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handle: 10261/61098
[EN] Allocation of photosynthates to defence responses at the expense of biomass increase is a common strategy amongst plants to cope with stress factors. Trees reduce the spread of decay by creating a secondary metabolite-rich reaction zone as fungal ingresses the sapwood. Reaction zone formation implies a sacrificial conversion of sapwood, thus, as decay progresses, the sapwood area of the tree is reduced. The relative contribution that reaction-zone formation and sapwood loss make to radial growth decrease is unclear. To answer this question we reconstructed radial-growth patterns in 100 Norway spruce (. Picea abies) trees with a range of reaction zone and sapwood disruption. Basal area increment (BAI) between 1960 and 2007 and its relationship with sapwood reduction and reaction zone formation was assessed using structural equation models (SEM). BAI data showed that over 10. years, trees with small or no decay columns (<40%) and a reaction zone shifted from a growth rate that was similar to trees without a reaction zone towards low growth rate similar to trees with large decay columns. The fitted SEM indicated that: (i) the effects of decay on growth would begin with the formation of the reaction zone, and (ii) the smaller sapwood in decayed trees as compared with healthy trees would not reduce radial growth, but would be in part the result of previous periods of low growth due to reaction-zone formation. © 2012 Elsevier B.V..
We are thankful to Stora Enso who provided the plots for the experiment. Carmen Romeralo and Heriberto Vélëz contributed to the field work. This research was partially funded by the project ‘Future Forests’, financed by the MISTRA Foundation for Strategic Research. Jonàs Oliva was funded by the post-doctoral grant 2008 BP A 00013 from the DURSI-GENCAT. J. Julio Camarero thanks the support of ARAID. We thank G. Sanguesa-Barreda for measuring tree rings. Comments and suggestions by two anonymous referees are greatly appreciated.
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