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Intervalidation of Dendrochronology and 14C Dating on a 700-yr Tree-Ring Sequence Originating from the Eastern Carpathians

Published online by Cambridge University Press:  27 May 2019

Gabriela O Sava ,
Ionel Popa ,
Tiberiu B Sava ,
Aurelia Meghea ,
Cristian Mănăilescu ,
Maria Ilie ,
Andrei Robu  and
Boglárka Tóth
Gabriela O Sava
Affiliation:
RoAMS Laboratory, Horia Hulubei National Institute for Physics and Nuclear Engineering, Reactorului 30, 077125, Măgurele-Bucharest, Romania Politehnica University of Bucharest, Splaiul Independenţei 313, 060042, Bucharest, Romania
Ionel Popa
Affiliation:
Marin Drăcea National Institute for Research and Development in Forestry, Calea Bucovinei 73 bis, 725100, Câmpulung Moldovenesc, Suceava, Romania
Tiberiu B Sava*
Affiliation:
RoAMS Laboratory, Horia Hulubei National Institute for Physics and Nuclear Engineering, Reactorului 30, 077125, Măgurele-Bucharest, Romania
Aurelia Meghea
Affiliation:
Politehnica University of Bucharest, Splaiul Independenţei 313, 060042, Bucharest, Romania
Cristian Mănăilescu
Affiliation:
RoAMS Laboratory, Horia Hulubei National Institute for Physics and Nuclear Engineering, Reactorului 30, 077125, Măgurele-Bucharest, Romania
Maria Ilie
Affiliation:
RoAMS Laboratory, Horia Hulubei National Institute for Physics and Nuclear Engineering, Reactorului 30, 077125, Măgurele-Bucharest, Romania
Andrei Robu
Affiliation:
RoAMS Laboratory, Horia Hulubei National Institute for Physics and Nuclear Engineering, Reactorului 30, 077125, Măgurele-Bucharest, Romania
Boglárka Tóth
Affiliation:
Anno Domini Dendrolab, Miercurea Ciuc, Romania
*
*Corresponding author. Email: [email protected].
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Abstract

We present a comparative study on a 700-yr sequence of dendrochronologically ordered tree-rings of Pinus cembra originating from Eastern Carpathians for the period AD 1009–1709. This period covers the solar minima of the Little Ice Age. The aim of this study was to assess the accuracy of our radiocarbon (14C) determinations interpreted on the IntCal13 calibration data and to observe any apparent offsets. The 14C measurements on single and double tree-rings were “wiggle-matched” to secure the dendrochronology cross-matching of all the Pinus cembra wood pieces. The results showed a very good agreement between the age datasets for four out of five wood trunks. However, for one of them a new cross-matching was performed after a quality assurance test, establishing an earlier 48-yr position, recommended by wiggle-matching Bayesian statistics and dendrochronological analysis. Following this adjustment, the quantification of the 14C level variability with respect to the IntCal13 calibration curve was obtained by calculating Δ14C for all tree-ring samples. As a final conclusion, an insignificant 14C concentration offset of –0.63 ± 3.76‰ was found for the Romanian samples.

Keywords

dendrochronologyEastern Carpathiansradiocarbon wiggle-matchingRoAMS
Type
Conference Paper
Information
Radiocarbon , Volume 61 , Issue 5: Radiocarbon 2018 Conference Proceedings Trondheim, Norway, June 17–22, 2018 Part 1 of 2 , October 2019 , pp. 1337 - 1343
Copyright
© 2019 by the Arizona Board of Regents on behalf of the University of Arizona 

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Footnotes

Selected Papers from the 23rd International Radiocarbon Conference, Trondheim, Norway, 17–22 June, 2018

