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Planktonic Foram Dates from the Indonesian Arc: Marine 14C Reservoir Ages and a Mythical AD 535 Eruption of Krakatau

Published online by Cambridge University Press:  09 February 2016

John Southon ,
Mahyar Mohtadi  and
Ricardo De Pol-Holz
John Southon*
Affiliation:
Earth System Science Department, University of California, Irvine, California 92697, USA
Mahyar Mohtadi
Affiliation:
MARUM, University of Bremen, Loebener Str., 28359 Bremen, Germany
Ricardo De Pol-Holz
Affiliation:
Department of Oceanography, Universidad de Concepción, Casilla 160-C, Concepción, Chile
*
Corresponding author. Email: [email protected].
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Abstract

The Indonesian Arc represents the subduction of the Indian-Australian plate beneath Asia. It has been the scene of catastrophic tectonic activity, including the recent 2004 M=9.1 Aceh earthquake and resulting Indian Ocean tsunami. We have dated planktonic forams associated with historic tephras (Tambora, 1815 and Krakatau, 1883) in marine sediment cores to determine radiocarbon reservoir ages for 2 locations along the arc. Our best estimates for 19th century regional reservoir corrections (ΔR) are +90 ± 40 yr for surface-dwelling species and +220 ± 40 yr for mixed planktic assemblages containing some upper thermocline species, but scatter in the data suggests that past surface reservoir ages may have varied by about ±100 yr. We used the results of this study to investigate a proposed very large AD 535 eruption at or near Krakatau. We find no evidence for ash from such an eruption, and although this is negative evidence, we consider it sufficiently strong to rule out any possibility that one took place.

Type
Radiocarbon Reservoir Effects
Information
Radiocarbon , Volume 55 , Issue 3: Proceedings of the 21st International Radiocarbon Conference (Part 2 of 2) , 2013 , pp. 1164 - 1172
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

