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Reconstructing Atmospheric CO2 Concentration Using Its Relationship with Carbon Isotope Variations in Annual Tree Ring of Red Pine

  • Choi, Woo-Jung (Department of Rural & Biosystems Engineering, Institute of Agricultural Science & Technology, Chonnam National University) ;
  • Lee, Kye-Han (Department of Forestry, Institute of Agricultural Science & Technology, Chonnam National University) ;
  • Lee, Sang-Mo (National Instrumentation Center for Environmental Management, Seoul National University) ;
  • Lee, Seung-Heon (Rural Research Institute, Korea Rural Community Corporation) ;
  • Kim, Han-Yong (Department of Applied Plant Science, Institute of Agricultural Science & Technology, Chonnam National University)
  • 투고 : 2010.12.07
  • 심사 : 2010.12.21
  • 발행 : 2010.12.30

초록

Carbon isotope ratio ($^{13}C/^{12}C$, expressed as ${\delta}^{13}C$) of tree ring can be proxy of atmospheric $CO_2$ concentration ([$CO_2$]) due to the inter-correlation between atmospheric [$CO_2$], ${\delta}^{13}C$ of atmospheric $CO_2$, and ${\delta}^{13}C$ of plant tissue that assimilates atmospheric $CO_2$. This study was conducted to investigate if ${\delta}^{13}C$ of tree ring of Pinus densiflora in polluted area may show a lower value than that in unpolluted area and to explore the possibility of reconstructing atmospheric [$CO_2$] using its relationship with ${\delta}^{13}C$ of tree ring. During the period between 1999 and 2005, ${\delta}^{13}C$ of tree annual ring tended to decrease over time, and the ${\delta}^{13}C$ in polluted area (-27.2‰ in 2009 to -28.3‰ in 2005) was significantly (P<0.001) lower than that (-26.0‰ in 1999 to -27.1‰ in 2005) in unpolluted area. This reflects a greater emission of $CO_2$ depleted in $^{13}C$ in the polluted area. Atmospheric [$CO_2$] was significantly (P<0.01) correlated with ${\delta}^{13}C$ of tree ring in a linear fashion. Using the linear regression equation, atmospheric [$CO_2$] in the polluted area was estimated to range from 392.3 ppm in 1999 to 410.9 ppm in 2005, and these values were consistently higher than the national atmospheric [$CO_2$] monitored at the Anmyoundo meteorological station (from 370.7 ppm in 1999 to 387.2 ppm in 2005). Our study suggested that it is possible to reconstruct atmospheric [$CO_2$] in a certain area using the relationship between tree ring ${\delta}^{13}C$ and atmospheric [$CO_2$].

