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Seasonal controls on the exchange of carbon and water in an Amazonian rain forest
Author(s) -
Hutyra Lucy R.,
Munger J. William,
Saleska Scott R.,
Gottlieb Elaine,
Daube Bruce C.,
Dunn Allison L.,
Amaral Daniel F.,
de Camargo Plinio B.,
Wofsy Steven C.
Publication year - 2007
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2006jg000365
Subject(s) - environmental science , eddy covariance , dry season , evergreen , evapotranspiration , ecosystem , wet season , canopy , ecosystem respiration , primary production , carbon cycle , growing season , water balance , atmospheric sciences , agronomy , ecology , biology , geotechnical engineering , geology , engineering
The long‐term resilience of Amazonian forests to climate changes and the fate of their large stores of organic carbon depend on the ecosystem response to climate and weather. This study presents 4 years of eddy covariance data for CO 2 and water fluxes in an evergreen, old‐growth tropical rain forest examining the forest's response to seasonal variations and to short‐term weather anomalies. Photosynthetic efficiency declined late in the wet season, before appreciable leaf litter fall, and increased after new leaf production midway through the dry season. Rates of evapotranspiration were inelastic and did not depend on dry season precipitation. However, ecosystem respiration was inhibited by moisture limitations on heterotrophic respiration during the dry season. The annual carbon balance for this ecosystem was very close to neutral, with mean net loss of 890 ± 220 kg C ha −1 yr −1 , and a range of −221 ± 453 (C uptake) to +2677 ± 488 (C loss) kg C ha −1 yr −1 over 4 years. The trend from large net carbon release in 2002 towards net carbon uptake in 2005 implies recovery from prior disturbance. The annual carbon balance was sensitive to weather anomalies, particularly the timing of the dry‐to‐wet season transition, reflecting modulation of light inputs and respiration processes. Canopy carbon uptake rates were largely controlled by phenology and light with virtually no indication of seasonal water limitation during the 5‐month dry season, indicating ample supplies of plant‐available‐water and ecosystem adaptation for maximum light utilization.

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