The DOI matches its Crossref record; 58 of the 58 references it cites were found in a registry or an index.
CARBON BALANCE AND VEGETATION DYNAMICS IN AN OLD‐GROWTH AMAZONIAN FOREST
Open accessAbstract
Amazon forests could be globally significant sinks or sources for atmospheric carbon dioxide, but carbon balance of these forests remains poorly quantified. We surveyed 19.75 ha along four 1‐km transects of well‐drained old‐growth upland forest in the Tapajós National Forest near Santarém, Pará, Brazil (2°51′ S, 54°58′ W) in order to assess carbon pool sizes, fluxes, and climatic controls on carbon balance. In 1999 there were, on average, 470 live trees per hectare with diameter at breast height (dbh) ≥10 cm. The mean (and 95% ci) aboveground live biomass was 143.7 ± 5.4 Mg C/ha, with an additional 48.0 ± 5.2 Mg C/ha of coarse woody debris (CWD). The increase of live wood biomass after two years was 1.40 ± 0.62 Mg C·ha−1·yr−1, the net result of growth (3.18 ± 0.20 Mg C·ha−1·yr−1 from mean bole increment of 0.36 cm/yr), recruitment of new trees (0.63 ± 0.09 Mg C·ha−1·yr−1, reflecting a notably high stem recruitment rate of 4.8 ± 0.9%), and mortality (−2.41 ± 0.53 Mg C·ha−1·yr−1 from stem death of 1.7% yr−1). The gain in live wood biomass was exceeded by respiration losses from CWD, resulting in an overall estimated net loss from total aboveground biomass of 1.9 ± 1.0 Mg C·ha−1·yr−1. The presence of large CWD pools, high recruitment rate, and net accumulation of small‐tree biomass, suggest that a period of high mortality preceded the initiation of this study, possibly triggered by the strong El Niño Southern Oscillation events of the 1990s. Transfer of carbon between live and dead biomass pools appears to have led to substantial increases in the pool of CWD, causing the observed net carbon release. The data show that biometric studies of tropical forests neglecting CWD are unlikely to accurately determine carbon balance. Furthermore, the hypothesized sequestration flux from CO 2 fertilization (<0.5 Mg C·ha−1·yr−1) would be comparatively small and masked for considerable periods by climate‐driven shifts in forest structure and associated carbon balance in tropical forests.
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Cites
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Carbon pools and flux of global forest ecosystems
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Observational Contrains on the Global Atmospheric Co 2 Budget
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Global climate change and terrestrial net primary production
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Improvements on Cross-Validation: The 632+ Bootstrap Method
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Terrestrial ecosystems and the carbon cycle
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Self-citationEstimating biomass and biomass change of tropical forests: A primer
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Towards robust regional estimates of CO2 sources and sinks using atmospheric transport models
Gurney, K. R., Law, R. M., Denning, A. S., Rayner, P. J., Baker, D., Bousquet, P., Bruhwiler, L., Chen, Y.-H., Ciais, P., Fan, S., et al. (2002) · Nature · doi:10.1038/415626a · Cited by 1,225
The Carbon Cycle and Atmospheric Carbon Dioxide
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Cited by
Lapola, D. M., Oyama, M. D., & Nobre, C. A. (2009) · Global Biogeochemical Cycles · doi:10.1029/2008gb003357 · Cited by 122
Ecosystem heterogeneity and diversity mitigate Amazon forest resilience to frequent extreme droughts
Longo, M., Knox, R. G., Levine, N. M., Alves, L. F., Bonal, D., Camargo, P. B., Fitzjarrald, D. R., Hayek, M. N., Restrepo‐Coupe, N., Saleska, S. R., et al. (2018) · New Phytologist · doi:10.1111/nph.15185 · Cited by 111
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Metadata
- Authors
- Rice, A. H., Pyle, E. H., Saleska, S. R., Hutyra, L., Palace, M., Keller, M., de Camargo, P. B., Portilho, K., Marques, D. F., & Wofsy, S. C.
- Venue
- Ecological Applications
- Publisher
- Wiley
- Published
- 2004-08
- Volume
- 14
- Issue
- sp4
- Pages
- 55-71
- ISSN
- 1051-0761 (ISSN-L)
- 1939-5582
- OpenAlex
- W2144142891
- Cited by
- 331
- References
- 58
- FWCI
- 20.72
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Rice, A. H., Pyle, E. H., Saleska, S. R., Hutyra, L., Palace, M., Keller, M., de Camargo, P. B., Portilho, K., Marques, D. F., & Wofsy, S. C. (2004). CARBON BALANCE AND VEGETATION DYNAMICS IN AN OLD‐GROWTH AMAZONIAN FOREST. Ecological Applications. https://doi.org/10.1890/02-6006
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