References

BIBLIOGRAPHY

Bayliss, A, Marshall, P, Tyers, C, Ramsey, CB, Cook, G, Freeman, S, Griffiths, S. 2017. Informing conservation: towards 14C wiggle-matching of short tree-ring sequences from medieval buildings in England. Radiocarbon 59:985–1007.Google Scholar
Botár, I, Boglárka, T, Grynaeus, A. 2015. Hidden dates. Dendrochronological research on medieval churches in Transylvania. Caiete ARA.Google Scholar
Ramsey, CB. 1995. Radiocarbon calibration and analysis of stratigraphy: the OxCal program. Radiocarbon 37(2):425–430.CrossRefGoogle Scholar
Ramsey, CB, van der Plicht, J, Weninger, B. 2001. “Wiggle matching” radiocarbon dates. Radiocarbon 43(2A):381–389.CrossRefGoogle Scholar
Cook, ER, Kairiukstis, LA. 1990. Methods of dendrochronology: applications in the environmental sciences. The Netherlands: Dordrecht. ISBN 0-7923-0586-8.CrossRefGoogle Scholar
Galimberti, M, Ramsey, CB, Manning, SW. 2004. Wiggle-match dating of tree-ring sequences. Radiocarbon 46:917–924.Google Scholar
Hong, W, Park, JH, Park, G, Sung, KS, Park, WK, Lee, JG. 2013. Regional offset of radiocarbon concentration and its variation in the Korean atmosphere from AD 1650–1850. Radiocarbon 55(2–3):753–762.Google Scholar
Kern, Z, Popa, I. 2016. Dendrochronological and radiocarbon analyses of subfossil oaks from the foothills of the Romanian Carpathians. Geochronometria 43:113–120.CrossRefGoogle Scholar
Manning, SW, Griggs, C, Lorentzen, B, Ramsey, CB, Chivall, D, Jull, AJT, Lange, TE. 2018. Fluctuating radiocarbon offsets observed in the southern Levant and implications for archaeological chronology debates. Proceedings of the National Academy of Sciences of the United States of America 115(24):6141–6146.CrossRefGoogle ScholarPubMed
NIST SRM 4990C. 1983. International Standard Reference Material for Contemporary Carbon-14.Google Scholar
Pearson, CL, Ważny, T, Kuniholm, PI, Botić, K, Durman, A and Seufer, K. 2014. Potential for a new multimillennial tree-ring chronology from subfossil Balkan river oaks. Radiocarbon 56(4):51–59.CrossRefGoogle Scholar
Popa, I, Kern, Z. 2009. Long-term summer temperature reconstruction inferred from tree-ring records from the Eastern Carpathians. Climate Dynamics 32:1107–1117.CrossRefGoogle Scholar
R.A.N. (Repertoriul Arheologic Naţional). 2018. http://ran.cimec.ro/sel.asp?Lang=EN.Google Scholar
Rădoane, M, Nechita, C, Chiriloaei, F, Rădoane, N, Popa, I, Roibu, C, Robu, D. 2015. Late Holocene fluvial activity and correlations with dendrochronology of subfossil trunks: case studies of northeastern Romania. Geomorphology 239:142–159.CrossRefGoogle Scholar
Rădoane, M, Chiriloaei, F, Sava, T, Nechita, C, Rădoane, N, Gâza, O. 2018. Holocene fluvial history of Romanian Carpathian Rivers. Quaternary International. doi.org/10.1016/j.quaint.2018.11.014.CrossRefGoogle Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Ramsey, CB, Buck, CE, Cheng, H, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Haflidason, H, Hajdas, I, Hatté, C, Heaton, TJ, Hoffmann, DL, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, Manning, SW, Niu, M, Reimer, RW, Richards, DA, Scott, EM, Southon, JR, Staff, RA, Turney, CSM, van der Plicht, J. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55(4):1869–1887.CrossRefGoogle Scholar
Rinn, F. 2010. TSAP-Win reference manual.Google Scholar
Sava, T, Simion, C, Gâza, O, Stanciu, I, Păceşilă, D, Sava, G, Wacker, L, Ştefan, B, Moşu, V, Ghiţă, D, Vasiliu, A. 2018. Status report on the sample preparation laboratory for radiocarbon dating at the new Bucharest RoAMS center. Radiocarbon 61(2):649–658. doi.org/10.1017/RDC.2018.123.CrossRefGoogle Scholar
Stuiver, M. 1980. Solar variability and climatic change during the current millennium. Nature 286:868–871.CrossRefGoogle Scholar
Stuiver, M, Polach, H. 1977. Discussion: reporting of 14C data. Radiocarbon 19(3):355–363.CrossRefGoogle Scholar
Scott, EM, Naysmith, P, Cook, GT. 2017, Should archaeologists care about 14C inter-comparison? Why? A summary report on SIRI. Radiocarbon 59(5):1589–1596.CrossRefGoogle Scholar
Wacker, L, Němec, M, Bourquin, J. 2010a. A revolutionary graphitization system: fully automated, compact and simple. Nuclear Instruments and Methods in Physics Research B 268(7–8):931–934.CrossRefGoogle Scholar
Wacker, L, Christl, M, Synal, H-A. 2010b. BATS: A new tool for AMS data reduction. Nuclear Instruments and Methods in Physics Research B 268(7–8):976–979.CrossRefGoogle Scholar
Ważny, T. 2009. Is there a separate tree-ring pattern for the Mediterranean oaks? Tree-rings, kings, and Old World archaeology and environment: papers presented in honor of Peter Ian Kuniholm. p. 41–50.Google Scholar
Ważny, T, Lorentzen, B, Köse, N, Akkemik, Ü, Boltryk, Y, Güner, T, Kyncl, J, Kyncl, T, Nechita, C, Sagaydak, S, Vasileva, JK. 2014. Bridging the gaps in tree-ring records: creating a high-resolution dendrochronological network for Southeastern Europe. Radiocarbon 56(4):39–50.CrossRefGoogle Scholar
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