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Climate warming and increasing atmospheric CO2 have contributed to increased intrinsic water-use efficiency on the northeastern Tibetan Plateau since 1850

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Abstract

We investigated the physiological responses of Tibetan juniper (Sabina tibetica) to changes in the atmospheric CO2 concentration (C a) and climate on the northeastern Tibetan Plateau based on annual tree-ring δ13C values since 1850. Intrinsic water-use efficiency (iWUE) increased, and the internal to ambient CO2 ratio (C i /C a) showed no significant trend from 1895 to 1974 in the study region, indicating an active response to changing C a. The long-term trends in iWUE in the naturally occurring trees were mainly caused by the anthropogenic increase in C a. However, from 1975 to 2002, iWUE increased rapidly at the study site (by 12.4 % compared with the overall mean from 1850 to 2002), which is greater than the expected increase due only to an active response to C a. Our analysis showed that decreased water availability caused by greater evaporation due to decreased precipitation and a warming growth environment from 1975 to 2002 may have reduced stomatal conductance, leading to a higher iWUE. The warming climate and increased C a accounted for 83.6 % of the variance in iWUE of Tibetan juniper on the northeastern Tibetan Plateau from 1975 to 2002.

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References

  • Andreu L, Planells O, Gutierrez E, Helle G, Schleser GH (2002) Increasing atmosphereric CO2 concentration is enhancing water-use efficiency in five Spanish forests. PhD dissertation, Universitat de Barcelona, Barcelona

  • Andreu-Hayles L, Planells O, GutiÉRrez E, Muntan E, Helle G, Anchukaitis KJ, Schleser GH (2011) Long tree-ring chronologies reveal 20th century increases in water-use efficiency but no enhancement of tree growth at five Iberian pine forests. Global Change Biol 17(6):2095–2112. doi:10.1111/j.1365-2486.2010.02373.x

    Article  Google Scholar 

  • Coplen TB (1995) Discontinuance of SMOW and PDB. Nature 375:285

    Article  CAS  Google Scholar 

  • Duquesnay A, Bréda N, Stievenard M, Dupouey JL (1998) Changes of tree-ring δ13C and water-use efficiency of beech (Fagus sylvatica L.) in north-eastern France during the past century. Plant Cell Environ 21(6):565–572

    Article  Google Scholar 

  • Ehleringer JR, Cerling TE (1995) Atmospheric CO2 and the ratio of intercellular to ambient CO2 concentrations in plants. Tree Physiol 15:105–111

    Article  PubMed  Google Scholar 

  • Farquhar GD, O’Leary MH, Berry JA (1982) On the relationship between carbon isotope discrimination and the intercellular carbon dioxide concentration in leaves. Austral J Plant Physiol 9:121–137

    Article  CAS  Google Scholar 

  • Farquhar GD, Ehleringer JR, Hubick KT (1989) Carbon isotope discrimination and photosynthesis. Ann Rev Plant Physiol Mol Biol 40(1):503–537. doi:10.1146/annurev.pp 40.060189.002443

    Article  CAS  Google Scholar 

  • Feng XH (1998) Long-term c i/c a response of trees in western North America to atmospheric CO2 concentration derived from carbon isotope chronologies. Oecologia 117:19–25

    Article  Google Scholar 

  • Feng XH (1999) Trends in intrinsic water-use efficiency of natural trees for the past 100–200 years: a response to atmospheric CO2 concentration. Geochim Cosmochim Acta 63(13–14):1891–1903. doi:10.1016/S0016-7037(99)00088-5

    Article  CAS  Google Scholar 

  • Feng XH, Epstein S (1995) Carbon isotopes of trees from arid environments and implications for reconstructing atmospheric CO2 concentration. Geochim Cosmochim Acta 59(12):2599–2608

    Article  CAS  Google Scholar 

  • Green JW (1963) Wood cellulose. In: Whistler RL (ed) Methods of carbohydrate chemistry III. Academic Press, London, pp 9–21

    Google Scholar 

  • Hietz P, Wanek W, Dunisch O (2005) Long-term trends in cellulose δ13C and water-use efficiency of tropical Cedrela and Swietenia from Brazil. Tree Physiol 25(6):745–752. doi:10.1093/treephys/25.6.745

