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BG | Articles | Volume 17, issue 19
Biogeosciences, 17, 4871–4882, 2020
https://doi.org/10.5194/bg-17-4871-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 17, 4871–4882, 2020
https://doi.org/10.5194/bg-17-4871-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 13 Oct 2020

Research article | 13 Oct 2020

Alpine Holocene tree-ring dataset: age-related trends in the stable isotopes of cellulose show species-specific patterns

Tito Arosio et al.

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Cited articles

Anderson, W. T., Sternberg, L., Pinzon, M., Gann-Troxler, T., Childers, D. L., and Duever, M.: Carbon isotopic composition of cypress trees from South Florida and changing hydrologic conditions, Dendrochronologia. 23, 1–10, https://doi.org/10.1016/j.dendro.2005.07.006, 2005. 
Arosio, T., Ziehmer M. M., Nicolussi K., Schlüchter C., and Leuenberger M.: Larch cellulose is significantly depleted in deuterium isotopes with respect to evergreen conifers, Front. Earth Sci., submitted, 2020. 
Bräker, O.U.: Der Alterstrend bei Jahrringdichten und Jahrringbreiten von Nadelhölzern und sein Ausgleich, Mitteilungen der forstlichen Bundesversuchsanstalt Wien, 142, 75–102, 1981. 
Brienen, R.J.W., Gloor, E., Clerici, S., Newton, R., Arppe, L., Boom, A., Bottrell, S., Callaghan, M., Heaton, T., Helama, S., and Helle, G.: Tree height strongly affects estimates of water-use efficiency responses to climate and CO2 using isotopes, Nat. Commun., 8, 1–10, https://doi.org/10.1038/s41467-017-00225-z, 2017. 
Coplen, T.B.: Reporting of stable hydrogen, carbon, and oxygen isotopic abundances (technical report), Pure Appl. Chem., 66, 273–276, https://doi.org/10.1351/pac199466020273, 1994. 
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Stable isotopes in tree-ring cellulose are tools for climatic reconstructions, but interpretation is challenging due to nonclimate trends. We analyzed the tree-age trends in tree-ring isotopes of deciduous larch and evergreen cembran pine. Samples covering the whole Holocene were collected at the tree line in the Alps. For cambial ages over 100 years, we prove the absence of age trends in δD, δ18O, and δ13C for both species. For lower cambial ages, trends differ for each isotope and species.
Stable isotopes in tree-ring cellulose are tools for climatic reconstructions, but...
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