Trees

, Volume 20, Issue 5, pp 571–586 | Cite as

Inter-annual and seasonal variability of radial growth, wood density and carbon isotope ratios in tree rings of beech (Fagus sylvatica) growing in Germany and Italy

  • M. V. Skomarkova
  • E. A. Vaganov
  • M. Mund
  • A. Knohl
  • P. Linke
  • A. Boerner
  • E.-D. Schulze
Original Article

Abstract

We investigated the variability of tree-ring width, wood density and 13C/12C in beech tree rings (Fagus sylvatica L.), and analyzed the influence of climatic variables and carbohydrate storage on these parameters. Wood cores were taken from dominant beech trees in three stands in Germany and Italy. We used densitometry to obtain density profiles of tree rings and laser-ablation-combustion-GC-IRMS to estimate carbon isotope composition (δ13C) of wood. The sensitivity of ring width, wood density and δ13C to climatic variables differed; with tree-ring width responding to environmental conditions (temperature or precipitation) during the first half of a growing season and maximum density correlated with temperatures in the second part of a growing season (July–September). δ13C variations indicate re-allocation and storage processes and effects of drought during the main growing season. About 20% of inter-annual variation of tree-ring width was explained by the tree-ring width of the previous year. This was confirmed by δ13C of wood which showed a contribution of stored carbohydrates to growth in spring and a storage effect that competes with growth in autumn. Only mid-season δ13C of wood was related to concurrent assimilation and climate. The comparison of seasonal changes in tree-ring maximum wood density and isotope composition revealed that an increasing seasonal water deficit changes the relationship between density and 13C composition from a negative relation in years with optimal moisture to a positive relationship in years with strong water deficit. The climate signal, however, is over-ridden by effects of stand density and crown structure (e.g., by forest management). There was an unexpected high variability in mid season δ13C values of wood between individual trees (−31 to −24‰) which was attributed to competition between dominant trees as indicated by crown area, and microclimatological variations within the canopy. Maximum wood density showed less variation (930–990 g cm−3). The relationship between seasonal changes in tree-ring structure and 13C composition can be used to study carbon storage and re-allocation, which is important for improving models of tree-ring growth and carbon isotope fractionation. About 20–30% of the tree-ring is affected by storage processes. The effects of storage on tree-ring width and the effects of forest structure put an additional uncertainty on using tree rings of broad leaved trees for climate reconstruction.

