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Near-Zero Δ14C Values at 32 kyr cal BP Observed in the High-Resolution 14C Record from U-Th Dated Sediment of Lake Lisan

Published online by Cambridge University Press:  18 July 2016

K van der Borg*
Affiliation:
Department of Physics and Astronomy, Utrecht University, Netherlands
M Stein
Affiliation:
Geological Survey of Israel, Jerusalem, Israel
A F M de Jong
Affiliation:
Department of Physics and Astronomy, Utrecht University, Netherlands
N Waldmann
Affiliation:
Institute of Earth Sciences, Hebrew University, Jerusalem, Israel
S L Goldstein
Affiliation:
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA.
*
Corresponding author. Email: [email protected].
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Abstract

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A high-resolution atmospheric radiocarbon record has been obtained for the interval of 17–36 kyr from U/Th-dated aragonite sediment of Lake Lisan. Reservoir age corrections were applied with reservoir ages of 200, 1250, and 2000 yr, which correlate with the different water levels of the lake. The present 14C record for Lake Lisan shows near resemblance with that of Lake Suigetsu: both converge to the value of Δ14C ∼0‰ at 32 kyr cal BP. Both also show significant differences compared to other reported high-resolution 14C records (e.g. Iceland Sea, Cariaco basin, and Bahamas speleothem). This inconsistency should be addressed by re-assessment of the basic assumptions behind the determination of calendar ages of the various records.

Type
Part II
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Bard, E, Arnold, M, Hamelin, B, Tisnerat-Laborde, N, Cabioch, G. 1998. Radiocarbon calibration by means of mass spectrometric 230Th /234U and 14C ages of corals: an updated database including samples from Barbados, Mururoa and Tahiti. Radiocarbon 40(3):1085–92.CrossRefGoogle Scholar
Bard, E. 1998. Geochemical and geophysical implications of the radiocarbon calibration. Geochimica et Cosmochimica Acta 62(12):2025–38.Google Scholar
Bartov, Y, Goldstein, SL, Stein, M, Enzel, Y. 2003. Catastrophic arid episodes in the Eastern Mediterranean linked with the North Atlantic Heinrich event. Geology 31:439–44.Google Scholar
Beck, JW, Richards, DA, Edwards, RL, Silverman, BW, Smart, PL, Donahue, DJ, Herrera-Osterheld, S, Burr, GS, Calsoyas, L, Jull, AJT, Biddulph, D. 2001. Extremely large variations of atmospheric 14C concentration during the last glacial period. Science 292:2453–7.CrossRefGoogle ScholarPubMed
Begin, ZB, Ehrlich, A, Nathan, Y. 1974. Lake Lisan—The precursor of the Dead Sea. Geological Society Survey Israel Bulletin 63:130.Google Scholar
Frank, M, Schwarz, B, Baumann, S, Kubik, PW, Suter, M, Mangini, A. 1997. A 200-kyr record of cosmogenic radionuclide production rate and geomagnetic field intensity from 10Be in globally stacked deep-sea sediments. Earth and Planetary Science Letters 149:121–9.Google Scholar
Guyodo, Y, Valet, J-P. 1996. Relative variations in geomagnetic intensity from sedimentary records: the past 200,000 years. Earth and Planetary Science Letters 143:2336.Google Scholar
Haase-Schramm, A, Goldstein, SL, Stein, M. 2004. U-Th dating of Lake Lisan aragonite (late Pleistocene Dead Sea) and implications for glacial East Mediterranean climate change. Geochimica et Cosmochimica Acta 68(5):9851005.CrossRefGoogle Scholar
Hughen, K, Lehman, S, Southon, J, Overpeck, J, Marchal, O, Herring, C, Turnbull, J. 2004. 14C activity and global carbon cycle changes over the past 50,000 years. Science 303:202–7.Google Scholar
Kaufman, A. 1971. U-series dating of Dead Sea Basin carbonates. Geochimica et Cosmochimica Acta 35: 1269–81.Google Scholar
Kitagawa, H, van der Plicht, J. 2000. A 40,000-yr varve chronology from Lake Suigetsu, Japan: extension of the 14C calibration curve. Radiocarbon 42(3):369–80.Google Scholar
Schramm, A, Stein, M, Goldstein, SL. 2000. Calibration of the 14C timescale to >40 ka by 234U-230Th dating of Lake Lisan sediments (Last Glacial Dead Sea). Earth and Planetary Science Letters 175:2740.Google Scholar
Stein, M, Starinsky, A, Katz, A, Goldstein, SL, Machlus, M, Schramm, A. 1997. Strontium isotopic, chemical and sedimentological evidence for the evolution of Lake Lisan and the Dead Sea. Geochimica et Cosmochimica Acta 61(18):3975–92.Google Scholar
Stein, M, Migowski, C, Bookman, R, Lazar, B. 2004. Temporal changes in radiocarbon reservoir age in the Dead Sea-Lake Lisan system. Radiocarbon, these proceedings.Google Scholar
Stuiver, M, Reimer, PJ, Bard, E, Warren Beck, J, Burr, GS, Hughen, KA, Kromer, B, McCormac, G, van der Plicht, J, Spurk, M. 1998. INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40(3):1041–83.Google Scholar
van der Borg, K, Alderliesten, C, de Jong, AFM, van den Brink, A, de Haas, AP, Kersemaekers, HJH, Raaymakers, JEM. 1997. Precision and mass fractionation in 14C analysis with AMS. Nuclear Instruments and Methods in Physics Research B 123:97101.Google Scholar
Voelker, AHL, Grootes, PM, Nadeau, M-J, Sarntheim, M. 2000. Radiocarbon levels in the Iceland Sea from 25–53 kyr and their link to the earth's magnetic field intensity. Radiocarbon 42(3):437–52.Google Scholar