.Google Scholar
Fairbridge, R W and Hillaire-Marcel, C, 1977, An 8000 year palaeoclimatic record of the ‘Double-Hale’ 45 year solar cycle: Nature, v 268, no. 5619, p 413–416.Google Scholar
Geyh, M A, 1969, Versuch einer chronologischen Gliederung des marinen Holozäns an der Nordseeküste mit Hilfe der statistischen Auswertung von 14C-Daten: Deutsche geol Gesell Zeitschr, v 118, p 351–360.10.1127/zdgg/118/1969/351Google Scholar
Geyh, M A 1971, Middle and young Holocene sea-level changes as global contemporary events: Geol fören Stockholm Förh, v 93, p 679–691.10.1080/11035897109451539Google Scholar
Geyh, M A and Jäkel, D, 1977, The climate of the Sahara during the Late Pleistocene and the Holocene on the basis of available radiocarbon dates: Natl Resources and Development, v 6, p 64–79.Google Scholar
Geyh, M A and Rohde, P, 1972, Weichselian chronostratigraphy, 14C dating and statistics, in Internatl geol cong, 24th, Proc: Montreal, sec 12, p 27–36.Google Scholar
Geyh, M A and Streif, J, 1970, Studies on coastal movements and sea-level changes by means of the statistical evaluation of 14C data, in Internatl symposium coastal geodesy, Proc: Munnich, p 599–611.Google Scholar
Jelgersma, S, 1961, Holocene sea-level changes in the Netherlands: Geol Stichting Med, v C VI 7, p 1–100.Google Scholar
de Jong, A F M, Mook, W G, and Becker, Bernd, 1979, Confirmation of Suess wiggles: 3200-3700 bc: Nature, v 280, no. 5717, p 48–49.10.1038/280048a0Google Scholar
Mörner, N-A, 1976, Eustatic changes during the last 8000 years in view of radiocarbon calibration and new information from the Kattegatt region and other northwestern European areas: Palaeogeog, Palaeoclimatol, Palaeoecol, v 19, p 63–85.Google Scholar
Shennan, I, 1978, Statistical evaluation of sea-level data, in Tooley, M, ed, IGCP Proj 61, Sea-level changes, Bull: Durham.Google Scholar
Sheppard, F P and Curray, J R, 1967, Carbon-14 determination of sea-level changes in stable areas: Progress in Oceanography, volume 4: Oxford, Pergamon Press, p 283–291.Google Scholar
Sonntag, C, Klitzsch, E, El Shazley, E M, Kalinke, C and Münnich, K O, 1978, Paläoklimatische information im Isotopengehalt 14C datierter Saharawässer: Kontinentaleffekt in D und 18O: Geol Rundshau, v 67, p 413–424.10.1007/BF01802798Google Scholar
Stuiver, Minze, 1969, Evidences for the variation of atmospheric 14C content in the Late Quaternary, in Turekian, K K, ed, Late Cenozoic glacial ages: New Haven, Yale Univ Press, p 57–70.Google Scholar
Tooley, M J, 1978, Sea-level changes during the Flandrian stage: Oxford, Clarendon Press, p 232.Google Scholar