Title
After trees die: Quantities and determinants of necromass across Amazonia
Date Issued
01 January 2009
Access level
open access
Resource Type
journal article
Author(s)
Chao K.J.
Phillips O.L.
Baker T.R.
Peacock J.
Lopez-Gonzalez G.
Torres-Lezama A.
Publisher(s)
European Geosciences Union
Abstract
The Amazon basin, one of the most substantial biomass carbon pools on earth, is characterised by strong macroecological gradients in biomass, mortality rates, and wood density from west to east. These gradients could affect necromass stocks, but this has not yet been tested. This study aims to assess the stocks and determinants of necromass across Amazonian forests. Field-based and literature data were used to find relationships between necromass and possible determinants. Furthermore, a simple model was applied to estimate and extrapolate necromass stocks acrossterra firmaAmazonian forests. In eight northwestern and three northeastern Amazonian permanent plots, volumes of coarse woody debris (≥10 cm diameter) were measured in the field and the density of each decay class was estimated. Forest structure and historical mortality data were used to determine the factors controlling necromass. Necromass is greater in forests with low stem mortality rates (northeast) rather than in forests with high stem mortality rates (northwest) (58.5±10.6 and 27.3±3.2 Mg ha-, respectively). Using all published necromass values, we find that necromass across terra firma forests in Amazonia is positively related to both forest dynamics (mortality mass inputs and a surrogate for decomposition rate (average wood density of living trees)) and forest structure (biomass), but is better explained by forest dynamics. We propose an improved method to estimate necromass for plots where necromass has not been measured. The estimates, together with other actual measurements of necromass, were scaled-up to project a total Amazonian necromass of 9.6±1.0 Pg C. The ratio of necromass (on average weighted by forest region) to coarse aboveground biomass is 0.127. Overall, we find (1) a strong spatial trend in necromass in parallel with other macroecological gradients and (2) that necromass is a substantial component of the carbon pool in the Amazon.
Start page
1615
End page
1626
Volume
6
Issue
8
Language
English
OCDE Knowledge area
Ecología
Scopus EID
2-s2.0-72049103215
Source
Biogeosciences
ISSN of the container
17264170
Sources of information:
Directorio de Producción Científica
Scopus