Abstract
Global warming is predicted to be most pronounced at high latitudes, and observational evidence over the past 25 years suggests that this warming is already under way1. One-third of the global soil carbon pool is stored in northern latitudes2, so there is considerable interest in understanding how the carbon balance of northern ecosystems will respond to climate warming3,4. Observations of controls over plant productivity in tundra and boreal ecosystems5,6 have been used to build a conceptual model of response to warming, where warmer soils and increased decomposition of plant litter increase nutrient availability, which, in turn, stimulates plant production and increases ecosystem carbon storage6,7. Here we present the results of a long-term fertilization experiment in Alaskan tundra, in which increased nutrient availability caused a net ecosystem loss of almost 2,000 grams of carbon per square meter over 20 years. We found that annual aboveground plant production doubled during the experiment. Losses of carbon and nitrogen from deep soil layers, however, were substantial and more than offset the increased carbon and nitrogen storage in plant biomass and litter. Our study suggests that projected release of soil nutrients associated with high-latitude warming may further amplify carbon release from soils, causing a net loss of ecosystem carbon and a positive feedback to climate warming.
This is a preview of subscription content, access via your institution
Relevant articles
Open Access articles citing this article.
-
Continuous decrease in soil organic matter despite increased plant productivity in an 80-years-old phosphorus-addition experiment
Communications Earth & Environment Open Access 12 July 2023
-
A globally relevant stock of soil nitrogen in the Yedoma permafrost domain
Nature Communications Open Access 14 October 2022
-
Permafrost cooled in winter by thermal bridging through snow-covered shrub branches
Nature Geoscience Open Access 07 July 2022
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Rent or buy this article
Prices vary by article type
from$1.95
to$39.95
Prices may be subject to local taxes which are calculated during checkout


References
Serreze, M. C. Observational evidence of recent change in the northern high-latitude environment. Clim. Change 46, 159–207 (2000)
Gorham, E. Northern peatlands: role in the carbon cycle and probable response to climatic warming. Ecol. Appl. 1, 182–195 (1991)
Oechel, W. C. et al. Acclimation of ecosystem CO2 exchange in the Alaskan Arctic in response to decadal climate warming. Nature 406, 978–981 (2000)
Goulden, M. L. et al. Sensitivity of boreal forest carbon balance to soil thaw. Science 279, 214–217 (1997)
Chapin, F. S. I., Shaver, G. R., Giblin, A. E., Nadelhoffer, K. J. & Laundre, J. A. Responses of arctic tundra to experimental and observed changes in climate. Ecology 76, 694–711 (1995)
Hobbie, S. E., Nadelhoffer, K. J. & Hogberg, P. A synthesis: The role of nutrients as constraints on carbon balances in boreal and arctic regions. Plant Soil 242, 163–170 (2002)
Shaver, G. R. et al. Global change and the carbon balance of the ecosystem. Bioscience 42, 433–442 (1992)
Nadelhoffer, K. J., Giblin, A. E., Shaver, G. R. & Laundre, J. A. Effects of temperature and substrate quality on element mineralization in six arctic soils. Ecology 72, 242–253 (1990)
Hobbie, S. E. Temperature and plant species control over litter decomposition in Alaskan tundra. Ecol. Monogr. 66, 503–522 (1996)
Vitousek, P. M. Nutrient cycling and nutrient use efficiency. Am. Nat. 119, 553–572 (1982)
Hobbie, S. E., Schimel, J. P., Trumbore, S. E. & Randerson, J. R. A mechanistic understanding of carbon storage and turnover in high-latitude soils. Glob. Change Biol. 6, 196–210 (2000)
Berg, N. & Matzner, E. Effect of N deposition on decomposition of plant litter and soil organic matter in forest systems. Environ. Rev. 5, 1–25 (1997)
Neff, J. C. et al. Variable effects of nitrogen additions on the stability and turnover of soil carbon. Nature 419, 915–917 (2002)
Dixon, R. K. et al. Carbon pools and flux of global forest ecosystems. Science 263, 185–190 (1994)
McKane, R. B. et al. Climatic effects on tundra carbon storage inferred from experimental data and a model. Ecology 78, 1170–1187 (1997)
Sturm, M., Racine, C. & Tape, K. Climate change: Increasing shrub abundance in the Arctic. Nature 411, 546–547 (2001)
Jonasson, S., Michelsen, A., Schmidt, I. K. & Nielsen, E. V. Responses in microbes and plants to changed temperature, nutrient and light regimes in the arctic. Ecology 80, 1828–1843 (1999)
