Skip to main navigation Skip to search Skip to main content

C-PEAT's global peatland carbon database (v.2025)

  • Julie Loisel*
  • , Angela Gallego-Sala
  • , Daniela Ransby
  • , Emily Rabel
  • , Cornelia Behrens
  • , Stefanie Schumacher
  • , Kathe Todd-Brown
  • , Vaasuki Marupaka
  • , Atte Korhola
  • , Alexandre Lamarre
  • , Barbara Fialkiewicz-Koziel
  • , Bas van Geel
  • , Christopher Bochicchio
  • , Charles Tarnocai
  • , David Anderson
  • , Dan Hammarlund
  • , David Large
  • , Dmitri Mauquoy
  • , Dorothy Peteet
  • , Dale Vitt
  • Dan Charman, David Beilman, Edgar Karofeld, Eric Klein, Eeva Stiina Tuittila, Frank Chambers, François De Vleeschouwer, Fraser Mitchell, Gael Le Roux, Gabriel Magnan, Gunnar Mallon, Glen MacDonald, Graeme Swindles, Ilka Bauer, Colin Prentice, Jukka Alm, Joan Bunbury, James Holmquist, Julia McCarroll, Jonathan Nichols, Andres Christen, Keith Barber, Liisa Ukonmaanaho, Lisa Belyea, Matthew Amesbury, Maarten Blaauw, Paul Hughes, Stephen Jackson, Patrick Moss, Yan Zhao, C-Peat Working Group Members
*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

8 Downloads (Pure)

Abstract

Field-based measurements are foundational to the study of short- and long-term peatland carbon dynamics. For decades, the scientific community has amassed hundreds of valuable empirical datasets in the form of peat core records from around the world. Those records typically include peat depth, basal age, peat organic matter content, peat dry bulk density, peat organic density, and/or carbon and nitrogen content. Once combined with chronological constraints and models, peat core time series can be used to estimate changes in peat-carbon accumulation rates through time. Consolidating these peat records can help improve global peat-carbon stock estimates and quantifications of past, present, and future greenhouse gas exchanges between peatlands and the atmosphere. Large-scale synthesis can also shed light on the sensitivity of peat-carbon accumulation processes to climate change and provide context for current and future global environmental change. We can also use spatial and temporal peat data to inform, validate, and benchmark existing models that include peatland representations. This paper presents the first formal version of PAGES' C-PEAT Global Peatland Carbon Database (GD), which is available for download in the PANGAEA and International Soil Carbon Network (ISCN) data repositories. The C-PEAT GD contains 267 independently catalogued peat cores and a large number of observations from those cores, including: peat depths, organic matter content values, dry bulk density values, organic density values, as well as carbon and nitrogen content values. Raw and calibrated chronological data are included for each individual dataset when available. The metadata fields are easily searchable and interoperable, as per PANGAEA's standards. The main objective of this article is to describe the structure and content of the database, itself aimed at increasing the use, assimilation, and interoperability of peat-core data across disciplines. The C-PEAT GD can be accessed at the PANGAEA data repository (10.1594/PANGAEA.986891; Loisel et al., 2025).

Original languageEnglish
Pages (from-to)6485-6502
Number of pages18
JournalEarth System Science Data
Volume18
Issue number9
DOIs
Publication statusPublished - 07 Sept 2026

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action

ASJC Scopus subject areas

  • General Earth and Planetary Sciences

Fingerprint

Dive into the research topics of 'C-PEAT's global peatland carbon database (v.2025)'. Together they form a unique fingerprint.

Cite this