AUTHOR=Almeida Rafael M. , Nóbrega Gabriel N. , Junger Pedro C. , Figueiredo Aline V. , Andrade Anízio S. , de Moura Caroline G. B. , Tonetta Denise , Oliveira Ernandes S. , Araújo Fabiana , Rust Felipe , Piñeiro-Guerra Juan M. , Mendonça Jurandir R. , Medeiros Leonardo R. , Pinheiro Lorena , Miranda Marcela , Costa Mariana R. A. , Melo Michaela L. , Nobre Regina L. G. , Benevides Thiago , Roland Fábio , de Klein Jeroen , Barros Nathan O. , Mendonça Raquel , Becker Vanessa , Huszar Vera L. M. , Kosten Sarian TITLE=High Primary Production Contrasts with Intense Carbon Emission in a Eutrophic Tropical Reservoir JOURNAL=Frontiers in Microbiology VOLUME=7 YEAR=2016 URL=https://www.frontiersin.org/journals/microbiology/articles/10.3389/fmicb.2016.00717 DOI=10.3389/fmicb.2016.00717 ISSN=1664-302X ABSTRACT=

Recent studies from temperate lakes indicate that eutrophic systems tend to emit less carbon dioxide (CO₂) 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.