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The Minoan Santorini Eruption and Tsunami Deposits in Palaikastro (Crete): Dating by Geology, Archaeology, 14C, and Egyptian Chronology

Published online by Cambridge University Press:  18 July 2016

Hendrik J Bruins ,
Johannes van der Plicht  and
J Alexander MacGillivray
Hendrik J Bruins*
Affiliation:
Ben-Gurion University of the Negev, Jacob Blaustein Institutes for Desert Research, Sede Boker Campus & Dept. of Bible, Archaeology and Ancient Near Eastern Studies, Beer Sheva, Israel
Johannes van der Plicht
Affiliation:
University of Groningen, Centre for Isotope Research, Nijenborgh, Groningen, The Netherlands & Leiden University, Faculty of Archaeology, Leiden, The Netherlands
J Alexander MacGillivray
Affiliation:
British School of Archaeology in Athens, Odos Souedias 52, 106 76 Athens, Greece
*
Corresponding author. Email: [email protected]
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Abstract

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Deposits from the Minoan Santorini (Thera) eruption in the eastern Mediterranean region constitute the most important regional stratigraphic marker in the chronological perplexity of the 2nd millennium BCE. Extensive tsunami deposits were discovered in Crete at the Minoan archaeological site of Palaikastro, containing reworked volcanic Santorini ash. Hence, airborne deposition of volcanic ash, probably during the 1st (Plinian) eruption phase, preceded the tsunami, which was apparently generated during the 3rd or 4th phase of the eruption, based on evidence from Thera. Average radiocarbon dates (uncalibrated) of animal bones in the Palaikastro tsunami deposits along the coast (3350 ± 25 BP) and at the inland archaeological site (3352 ± 23 BP) are astoundingly similar to the average 14C date for the Minoan Santorini eruption at Akrotiri on Thera (3350 ± 10 BP). The wiggle-matched 14C date of the eruption in calendar years is 1627–1600 cal BCE. Late Minoan IA pottery is the youngest element in the Palaikastro tsunami deposits, fitting with the LM IA archaeological date for the Santorini eruption, conventionally linked at ~1500 BCE with Dynasty XVIII of the historical Egyptian chronology. The reasons for the discrepancy of 100–150 yr between 14C dating and Egyptian chronology for part of the 2nd millennium BCE are unknown. 14C dates from Tell el-Dabca in the eastern Nile Delta show that the 14C age of the Santorini eruption matches with 14C results from 18th Dynasty strata C3 and C2, thereby confirming grosso modo the conventional archaeo-historical correlations between the Aegean and Egypt. We propose that a dual dating system is used in parallel: (1) archaeological material-cultural correlations linked to Egyptian chronology; (2) 14C dating. Mixing of dates from the 2 systems may lead to erroneous archaeological and historical correlations. A “calibration curve” should be established between Egyptian chronology and 14C dating for the 2nd millennium BCE, which may also assist to resolve the cause of the discrepancy.

Type
14C Chronologies, Dendrochronology, Wiggle-Matching, and Calibration Tools
Information
Radiocarbon , Volume 51 , Issue 2 , 2009 , pp. 397 - 411
Copyright
Copyright © 2009 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Aerts-Bijma, AT, van der Plicht, J, Meijer, HAJ. 2001. Automatic AMS sample combustion and CO2 collection. Radiocarbon 43(2A):293–8.CrossRefGoogle Scholar
Betancourt, PP, Goldberg, P, Hope Simpson, R, Vitaliano, CJ. 1990. Excavations at Pseira: the evidence for the Theran eruption. In: Hardy, DA, Renfrew, AC, editors. Thera and the Aegean World III. Volume 3. London: The Thera Foundation. p 96–9.Google Scholar
Bietak, M. 1997. Avaris, capital of the Hyksos kingdom: new results of excavations. In: Oren, ED, editor. The Hyksos: New Historical and Archaeological Perspectives. Philadelphia: The University Museum, University of Pennsylvania. p 87–139.Google Scholar
Bietak, M. 2003. Science versus archaeology: problems and consequences of high Aegean chronology. In: Bietak, M, editor. The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium B.C.—II. Vienna: Austrian Academy of Sciences. p 23–33.Google Scholar
Bietak, M, Höflmayer, F. 2007. Introduction: high and low chronology. In: Bietak, M, Czerny, E, editors. The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium B.C.—III. Vienna: Austrian Academy of Sciences. p 13–23.Google Scholar
