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Radiocarbon Results from a 13-Kyr BP Coral from the Huon Peninsula, Papua New Guinea

Published online by Cambridge University Press:  18 July 2016

G S Burr ,
Chrystie Galang ,
F W Taylor ,
Christina Gallup ,
R Lawrence Edwards ,
Kirsten Cutler  and
Bill Quirk
G S Burr
Affiliation:
University of Arizona, NSF-Arizona AMS Laboratory, Tucson, Arizona 85721, USA.
Chrystie Galang
Affiliation:
University of Arizona, NSF-Arizona AMS Laboratory, Tucson, Arizona 85721, USA.
F W Taylor
Affiliation:
Institute for Geophysics, The University of Texas at Austin, 4412 Spicewood Springs Road, Bld. 600, Austin, Texas 78759-8500, USA.
Christina Gallup
Affiliation:
University of Minnesota Duluth Geological Sciences, Room 229 HHD175, 10 University Drive, Duluth, Minnesota 55812, USA
R Lawrence Edwards
Affiliation:
Minnesota Isotope Laboratory, Department of Geology and Geophysics, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, Minnesota 55455, USA.
Kirsten Cutler
Affiliation:
Minnesota Isotope Laboratory, Department of Geology and Geophysics, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, Minnesota 55455, USA.
Bill Quirk
Affiliation:
University Medical Center, University of Arizona, Tucson, Arizona 85721, USA.
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Abstract

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This paper presents radiocarbon results from a single Goniastrea favulus coral from Papua New Guinea which lived continuously between 13.0 and 13.1 kyr BP. The specimen was collected from a drill core on the Huon Peninsula and has been independently dated with 230Th. A site-specific reservoir correction has been applied to the results, and coral growth bands were used to calibrate individual growth years. Alternating density bands, which are the result of seasonal growth variations, were subsampled to provide 2 integrated 6-month 14C measurements per year. This allows for 20 independent measurements to be averaged for each decadal value of the 14C calibration, making these results the highest resolution data set available for this brief time range. The finestructure of the data set exhibits 14C oscillations with frequencies on the order of 4 to 10 yr, similar to those observed in modern coral 14C records.

Type
Articles
Information
Radiocarbon , Volume 46 , Issue 3: IntCal04: Calibration Issue, Guest Editor: PAULA J REIMER , 2004 , pp. 1211 - 1224
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Bard, E, Hamelin, B, Fairbanks, RG, Zindler, A. 1990. Calibration of the 14C time scale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals. Nature 345:405–10.Google Scholar
Bard, E, Arnold, M, Fairbanks, RG, Hamelin, B. 1993. 230Th-234U and 14C ages obtained by mass spectrometry on corals. Radiocarbon 35(1):191–9.Google Scholar
Bard, E, Hamelin, B, Arnold, M, Montaggioni, L, Cabioch, G, Faure, G, Rougerie, F. 1996. Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge. Nature 382:241–4Google Scholar
Bevington, PR, Robinson, DK. 1992. Data Reduction and Error Analysis for the Physical Sciences. New York: McGraw-Hill, Inc. 328 p.Google Scholar
Brown, TA, Farwell, GW, Grootes, PM, Schmidt, FH, Stuiver, M. 1993. Intra-annual variability of the radiocarbon content of corals from the Galapagos Islands. Radiocarbon 35(2):245–51.Google Scholar
Burr, GS, Edwards, RL, Donahue, DJ, Druffel, ERM, Taylor, FW. 1992. Mass spectrometric 14C and U-Th measurements in coral. Radiocarbon 34(3):611–8.Google Scholar
Burr, GS, Beck, JW, Taylor, FW, Récy, J, Edwards, RL, Cabioch, G, Corrège, T, Donahue, DJ, O'Malley, JM. 1998. A high-resolution radiocarbon calibration between 11,700 and 12,400 calendar years BP derived from 230Th ages of corals from Espiritu Santo Island, Vanuatu. Radiocarbon 40(3):1093–105.Google Scholar
Cabioch, G, Banks-Cutler, K, Beck, JW, Burr, GS, Corrège, T, Edwards, RL, Taylor, FW. 2003. Continuous reef growth during the last 23 cal kyr BP in a tectonically active zone (Vanuatu, southwest Pacific). Quaternary Science Reviews 22:1771–86.Google Scholar
Chappell, J, Polach, H. 1991. Post-glacial sea-level rise from a coral record at Huon Peninsula, Papua New Guinea. Nature 349:147–9.Google Scholar
Cutler, KA, Edwards, RL, Taylor, FW, Cheng, H, Adkins, J, Gallup, CD, Cutler, PM, Burr, GS, Bloom, AL. 2003. Rapid sea-level fall and deep-ocean temperature change since the last interglacial period. Earth and Planetary Science Letters 206:253–71.Google Scholar
Donahue, DJ, Linick, TW, Jull, AJT. 1990. Isotope-ratio and background corrections for accelerator mass spectrometry radiocarbon measurements. Radiocarbon 32(2):135–42.Google Scholar
Druffel, ERM. 1997. Geochemistry of corals: proxies of past ocean chemistry, ocean circulation, and climate. Proceedings National Academy of Sciences 94:8354–61.Google Scholar
Edwards, RL, Beck, JW, Burr, GS, Donahue, DJ, Chappell, JMA, Bloom, AL, Druffel, ERM, Taylor, FW. 1993. A large drop in atmospheric 14C/12C and reduced melting in the Younger Dryas, documented with 230Th ages of corals. Science 260:962–8.Google Scholar
Gagan, MK, Ayliffe, LK, Beck, JW, Cole, JE, Druffel, ERM, Dunbar, RB, Schrag, DP. 2000. New views of tropical paleoclimates from corals. Quaternary Science Reviews 19:45–64.Google Scholar
Guilderson, TP, Schrag, DP, Kashgarian, M, Southon, J. 1998. Radiocarbon variability in the western equatorial Pacific inferred from a high-resolution coral record from Nauru Island. Journal of Geophysical Research-Oceans 103(C11):24,641–50.Google Scholar
Guilderson, TP, Schrag, DP. 1998. Abrupt shift in subsurface temperatures in the tropical Pacific associated with changes in El Niño. Science 281:240–3.Google Scholar
Moore, MD, Schrag, DP, Kashgarian, M. 1997. Coral radiocarbon constraints on the source of the Indonesian throughflow. Journal of Geophysical Research 102(C6):12,359–65.Google Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Herring, C, Hughen, KA, Kromer, B, McCormac, G, Manning, S, Bronk Ramsey, C, Reimer, RW, Remmele, S, Southon, JR, Stuiver, M, Talamo, S, Taylor, FW, van der Plicht, J, Weyhenmeyer, CE. 2004. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon, this issue.Google Scholar
Stuiver, M, Reimer, PJ, Bard, E, Beck, JW, 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
Taylor, FW, Frohlich, C, Lecolle, J, Strecker, M. 1987. Analysis of partially emerged corals and reef terraces in the central Vanuatu arc: comparison of contemporary coseismic and nonseismic with Quaternary vertical movements. Journal of Geophysical Research 92: 4905–33.Google Scholar
Tudhope, AW, Chilcott, CP, McCulloch, MT, Cook, ER, Chappell, J, Ellam, RM, Lea, DW, Lough, JM, Shimmield, GB. 2001. Variability in the El Niño-Southern Oscillation through a glacial-interglacial cycle. Science 291:1511–7.Google Scholar