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δ13Cp Values from Radiocarbon-Dated Plant Matter as an Important but Underexploited Resource for Terrestrial Paleoclimate Analysis and Archaeology

Published online by Cambridge University Press:  09 February 2016

Brandon L Drake*
Affiliation:
Department of Anthropology, University of New Mexico, 1 University of New Mexico, Albuquerque, New Mexico, USA. Email: b.lee.drake@gmail.com

Abstract

Variation in stable carbon isotope ratios in C3 plants can be influenced by climatic and environmental factors. For archaeologists, who regularly collect the measured values of these data as a part of the radiocarbon date reporting process, there is promise in using these data to create a local record of paleoclimatic change relevant to their study areas. Plant Δ13C can be expressed as δ13C values (carbon isotopic discrimination) that can be used in modern experimental studies for stronger paleoclimatic/paleoenvironmental interpretations. As values of Δ13C vary in different species, taxonomic information is necessary for interpretation. In the present study, a record of Irish oak δ13C data are used to construct a local climate history for Ireland. Wetter periods in Ireland inferred from δ13C data correspond to warmer Northern Hemisphere temperatures, in agreement with climate models. Values of δ13C from other species are used to illustrate the importance of using data from taxa with known relationships between climate and stable carbon isotope fractionation.

Type
Paleoclimatology and Paleohydrology
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

