Oceans, Rivers and Lakes: Energy and Substance Transfers at Interfaces 1998
DOI: 10.1007/978-94-011-5266-2_7
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Benthic influence on the metabolism of a shallow tropical lagoon (Lagoa da Barra, Brazil)

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Cited by 4 publications
(5 citation statements)
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“…These patterns can be driven by either biological or physical processes. Carmouze et al (1998) suggested that the seasonal switch from autotrophy to heterotrophy in several subtropical lagoons in Brazil was driven by low phytoplankton activity in the winter as temperature and irradiance levels became less conducive to growth. Conversely, Reyes & Merino (1991) attributed strong winter heterotrophy in a macrophytedominated tropical lagoon to resuspension and rapid degradation of organic-rich sediments during winter storms.…”
Section: Patterns Of Autotrophy and Heterotrophymentioning
confidence: 99%
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“…These patterns can be driven by either biological or physical processes. Carmouze et al (1998) suggested that the seasonal switch from autotrophy to heterotrophy in several subtropical lagoons in Brazil was driven by low phytoplankton activity in the winter as temperature and irradiance levels became less conducive to growth. Conversely, Reyes & Merino (1991) attributed strong winter heterotrophy in a macrophytedominated tropical lagoon to resuspension and rapid degradation of organic-rich sediments during winter storms.…”
Section: Patterns Of Autotrophy and Heterotrophymentioning
confidence: 99%
“…Most metabolism studies to date have been performed in relatively deep coastal systems where the dominant autotrophs are phytoplankton. In shallow-water systems, benthic photoautotrophy is likely to be a key driver of total metabolism (Kenney et al 1988, D'Avanzo et al 1996, Carmouze et al 1998. Data on the trophic status of shallow lagoons and bays are equivocal, with some showing balanced metabolism or slight autotrophy either on a seasonal or annual basis (Reyes & Merino 1991, D'Avanzo et al 1996, Carmouze et al 1998) and others indicating heterotrophy (Nowicki & Nixon 1985, Flores-Verdugo et al 1988.…”
Section: Introductionmentioning
confidence: 99%
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“…The flux of benthic nutrients through the sediment-water interface is a result of several microbial processes, such as ammonification, nitrification, denitrification, methanogenesis, oxidative phosphorylation and sulfate reduction, among others (CARMOUZE et al, 1998). Along with these processes, several authors have emphasized the enhanced effects of the bioturbation process performed by benthic macroinvertebrates in the flux of these nutrients (RYSGAARD et al, 1995;ROCHA, 1998;MULSOW and BOUDREAU, 1998).…”
Section: Introductionmentioning
confidence: 99%