Bietak, M, Dorner, J, Jánosi, P. 2001. Ausgrabungen in dem Palastbezirk von Avaris. Vorberichte Tell el-Dabca/cEzbet Helmi 1993–2000. Ägypte und Levante 11:27–119.Google Scholar
Bronk Ramsey, C. 1995. Radiocarbon calibration and analysis of stratigraphy: the OxCal program. Radiocarbon 37(2):425–30.Google Scholar
Bronk Ramsey, C. 2001. Development of the radiocarbon calibration program. Radiocarbon 43(2A):355–63.Google Scholar
Bronk Ramsey, C, Manning, SW, Galimberti, M. 2004. Dating the volcanic eruption at Thera. Radiocarbon 46(1):325–44.Google Scholar
Bruins, HJ. 2007. Charcoal radiocarbon dates of Tell el-Daba. In: Bietak, M, Czerny, E, editors. The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium B.C.—III. Vienna: Austrian Academy of Sciences. p 65–77.Google Scholar
Bruins, HJ, Mook, WG. 1989. The need for a calibrated radiocarbon chronology of Near Eastern archaeology. Radiocarbon 31(3):1019–29.Google Scholar
Bruins, HJ, van der Plicht, J. 2003. Assorting and synchronising archaeological and geological strata with radiocarbon: the Southern Levant in relation to Egypt and Thera. In: Bietak, M, editor. The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium B.C.—II. Vienna: Austrian Academy of Sciences. p 35–42.Google Scholar
Bruins, HJ, MacGillivray, JA, Synolakis, CE, Benjamini, C, Keller, J, Kisch, HJ, Klügel, A, van der Plicht, J. 2008. Geoarchaeological tsunami deposits at Palaikastro (Crete) and the Late Minoan IA eruption of Santorini. Journal of Archaeological Science 35(1):191–212.Google Scholar
Dominey-Howes, DTM. 2004. A re-analysis of the Late Bronze Age eruption and tsunami of Santorini, Greece, and the implications for the volcano-tsunami hazard. Journal of Volcanology and Geothermal Research 130(1–2):107–32.CrossRefGoogle Scholar
Doumas, CG. 1983. Thera: Pompeii of the Ancient Aegean. London: Thames and Hudson.Google Scholar
Doumas, C, Papazoglou, L. 1980. Santorini tephra from Rhodes. Nature 287(5780):322–4.CrossRefGoogle Scholar
Driessen, J, Macdonald, CF. 1997. The Troubled Island, Minoan Crete Before and After the Santorini Eruption. Aegaeum 17. Université de Liège, Liège and University of Texas, Austin.Google Scholar
Druitt, TH, Edwards, L, Mellors, RM, Pyle, DM, Sparks, RSJ, Lanphere, M, Davies, M, Barreiro, B. 1999. Santorini Volcano. London: Geological Society, Special Memoir 19.Google Scholar
Friedrich, WL. 2000. Fire in the Sea: The Santorini Volcano. Cambridge: Cambridge University Press.Google Scholar
Friedrich, WL, Kromer, B, Friedrich, M, Heinemeier, J, Pfeiffer, T, Talamo, S. 2006. Santorini eruption radiocarbon dated to 1627–1600 B.C. Science 312(5773): 548.Google Scholar
Keller, J. 1980. Prehistoric pumice tephra on Aegean islands. In: Doumas, C, editor. Thera and the Aegean World, Volume II. London: The Thera Foundation. p 49–56.Google Scholar
Kitchen, KA. 1987. The basics of Egyptian Chronology in relation to the Bronze Age. In: Åstrom, P, editor. High, Middle or Low. Acts of an International Colloquium in Absolute Chronology. Göteborg: Åstroms. p 37–55.Google Scholar
Kitchen, KA. 1996. The historical chronology of ancient Egypt: a current assessment. Acta Archaeologica 67:1–18.Google Scholar
Krauss, R, Hornung, E. 2006. Ancient Egyptian Chronology. Leiden: Brill.Google Scholar
MacGillivray, JA, Sackett, LH, Driessen, J, Smyth, D. 1987. Excavations at Palaikastro 1986. The Annual of the British School of Archaeology at Athens 82:135–54, Plates 19–24.Google Scholar
MacGillivray, JA, Sackett, LH, Driessen, J, Smyth, D. 1991. Excavations at Palaikastro 1990. The Annual of the British School of Archaeology at Athens 86:121–47, Plates 6–16.Google Scholar
MacGillivray, JA, Sackett, LH, Driessen, J, Farnoux, A, Smyth, D. 1992. Excavations at Palaikastro 1991. The Annual of the British School of Archaeology at Athens 87:121–52, Plates 3–7.Google Scholar
MacGillivray, JA, Sackett, LH, Driessen, J, Hemingway, S. 1998. Excavations at Palaikastro 1994 and 1996. The Annual of the British School of Archaeology at Athens 93:221–68, Plates 38–50.Google Scholar
Manning, SW. 1999. A Test of Time—The Volcano of Thera and the Chronology and History of the Aegean and East Mediterranean in the Mid Second Millennium BC. Oxford: Oxbow Books.Google Scholar
Manning, SW, Bronk Ramsey, C, Kutschera, W, Higham, T, Kromer, B, Steier, P, Wild, EM. 2006. Chronology for the Aegean Late Bronze Age 1700–1400 B.C. Science 312(5773):565–9.CrossRefGoogle ScholarPubMed