Aguilera, M, Espinar, C, Ferrio, JP, Pérez, G, Voltas, J. 2009. A map of autumnal precipitation for the third millennium BC in the Eastern Iberian Peninsula from charcoal carbon isotopes. Journal of Geochemical Exploration 102(3):157–65.CrossRefGoogle Scholar
Alley, RB. 2004. GISP2 Ice Core Temperature and Accumulation Data. IGBP PAGES World Data Center for Paleoclimatology Data Contribution Series #2004-013. NOAA/NGDC Paleoclimatology Program, Boulder, Colorado, USA.Google Scholar
Barry, D, Hartigan, JA. 1993. A Bayesian analysis for change point problems. Journal of the American Statistical Association 35(3):309–19.Google Scholar
Becker, B, Kromer, B, Trimborn, P. 1991. A stable-isotope tree-ring timescale of the Late Glacial/Holocene boundary. Nature 353(6345):647–9.CrossRefGoogle Scholar
Beerling, DJ. 1994. Predicting leaf gas exchange and δ13C responses to the past 30,000 years of global environmental change. New Phytologist 128(3):425–33.CrossRefGoogle Scholar
Binford, LR. 1962. Archaeology as anthropology. American Antiquity 28:217–25.CrossRefGoogle Scholar
Binford, LR. 1965. Archaeological systematics and the study of culture process. American Antiquity 31:203–10.CrossRefGoogle Scholar
Biasing, TJ, Broniak, CT, Marland, G. 2004. Estimates of monthly carbon dioxide emissions and associated δ13C values from fossil-fuel consumption in the USA. In: Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, US Department of Energy, Oak Ridge, Tennessee, USA. doi:10.3334/CDIAC/ffe.001.Google Scholar
Bowling, DR, McDowell, NG, Bond, BJ, Law, BE, Ehleringer, JR. 2002. 13C content of ecosystem is linked to precipitation and vapor pressure deficit. Oecologia 131:113–24.CrossRefGoogle ScholarPubMed
Cernusak, LA, Tcherkez, G, Keitel, C, Cornwell, WK, Santiago, LS, Knohl, A, Barbour, MM, Williams, DG, Reich, PB, Ellsworth, DS, Dawson, TE, Griffiths, HG, Farquhar, GD, Wright, IJ. 2009. Why arc non-photosynthetic tissues generally 13C enriched compared with leaves in C3 plants? Review and synthesis of current hypotheses. Functional Plant Biology 36:199213.CrossRefGoogle Scholar
Cullen, HM, deMenocal, PB, Hemming, S, Hemming, G, Brown, FH, Guilderson, T, Sirocko, F. 2000. Climate change and the collapse of the Akkadian Empire; evidence from the deep sea. Geology 28(4):379–82.2.0.CO;2>CrossRefGoogle Scholar
Diefendorf, A, Mueller, K, Wing, S, Koch, P, Freeman, K. 2010. Global patterns in leaf δ13C discrimination and implications for studies of past and future climate. Proceedings of the National Academy of Sciences of the USA 13:5738–43.Google Scholar
Drake, BL. 2012. The influence of climatic change on the Late Bronze Age collapse and the Greek Dark Ages. Journal of Archaeological Science 39(6):1862–70.CrossRefGoogle Scholar
Drake, BL, Hanson, DT, Boone, JL. 2012. The use of radiocarbon-derived Δ13C as a paleoclimate indicator: applications in the Lower Alentejo of Portugal. Journal of Archaeological Science 39(9):2888–96.CrossRefGoogle Scholar
Dupouey, JL, Leavitt, S, Choisnel, E, Jourdain, S. 1993. Modeling carbon isotope fractionation in tree rings based on effective evapotranspiration and soil water status. Plant, Cell, and Environment 16:939–47.CrossRefGoogle Scholar
Eamus, D, Myers, B, Duff, G, Williams, D. 1999. Seasonal changes in photosynthesis in 8 savanna tree species. Tree Physiology 19:665–71.CrossRefGoogle Scholar
Ehdaie, B, Waines, JG. 1994. Genetic analysis of carbon isotope discrimination and agronomic characters in a bread wheat cross. Theoretical and Applied Genetics 88:1023–8.CrossRefGoogle Scholar
Elsig, J, Schmitt, J, Leuenberger, D, Schneider, R, Eyer, M, Leuenberger, M, Joos, F, Fischer, H, Stocker, TF. 2009. Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core. Nature 461(7263):507–10.CrossRefGoogle ScholarPubMed
English, NB, Betancourt, JL, Dean, JS, Quade, J. 2001. Strontium isotopes reveal distant sources of architectural timber in Chaco Canyon, New Mexico. Proceedings of the National Academy of Sciences of the USA 98(21):11,8916.CrossRefGoogle ScholarPubMed
Erdman, C, Emerson, JW. 2007. bC: an R package for performing a Bayesian analysis of change point problems. Journal of Statistical Software 23(3):113.CrossRefGoogle Scholar
Farquhar, G, Richards, R. 1984. Isotopic composition of plant carbon correlates with water-use efficiency of wheat genotypes. Australian Journal of Plant Physiology 11:539–52.Google Scholar
Farquhar, G, O'Leary, M, Berry, J. 1982. On the relationship between carbon isotope discrimination and intercellular carbon dioxide concentration in leaves. Australian Journal of Plant Physiology 9:121–37.Google Scholar
Farquhar, G, Ehleringer, J, Hubick, K. 1989. Carbon isotope discrimination and photosynthesis. Annual Review of Plant Physiology and Plant Molecular Biology 40:503–37.CrossRefGoogle Scholar
