Mineral Stabilization Slows Losses of Peatland Carbon Following Long-Term Drainage for Agriculture.

Authors

Katy J Faulkner, Katerina Georgiou, David A Coomes, Philippa Ascough, Anna Basford, Rodney G O Burton, Romy Copley, Emma Keerberg, Alanie Lapina, Kimber Moreland, Christopher Evans, Ross Morrison, Adam F A Pellegrini

Published in

Global change biology. Volume 32. Issue 7. Pages e70985.

Abstract

Cultivated peatlands are a major CO₂ emission source, but the processes that regulate the decomposition of drained peat are debated, especially as drained peat becomes increasingly shallow. Many cultivated peatlands are underlain by a mineral soil layer. Surface subsidence, oxidation and tillage reduce the peat thickness, which intermixes peat with minerals as peat is lost. A key question is whether this mixing can reduce emissions by making soil organic carbon (SOC) more stable by transforming particulate organic carbon (POC)-which dominates the carbon stock in deep drained peatlands and is readily accessible to microbial decomposers-into mineral-associated organic carbon (MAOC), which is less accessible to decomposers. To explore this question, we surveyed ten sites across the East Anglian Fens in England, a once extensive (~3900 km²) peatland landscape that has been drained for cultivation since the mid-seventeenth century. We used variation in cultivation to establish a peat loss gradient to evaluate how topsoil SOC (0-40 cm) and its forms change as peat is lost. As the peat was lost, the soils became rich in minerals (rising from 46% to 88% silt+clay content), resulting in an initial 11-fold rise in newly-formed MAOC, but a monotonic decline and near-total loss of POC. POC turnover times were 3158 ± 62 years, indicative of peat, and POC was always older than MAOC; consequently, microbially-processed peat along with gradual contributions of recently fixed carbon were sources of MAOC. A four-month laboratory incubation showed that the MAOC:POC ratio was negatively correlated with respiration. We conclude that long-term carbon retention via MAOC formation has the potential to reduce carbon loss from degraded, mineral-mixed peatlands. However, because this MAOC pool is itself vulnerable to loss under continued agricultural drainage, this mechanism is expected to slow rather than halt long-term soil carbon loss from drained peatlands.

PMID:
42422978
Bibliographic data and abstract were imported from PubMed on 09 Jul 2026.

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