Seasonal variation in net ecosystem CO2 exchange of a Brazilian seasonally dry tropical forest

• Published in: Scientific reports Vol. 10; no. 1; p. 9454
• Main Authors: Mendes, Keila R., Campos, Suany, da Silva, Lindenberg L., Mutti, Pedro R., Ferreira, Rosaria R., Medeiros, Salomão S., Perez-Marin, Aldrin M., Marques, Thiago V., Ramos, Tarsila M., de Lima Vieira, Mariana M., Oliveira, Cristiano P., Gonçalves, Weber A., Costa, Gabriel B., Antonino, Antonio C. D., Menezes, Rômulo S. C., Bezerra, Bergson G., Santos e Silva, Cláudio M.
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 11.06.2020; Nature Publishing Group
• Subjects: 704/106; 704/47; Air temperature; Carbon; Carbon dioxide; Carbon sinks; Diurnal; Dry forests; Dry season; Ecosystems; Forest ecosystems; Humanities and Social Sciences; multidisciplinary; Primary production; Rainfall; Science; Science (multidisciplinary); Seasonal variations; Soil temperature; Terrestrial ecosystems; Tropical forests
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-020-66415-w

Forest ecosystems sequester large amounts of atmospheric CO 2 , and the contribution from seasonally dry tropical forests is not negligible. Thus, the objective of this study was to quantify and evaluate the seasonal and annual patterns of CO 2 exchanges in the Caatinga biome, as well as to evaluate the ecosystem condition as carbon sink or source during years. In addition, we analyzed the climatic factors that control the seasonal variability of gross primary production (GPP), ecosystem respiration (R eco ) and net ecosystem CO 2 exchange (NEE). Results showed that the dynamics of the components of the CO 2 fluxes varied depending on the magnitude and distribution of rainfall and, as a consequence, on the variability of the vegetation state. Annual cumulative NEE was significantly higher (p < 0.01) in 2014 (−169.0 g C m −2 ) when compared to 2015 (−145.0 g C m −2 ) and annual NEP/GPP ratio was 0.41 in 2014 and 0.43 in 2015. Global radiation, air and soil temperature were the main factors associated with the diurnal variability of carbon fluxes. Even during the dry season, the NEE was at equilibrium and the Caatinga acted as an atmospheric carbon sink during the years 2014 and 2015.