2010
DOI: 10.1038/ismej.2010.13
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Bacteriochlorophyll and community structure of aerobic anoxygenic phototrophic bacteria in a particle-rich estuary

Abstract: Photoheterotrophic microbes use organic substrates and light energy to satisfy their demand for carbon and energy and seem to be well adapted to eutrophic estuarine and oligotrophic oceanic environments. One type of photoheterotroph, aerobic anoxygenic phototrophic (AAP) bacteria, is especially abundant in particle-rich, turbid estuaries. To explore questions regarding the controls of these photoheterotrophic bacteria, we examined their abundance by epifluorescence microscopy, concentrations of the light-harve… Show more

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Cited by 58 publications
(57 citation statements)
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“…Similarly, no clear link between AAP bacterial abundance and oligotrophy was established since abundances of AAP bacteria can be high in estuarine, coastal and shelf waters (e.g. Cottrell et al, 2010;Waidner and Kirchman, 2007). AAP bacteria were found to be more abundant in the upper layers of the photic zone than below the sunlit layers of the water column of the Mediterranean Sea.…”
Section: Bacterial Productionmentioning
confidence: 99%
See 1 more Smart Citation
“…Similarly, no clear link between AAP bacterial abundance and oligotrophy was established since abundances of AAP bacteria can be high in estuarine, coastal and shelf waters (e.g. Cottrell et al, 2010;Waidner and Kirchman, 2007). AAP bacteria were found to be more abundant in the upper layers of the photic zone than below the sunlit layers of the water column of the Mediterranean Sea.…”
Section: Bacterial Productionmentioning
confidence: 99%
“…Depth distributions of Chl-a concentrations included a well defined deep chlorophyll maximum (DCM), more pronounced in the western basin, and deepening from west (∼40 to 80 m) to east (from 80 to >100 m) ( Fig. 2; see also Crombet et al, 2011). Surface Mediterranean waters were depleted in nutrients and the thickness of this depleted layer increased towards the east from about 10 m in the Gulf of Lion to more than 100 m in the Levantine basin (for details see Pujo-Pay et al, 2011).…”
Section: Environmental Settingmentioning
confidence: 99%
“…Surface-associated marine microbiota participate in a plethora of C cycling processes. Photosynthetic and chemolithoautotrophic CO 2 fixation (102,(142)(143)(144)(145)(146)(147)(148), aerobic anoxygenic phototrophic energy conservation (149)(150)(151), seawater methane production and oxidation (143,146,147,152), degradation of biopolymers and other organic matter (102,117,145,153), and heterotrophic respiration (102,104,113,145) are all enhanced on surfaces. N cycling processes such as N 2 fixation (154,155), nitrification (142,143,(156)(157)(158), denitrification (158)(159)(160)(161), dissimilatory nitrate reduction (158,159), anaerobic ammonium oxidation (anammox) (158,162,163), and nitrogenous organic compound degradation (158,(164)(165)(166) are also activities associated with surfaces and can be particularly important at specific depths in the water column.…”
Section: Physiological Challenges and Deleterious Effects Of Microbiamentioning
confidence: 99%
“…In some coastal mesotrophic estuaries, AAP bacteria exceeded 10%, which might be ascribed to the numerous particles in these environments [7][8]. In the South Pacific Ocean, the proportion of AAP bacteria was approximately 25% of total bacterioplankton, suggesting the potential contribution of other environmental variables [9].…”
mentioning
confidence: 99%