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Seasonal variations in the 14C Content of Tree Rings: Influences on Radiocarbon Calibration and Single-Year Curve Construction

Published online by Cambridge University Press:  26 July 2018

Liam McDonald Open the ORCID record for Liam McDonald [Opens in a new window] ,
David Chivall ,
Daniel Miles  and
Christopher Bronk Ramsey
Liam McDonald
Affiliation:
Research Laboratory for Archaeology and the History of Art, University of Oxford, Oxford OX1 3TG, United Kingdom
David Chivall
Affiliation:
Research Laboratory for Archaeology and the History of Art, University of Oxford, Oxford OX1 3TG, United Kingdom
Daniel Miles
Affiliation:
Research Laboratory for Archaeology and the History of Art, University of Oxford, Oxford OX1 3TG, United Kingdom
Christopher Bronk Ramsey*
Affiliation:
Research Laboratory for Archaeology and the History of Art, University of Oxford, Oxford OX1 3TG, United Kingdom
*
*Corresponding author. Email: [email protected].
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Abstract

To examine the implications of seasonality for the construction of a single-year calibration curve we obtained separate dates on earlywood and latewood fractions of tree rings originating from England and dendrochronologically dated between AD 1352 and AD 1442. These demonstrated that an average difference of 26±15 yr exists between earlywood and latewood and that this difference can be as high as 33±19 yr during periods of high radiocarbon (14C) production. It is argued that this difference is due to both changes in atmospheric 14C and the incorporation of stored carbohydrates into earlywood. Based on this, it was possible to separate an atmospheric and physiological contribution to this difference. Our modeling indicates that storage can produce a difference of up to 10 years between earlywood and latewood. This suggests that full-year tree rings from deciduous trees may be less appropriate for the construction of a single-year calibration curve and that specific atmospheric events can be more easily detected by measuring only latewood.

Keywords

atmospheric 14Ccarbon storagedendrochronologyseasonalitysingle-year calibration using dendrochronology
Type
Research Article
Information
Radiocarbon , Volume 61 , Issue 1 , February 2019 , pp. 185 - 194
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

