Limited recovery of soil organic matter composition in fen peatlands after rewetting
| Authors |
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|---|---|
| Publication date | 01-2026 |
| Journal | Geoderma |
| Article number | 117646 |
| Volume | Issue number | 465 |
| Number of pages | 13 |
| Organisations |
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| Abstract |
Approximately half of Europe’s peatlands have been extensively drained
for agriculture, forestry, and peat extraction, with lowland fens
disproportionately affected due to their high nutrient availability and
productivity post-drainage. Peatland rewetting has gained importance as a
strategy to mitigate carbon losses and restore biodiversity; however,
its effectiveness in reestablishing below-ground processes remains
uncertain. Soil organic matter (SOM) dynamics play a crucial role in
peatland restoration outcomes, influencing peat structural integrity and
hydrological properties, as well as the availability of substrates and
nutrients for microbial and plant communities. Here, we present a
Europe-wide assessment of the effects of fen drainage and rewetting on
SOM molecular composition, analyzing fens with contrasting hydrological
status (undrained, drained, and rewetted) across three depths (0 − 5,
15 − 20, and 45 − 50 cm) using pyrolysis–gas chromatography/mass
spectrometry (Py-GC/MS). Despite considerable variability induced by
site-specific heterogeneity, the molecular composition of undrained fens
clearly reflected the dominant contributions of sedges, grasses, and
brown mosses to peat formation in fens, with characteristic
stratification. Drainage consistently led to a decline in components
from plant biopolymers (carbohydrates and lignins) across sites, and an
increase in microbially altered compounds (N-compounds, benzenes, and
aliphatics), with the most pronounced effects at intermediate depths
(15 − 20 cm). Rewetting partially reversed these alterations, with some
fens exhibiting a shift in molecular composition reverting toward
undrained conditions, particularly in sites rewetted for longer periods.
However, significant differences remained between rewetted and
undrained fens. Our findings suggest that while rewetting over time can
facilitate partial recovery of carbon dynamics, the below-ground legacy
of drainage-induced alterations can persist, at least for a timescale of
several decades.
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| Document type | Article |
| Note | With supplementary file. |
| Language | English |
| Published at | https://doi.org/10.1016/j.geoderma.2025.117646 |
| Downloads |
1-s2.0-S0016706125004872-main
(Final published version)
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| Supplementary materials | |
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