Artigo

Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency

Understanding how tropical forest carbon balance will respond to global change requires knowledge of individual heterotrophic and autotrophic respiratory sources, together with factors that control respiratory variability. We measured leaf, live wood, and soil respiration, along with additional envi...

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Autor principal: Chambers, Jeffrey Quintin
Outros Autores: Tribuzy, Edgard Siza, Toledo, Ligia C., Crispim, Bianca F., Higuchi, Niro, Santos, Joaquim dos, Araüjo, Alessandro Carioca de, Kruijt, Bart J., Nobre, Antônio Donato, Trumbore, Susan Elizabeth
Grau: Artigo
Idioma: English
Publicado em: Ecological Applications 2020
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Acesso em linha: https://repositorio.inpa.gov.br/handle/1/18902
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spelling oai:repositorio:1-18902 Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency Chambers, Jeffrey Quintin Tribuzy, Edgard Siza Toledo, Ligia C. Crispim, Bianca F. Higuchi, Niro Santos, Joaquim dos Araüjo, Alessandro Carioca de Kruijt, Bart J. Nobre, Antônio Donato Trumbore, Susan Elizabeth Carbon Balance Global Change Net Ecosystem Exchange Net Primary Production Nutrient Use Efficiency Respiration Soil Respiration Tropical Forest Amazonia South America Understanding how tropical forest carbon balance will respond to global change requires knowledge of individual heterotrophic and autotrophic respiratory sources, together with factors that control respiratory variability. We measured leaf, live wood, and soil respiration, along with additional environmental factors over a 1-yr period in a Central Amazon terra firme forest. Scaling these fluxes to the ecosystem, and combining our data with results from other studies, we estimated an average total ecosystem respiration (R eco) of 7.8 μmol·m-2·s-1. Average estimates (per unit ground area) for leaf, wood, soil, total heterotrophic, and total autotrophic respiration were 2.6, 1.1, 3.2, 5.6, and 2.2 μmol·m-2·s-1, respectively. Comparing autotrophic respiration with net primary production (NPP) estimates indicated that only ∼30% of carbon assimilated in photosynthesis was used to construct new tissues, with the remaining 70% being respired back to the atmosphere as autotrophic respiration. This low ecosystem carbon use efficiency (CUE) differs considerably from the relatively constant CUE of ∼0.5 found for temperate forests. Our Reco estimate was comparable to the above-canopy flux (Fac) from eddy covariance during defined sustained high turbulence conditions (when presumably Fac = Reco) of 8.4 (95% CI = 7.5-9.4). Multiple regression analysis demonstrated that ∼50% of the nighttime variability in Fac was accounted for by friction velocity (u*, a measure of turbulence) variables. After accounting for u* variability, mean Fac varied significantly with seasonal and daily changes in precipitation. A seasonal increase in precipitation resulted in a decrease in Fac, similar to our soil respiration response to moisture. The effect of daily changes in precipitation was complex: precipitation after a dry period resulted in a large increase in Fac, whereas additional precipitation after a rainy period had little effect. This response was similar to that of surface litter (coarse and fine), where respiration is greatly reduced when moisture is limiting, but increases markedly and quickly saturates with an increase in moisture. 2020-06-15T22:03:48Z 2020-06-15T22:03:48Z 2004 Artigo https://repositorio.inpa.gov.br/handle/1/18902 en Volume 14, Número 4 SUPPL., Pags. S72-S88 Restrito Ecological Applications
institution Instituto Nacional de Pesquisas da Amazônia - Repositório Institucional
collection INPA-RI
language English
topic Carbon Balance
Global Change
Net Ecosystem Exchange
Net Primary Production
Nutrient Use Efficiency
Respiration
Soil Respiration
Tropical Forest
Amazonia
South America
spellingShingle Carbon Balance
Global Change
Net Ecosystem Exchange
Net Primary Production
Nutrient Use Efficiency
Respiration
Soil Respiration
Tropical Forest
Amazonia
South America
Chambers, Jeffrey Quintin
Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency
topic_facet Carbon Balance
Global Change
Net Ecosystem Exchange
Net Primary Production
Nutrient Use Efficiency
Respiration
Soil Respiration
Tropical Forest
Amazonia
South America
description Understanding how tropical forest carbon balance will respond to global change requires knowledge of individual heterotrophic and autotrophic respiratory sources, together with factors that control respiratory variability. We measured leaf, live wood, and soil respiration, along with additional environmental factors over a 1-yr period in a Central Amazon terra firme forest. Scaling these fluxes to the ecosystem, and combining our data with results from other studies, we estimated an average total ecosystem respiration (R eco) of 7.8 μmol·m-2·s-1. Average estimates (per unit ground area) for leaf, wood, soil, total heterotrophic, and total autotrophic respiration were 2.6, 1.1, 3.2, 5.6, and 2.2 μmol·m-2·s-1, respectively. Comparing autotrophic respiration with net primary production (NPP) estimates indicated that only ∼30% of carbon assimilated in photosynthesis was used to construct new tissues, with the remaining 70% being respired back to the atmosphere as autotrophic respiration. This low ecosystem carbon use efficiency (CUE) differs considerably from the relatively constant CUE of ∼0.5 found for temperate forests. Our Reco estimate was comparable to the above-canopy flux (Fac) from eddy covariance during defined sustained high turbulence conditions (when presumably Fac = Reco) of 8.4 (95% CI = 7.5-9.4). Multiple regression analysis demonstrated that ∼50% of the nighttime variability in Fac was accounted for by friction velocity (u*, a measure of turbulence) variables. After accounting for u* variability, mean Fac varied significantly with seasonal and daily changes in precipitation. A seasonal increase in precipitation resulted in a decrease in Fac, similar to our soil respiration response to moisture. The effect of daily changes in precipitation was complex: precipitation after a dry period resulted in a large increase in Fac, whereas additional precipitation after a rainy period had little effect. This response was similar to that of surface litter (coarse and fine), where respiration is greatly reduced when moisture is limiting, but increases markedly and quickly saturates with an increase in moisture.
format Artigo
author Chambers, Jeffrey Quintin
author2 Tribuzy, Edgard Siza
Toledo, Ligia C.
Crispim, Bianca F.
Higuchi, Niro
Santos, Joaquim dos
Araüjo, Alessandro Carioca de
Kruijt, Bart J.
Nobre, Antônio Donato
Trumbore, Susan Elizabeth
author2Str Tribuzy, Edgard Siza
Toledo, Ligia C.
Crispim, Bianca F.
Higuchi, Niro
Santos, Joaquim dos
Araüjo, Alessandro Carioca de
Kruijt, Bart J.
Nobre, Antônio Donato
Trumbore, Susan Elizabeth
title Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency
title_short Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency
title_full Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency
title_fullStr Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency
title_full_unstemmed Respiration from a tropical forest ecosystem: Partitioning of sources and low carbon use efficiency
title_sort respiration from a tropical forest ecosystem: partitioning of sources and low carbon use efficiency
publisher Ecological Applications
publishDate 2020
url https://repositorio.inpa.gov.br/handle/1/18902
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score 11.653393