Relationship between soils and Amazon forest biomass: A landscape-scale study

Citation
Wf. Laurance et al., Relationship between soils and Amazon forest biomass: A landscape-scale study, FOREST ECOL, 118(1-3), 1999, pp. 127-138
Citations number
78
Categorie Soggetti
Plant Sciences
Journal title
FOREST ECOLOGY AND MANAGEMENT
ISSN journal
03781127 → ACNP
Volume
118
Issue
1-3
Year of publication
1999
Pages
127 - 138
Database
ISI
SICI code
0378-1127(19990614)118:1-3<127:RBSAAF>2.0.ZU;2-6
Abstract
Above-ground dry biomass of living trees including palms was estimated in 6 5 l ha plots spanning a 1000 km(2) landscape in central Amazonia. The study area was located on heavily weathered, nutrient-poor soils that are widesp read in the Amazon region. Biomass values were derived by measuring the dia meter-at-breast-height (DBH) of all greater than or equal to 10 cm trees in each plot, then using an allometric equation and correction factor for sma ll trees to estimate total tree biomass. Detailed information on soil textu re, organic carbon, available water capacity, pH, macro- and micro-nutrient s, and trace elements was collected from soil surface samples (0-20 cm) in each plot, while slope was measured with a clinometer. Biomass estimates va ried more than two-fold, from 231 to 492 metric tons ha(-1), with a mean of 356 +/- 47 tons ha(-1). Simple correlations with stringent (p < 0.006) Bon ferroni corrections suggested that biomass was positively associated with t otal N, total exchangeable bases, K+, Mg2+, clay, and organic C in soils, a nd negatively associated with Zn+, aluminum saturation, and sand. An ordina tion analysis revealed one major and several minor soil gradients in the st udy area, with the main gradient discriminating sites with varying proporti ons of clay (with clayey soils having higher concentrations of total N, org anic C, most cations, and lower aluminum saturation and less sand). A multi ple regression analysis revealed that the major clay-nutrient gradient was the only significant predictor, with the model explaining 32.3% of the tota l variation in biomass. Results of the analysis suggest that soil-fertility parameters can account for a third or more of the variation in above-groun d biomass in Amazonian terra-firme forests. We suggest that, because the co nversion of forest to pasture tends to reduce the nitrogen, clay, organic c arbon, and nutrient contents of soils, forests that regenerate on formerly cleared lands may have lower biomass than the original forest, especially i n areas with low soil fertility. (C) 1999 Elsevier Science B.V. All rights reserved.