REFERENCES

Barbaroux, C, Bréda, N. 2002. Contrasting distribution and seasonal dynamics of carbohydrate reserves in stem wood of adult ring-porous sessile oak and diffuse-porous beech trees. Tree Physiology 22(17):1201–1210.Google Scholar
Baxter, MS, Walton, A. 1971. Fluctuations of atmospheric carbon-14 during the past century. Proceedings of the Royal Society of London 321:105–127.Google Scholar
Bayliss, A, Marshall, P, Tyers, C, Bronk Ramsey, C, Cook, G, Freeman, SPHT, Griffiths, S. 2017. Informing conservation: towards 14C wiggle-matching of short tree-ring sequences from medieval buildings in England. Radiocarbon 59(3):985–1007.Google Scholar
Bronk Ramsey, C, Buck, CE, Manning, SW, Reimer, P, van der Plicht, H. 2006. Developments in radiocarbon calibration for archaeology. Antiquity 80(310):783–798.Google Scholar
Bronk Ramsey, C, Ditchfield, P, Humm, M. 2004. Using a gas ion source for radiocarbon AMS and GC-AMS. Radiocarbon 46(1):25–32.Google Scholar
Carbone, MS, Czimczik, CE, Keenan, TF, Murakami, PF, Pederson, N, Schaberg, PG, Xu, X, Richardson, AD. 2013. Age, allocation and availability of nonstructural carbon in mature red maple trees. New Phytologist 200:1145–1155.Google Scholar
Chapin, FS, Schulze, ED, Mooney, HA. 1990. The ecology and economics of storage in plants. Annual Reviews of Ecology and Systematics 21:423–447.Google Scholar
Damon, PE, Lerman, JC, Long, A. 1978. Temporal fluctuations of atmospheric 14C: causal factors and implications. Annual Review of Earth Planetary Science 6:457–494.Google Scholar
Dee, M, Bronk Ramsey, C. 2000. Refinement of graphite target production at ORAU. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 172:449–453.Google Scholar
Dee, MW, Pope, BJS. 2016. Anchoring historical sequences using a new source of astro-chronological tie-points. Proceedings of the Royal Society A 472:20160263.Google Scholar
Dietze, MC, Sala, A, Carbone, MS, Czimczik, CI, Mantooth, JA, Richardson, AD, Vargas, R. 2014. Nonstructural carbon in woody plants. Annual Review of Plant Biology 65(1):667–687.Google Scholar
Gaudinski, JB, Torn, MS, Riley, WJ, Swanston, C, Trumbore, SE, Joslin, JD, Majdi, H, Dawson, TE, Hanson, PJ. 2009. Use of stored carbon reserves in growth of temperate tree roots and leaf buds: analyses using radiocarbon measurements and modeling. Global Change Biology 15(4):992–1014.Google Scholar
Gessler, A, Treydte, K. 2016. The fate and age of carbon - insights into the storage and remobilization dynamics in trees. New Phytologist 209:1338–1340.Google Scholar
Green, JW. 1963. Wood cellulose. In: Whistler RL, Wolfrom ML, Bemiller JN, editors. Methods in Carbohydrate Chemistry; Cellulose. New York: Academic Press. p. 9–21.Google Scholar
Güttler, DF, Adolphi, F, Beer, J, Bleicher, N, Boswijk, G, Christl, M, Hogg, A, Palmer, J, Vockenhuber, C, Wacker, L, et al. 2015. Rapid increase in cosmogenic 14C in AD 775 measured in New Zealand kauri trees indicates short-lived increase in 14C production spanning both hemispheres. Earth and Planetary Science Letters 411:290–297.Google Scholar
Güttler, DF, Wacker, L, Kromer, B, Friedrich, M, Synal, H-A. 2013. Evidence of 11-year solar cycles in tree rings from 1010 to 1110 AD – progress on high precision AMS measurements. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 294(January):459–463.Google Scholar
Hogg, A, Hua, Q, Blackwell, PG, Niu, M, Buck, CE, Guilderson, TP, Heaton, TJ, Palmer, JG, Reimer, PJ, Reimer, RW, et al. 2013. SHCal13 southern hemisphere calibration, 0-50,000 years cal BP. Radiocarbon 55(4):1889–1903.Google Scholar
Höll, W. 1985. Seasonal fluctuation of reserve materials in the trunkwood of spruce [Picea Abies (L.) Karst]. Journal of Plant Physiology 117(4):355–362.Google Scholar
Keel, SG, Siegwolf, RT, Kötner, C. 2006. Canopy CO2 enrichments permits tracing the fate of recently assimilated carbon in a mature deciduous forest. New Phytologist 172(2):319–329.Google Scholar
Kitagawa, H, Mukai, H, Nojiri, Y, Shibata, Y, Kobayashi, T, Nojiri, T. 2004. Seasonal and secular variations of atmospheric 14CO2 over the Western Pacific since 1994. Radiocarbon 46(2):901–910.Google Scholar
Kromer, B, Manning, SW, Kuniholm, PI, Newton, MW, Spurk, M, Levin, I. 2001. Regional 14CO2 offsets in the troposphere: magnitude, mechanisms, and consequences. Science 294(5551):2529–2532.Google Scholar
Levin, I, Kromer, B. 2004. The tropospheric 14CO2 level in mid-latitudes of the northern hemisphere (1959–2003). Radiocarbon 46(3):1261–1272.Google Scholar
Mekhaldi, F, Muscheler, R, Adolphi, F, Aldahan, A, Beer, J, McConnell, JR, Possnert, G, Sigl, M, Svensson, A, Synal, H-A, et al. 2015. Multiradionuclide evidence for the solar origin of the cosmic-ray events of AD 774/5 and 993/4. Nature Communications 6:8611.Google Scholar
Miles, DH, Worthington, MJ. 1999. Tree-ring dates. Vernacular Architect 30(1):98–113.Google Scholar
Miyake, F, Masuda, K, Nakamura, T. 2013. Another rapid event in the carbon-14 content of tree rings. Nature Communications 4:1748.Google Scholar
Miyake, F, Nagaya, K, Masuda, K, Nakamura, T. 2012. A signature of cosmic-ray increase in AD 774-775 from tree rings in Japan. Nature 486:240–242.Google Scholar
Muhr, J, Messier, C, Delagrange, S, Trumbore, S, Xu, X, Hartmann, H. 2016. How fresh is maple syrup? Sugar maple trees mobilize carbon stored several years previously during early springtime sap-ascent. The New Phytologist 209(4):1410–1416.Google Scholar
Olsson, IU, Possnert, G. 1992. 14C activity in different sections and chemical fractions of oak tree rings, AD 1938–1981. Radiocarbon 34(3):757–767.Google Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Cheng, H, Edwards, RL, Friedrich, M, et al. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55(4):1869–1887.Google Scholar
Richardson, AD, Carbone, MS, Huggett, BA, Furze, ME, Czimczik, CI, Walker, JC, Xu, X, Schaberg, PG, Murakami, P. 2015. Distribution and mixing of old and new nonstructural carbon in two temperate trees. New Phytologist 206(2):590–597.Google Scholar
Richardson, AD, Carbone, MS, Keenan, TF, Czimczik, CI, Hollinger, DY, Murakami, P, Schaberg, PG, Xu, X. 2013. seasonal dynamics and age of stemwood nonstructural carbohydrates in temperate forest trees. New Phytologist 197(3):850–861.Google Scholar
Rinne, KT, Boettger, T, Loader, NJ, Robertson, I, Switsur, VR, Waterhouse, VR. 2005. On the purification of α-cellulose from resinous wood for stable isotope (H, C and O) analysis. Chemical Geology 222(1–2):75–82.Google Scholar
Roth, R, Joos, F. 2013. A reconstruction of radiocarbon production and total solar irradiance from the Holocene 14C and CO2 records: implications of data and model uncertainties. Climate of the Past 9(4):1879–1909.Google Scholar
Sauter, JJ. 1980. Seasonal variation of amino acids and amides in the xylem sap of Salix . Z. Pflanzenphysiol 98:377–391.Google Scholar
Schuur, EAG, Trumbore, SE, Druffel, ERM. editors. 2016. Radiocarbon and Climate Change: Mechanisms, Applications, and Laboratory Techniques. Switzerland: Springer.Google Scholar
Southon, JR, Magana, AL. 2010. A comparison of cellulose extraction and ABA pretreatment methods for AMS 14C dating of ancient wood. Radiocarbon 52(2–3):1371–1379.Google Scholar
Speer, JH. 2010. Fundamentals of Tree-Ring Research. Tucson: University of Arizona Press.Google Scholar
Staff, RA, Reyndard, L, Brock, F, Bronk Ramsey, C. 2014. Wood pretreatment protocols and measurement of tree-ring standards at the Oxford radiocarbon accelerator unit (ORAU). Radiocarbon 56(2):709–715.Google Scholar
Stuiver, M, Braziunas, TF. 1993. Sun, ocean, climate and atmospheric 14CO2: an evaluation of causal and spectral relationships. The Holocene 3 (4):289–305.Google Scholar
Wacker, L, Güttler, D, Hurni, JP, Synal, H-A, Walti, N. 2014. Radiocarbon dating to a single-year by means of rapid atmospheric 14C changes. Radiocarbon 56(2):573–579.Google Scholar