Francey, B, Allison, C, Etheridge, D, Trudinger, C, Enting, I, Leuenberger, M, Lagenfelds, R, Michel, E, Steele, L. 1999. A 1000-year high precision record of δ13C in atmospheric CO2 . Tellus B 51(2):170–93.CrossRefGoogle Scholar
Hall, G, Woodborne, S, Pienaar, M. 2008. Stable carbon isotope ratios from archaeological charcoal as paleoenvironmental indicators. Chemical Geology 247: 384400.CrossRefGoogle Scholar
Heaton, THE, Jones, G, Halstead, P, Tsipropoulos, T. 2009. Variations in the 13C/12C ratios of modern wheat grain, and implications for interpreting data from Bronze Age Assiros Toumba, Greece. Journal of Archaeological Science 36(10):2224–33.CrossRefGoogle Scholar
Indermühle, A, Stocker, TF, Joos, F, Fischer, H, Smith, HJ, Deck, B, Mastroianna, D, Tschumi, J, Blunier, T, Meyer, R, Stauffer, B. 1999. Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, Antarctica. Nature 398(6723):121–6.CrossRefGoogle Scholar
Leavitt, SW. 2008. Tree-ring isotopic pooling without regard to mass: no difference from averaging δ13C values of each tree. Chemical Geology 252:52–5.CrossRefGoogle Scholar
Leavitt, SW, Long, A. 1986. Trends of 13C/12C ratios in piñon tree-rings of the American Southwest and the global carbon cycle. Radiocarbon 28(2A):376–82.CrossRefGoogle Scholar
Leavitt, SW, Long, A. 1988. Stable-carbon isotope chronologies from trees in the Southwestern United States. Global Biochemical Cycles 2(3):189–98.CrossRefGoogle Scholar
Lourantou, A, Lavric, P, Khler, J-M, Barnola, D, Paillard, E, Raynaud, MD, Chappellaz, J. 2010. Constraint of the CO2 rise by new atmospheric carbon isotopic measurements during the last deglaciation. Global Biogeochemical Cycles 24: GB2015, doi:10.1029/2009GB003545.CrossRefGoogle Scholar
McCarroll, D, Pawellek, F. 2001. Stable carbon isotope ratios of Pinus sylvesteris from northern Finland and the potential for extracting a climate signal from the long Fennoscandian chronologies. The Holocene 11(5): 517–26.CrossRefGoogle Scholar
McCormac, FG, Baillie, MG, Pilcher, JR, Brown, DM, Hoper, ST. 1994. δ13C measurements from the Irish oak chronology. Radiocarbon 36(1):2735.CrossRefGoogle Scholar
Mohammady, S, Arminian, A, Khazaei, H, Kozak, M. 2009. Does water-use efficiency explain the relationship between carbon isotope discrimination and wheat grain yield? Acta Agriculturae Scandinavica B 59:385–8.Google Scholar
Monneveux, P, Reynolds, MP, Trethowan, R, Gonza ìlez-Santoyo, H, Peña, RJ, Zapata, F. 2005. Relationship between grain yield and carbon isotope discrimination in bread wheat under four water regimes. European Journal of Agronomy 22:231–42.CrossRefGoogle Scholar
Ponton, S, Dupouey, JL, Bréda, N, Feullat, F, Bodénès, C, Dreyer, E. 2001 Carbon isotope discrimination and wood anatomy variations in mixed stands of Quercus robur and Quercus petraea . Plant, Cell, and Environment 24:861–8.CrossRefGoogle Scholar
Riehl, S. 2008. Climate and agriculture in the Near East: a synthesis of the archaeobotanical and stable-carbon isotope evidence. Vegetation History and Archaeobotany 17(Supplement 1):S43S51.CrossRefGoogle Scholar
Robinson, WJ, Rose, MR. 1979. Preliminary Annual and Seasonal Dendroclimatic Reconstruction for the Northwest Plateau, Southwest Colorado, Southwest Mountains, and Northern Mountains, Climatic Regions, A.D. 900-1969. Manuscript on File at the Laboratory of Tree-Ring Research, University of Arizona, Tucson.Google Scholar
Roussel, M, Dreyer, E, Montpied, P, Le-Provost, G, Guehl, JM, Brendel, O. 2009. The diversity of 13C isotope discrimination in a Quercus robur full-sib family is associated with differences in intrinsic water use efficiency, transpiration efficiency, and stomatal conductance. Journal of Experimental Botany 60(8): 2419–31.CrossRefGoogle Scholar
Seibt, U, Rajabi, A, Griffiths, H. 2008. Carbon isotopes and water use efficiency: sense and sensitivity. Oecologia 155:441–54.CrossRefGoogle ScholarPubMed
Sheenan, S. 2002. Genes, Memes, and Human History: Darwinian Archaeology and Cultural Evolution. London: Thames and Hudson.Google Scholar
Smith, HJ, Fischer, H, Mastroianni, D, Deck, B, Wahlen, M. 1999. Dual modes of the carbon cycle since the Last Glacial Maximum. Nature 400:248–50.CrossRefGoogle ScholarPubMed
Stuiver, M, Polach, HA. 1977. Discussion: reporting of 14C data. Radiocarbon 19(3):355–63.CrossRefGoogle Scholar
Trigger, BG. 2007. A History of Archaeological Thought. 2nd edition. Cambridge: Cambridge University Press.Google Scholar
Trouet, V, Esper, J, Graham, NE, Baker, A, Scourse, JD, Frank, DC. 2009. Persistent positive North Atlantic Oscillation mode dominated the Medieval Climate Anomaly. Science 324(5923):7880.CrossRefGoogle ScholarPubMed
Werner, C, Máguas, C. 2010. Carbon isotope discrimination as a tracer of functional traits in a Mediterranean macchia plant community. Functional Plant Biology 37:467–77.CrossRefGoogle Scholar