Abram, NJ, Gagan, MK, Liu, Z, Hantoro, WS, McCulloch, MT, Surwargadi, BW. 2007. Seasonal characteristic of the Indian Ocean Dipole during the Holocene epoch. Nature 445(7125):299–302.Google Scholar
Beauregard, JL. 2001. Explosive rhyodacitic volcanism: the evolution and frequency of pre-1883 eruptions at Krakatau volcano, Indonesia [PhD dissertation]. University of Rhode Island. 379 p.Google Scholar
Berger, R, Taylor, RE, Libby, WF. 1966. Radiocarbon content of marine shells form the California and Mexican west coast. Science 153(3738):864–6.Google Scholar
Broecker, WS. 1991. The great ocean conveyor. Oceanography 4:79–89.Google Scholar
Bronto, S. 1989. Volcanic geology of Galunggung, West Java, Indonesia [PhD dissertation]. University of Canterbury. 490 p.Google Scholar
Gupta, A. 1996. Erosion and sediment yield in Southeast Asia: a regional perspective. In: Walling, DE, Webb, BW, editors. Erosion and Sediment Yield: Global and Regional Perspectives. Proceedings of the Exeter Symposium, July 1996. International Association for Hydrological Sciences Publication no. 236. p 215–22.Google Scholar
Ingram, BL, Southon, JR. 1996. Reservoir ages in eastern Pacific coastal and estuarine waters. Radiocarbon 38(3):573–82.Google Scholar
Jones, KB, Hodgins, GL, Dettman, DL, Andrus, CT, Nelson, A, Etayo-Cadavid, MR 2007. Seasonal variations in Peruvian marine reservoir age from pre-bomb Argopecten purpuratus shell carbonate. Radiocarbon 49(2):877–88.Google Scholar
Keys, D. 1999. Catastrophe: An Investigation into the Origins of the Modern World. New York: Ballantine. 368 p.Google Scholar
Larsen, LB, Vinther, BM, Briffa, KR, Melvin, TM, Clausen, HB, Jones, PD, Siggard-Andersen, M-L, Hammer, CU, Eronen, M, Grudd, H, Gunnarson, BE, Hantemirov, RM, Naurzbaev, MM, Nicolussi, K. 2008. New ice core evidence for a volcanic cause for the AD 536 dust veil. Geophysical Research Letters 35:L04708, doi: 10.1029/2007GL032450.Google Scholar
Lay, T, Kanamori, H, Ammon, CJ, Nettles, M, Ward, SN, Aster, RC, Beck, SL, Bilek, SL, Brudzinski, MR, Butler, R, DeShon, HR, Ekstrom, G, Satake, K, Sipkin, S. 2005. The great Sumatra-Andaman earthquake of 26 December 2004. Science 308(5725):1127–33.Google Scholar
Mohtadi, M, Steinke, S, Groenveld, J, Fink, HG, Rixen, T, Hebblen, D, Donner, B, Herunadi, B. 2009. Low latitude control and seasonal and interannual changes in planktonic foraminiferal flux and shell geochemistry off south Java. Paleoceanography 24:PA1201, doi: 10.1029/2008PA001636.Google Scholar
Mohtadi, M, Oppo, DW, Luckge, A, De Pol-Holz, R, Steinke, S, Groeneveld, J, Hemme, N, Hebblen, D. 2011. Reconstructing the thermal structure of the upper ocean: insights from planktic foraminifera shell chemistry and alkenones in modern sediments of the tropical eastern Indian Ocean. Paleoceanography 26:PA3219, doi: 10.1029/2011PA002132.CrossRefGoogle Scholar
Newcomb, KR, McGann, WR. 1987. Seismic history and seismotectonics of the Sunda Arc. Journal of Geophysical Research 92(B1):421–39.Google Scholar
Newton, A, Thunell, R, Stott, A. 2006. Climate and hydro-graphic variability in the Indo-Pacific Warm Pool during the last millennium. Geophysical Research Letters 33:L19710, doi:10.1029/2006GL027234.CrossRefGoogle Scholar
Oppo, D, Rosenthal, Y, Linsley, BK. 2009. 2,000-year-long temperature and hydrology reconstructions from the Indo-Pacific warm pool. Nature 460(7259):1113–6.CrossRefGoogle ScholarPubMed
Ortlieb, L, Vargas, G, Saliège, J-F. 2011. Marine radiocarbon reservoir effect along the northern Chile-southern Peru coast (14–24°S) throughout the Holocene. Quaternary Research 75(1):91–103.CrossRefGoogle Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Burr, GS, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Hajdas, I, Heaton, T, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, McCormac, FG, Manning, SW, Reimer, RW, Richards, DA, Southon, JR, Talamo, S, Turney, CSM, van der Plicht, J, Weyhenmeyer, CE. 2009. IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51(4):1111–50.Google Scholar
Schmidt, DN, Elliott, T, Kasemann, SA. 2008. The influences of growth rates on planktic foraminfers as proxies for paleostudies – a review. In: Austin, WEN, James, RH, editors. Biogeochemical Controls on Paleoceanographic Environmental Proxies. Geological Society Special Publication 303. Wiltshire: Cromwell Press. p 73–86.Google Scholar
Self, S, Rampino, MR, Newton, MS, Wolff, JA. 1984. Volcanological study of the great Tambora eruption of 1815. Geology 12(11):659–63.2.0.CO;2>CrossRefGoogle Scholar
Simkin, T, Siebert, L. 1994. Volcanoes of the World. 2nd edition. Tucson: Geoscience Press. 369 p.Google Scholar
Sprintall, J, Potemra, JT, Hautala, SL, Bray, NA, Pandoe, WW. 2003. Temperature and salinity variability in the exit passages of the Indonesian Throughflow. Deep-Sea Research II 50(12):2183–204.Google Scholar
Stothers, RB. 1984. Mystery cloud of AD 536. Nature 307(5949):344–5.Google Scholar
Susanto, RD, Gordon, RL, Zheng, Q. 2001. Upwelling along the coasts of Java and Sumatra and its relation to ENSO. Geophysical Research Letters 28(8):1599–602.Google Scholar
Verbeek, R. 1885. Krakatau. Batavia: State Press. 495 p.Google Scholar
Whitten, T, Soeriaatmadji, RE, Afiff, SA. 1996. The Ecology of Indonesia Series II: The Ecology of Java and Bali. Hong Kong: Periplus Editions. 1009 p.Google Scholar
Wjiffels, S, Bray, N, Hautala, S, Meyers, G, Morawitz, G. 1996. The WOCE Indonesian Throughflow repeat hydrography sections: 110 and 1R6. WOCE Newsletter 24:25–8.Google Scholar
Wohletz, K. 2000. Were the Dark Ages triggered by volcano-related climate changes in the 6th century? [abstract]. EOS 81(48):F1305.Google Scholar