No Long‐Term Decay in α‐Cellulose of Living and Relict Trees From the European Alps Over the Past 8,000 years

Abstract Tree‐ring α‐cellulose stable isotopes of living trees and dead woods are increasingly used for high‐resolution paleoclimate reconstructions spanning centuries to millennia. However, the potential effects of wood decay on α‐cellulose content (CC) and the composition of tree‐ring stable isotopes remain largely unexplored. Here, we present α‐cellulose content measurements from relict and living trees in the European Alps spanning the past 8,000 years. This study addresses whether preservation context alters the isotopic integrity of α‐cellulose. We assess the temporal stability of CC, its dependence on tree species, preservation conditions and wood type (subfossil, dry dead, living), as well as its relationship with α‐cellulose stable carbon, oxygen, and hydrogen isotopes (δ 13 C, δ 18 O, δ 2 H). Our results show that α‐cellulose remains stable over millennia under alpine conditions. Our results not only confirm the suitability of relict wood for tree‐ring stable isotopic analysis and paleoclimate reconstructions, but also provide insights for the improvement of global carbon cycle models.

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Publication Details

Journal
Paleoceanography and Paleoclimatology
Published
2025-09-26
DOI
https://doi.org/10.1029/2025pa005170
Citations
1
Primary Topic
Archaeology and ancient environmental studies
Type
article
Field-Weighted Citation Impact
4.33

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article

No Long‐Term Decay in α‐Cellulose of Living and Relict Trees From the European Alps Over the Past 8,000 years

Valentina Vitali, Ulf Büntgen, Kurt Nicolussi, Tito Arosio et al.
1 citations
Paleoceanography and Paleoclimatology
Archaeology and ancient environmental studies
4.33
article

No Long‐Term Decay in α‐Cellulose of Living and Relict Trees From the European Alps Over the Past 8,000 years

Valentina Vitali, Ulf Büntgen, Kurt Nicolussi, Tito Arosio, Markus Leuenberger, Matthias M Saurer, Tatiana Bebchuk, Agata Buchwał
article en
1 citations

Abstract

Abstract Tree‐ring α‐cellulose stable isotopes of living trees and dead woods are increasingly used for high‐resolution paleoclimate reconstructions spanning centuries to millennia. However, the potential effects of wood decay on α‐cellulose content (CC) and the composition of tree‐ring stable isotopes remain largely unexplored. Here, we present α‐cellulose content measurements from relict and living trees in the European Alps spanning the past 8,000 years. This study addresses whether preservation context alters the isotopic integrity of α‐cellulose. We assess the temporal stability of CC, its dependence on tree species, preservation conditions and wood type (subfossil, dry dead, living), as well as its relationship with α‐cellulose stable carbon, oxygen, and hydrogen isotopes (δ 13 C, δ 18 O, δ 2 H). Our results show that α‐cellulose remains stable over millennia under alpine conditions. Our results not only confirm the suitability of relict wood for tree‐ring stable isotopic analysis and paleoclimate reconstructions, but also provide insights for the improvement of global carbon cycle models.

Paleoceanography and PaleoclimatologyVol. 40(10)
University of Bern (CH), Oeschger Centre for Climate Change Research (CH), University of Arizona (US), Universität Innsbruck (AT), Masaryk University (CZ), University of Cambridge (GB), Swiss Federal Institute for Forest, Snow and Landscape Research (CH), Institute of Forest Ecology of the Slovak Academy of Sciences (SK), Czech Academy of Sciences, Global Change Research Institute (CZ), Adam Mickiewicz University in Poznań (PL)
National Science Foundation, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Austrian Science Fund
Openalex Percentile: Top 6%
Archaeology and ancient environmental studies
4.33
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