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Comparison of the mass and energy exchange of a pasture and a mature transitional tropical forest of the southern Amazon Basin during a seasonal transition
Author(s) -
PrianteFilho Nicolau,
Vourlitis George L.,
Hayashi Mauro Massao Shiota,
Nogueira José De Souza,
Campelo José Holanda,
Nunes Paulo César,
Souza Luciana Sanches E,
Couto Eduardo Guimarães,
Hoeger Wander,
Raiter Fernando,
Trienweiler Jansen Luiz,
Miranda Eduardo Jacusiel,
Priante Pedro Correto,
Fritzen Clóvis Lasta,
Lacerda Moacir,
Pereira Luiz Carlos,
Biudes Marcelo Sacardi,
Suli George Sanches,
Shiraiwa Shozo,
Paulo Sérgio Roberto Do,
Silveira Marcos
Publication year - 2004
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1529-8817.2003.00775.x
Subject(s) - eddy covariance , pasture , environmental science , ecosystem , ecosystem respiration , atmospheric sciences , geography , ecology , forestry , biology , physics
This research utilized tower‐based eddy covariance to quantify the trends in net ecosystem mass (CO 2 and H 2 O vapor) and energy exchange of important land‐cover types of NW Mato Grosso during the March–December 2002 seasonal transition. Measurements were made in a mature transitional (ecotonal) tropical forest near Sinop, Mato Grosso, and a cattle pasture near Cotriguaçú, Mato Grosso, located 500 km WNW of Sinop. Pasture net ecosystem CO 2 exchange (NEE) was considerably more variable than the forest NEE over the seasonal transition, and the pasture had significantly higher rates of maximum gross primary production in every season except the dry–wet season transition (September–October). The pasture also had significantly higher rates of whole‐ecosystem dark respiration than the forest during the wetter times of the year. Average (±95% CI) rates of total daily NEE during the March–December 2002 measurement period were 26±15 mmol m −2 day −1 for the forest (positive values indicate net CO 2 loss by the ecosystem) and −38±26 mmol m −2 day −1 for the pasture. While both ecosystems partitioned more net radiation ( R n ) into latent heat flux ( L e ), the forest had significantly higher rates of L e and lower rates of sensible heat flux ( H ) than the pasture; a trend that became more extreme during the onset of the dry season. Large differences in pasture and forest mass and energy exchange occurred even though seasonal variations in micrometeorology (air temperature, humidity, and radiation) were relatively similar for both ecosystems. While the short measurement period and lack of spatial replication limit the ability to generalize these results to pasture and forest regions of the Amazon Basin, these results suggest important differences in the magnitude and seasonal variation of NEE and energy partitioning for pasture and transitional tropical forest.