Keywords

Carbohydrate storage Climate Dendrochonology Drought Stable carbon isotopes 

References

  1. Barbour MM, Hunt JE, Dungan RJ, Turnbull MH, Brailsford GW, Farquhar GD, Whitehead D (2005) Variation in the degree of coupling between delta C-13 of phloem sap and ecosystem respiration in two mature Nothofagus forests. New Phytol 166:497–512PubMedCrossRefGoogle Scholar
  2. Bascietto M, Cherubini P, Scarascia-Mugnozza G (2004) Tree rings from a European beech forest chronosequence are useful for detecting growth trends and carbon sequestration. Can J For Res 34:481–492CrossRefGoogle Scholar
  3. Bouriaud O, Breda N, Le Moguedes G, Nepveu G (2004) Modelling variability of wood density in beech as affected by ring age, radial growth and climate. Trees 18:264–276Google Scholar
  4. Briffa KR, Schweingruber FH, Jones PD, Osborn TJ, Harris IC, Shiyatov SG, Vaganov EA, Grudd H (1998) Trees tell of past climates: but are they speaking less clearly today? Phil Transact Royal Soc London 353:65–73CrossRefGoogle Scholar
  5. Briffa KR, Osborn TJ, Schweingruber FH (2004) Large-scale temperature inferences from tree rings: a review. Glob Panet Change 40:11–26CrossRefGoogle Scholar
  6. Brugnoli E, Farquhar GD (2000) Photosynthetic fractionation of carbon isotopes. Adv Phytol Physiol Metab 9:399–434Google Scholar
  7. Ciais P, et al. (2005) An unprecedented reduction in the primary productivity of Europe during 2003 caused by heat and drought. Nature 437:529–533PubMedCrossRefGoogle Scholar
  8. Collatz ER, Ball JT, Grivet C, Berry JA (1991) Physiological and environmental regulation of stomatal conductance, photosynthesis and transpiration: A model that includes a laminar boundary layer. Agric Forst Met 54:107–136CrossRefGoogle Scholar
  9. Cook ER, Peters K (1981) The smoothing spline: A new approach to standardizing forest interior tree-ring width series for dendroclimatic studies. Tree-Ring Bull 41:45–53Google Scholar
  10. Cook ER, Briffa KR, Shiyatov SG, Mazepa VS (1990) Tree-ring standardization and growth-trend estimation. In: Cook ER, Kairiukstis LA (eds) Methods of dendrochronology. Application in the environmental sciences. Kluwer Academic Publisher, Dordrecht, The Netherlands, pp 104–123Google Scholar
  11. De Silva MP (1979) 13Carbon-isotope decrease in annual-rings of twentieth-century trees. Zeitschrift für Naturforschung 34:644–646Google Scholar
  12. Duquesnay A, Breda N, Stievenard M, Dupouey JL (1998) Changes of tree-ring delta C-13 and water-use efficiency of beech (Fagus sylvatica L.) in north-eastern France during the past century. Plant Cell Env 21:565–572CrossRefGoogle Scholar
  13. Ehleringer JR, Field CB, Lin ZF, Kuo CY (1986) Leaf carbon isotope and mineral composition in subtropical plants along a irradiance decline. Oecologia 70:520–526CrossRefGoogle Scholar
  14. Epron D, Godard D, Cornic G, Genty B (1995) Limitations of net CO2 assimilation rate by internal resistence to CO2 transfer in the leaf of two tree species (Fagus sylvatica L. and Castanea sativa Mill.). Plant Cell Environ 18:43–51 CrossRefGoogle Scholar
  15. FAO (1998) World reference base of soil resources. Food and Agriculture Organization of the United Nations, Rome, Italy. Rep. 84Google Scholar
  16. Freyer HD, Belacy N (1993) 13C/12C Records in northern hemispheric trees during the past 500 years—Anthropogenic impact and climatic superpositions. J Geophys Res 88:6844–6852CrossRefGoogle Scholar
  17. Gäumann E (1935) Über den Stoffhaushalt der Buche. Berichte Deutsche Botanische Gesellschaft 53:366–377Google Scholar
  18. Gleixner G, Danier HJ, Werner RA, Schmidt HL (1993) Correlations between the C-13 content of primary and secondary plant-products in different cell compartments and that in decomposing basidiomycetes. Plant Physiol 102:1287–1290PubMedGoogle Scholar