Bret-Harte, M. S., Shaver, G. R. & Chapin, F. S. I. Primary and secondary stem growth in arctic shrubs: Implications for community response to environmental change. J. Ecol. 90, 251–267 (2002)
Shaver, G. R. et al. Species composition interacts with fertilizer to control long-term change in tundra productivity. Ecology 82, 3163–3181 (2001)
Shaver, G. R. & Chapin, F. S. I. Production:biomass relationships and element cycling in constrating arctic vegetation types. Ecol. Monogr. 61, 1–31 (1991)
Nadelhoffer, K. J., Johnson, L. C., Laundre, J. A., Giblin, A. E. & Shaver, G. R. Fine root production and nutrient content in wet and moist arctic tundras as influenced by chronic fertilization. Plant Soil 242, 107–113 (2002)
Hobbie, S. E. & Chapin, F. S. III The response of tundra plant biomass, aboveground production, nitrogen, and CO2 flux to experimental warming. Ecology 79, 1526–1544 (1998)
Hobbie, S. E. & Gough, L. Litter decomposition in moist acidic and non-acidic tundra with different glacial histories. Oecologia 140, 113–124 (2004)
Weintraub, M. N. & Schimel, J. P. Interactions between carbon and nitrogen mineralization and soil organic matter chemistry in arctic tundra soils. Ecosystems 6, 129–143 (2003)
Moore, J. C., McCann, K., Setala, H. & De Ruiter, P. C. Top-down is bottom-up: does predation in the rhizosphere regulate aboveground dynamics? Ecology 84, 846–857 (2003)
Giblin, A. E., Nadelhoffer, K. J., Shaver, G. R., Laundre, J. A. & McKerrow, A. J. Biogeoghemical diversity along a riverside toposequence in arctic alaska. Ecol. Monogr. 61, 415–435 (1991)
Michaelson, G. J., Ping, C. L. & Kimble, J. M. Carbon storage and distribution in tundra soils of arctic Alaska, U.S.A. Arctic Alpine Res. 28, 414–424 (1996)
Bliss, L. C. & Matveyeva, N. V. in Arctic Ecosystems in a Changing Climate (ed. Chapin, F. S. I.) (Academic, San Diego, California, 1992)
Systat for Windows: Statistics Version 7 7th edn (SYSTAT, Inc., Evanston, Illinois, 1997).
Kirschbaum, M. U. F. Will changes in soil organic carbon act as a positive or negative feedback on global warming? Biogeochemistry 48, 21–51 (2000)
Acknowledgements
This research was supported by NSF, NASA, the Arctic LTER programme and an NSF Postdoctoral Fellowship to M.C.M. We thank E. Mitchell, M. Sommerkorn and M. Williams for assistance with the belowground harvest and J. Laundre for laboratory analyses. S. Hobbie and the UF Plant Ecology group provided comments that improved this manuscript.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Competing interests
The authors declare that they have no competing financial interests.
Supplementary information
Supplementary Figure 1
Effects of fertilization on the components of aboveground net primary productivity (ANPP) in tundra near Toolik Lake, Alaska. Values are means (± 1 standard error) (n=4). Fertilized plots have received 10 g N m-2 yr-1 and 5 g P m-2 yr-1 since 1981. ANPP components were determined through destructive harvests, and data from 1981-1995 harvests are reported in Shaver et al. (2001). Year 2000 data are from this study. (PPT 71 kb)
Supplementary Table 1
Effects of 20 years of fertilization on soil properties of Alaskan tundra. Fertilized tundra near Toolik Lake, Alaska, has received 10 g N m-2 yr-1 and 5 g P m-2 yr-1 since 1981. Means ± 1 standard error are reported by soil layers (litter, shallow organic, deep organic, and mineral) for the following properties: layer depth (cm), bulk density (g cm-3), % C, %N and C:N ratio of bulk soil, and NH4+ and NO3- concentration. Significant differences between treatments are indicated by * (P<0.05), ** (P<0.01), or *** (P<0.001). (DOC 36 kb)
Rights and permissions
About this article
Cite this article
Mack, M., Schuur, E., Bret-Harte, M. et al. Ecosystem carbon storage in arctic tundra reduced by long-term nutrient fertilization. Nature 431, 440–443 (2004). https://doi.org/10.1038/nature02887
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1038/nature02887
This article is cited by
-
Continuous decrease in soil organic matter despite increased plant productivity in an 80-years-old phosphorus-addition experiment
Communications Earth & Environment (2023)
-
Dynamic carbon-nitrogen coupling under global change
Science China Life Sciences (2023)
-
Whole-Ecosystem Warming Increases Plant-Available Nitrogen and Phosphorus in an Ombrotrophic Bog
Ecosystems (2023)
-
Nitrogen enrichment enhances thermal acclimation of soil microbial respiration
Biogeochemistry (2023)
-
Goose Feces Effects on Subarctic Soil Nitrogen Availability and Greenhouse Gas Fluxes
Ecosystems (2023)
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.