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TitrePuzzling Zn isotopes in spruce tree-ring series
AuteurDinis, L; Gammon, P; Savard, M M; Bgin, C; Girard, I; Vaive, J
SourceChemical Geology vol. 476, 2018 p. 171-179, https://doi.org/10.1016/j.chemgeo.2017.11.015
Année2018
Séries alt.Ressources naturelles Canada, Contribution externe 20182080
ÉditeurElsevier B.V.
Documentpublication en série
Lang.anglais
DOIhttps://doi.org/10.1016/j.chemgeo.2017.11.015
Mediapapier; en ligne; numérique
ProgrammeDéveloppement durable des sables bitumineux, Géosciences de l'environnement
Résumé(disponible en anglais seulement)
Zinc (Zn) isotopes have shown promise for investigating biogeochemical processes and tracing sources of Zn for environmental studies. This study, the first in its kind, investigates Zn isotopic ratios in tree rings and soils of two sites in the Northern Athabasca Oil Sands Region (NAOSR) of Alberta, Canada. To this end, we have developed an appropriate protocol to analyze tree-ring ?66Zn values by pooling year-equivalent tree rings of four individual trees for both sites. The results of combined tree-ring Zn concentrations show minimal variation in heartwood, with a statistically significant decrease after 1979 and 1986 for site 1 and site 2, respectively. For site 1, tree-ring ?66ZnJMC Lyon ratios vary between 0.83 ± 0.08 to 0.54 ± 0.07ä with a statistically significant decrease from 1877 to 2008. For site 2, ?66ZnJMC Lyon ratios range from 0.78 ± 0.02 to 0.59 ± 0.07ä with the lowest values obtained for the outermost ring closest to the bark. However, this site does not display statistically significant long-term trend. In comparison to the tree rings, adsorbed Zn within soil organic horizons is relatively enriched in heavy isotopes (?66ZnJMC Lyon of 1.00 ± 0.20 to 1.12 ± 0.10 and 0.81 ± 0.10 to 0.86 ± 0.06ä for sites 1 and 2, respectively). Tree-ring and soil organic horizons ?66Zn values are also substantially heavier than the value reported for adsorbed Zn in NAOSR tailing sands (?66ZnJMC Lyon = 0.35 ± 0.06ä). The heavy signature in the organic horizons may be a product of Zn biogeochemical cycling through soil processes and uptake by trees, although Zn atmospheric deposition from the NAOSR cannot be discounted. On the other hand, tree physiological processes, particularly radial translocation, could have potentially influenced the studied tree-ring Zn concentration and isotopic characteristics. However, this mechanism has not received substantial research. The ?66Zn analyses in different wood components are required before its influence on ?66Zn values can be properly assessed and tree-ring ?66Zn can be used as environmental indicators. © 2017
GEOSCAN ID310628