The DOI matches its Crossref record; 87 of the 87 references it cites were found in a registry or an index.
Rhizosphere processes are quantitatively important components of terrestrial carbon and nutrient cycles
Abstract
While there is an emerging view that roots and their associated microbes actively alter resource availability and soil organic matter (SOM) decomposition, the ecosystem consequences of such rhizosphere effects have rarely been quantified. Using a meta‐analysis, we show that multiple indices of microbially mediated C and nitrogen (N) cycling, including SOM decomposition, are significantly enhanced in the rhizospheres of diverse vegetation types. Then, using a numerical model that combines rhizosphere effect sizes with fine root morphology and depth distributions, we show that root‐accelerated mineralization and priming can account for up to one‐third of the total C and N mineralized in temperate forest soils. Finally, using a stoichiometrically constrained microbial decomposition model, we show that these effects can be induced by relatively modest fluxes of root‐derived C, on the order of 4% and 6% of gross and net primary production, respectively. Collectively, our results indicate that rhizosphere processes are a widespread, quantitatively important driver of SOM decomposition and nutrient release at the ecosystem scale, with potential consequences for global C stocks and vegetation feedbacks to climate.
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Cites
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Kuzyakov, Y., Friedel, J. K., & Stahr, K. (2000) · Soil Biology and Biochemistry · doi:10.1016/s0038-0717(00)00084-5 · Cited by 3,040
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Jones, D. L. (1998) · Plant and Soil · doi:10.1023/a:1004356007312 · Cited by 2,439
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Fontaine, S., Barot, S., Barré, P., Bdioui, N., Mary, B., & Rumpel, C. (2007) · Nature · doi:10.1038/nature06275 · Cited by 2,279
Priming effects: Interactions between living and dead organic matter
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Large-scale forest girdling shows that current photosynthesis drives soil respiration
Högberg, P., Nordgren, A., Buchmann, N., Taylor, A. F. S., Ekblad, A., Högberg, M. N., Nyberg, G., Ottosson-Löfvenius, M., & Read, D. J. (2001) · Nature · doi:10.1038/35081058 · Cited by 1,868
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Life and death in the soil microbiome: how ecological processes influence biogeochemistry
Sokol, N. W., Slessarev, E., Marschmann, G. L., Nicolas, A., Blazewicz, S. J., Brodie, E. L., Firestone, M. K., Foley, M. M., Hestrin, R., Hungate, B. A., et al. (2022) · Nature Reviews Microbiology · doi:10.1038/s41579-022-00695-z · Cited by 1,179
Microbial formation of stable soil carbon is more efficient from belowground than aboveground input
Sokol, N. W., & Bradford, M. A. (2019) · Nature Geoscience · doi:10.1038/s41561-018-0258-6 · Cited by 891
Sokol, N. W., Kuebbing, S. E., Karlsen‐Ayala, E., & Bradford, M. A. (2019) · New Phytologist · doi:10.1111/nph.15361 · Cited by 631
Biogeochemical cycles and biodiversity as key drivers of ecosystem services provided by soils
Smith, P., Cotrufo, M. F., Rumpel, C., Paustian, K., Kuikman, P. J., Elliott, J. A., McDowell, R., Griffiths, R. I., Asakawa, S., Bustamante, M., et al. (2015) · SOIL · doi:10.5194/soil-1-665-2015 · Cited by 532
Controls and Adaptive Management of Nitrification in Agricultural Soils
Norton, J., & Ouyang, Y. (2019) · Frontiers in Microbiology · doi:10.3389/fmicb.2019.01931 · Cited by 404
Metadata
- Authors
- Finzi, A. C., Abramoff, R. Z., Spiller, K. S., Brzostek, E. R., Darby, B. A., Kramer, M. A., & Phillips, R. P.
- Venue
- Global Change Biology
- Publisher
- Wiley
- Published
- 2015-01-28
- Volume
- 21
- Issue
- 5
- Pages
- 2082-2094
- ISSN
- 1354-1013 (ISSN-L)
- 1365-2486
- OpenAlex
- W2162844667
- Cited by
- 630
- References
- 87
- FWCI
- 35.45
- Type
- journal article
- Language
- en
- Open access
- closed
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- Finzi, A. C., Abramoff, R. Z., Spiller, K. S., Brzostek, E. R., Darby, B. A., Kramer, M. A., & Phillips, R. P. (2015). Rhizosphere processes are quantitatively important components of terrestrial carbon and nutrient cycles. Global Change Biology. https://doi.org/10.1111/gcb.12816
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