  19. Götlicher S, Knohl A, Wanek W, Buchmann N, Richter A (2005) Short term changes in carbon isotope composition of soluble carbohydrates and starch: from canopy leaves to the root system. Rapid Commun Mass Spectrom 20:653–660CrossRefGoogle Scholar
  20. Hauser S (2003) Dynamik hochaufgelöster radialer Schaftveränderungen und des Dickenwachstums bei Buche (Fagus sylvatica L.) der Schwäbischen Alb unter dem Einfluß von Witterung und Bewirtschaftung. Dissertation, Uni Freiburg. http://freidok.ub.uni-freiburg.de/volltext/1121/
  21. Helle G, Schleser GH (2004) Beyond CO2-fixation by Rubisco—an interpretation of 13C/12C variations in tree rings from novel intra-seasonal studies on broad-leaf trees. Plant Cell Environ 27:367–380CrossRefGoogle Scholar
  22. Hilton GM, Packam JR (2003) Variation in the masting of common beech (Fagus sylvatica L.) in northern Europe over two centuries (1800–2001). Forestry 76:319–328CrossRefGoogle Scholar
  23. Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull 44:69–75Google Scholar
  24. Holmes RL (1992) Program COFECHA: Version 3. The University of Arizona. TucsonGoogle Scholar
  25. Kagawa A, Naito D, Sugimoto A, Maximov TC (2002) Effects of spatial and temporal variability in soil moisture on widths and δ 13C values of eastern Siberian tree rings. J Geophys Res 108: DOI: 10.1029/2002JD003019Google Scholar
  26. Kirdyanov AV (1999) Use of wood density characteristics in dendroclimatology. Siberian J Ecol 2:193–201Google Scholar
  27. Keitel C, Adams MA, Holst T, Matzarakis A, Mayer H, Rennenberg H, Gessler A (2003) Carbon and oxygen isotope composition of organic compounds in the phloem sap provides a short-term measure for stomatal conductance of European beech (Fagus sylvatica L.). Plant Cell Environ 26:1157–1168CrossRefGoogle Scholar
  28. Knohl A, Buchmann N (2005) Partitioning the net CO2 flux of a deciduous forest into respiration and assimilation using stable carbon isotopes. Global Biogeochem Cycles 19:GB4008CrossRefGoogle Scholar
  29. Knohl A, Schulze ED, Kolle O, Buchmann N (2003) Large carbon uptake by an unmanaged 250-year-old deciduous forest in Central Germany. Agric For Meteorol 118:151–167CrossRefGoogle Scholar
  30. Knohl A, Werner RA, Brand WA, Buchmann N (2005) Short-term variations in δ 13C of ecosystem respiration reveals link between assimilation and respiration in a deciduous forest. Oecologia 142:70–82PubMedCrossRefGoogle Scholar
  31. Kozlowski TT, Pallardy SG (1997) Growth control in woody plants. Academic, San Diego, 641 pGoogle Scholar
  32. Kramer H, Kätsch C (1982) Zum jahreszeitlichen Ablauf des sekundären Dickenwachstums im Kalkbuchenwald. Forstarchiv 53:87–93Google Scholar
  33. Leavitt SW (2002) Prospects for reconstruction of seasonal environment from tree-ring δ 13C: baseline findings from the Great Lakes area, USA. Chem Geol 191:47–58CrossRefGoogle Scholar
  34. Leavitt SW, Long A (1985) An atmospheric 13C/12C reconstruction generated through removal of climate effects from tree-ring 13C/12C measurements. Tellus 35B:92–102Google Scholar
  35. Leavitt SW, Long A (1991) Seasonal stable-iotope variability in tree rings: possible palaeoenvironmental signals. Chem Geol 87:59–70Google Scholar
  36. McCarrol D, Loader NJ (2004) Stable isotopes in tree rings. Quatern Sci Rev 23:771–801CrossRefGoogle Scholar
  37. McNulty SG, Swank WT (1995) Wood delta-C-13 as a measure of annual basal area growth and soil–water stress in a Pinus strobus forest. Ecology 76:1581–1586CrossRefGoogle Scholar
  38. Mund M (2004) Carbon pools of European beech forests (Fagus sylvatica) under different silvicultural management. Berichte des Forschungszentrums Waldökosysteme. Göttingen, Reihe A Bd 189, 226 pGoogle Scholar
