Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 6, issue 8
Biogeosciences, 6, 1615-1626, 2009
https://doi.org/10.5194/bg-6-1615-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Biogeochemistry and function of Amazon Forest

Biogeosciences, 6, 1615-1626, 2009
https://doi.org/10.5194/bg-6-1615-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  11 Aug 2009

11 Aug 2009

After trees die: quantities and determinants of necromass across Amazonia

K.-J. Chao2,1, O. L. Phillips1, T. R. Baker1, J. Peacock1, G. Lopez-Gonzalez1, R. Vásquez Martínez3, A. Monteagudo3,4, and A. Torres-Lezama5 K.-J. Chao et al.
  • 1Earth and Biosphere Institute, School of Geography, University of Leeds, LS2 9JT, Leeds, UK
  • 2International Master Program of Agriculture, College of Agriculture and Natural Resources, National Chung Hsing University, Taichung 40227, Taiwan
  • 3Proyecto Flora del Perú, Jardín Botánico de Missouri, Oxapampa, Peru
  • 4Herbario Vargas, Universidad Nacional San Antonio Abad del Cusco, Cusco, Peru
  • 5INDEFOR, Facultad de Ciencias Forestales y Ambientales, Universidad de Los Andes, Mérida, Venezuela

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 across terra firma Amazonian 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−1, 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.

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