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Carbon Isotopic Composition of Tree Rings as A Tool for Biomonitoring CO2 Level

Published online by Cambridge University Press:  18 July 2016

Sławomira Pawełczyk
Affiliation:
Institute of Physics, Radiocarbon Laboratory, Silesian University of Technology, Krzywoustego 2, 44-100 Gliwice, Poland
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Abstract

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Carbon isotopes are widely used as indicators in the study of atmospheric CO2 variability in space and time. Preliminary results are part of a project investigating 13C and 14C concentration changes during the last 150 yr in Poland, both in industrial and ecologically clean regions, using annual tree rings (Pinus sylvestris, Populus nigra). The results describe the local Suess effect recorded in the industrial Kraków and Upper Silesia regions compared to changes of background radiocarbon concentration caused by global human activity in a “clean region,” Augustów Wilderness. The δ13C record also shows the influence of the local Suess effect.

Type
Part II
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Awsiuk, R, Pazdur, MF. 1986. Regional Suess effect in the Upper Silesia urban area. Radiocarbon 28(2A):655–60.CrossRefGoogle Scholar
Damon, PE, Cheng, S, Linck, TW. 1989. Fine and hyper-fine structure in the spectrum of secular variations of atmospheric 14C. Radiocarbon 31(3):704–18.CrossRefGoogle Scholar
De Jong, AFM, Mook, WG. 1982. An anomalous Suess effect above Europe. Nature 298:13.CrossRefGoogle Scholar
Florkowski, T, Kuc, T. 1979. Carbon isotopes and sulphur content as indicators of atmospheric pollution from burning fossil fuels. Environment International 2: 431–5.CrossRefGoogle Scholar
Green, JW. 1963. Wood cellulose. In: Whistler, RL, editor. Carbohydrate Chemistry III. San Diego: Academic Press. p 921.Google Scholar
Keeling, CD, Bascetow, RB, Carter, AF, Piper, SC, Whorf, TP, Heimann, M, Mook, WM, Roeloffzen, H. 1989. A three-dimensional model of atmospheric CO2 transport based on observed winds: 1. Analysis of observational data. In: Petersen, DH, editor. Aspects of Climate Variability in the Pacific and Western Americas. Geophysical Monographs 55:165236.Google Scholar
Kuc, T. 1986. Carbon isotopes in atmospheric CO2 of the Kraków region: a two-year record. Radiocarbon 28(2A):649–54.CrossRefGoogle Scholar
Kuc, T, Zimnoch, M. 1998. Changes of the CO2 sources and sinks in a polluted urban area (southern Poland) over the last decade, derived from the carbon isotope composition. Radiocarbon 40(1):417–23.Google Scholar
Levin, I, Graul, R, Trivett, NBA. 1995. Long-term observations of atmospheric CO2 and carbon isotopes at continental sites in Germany. Tellus 47B:2334.CrossRefGoogle Scholar
Levin, I, Hesshaimer, V. 2000. Radiocarbon—a unique tracer of global carbon cycle dynamic. Radiocarbon 42(1):6980.CrossRefGoogle Scholar
Levin, I, Kromer, B. 1997. Twenty years of high-precision atmospheric 14CO2 observations at Schauinsland station, Germany. Radiocarbon 39(2):205–18.CrossRefGoogle Scholar
Levin, I, Schuchard, J, Kromer, B, Münnich, KO. 1989. The continental European Suess effect. Radiocarbon 31(3):431–40.CrossRefGoogle Scholar
Loader, NJ, Robertson, I, Barker, AC, Switsur, VR, Waterhouse, JS. 1997. An improved technique for the bath processing of small wholewood samples to α-cellulose. Chemical Geology 136:313–7.CrossRefGoogle Scholar
Marland, G, Boden, TA, Andres, RJ. 2001. Global, regional, and national fossil fuel CO2 emissions. 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. http://cdiac.ornl.gov/ndps/ndp030.html.Google Scholar
Nydal, R, Lövseth, K. 1983. Tracing bomb 14C in the atmosphere. Journal of Geophysical Research 88:3621–42.Google Scholar
Oeschger, H, Siegenthaler, U, Schotterer, U, Gugelmann, A. 1975. A box-diffusion model to study the carbon dioxide exchange in nature. Tellus 27:169–92.Google Scholar
Pazdur, A, Matyja, S, Rakowski, AZ. 1998. Radiocarbon concentration measurements in contemporary tree rings from Upper Silesia. RMZ-Materials and Geoenvironment 45(1–2):255–7.Google Scholar
Rakowski, AZ, Pawe$lSczyk, S, Pazdur, A. 2001. Changes of 14C concentration in modern trees from Upper Silesia region, Poland. Radiocarbon 43(2):633–43.CrossRefGoogle Scholar
Robertson, I, Waterhouse, J. 1998. Trees of knowledge. Chemistry in Britain. London: Royal Society of Chemistry. p 2730.Google Scholar
Schleser, GH, Helle, G, Lucke, A, Vos, H. 1999. Isotope signals as climate proxies: the role of transfer functions in the study of terrestrial archives. Quaternary Science Reviews 18:927–43.CrossRefGoogle Scholar
Sheu, DD, Kou, P, Chiu, C-H, Chen, M-J. 1997. Variability of tree rings in Taiwan fir: growth effect and response to May–October temperatures. Geochimica et Cosmochimica Acta 60(1):171–7.Google Scholar
Siegenthaler, U, Oeschger, H. 1987. Biospheric CO2 emmision during the past 200 years reconstructed by de-convolution of ice core data. Tellus 39:140–54.Google Scholar
Stuiver, M, Quay, P. 1981. Atmospheric 14C changes resulting from fossil fuel CO2 release and cosmic ray flux variability. Earth and Planetary Science Letters 53:349–62.CrossRefGoogle Scholar
Switsur, VR, Waterhouse, JS, Field, EM, Carter, AHC. 1996. Climatic signals from stable isotopes in Oak tree rings from East Anglia, Great Britain. In: Dean, JS, Meko, DM, Swetnam, TW, editors. Tree Rings, Environment and Humanity. Tucson, Arizona: Radiocarbon. p 637–45.Google Scholar
Tans, PP, Mook, WG. 1980. Past atmospheric CO2 levels and the 13C/12C ratios in tree rings. Tellus 32:268–83.Google Scholar