  39. Polge H (1966) Etablissement des courbes de variation de la densite du bois par exploration densitometrique de radiographies d’echantillons preleves a la tariere sur des arbres vivants. Ann Sci For 23:3–115CrossRefGoogle Scholar
  40. Rinn F (1996) Tsap V 3.6 Reference manual: computer program for tree-ring analysis and presentation. Bierhelder Weg 20, D-69126, Heidelberg, Germany, 263 pGoogle Scholar
  41. Sass U, Eckstein D (1995) The variability of vessel size in beech (Fagus sylvatica L.) and its ecophysiological interpretation. Trees 9:247–252CrossRefGoogle Scholar
  42. Scarazzia A, Mata K, Matteucci G, Yakir D, Moscatello S, Brugnoli E (2004) Comparisons of δ 13C of photosynthetic products and ecosystem respiratory CO2 and their responses to seasonal climate variability. Oecologia 140:340–351PubMedCrossRefGoogle Scholar
  43. Schulze B, Wirth C, Linke P, Brand WA, Kuhlmann I, Horna V, Schulze E-D (2004) Laser-Ablation-Combustion-GC-IRMS—A new method for online analysis of intra-annual variation of δ 13C in tree-ring. Tree Physiol 24:1193–1201PubMedGoogle Scholar
  44. Schweingruber FH (1988) Tree-ring: Basics and applications of dendrochronology. Reidel. Publ., Dordrecht, 276 pGoogle Scholar
  45. Schweingruber FH, Briffa KR (1996) Tree-ring density for climate reconstruction. In: Jones PD, Raymond SV, Jouzel J (eds) Climatic variations and forcing mechanisms of the last 2000 years. Springer, Berlin Heidelberg New York, pp 43–66Google Scholar
  46. Shiyatov SG (1986) Dendrochronology of upper timberline in ural mountains. Nauka, Moscow, 136 pp (in Russian)Google Scholar
  47. Stuiver M, Burk RL, Quay PD (1984) C-13/C-12 Ratios in tree rings and the transfer of biospheric carbon to the atmosphere. J Geophys Res Atmosph 89:1731–1748Google Scholar
  48. Tang KL, Feng XH, Funkhouser G (1999) The delta C-13 of tree rings in full-bark and strip-bark bristlecone pine trees in the White Mountains of California. Global Change Biol 5:33–40CrossRefGoogle Scholar
  49. Vaganov EA (1990) The traheidogram method in tree-ring analysis and its application. In: Cook ER, Kairiuktis LA (eds.) Methods of dendrochronology. Application in the environmental sciences. Kluwer Academic Publisher, Dordrecht, The Netherlands, pp. 63–75Google Scholar
  50. Vaganov EA, Shashkin EA (2000) Growth and tree-ring structure of conifers. Nauka, Novosibirsk, 232 pp (in Russian)Google Scholar
  51. Vaganov EA, Shashkin AV, Sviderskaya IV, Vysotskaya LG (1985) Histometric analysis of woody plant growth. Nauka, Novosibirsk, 108 pp (in Russian)Google Scholar
  52. Vaganov EA, Shiyatov SG, Mazepa VS (1996) Dendroclimatic study in ural-Siberian subarctic. Nauka, Novosibirsk, 244 pp (in Russian)Google Scholar
  53. Warren CR, McGrath JF, Adams MA (2001) Water availability and carbon isotope discrimination in conifers. Oecologia 127:476–486CrossRefGoogle Scholar
  54. Wilson AT, Grinsted WA (1977) 12C/13C in cellulose and lignin as paleothermometers. Nature 265:133–135CrossRefGoogle Scholar
  55. Zahner R, Oliver WW (1962) The influence of thinning and pruning on the date of summerwood initiation in red and jack pines. For Sci 8:51–63Google Scholar

Copyright information

© Springer-Verlag 2006

Authors and Affiliations

  • M. V. Skomarkova
    • 1
  • E. A. Vaganov
    • 1
  • M. Mund
    • 2
  • A. Knohl
    • 2
    • 3
  • P. Linke
    • 2
  • A. Boerner
    • 2
  • E.-D. Schulze
    • 2
  1. 1.Institute of Forest SB RASAkademgorodokKrasnoyarskRussia
  2. 2.Max-Planck Institute for BiogeochemistryJenaGermany
  3. 3.ESPM DepartmentUniversity of CaliforniaBerkeleyUSA

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