A Retrospective Isotopic Study of Spruce Decline in the Vosges Mountains (France)
2003
Poszwa, Anne | Wickman, Tonie | Dambrine, Etienne | Ferry, Bruno | Dupouey, Jean-Luc | Helle, Gerdhard | Schleser, Gerdhard | Bréda, Nathalie | Institut National de la Recherche Agronomique (INRA) | KTH Royal Institute of Technology [Stockholm] (KTH) | Laboratoire d'Etudes des Ressources Forêt-Bois (LERFoB) ; Institut National de la Recherche Agronomique (INRA)-AgroParisTech | Ecologie et Ecophysiologie Forestières [devient SILVA en 2018] (EEF) ; Institut National de la Recherche Agronomique (INRA)-Université de Lorraine (UL) | Institut für Chemie und Dynamik der Geosphäre - Troposphäre (ICG-2) ; Forschungszentrum Jülich GmbH | Centre de recherche de Jülich | Jülich Research Centre (FZJ) ; Helmholtz-Gemeinschaft = Helmholtz Association-Helmholtz-Gemeinschaft = Helmholtz Association
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Mostrar más [+] Menos [-]Inglés. The objective of this study was to assess the time variation of mineral and water stress levels across the life of a declining, Mg-deficient, spruce stand, in order to clarify the factors that caused the decline. Since 1985, strong soil acidification linked to a large leaching of nitrate and base cations was measured at the study site. In 1994, 5 trees were felled and tree rings were measured and analysed for Ca, Mg, K, Sr, 13 C/ 12 C and 87 Sr/ 86 Sr isotopic ratios. Strontium pools and fluxes as well as root Sr isotope ratio in relation to depth were also measured. Wood chemical concentrations and isotope ratios were strongly related to the dominance status of each tree. On average during the study period, the 87 Sr/ 86 Sr ratio of spruce wood decreased. Using a mechanistic model computing long term variations of 87 Sr/ 86 Sr ratio in trees and soils, we reproduced the observed trend by simulating soil acidification-increasing Sr drainage from the whole profile, and particularly from the organic horizon-, and root uptake becoming more superficial with time. Between 1952 and 1976, tree ring 13 C decreased strongly and continuously, which, in addition to other factors, might be related to an increase in water stress. Thus, a decrease in rooting depth, possibly related to soil acidification, appeared as a possible cause for the long term increase in water stress. The extreme drought event of 1976 appears to have revealed and triggered the decline.
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