Tree species affect the vertical distribution of soil organic carbon and total nitrogen
- Author
- Christina Steffens, Christian Beer, Stephanie Schelfhout (UGent) and Lars Vesterdal
- Organization
- Abstract
- Background Forest soils are considered sinks for atmospheric C. Many studies revealed that tree species and their mycorrhizal association affect forest floor and topsoil organic C (OC) and total N, while the knowledge of their effect on subsoil OC and N is still scarce. Aims We aimed to identify (1) tree species and mycorrhizal association effects on forest floor, topsoil (0-30 cm) and subsoil (30-80 cm) OC and N stocks and vertical distribution and (2) drivers for soil OC and N distribution. Methods We sampled forest floor, topsoil and subsoil under Fagus sylvatica L., Quercus robur L., Acer pseudoplatanus L. and Fraxinus excelsior L. in four Danish common garden experiments along a gradient in soil texture and determined OC and N stocks. Results Total N (forest floor + soil) was higher under oak than beech, while total OC was unaffected by species. Forest floor C and N were higher under oak and beech, both ectomycorrhizal species (ECM), compared to under maple and ash, which are both arbuscular mycorrhizal species (AM). Relatively more OC and N were transferred to the topsoil under AM than ECM species, and this could be explained by greater endogeic earthworm biomass in AM species. In contrast, a higher proportion of OC was stored under ECM than AM species in the subsoil, and here OC correlated negatively with anecic earthworms. Subsoil N was highest under oak. Conclusions Tree species and in particular their mycorrhizal association affected the vertical distribution of soil OC and N. Tree species differences in topsoil OC and N were not mirrored in the subsoil, and this highlights the need to address the subsoil in future studies on AM- versus ECM-mediated soil OC and N stocks.
- Keywords
- broadleaved tree species, earthworms, forest floor, mycorrhizal association, soil pH, temperate forest, LITTER DECOMPOSITION, MINERAL SOIL, LEAF-LITTER, STOCKS, TEMPERATE, MATTER, STABILIZATION, MECHANISMS, FRAMEWORK, TURNOVER
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Citation
Please use this url to cite or link to this publication: http://hdl.handle.net/1854/LU-8768109
- MLA
- Steffens, Christina, et al. “Tree Species Affect the Vertical Distribution of Soil Organic Carbon and Total Nitrogen.” JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, vol. 185, no. 6, 2022, pp. 864–75, doi:10.1002/jpln.202200165.
- APA
- Steffens, C., Beer, C., Schelfhout, S., & Vesterdal, L. (2022). Tree species affect the vertical distribution of soil organic carbon and total nitrogen. JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, 185(6), 864–875. https://doi.org/10.1002/jpln.202200165
- Chicago author-date
- Steffens, Christina, Christian Beer, Stephanie Schelfhout, and Lars Vesterdal. 2022. “Tree Species Affect the Vertical Distribution of Soil Organic Carbon and Total Nitrogen.” JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE 185 (6): 864–75. https://doi.org/10.1002/jpln.202200165.
- Chicago author-date (all authors)
- Steffens, Christina, Christian Beer, Stephanie Schelfhout, and Lars Vesterdal. 2022. “Tree Species Affect the Vertical Distribution of Soil Organic Carbon and Total Nitrogen.” JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE 185 (6): 864–875. doi:10.1002/jpln.202200165.
- Vancouver
- 1.Steffens C, Beer C, Schelfhout S, Vesterdal L. Tree species affect the vertical distribution of soil organic carbon and total nitrogen. JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE. 2022;185(6):864–75.
- IEEE
- [1]C. Steffens, C. Beer, S. Schelfhout, and L. Vesterdal, “Tree species affect the vertical distribution of soil organic carbon and total nitrogen,” JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, vol. 185, no. 6, pp. 864–875, 2022.
@article{8768109,
abstract = {{Background Forest soils are considered sinks for atmospheric C. Many studies revealed that tree species and their mycorrhizal association affect forest floor and topsoil organic C (OC) and total N, while the knowledge of their effect on subsoil OC and N is still scarce. Aims We aimed to identify (1) tree species and mycorrhizal association effects on forest floor, topsoil (0-30 cm) and subsoil (30-80 cm) OC and N stocks and vertical distribution and (2) drivers for soil OC and N distribution. Methods We sampled forest floor, topsoil and subsoil under Fagus sylvatica L., Quercus robur L., Acer pseudoplatanus L. and Fraxinus excelsior L. in four Danish common garden experiments along a gradient in soil texture and determined OC and N stocks. Results Total N (forest floor + soil) was higher under oak than beech, while total OC was unaffected by species. Forest floor C and N were higher under oak and beech, both ectomycorrhizal species (ECM), compared to under maple and ash, which are both arbuscular mycorrhizal species (AM). Relatively more OC and N were transferred to the topsoil under AM than ECM species, and this could be explained by greater endogeic earthworm biomass in AM species. In contrast, a higher proportion of OC was stored under ECM than AM species in the subsoil, and here OC correlated negatively with anecic earthworms. Subsoil N was highest under oak. Conclusions Tree species and in particular their mycorrhizal association affected the vertical distribution of soil OC and N. Tree species differences in topsoil OC and N were not mirrored in the subsoil, and this highlights the need to address the subsoil in future studies on AM- versus ECM-mediated soil OC and N stocks.}},
author = {{Steffens, Christina and Beer, Christian and Schelfhout, Stephanie and Vesterdal, Lars}},
issn = {{1436-8730}},
journal = {{JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE}},
keywords = {{broadleaved tree species,earthworms,forest floor,mycorrhizal association,soil pH,temperate forest,LITTER DECOMPOSITION,MINERAL SOIL,LEAF-LITTER,STOCKS,TEMPERATE,MATTER,STABILIZATION,MECHANISMS,FRAMEWORK,TURNOVER}},
language = {{eng}},
number = {{6}},
pages = {{864--875}},
title = {{Tree species affect the vertical distribution of soil organic carbon and total nitrogen}},
url = {{http://doi.org/10.1002/jpln.202200165}},
volume = {{185}},
year = {{2022}},
}
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