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참고문헌

  1. IPCC (Intergovernmental Panel on Climate Change), 2007. Contribution of Working Groups I, II and III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. IPCC, Geneva, Switzerland.
  2. Bert, D., Leavitt, S.W., Dupouey, J.L., 1997. Variations of wood δ13C and water-use efficiency of Abies alba during the last century. Ecology 78, 1588–1596.
  3. Bukata, A.R., Kyser, T.K., 2007. Carbon and nitrogen isotope variations in tree-rings as records of perturbations in regional carbon and nitrogen cycle. Environ. Sci. Technol. 41, 1331-1338. https://doi.org/10.1021/es061414g
  4. Choi, W.J., Chang, S.X., Bhatti, J.S., 2007. Drainage affects tree growth and C and N dynamics in a minerotrophic peatland. Ecology 88, 443-453. https://doi.org/10.1890/0012-9658(2007)88[443:DATGAC]2.0.CO;2
  5. Choi, W.J., Lee, S.M., Chang, S.X., Ro, H.M., 2005. Variations of $\delta^{13}C$ and $\delta^{15}N$ in Pinus densiflora tree-rings and their relationship to environmental changes in eastern Korea. Water Air Soil Pollut. 164, 173-187. https://doi.org/10.1007/s11270-005-2253-y
  6. Edwards, T.W.D., Graf, W., Trimborn, P., Stichler, W., Lipp, J., Payer, H.D., 2000. $\delta^{13}C$ response surface resolves humidity and temperature signals in trees. Geochim. Cosmochim. Ac. 64, 161-167. https://doi.org/10.1016/S0016-7037(99)00289-6
  7. Elhani, S., Guehl, J.M., Nys, C., Picard, J.F., Dupouey, J.L., 2005. Impact of fertilization on tree-ring $\delta^{15}N$ and $\delta^{13}C$ in beech stands: A retrospective analysis. Tree Physiol. 25, 1437-1446. https://doi.org/10.1093/treephys/25.11.1437
  8. Farquhar, G.D., Ehleringer, J.R., Hubick, K.T., 1989. Carbon isotope discrimination and photosynthesis. Ann. Rev. Plant Physiol. Plant Mol. Biol. 40, 503-537. https://doi.org/10.1146/annurev.pp.40.060189.002443
  9. February, E.C., Stock, W.D., 1999. Declining trend in the $^{13}C$/$^{12}C$ ratio of atmospheric carbon dioxide from tree rings of South African Widdringtonia cedarbergensis. Quaternary Res. 52, 229–236.
  10. Freyer, H.D., Belacy, N., 1983. $^{12}C$/$^{13}C$ records in Northern Hemispheric trees during the past 500 years: anthropogenic impact and climatic superpositions. J. Geophys. Res. 88, 6844-6852. https://doi.org/10.1029/JC088iC11p06844
  11. Friedli, H., Lotscher, H., Oeschger, H., Siegenthaler, U., Stauffer, B., 1986. Ice core recorder of the $^{13}C$/$^{12}C$ ratio of atmospheric $CO_{2}$ in the past two centuries. Nature 324, 237-238. https://doi.org/10.1038/324237a0
  12. Heaton, T.H.E., Crossley, A., 1995. Carbon isotope variations in a plantation of Sitka spruce, and the effect of acid mist. Oecologia 103, 109-117. https://doi.org/10.1007/BF00328431
  13. Kwak, J.H., Choi, W.J., Lim, S.S., Arshad, M.A., 2009a. $\delta^{13}C$, $\delta^{15}C$, N concentration, and Ca-to-Al ratios of forest samples from Pinus densiflora stands in rural and industrial areas. Chem. Geol. 264, 385-393. https://doi.org/10.1016/j.chemgeo.2009.04.002
  14. Kwak, J.H., Lim, S.S., Park, H.J., Lee, S.I., Lee, K.H., Kim, H.Y., Chang, S.X., Lee, S.M., Ro, H.M., Choi, W.J., 2009b. Relating tree ring chemistry of Pinus densiflora to precipitation acidity in an industrial area of South Korea. Water Air Soil Pollut. 199, 95-106. https://doi.org/10.1007/s11270-008-9862-1
  15. Kwak, J.H., Lim, S.S., Park, H.J., Lee, S.I., Lee, D.S., Lee, K.H., Han, G.H., Ro, H.M., Lee, S.M., 2009c. Isotope ratio of mineral N in Pinus densiflora forest soils in rural and industrial areas: potential indicator of atmospheric N deposition and soil N loss. Korean J. Soil Sci. Fert. 42, 46-52.
  16. Loader, N.J., Robertson, I., McCarroll, D., 2003. Comparison of stable carbon isotope ratios in the whole wood, cellulose and lignin of oak tree-rings. Palaeogeogr. Palaeocl. Palaeoecol.196, 395-407. https://doi.org/10.1016/S0031-0182(03)00466-8
  17. McCarroll, D., Gagen, M.H., Loader, N.J., Robertson, I., Anchukaitis, K.J., Los, S., Young, G.H.F., Jalkanen, R., Kirchhefer, A., Waterhouse, J., 2009. Correction of tree ring stable carbon isotope chronologies for changes in the carbon dioxide content of the atmosphere. Geochim. Cosmochim. Ac. 73, 1539-1547. https://doi.org/10.1016/j.gca.2008.11.041
  18. Sakata, M., Suzuki, K., 2000. Evaluating possible causes for the decline of Japanese fir (Abies firma) forests based on $\delta^{13}C$ records of annual growth rings. Environ. Sci. Technol. 34, 373-376. https://doi.org/10.1021/es990301c
  19. Saurer, M., Maurer, S., Matyssek, R., Landolt, W., Siegenthaler, G.G.U., 1995. The influence of ozone and nutrition on $\delta^{13}C$ in Betula pendula. Oecologia 103, 397-406. https://doi.org/10.1007/BF00328677
  20. Wagner, R., Wagner, E., 2006. Influence of air pollution and site conditions on trends of carbon and oxygen isotope ratios in tree ring cellulose. Isot. Environ. Health Sci. 42, 351-365. https://doi.org/10.1080/10256010600991078

피인용 문헌

  1. Historical responses of Quercus variabilis growth to environmental changes in Southern Korea: Evidence from tree ring width and δ 13C vol.56, pp.5, 2013, https://doi.org/10.1007/s13765-013-3102-0
  2. A short overview on linking annual tree ring carbon isotopes to historical changes in atmospheric environment vol.8, pp.2, 2012, https://doi.org/10.1080/21580103.2012.672017