The cascade of C:N:P stoichiometry in an ombrotrophic peatland: from plants to peat
Open accessAbstract
Northern peatlands are important carbon (C) sinks and while the patterns of C accumulation have been frequently investigated, nitrogen (N) and phosphorus (P) accumulation are often neglected. Here we link the C:N:P stoichiometry from foliar plant tissues, through senescent litters to peat, and determine C, N and P accumulation rates at Mer Bleue Bog, eastern Canada. Average C:N:P ratios changed from 794:17:1 in the foliar tissues to 911:10:1 in litter and 1285:32:1 in acrotelm peat. The increase in C:N and C:P ratios from mature to senescent tissues is related to nutrient resorption. The increase in C:P and N:P ratios in peat, which was contrary to that observed in Canadian forest soils, may be related to plant/mycorrhizae uptake of P. The long-term apparent rates of C, N and P accumulation were 29.5 ± 2.1 (SE) g C, 0.87 ± 0.01 g N and 0.017 ± 0.002 g P m −2 yr −1 , respectively. The significant correlation between the accumulation rates of N and P and that of C suggests more attention be placed on C:N:P stoichiometry in peatland biogeochemistry, in particular in understanding why C:P ratios are so large in the lower parts of the profile.
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Early Devonian coaly shales indicate extensive peatlands 410-400 Ma and have C/N of 44-119, comparable to modern peatlands where C/P ratios tend to increase with depth to C/P >3,000.
“Furthermore, Early Devonian coaly shales indicate extensive peatlands 410 -400 Ma and have C/N of 44 -119 (28), comparable to that in modern peatlands where N/P and C/P ratios tend to increase with depth to C/P > 3,000 (34).”
From Earliest land plants created modern levels of atmospheric oxygen (2016) · cites this paper as [34]
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- Authors
- Wang, M., Moore, T. R., Talbot, J., & Richard, P. J. H.
- Affiliations
- McGill University (CA)
- Université de Montréal (CA)
- Corresponding author
- Wang, Meng
- Venue
- Environmental Research Letters
- Publisher
- IOP Publishing
- Published
- 2014-01-01
- Volume
- 9
- Issue
- 2
- Pages
- 024003
- ISSN
- 1748-9326 (ISSN-L)
- OpenAlex
- W2147619265
- Cited by
- 65
- References
- 35
- Citations by year
- 2026: 3 · 2025: 2 · 2024: 5 · 2023: 4 · 2022: 12 · 2021: 7 · 2020: 3 · 2019: 6 · 2018: 7 · 2017: 4 · 2016: 5 · 2015: 2 · 2014: 5
- FWCI
- 4.64
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- Locations
- Environmental Research Letters (publishedVersion, cc-by)
- eScholarship@McGill (McGill) (submittedVersion)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion)
- eScholarship@McGill (McGill) (submittedVersion, cc-by)
- Topics
- Physical Sciences › Environmental Science › Ecology › Peatlands and Wetlands Ecology
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Climate change and permafrost
- Keywords
- C:N:P stoichiometry, ombrotrophic peatlands, peat formation, nutrient resorption, phosphorus accumulation, nitrogen accumulation, carbon accumulation, Mer Bleue bog, peatland carbon sink
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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