The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here: https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

Johannes Edvardsson

Johannes Edvardsson

Researcher

Johannes Edvardsson

Peatland trees record strong and temporally stable hydroclimate information in tree-ring δ13C and δ18O

Author

  • Karolina Janecka
  • Kerstin Treydte
  • Silvia Piccinelli
  • Loïc Francon
  • Marçal Argelich Ninot
  • Johannes Edvardsson
  • Christophe Corona
  • Veiko Lehsten
  • Markus Stoffel

Summary, in English

Peatland trees are valuable archives of paleoclimatic information; however, gaps persist in understanding the relationships between tree growth, peatland hydrology, and hydroclimate variables. While previous research in peatlands has mainly focused on tree-ring widths (TRW), yielding inconclusive results, the potential of stable carbon (δ13C) and oxygen (δ18O) isotopes in tree rings remains unexplored. In this study, we develop TRW, δ13C, and δ18O chronologies of Scots pine trees located in a Swedish peatland and a reference site on bedrock with a mineral soil layer. We assess their responses to hydroclimate conditions and evaluate their potential for reconstructing hydroclimate variations. Our findings show significant differences in mean TRW and δ13C values between the peatland and reference sites. Moreover, while TRWs do not exhibit distinct common patterns between sites, both δ13C and δ18O site chronologies show uniform year-to-year variations across all sites. Some discrepancies for TRW and δ13C site chronologies emerge, however, regarding multi-decadal trends. While the climate sensitivity of TRW is weak and non-homogenous, the δ13C and δ18O peatland and reference chronologies contain robust and consistent signals, with a maximum sensitivity to water table, precipitation, and vapor pressure deficit (VPD) variations during summer. Both δ13C and δ18O chronologies show stable relationships with three key hydroclimate variables over time. In conclusion, while TRWs from living peatland pines at our sites have limited potential to record high-frequency hydroclimate information, δ13C and δ18O chronologies can serve as excellent proxies for the reconstruction of past hydroclimate changes.

Department/s

  • BECC: Biodiversity and Ecosystem services in a Changing Climate
  • Department of Geology
  • Dept of Physical Geography and Ecosystem Science
  • MERGE: ModElling the Regional and Global Earth system

Publishing year

2025-10

Language

English

Pages

1679-1697

Publication/Series

Climate of the Past

Volume

21

Issue

10

Document type

Journal article

Publisher

Copernicus GmbH

Topic

  • Climate Science
  • Palaeontology and Palaeoecology

Status

Published

ISBN/ISSN/Other

  • ISSN: 1814-9324