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(Referência obtida automaticamente do Web of Science, por meio da informação sobre o financiamento pela FAPESP e o número do processo correspondente, incluída na publicação pelos autores.)

High Primary Production Contrasts with Intense Carbon Emission in a Eutrophic Tropical Reservoir

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Autor(es):
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Almeida, Rafael M. [1] ; Nobrega, Gabriel N. [2] ; Junger, Pedro C. [3] ; Figueiredo, Aline V. [4] ; Andrade, Anizio S. [5] ; de Moura, Caroline G. B. [5] ; Tonetta, Denise [6] ; Oliveira, Jr., Ernandes S. [7] ; Araujo, Fabiana [4] ; Rust, Felipe [1] ; Pineiro-Guerra, Juan M. [8, 9] ; Mendonca, Jr., Jurandir R. [4] ; Medeiros, Leonardo R. [5] ; Pinheiro, Lorena [10] ; Miranda, Marcela [1] ; Costa, Mariana R. A. [4] ; Melo, Michaela L. [11] ; Nobre, Regina L. G. [5] ; Benevides, Thiago [3] ; Roland, Fabio [1] ; de Klein, Jeroen [12] ; Barros, Nathan O. [1] ; Mendonca, Raquel [1, 13] ; Becker, Vanessa [4] ; Huszar, Veral. M. [14] ; Kosten, Sarian [7]
Número total de Autores: 26
Afiliação do(s) autor(es):
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[1] Univ Fed Juiz de Fora, Inst Ciencias Biol, Dept Biol, Aquat Ecol Lab, Juiz De Fora - Brazil
[2] Univ Sao Paulo, Escola Super Agr Luiz de Queiroz, Dept Ciencia Solo, Piracicaba - Brazil
[3] Univ Fed Rio de Janeiro, Lab Limnol, Rio De Janeiro - Brazil
[4] Univ Fed Rio Grande do Norte, Lab Water Resources & Environm Sanitat, BR-59072970 Natal, RN - Brazil
[5] Univ Fed Rio Grande do Norte, Lab Limnol, BR-59072970 Natal, RN - Brazil
[6] Univ Fed Santa Catarina, Lab Freshwater Ecol, Florianopolis, SC - Brazil
[7] Radboud Univ Nijmegen, Dept Aquat Ecol & Environm Biol, Inst Water & Wetland Res, NL-6525 ED Nijmegen - Netherlands
[8] Univ Republica, Fac Ciencias, Montevideo - Uruguay
[9] Univ Republica, Dept Ecol Teor & Aplicada, Ctr Univ Reg Este, Montevideo - Uruguay
[10] Univ Fed Estado Rio de Janeiro, Dept Ciencias Nat, Rio De Janeiro - Brazil
[11] Univ Fed Sao Carlos, Lab Microbial Proc & Biodivers, BR-13560 Sao Carlos, SP - Brazil
[12] Wageningen Univ, Aquat Ecol & Environm Sci, NL-6700 AP Wageningen - Netherlands
[13] Uppsala Univ, Dept Ecol & Genet, Uppsala - Sweden
[14] Univ Fed Rio de Janeiro, Museu Nacl, Lab Ficol, Rio De Janeiro - Brazil
Número total de Afiliações: 14
Tipo de documento: Artigo Científico
Fonte: FRONTIERS IN MICROBIOLOGY; v. 7, MAY 18 2016.
Citações Web of Science: 22
Resumo

Recent studies from temperate lakes indicate that eutrophic systems tend to emit less carbon dioxide (Co-2) and bury more organic carbon (OC) than oligotrophic ones, rendering them CO2 sinks in some cases. However, the scarcity of data from tropical systems is critical for a complete understanding of the interplay between eutrophication and aquatic carbon (C) fluxes in warm waters. We test the hypothesis that a warm eutrophic system is a source of both CO2 and CH4 to the atmosphere, and that atmospheric emissions are larger than the burial of OC in sediments. This hypothesis was based on the following assumptions: (i) OC mineralization rates are high in warm water systems, so that water column CO2 production overrides the high C uptake by primary producers, and (ii) increasing trophic status creates favorable conditions for CH4 production. We measured water-air and sediment-water CO2 fluxes, CH4 diffusion, ebullition and oxidation, net ecosystem production (NEP) and sediment OC burial during the dry season in a eutrophic reservoir in the semiarid northeastern Brazil. The reservoir was stratified during daytime and mixed during nighttime. In spite of the high rates of primary production (4858 +/- 934 mg C m(-2) d(-1)), net heterotrophy was prevalent due to high ecosystem respiration (5209 +/- 992 mg C m(-2) d(-1)). Consequently, the reservoir was a source of atmospheric CO2 (518 +/- 182 mg C m(-2) d(-1)). In addition, the reservoir was a source of ebullitive (17 +/- 10 mg C m(-2) d(-1)) and diffusive CH4 (11 +/- 6 mg C m(-2) d(-1)). OC sedimentation was high (1162 mg C m(-2) d(-1)), but our results suggest that the majority of it is mineralized to CO2 (722 +/- 182 mg C m(-2) d(-1)) rather than buried as OC (440 mg C m(-2) d(-1)). Although temporally resolved data would render our findings more conclusive, our results suggest that despite being a primary production and OC burial hotspot, the tropical eutrophic system studied here was a stronger CO2 and CH4 source than a C sink, mainly because of high rates of OC mineralization in the water column and sediments. (AU)

Processo FAPESP: 14/11778-5 - Solos subaquáticos de pradarias marinhas (seagrass bed) do Brasil: biogeoquímica, gênese e classificação
Beneficiário:Gabriel Nuto Nóbrega
Modalidade de apoio: Bolsas no Brasil - Doutorado