    Article  PubMed  CAS  Google Scholar 

  • Jin LY, Qin NS, Gou XH, Chen FH, Li JB (2005) Series of spring maximum temperature in southern Qinghai Plateau and analysis of its variations during the last 450 years (in Chinese). Quat Sci 25:193–201

    Google Scholar 

  • Jones P, Humle M (1996) Calculating regional climatic time series for temperature and precipitation: methods and illustrations. Int J Climatol 16:361–377

    Article  Google Scholar 

  • Leavitt SW (2008) Tree-ring isotopic pooling without regard to mass: no difference from averaging δ13C values of each tree. Chem Geol 252:52–55

    Article  CAS  Google Scholar 

  • Leavitt SW, Idso SB, Kimball BA, Burns JM, Sinha A, Stott L (2003) The effect of long-term atmospheric CO2 enrichment on the intrinsic water-use efficiency of sour orange trees. Chemosphere 50(2):217–222. doi:10.1016/S0045-6535(02)00378-8

    Article  PubMed  CAS  Google Scholar 

  • Leavitt SW, Treydte K, Yu L (2010) Environment in time and space: opportunities from Tree-ring isotope networks. In: West JB, Bowen GJ, Dawson TE, Tu KP (eds) Isoscapes: understanding movement, pattern, and process on earth through isotope mapping. Springer, Dordrecht, pp 113–135

    Google Scholar 

  • Liu XH, Shao XM, Wang LL, Liang EY, Qin DH, Ren JW (2008) Response and dendroclimatic implications of δ13C in tree rings to increasing drought on the northeastern Tibetan Plateau. J Geophys Res 113:G03015. doi:10.1029/2007jg000610

    Article  Google Scholar 

  • Liu XH, Liu Y, Xu GB, Cai QF, An WL, Wang WZ (2010) Pretreatment of the tree-ring samples for stable isotope analysis (in Chinese). J Glaciol Geocryol 32(06):1242–1250

    Google Scholar 

  • Liu XH, An WL, Liang EY, Wang WZ, Shao XM, Huang L, Qin DH (2011) Spatiotemporal variability in tree ring’s δ13C of Picea crassifolia in the Qilian Mountains: climatic significance and responses to rising CO2. Sci Cold Arid Regions 3:93–102

    Article  Google Scholar 

  • Marshall JD, Monserud RA (1996) Homeostatic gas-exchange parameters inferred from 13C/12C in tree rings of conifers. Oecologia 105(1):13–21

    Article  Google Scholar 

  • McCarroll D, Loader NJ (2004) Stable isotopes in tree rings. Quat Sci Rev 23(7–8):771–801

    Article  Google Scholar 

  • McCarroll D, Gagen MH, Loader NJ, Robertson I, Anchukaitis KJ, Los S, Young GHF, Jalkanen R, Kirchhefer A, Waterhouse JS (2009) Correction of tree ring stable carbon isotope chronologies for changes in the carbon dioxide content of the atmosphere. Geochim Cosmochim Acta 73(6):1539–1547. doi:10.1016/j.gca.2008.11.041

    Article  CAS  Google Scholar 

  • Mitchell TD, Jones PD (2005) An improved method of constructing a database of monthly climate observations and associated high-resolution grids. Int J Climatol 25:693–712. doi:10.1002/joc.1181

    Article  Google Scholar 

  • Murakami T (1987) Orography and monsoons. In: Fien JS, Stephens PL (eds) Monsoons. Wiley, New York, pp 331–364

    Google Scholar 

  • Qin NS, Shao XM, Jin LY, Wang QC, Zhu XD, Wang Z, Li JB (2003) Climate change over southern Qinghai Plateau in the past 500 years recorded in Sabina tibetica tree rings. Chinese Sci Bull 48(22):2483–2487. doi:10.1360/03wd0088

    Google Scholar 

  • Robertson I, Waterhouse JS, Barker AC, Carter AHC, Switsur VR (2001) Oxygen isotope ratios of oak in east England: implications for reconstructing the isotopic composition of precipitation. Earth Planet Sci Lett 191:21–31. doi:S0012-821X(01)00399-5