Marinatos, S. 1939. The volcanic destruction of Minoan Crete. Antiquity 13:425–39.Google Scholar
McCoy, FW. 1980. The upper Thera (Minoan) ash in deep-sea sediments: distribution and comparison with other ash layers. In: Doumas, C, editor. Thera and the Aegean World. Volume II. London: The Thera Foundation. p 49–56.Google Scholar
McCoy, FW, Dunn, S. 2002. Modelling the climatic effects of the LBA eruption of Thera: new calculations of tephra volumes may suggest a significantly larger eruption than previously reported (abstract). In: Proceedings of the Chapman Conference on Volcanism and the Earth's Atmosphere. American Geophysical Union, Santorini, Greece. p 21–2.Google Scholar
McCoy, FW, Heiken, G. 2000a. The Late Bronze Age explosive eruption of Thera (Santorini), Greece: regional and local effects. In: McCoy, FW, Heiken, G, editors. Volcanic Hazards and Disasters in Human Antiquity. Geological Society of America Special Paper 345. p 43–70.Google Scholar
McCoy, FW, Heiken, G. 2000b. Tsunami generated by the Late Bronze Age eruption of Thera (Santorini), Greece. Pure and Applied Geophysics 157(6–8):1227–56.Google Scholar
Minoura, K, Imamura, F, Kuran, U, Nakamura, T, Papadopoulos, GA, Takahashi, T, Yalciner, AC. 2000. Discovery of Minoan tsunami deposits. Geology 28(1):59–62.Google Scholar
Mook, WG, Waterbolk, HT. 1985. Handbook for Archaeologists. No. 3. Radiocarbon Dating. Strasbourg: European Science Foundation.Google Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Bertrand, CJH, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Hogg, AG, 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 46(3):1029–58.Google Scholar
Sigurdsson, H, Carey, S. 1989. Plinian and co-ignimbrite tephra fall from the 1815 eruption of Tambora volcano. Bulletin of Volcanology 51(4):243–70.Google Scholar
Sigurdsson, H, Carey, S, Alexandri, M, Vougioukalakis, G, Croff, K, Roman, C, Sakellariou, D, Anagnostou, C, Rousakis, G, Ioakim, C, Gogou, A, Ballas, D, Misaridis, T, Nomikou, P. 2006. Marine investigations of Greece's Santorini volcanic field. Eos, Transactions American Geophysical Union 87(34):337–48.Google Scholar
Soles, JS, Davaras, C. 1990. Theran ash in Minoan Crete: new excavations on Mochlos. In: Hardy, DA, Renfrew, AC, editors. Thera and the Aegean World III. Volume 3. London: The Thera Foundation. p 89–95.Google Scholar
Soles, JS, Taylor, SR, Vitaliano, CJ. 1995. Tephra samples from Mochlos and their chronological implication for Neopalatial Crete. Archaeometry 37(2):385–93.Google Scholar
Thorarinsson, S. 1978. Some comments on the Minoan eruption of Santorini. In: Doumas, C, editor. Thera and the Aegean World I, Part One: Geosciences. London: Thera and the Aegean World. p 263–75.Google Scholar
van der Plicht, J, Bruins, HJ. 2001. Radiocarbon dating in Near-Eastern contexts: confusion and quality control. Radiocarbon 43(3):1155–66.Google Scholar
van der Plicht, J, Wijma, S, Aerts, AT, Pertuisot, MH, Meijer, HAJ. 2000. The Groningen AMS facility: status report. Nuclear Instruments and Methods in Physics Research B 172(1–4):58–65.Google Scholar
Vitaliano, CJ, Vitaliano, DB. 1974. Volcanic tephra on Crete. American Journal of Archaeology 78:19–24.Google Scholar
Ward, WA. 1992. The present status of Egyptian Chronology. Bulletin of the American Schools of Oriental Research 288:53–66.Google Scholar
Warren, PM. 2007. A new pumice analysis from Knossos and the end of Late Minoan I A. In: Bietak, M, Czerny, E, editors. The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium B.C.—III. Vienna: Austrian Academy of Sciences. p 495–9.Google Scholar
Warren, PM, Hankey, V. 1989. Aegean Bronze Age Chronology. Bristol: Bristol Classical Press.Google Scholar
Watkins, ND, Sparks, RSJ, Sigurdsson, H, Huang, TC, Federman, A, Carey, S, Ninkovich, D. 1978. Volume and extent of the Minoan tephra from Santorini Volcano: new evidence from deep-sea sediment cores. Nature 271(5641):122–6.CrossRefGoogle Scholar
Wiener, MH. 2003. Time out: the current impasse in Bronze Age archaeological dating. In: Foster, KP, Laffineur, R, editors. METRON: Measuring the Aegean Bronze Age. Aegaeum 24. Université de Liège, Liège and University of Texas, Austin. p 363–99.Google Scholar
Wiener, MH. 2007. Times change: the current state of the debate in Old World chronology. In: Bietak, M, Czerny, E, editors. The Synchronisation of Civilisations in the Eastern Mediterranean in the Second Millennium B.C.—III. Vienna: Austrian Academy of Sciences. p 25–47.Google Scholar