    Article  CAS  Google Scholar 

  • Saurer M, Siegwolf RTW, Schweingruber FH (2004) Carbon isotope discrimination indicates improving water-use efficiency of trees in northern Eurasia over the last 100 years. Global Change Biol 10:2109–2120. doi:10.1111/j.1365-2486.2004.00869.x

    Article  Google Scholar 

  • Schweingruber FH (ed) (1988) Tree rings: basics and applications of dendrochronology. Academic Press, Dordrecht

    Google Scholar 

  • Silva LCR, Anand M, Leithead MD (2010) Recent widespread tree growth decline despite increasing atmospheric CO2. Plosone 5(7):e11543. doi:10.1371/journal.pone.0011543

    Google Scholar 

  • Stokes MA, Smiley TL (eds) (1968) An introduction to tree-ring dating. The University of Chicago Press, Chicago

    Google Scholar 

  • Sun HL, Zheng D (eds) (1998) Formation, evolution and development of Tibetan Plateau (in Chinese). Guangdong Science and Technology Press, Guangzhou

    Google Scholar 

  • Tang MC, Sheng ZB, Chen YY (1979) On climatic characteristics of the Xizang Plateau monsoon (in Chinese). Acta Geograph Sinica 34(1):33–42

    Google Scholar 

  • Tang K, Feng X, Funkhouser G (1999) The δ13C of tree rings in full-bark and strip-bark bristlecone pine trees in the White Mountains of California. Global Change Biol 5(1):33–40. doi:10.1046/j.1365-2486.1998.00204.x

    Article  Google Scholar 

  • Wang JXL, Gaffen DJ (2001) Late-twentieth-century climatology and trends of surface humidity and temperature in China. J Clim 141:2833–2845

    Article  Google Scholar 

  • Wang SW, Ye JL, Gong DY, Zhu JH, Yao TD (1998) Construction of mean annual temperature series for the last one hundred years in China (in Chinese). Quart J Appl Meteorol 9(4):392–401

    Google Scholar 

  • Waterhouse JS, Switsur VR, Barker AC, Carter AHC, Hemming DL, Loader NJ, Robertson I (2004) Northern European trees show a progressively diminishing response to increasing atmospheric carbon dioxide concentrations. Quat Sci Rev 23(7–8):803–810

    Article  Google Scholar 

  • Williams DG, Ehleringer JR (1996) Carbon isotope discrimination in three semi-arid woodland species along a monsoon gradient. Oecologia 106:455–460

    Article  Google Scholar 

  • Xu GB, Chen T, Liu XH, Jin LY, An WL, Wang WZ (2011) Summer temperature variations recorded in tree-ring δ13C values on the northeastern Tibetan Plateau. Theor Appl Climatol 105:51–63. doi:10.1007/s00704-010-0370-z

    Article  Google Scholar 

Download references

Acknowledgments

This research was supported by the Global Change Research Program of China (2010CB951401), by the National Natural Science Foundation of China (41171167, 41121001, 40871002 and 31200299), and by the Knowledge Innovation Project of the Chinese Academy of Sciences (KZCX2-YW-QN308). We thank the journal’s anonymous reviewers and the journal’s editor, whose comments and suggestions helped us to improve the paper.

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Correspondence to Xiaohong Liu.

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Communicated by A. Braeuning.

Special topic: Dendroecology in Asia.

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468_2013_855_MOESM1_ESM.tif

Fig. S1 Trends in (a) the δ13Craw chronology, (b) the δ13Cc chronology, and (c) δ13Cpin chronology over time. Linear and nonlinear regression plotted from 1850 to 2002, from 1895 to 2002, from 1950 to 2002, and from 1975 to 2002. Only statistically significant (p < 0.05) trends are presented (TIFF 767 kb)

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Xu, G., Liu, X., Qin, D. et al. Climate warming and increasing atmospheric CO2 have contributed to increased intrinsic water-use efficiency on the northeastern Tibetan Plateau since 1850. Trees 27, 465–475 (2013). https://doi.org/10.1007/s00468-013-0855-3

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