2012
DOI: 10.3389/fmicb.2012.00153
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The distribution of ammonia-oxidizing betaproteobacteria in stands of Black mangroves (Avicennia germinans)

Abstract: The distribution of species of aerobic chemolitho-autotrophic microorganisms such as ammonia-oxidizing bacteria are governed by pH, salinity, and temperature as well as the availability of oxygen, ammonium, carbon dioxide, and other inorganic elements required for growth. Impounded mangrove forests in the Indian River Lagoon, a coastal estuary on the east coast of Florida, are dominated by mangroves, especially stands of Black mangrove (Avicennia germinans) that differ in the size and density of individual pla… Show more

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Cited by 14 publications
(14 citation statements)
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“…Half saturation constants (K m ) for betaproteobacterial ammonia oxidation range from 10 to 3300 μM (NH 3 + NH 4 + ) (Stehr et al ., ; Pommerening‐Röser et al ., ; Jiang and Bakken, ; Schramm et al ., ; Bollmann et al ., ). The presence and growth of Nitrosospira cluster 1 in sediments with ammonium concentrations < 10 μM thus likely position them among the AOB with the highest ammonia affinities; adaptation of Nitrosospira cluster 1 to low ammonium was also previously indicated by their increased relative abundance in oligotrophic compared with eutrophic mangrove sediment (Laanbroek et al ., ). Whether Nitrosospira cluster 1 is able to compete for ammonium with high‐affinity AOA, whose K m is in the nM range, cannot be resolved on the basis of our data.…”
Section: Resultsmentioning
confidence: 97%
“…Half saturation constants (K m ) for betaproteobacterial ammonia oxidation range from 10 to 3300 μM (NH 3 + NH 4 + ) (Stehr et al ., ; Pommerening‐Röser et al ., ; Jiang and Bakken, ; Schramm et al ., ; Bollmann et al ., ). The presence and growth of Nitrosospira cluster 1 in sediments with ammonium concentrations < 10 μM thus likely position them among the AOB with the highest ammonia affinities; adaptation of Nitrosospira cluster 1 to low ammonium was also previously indicated by their increased relative abundance in oligotrophic compared with eutrophic mangrove sediment (Laanbroek et al ., ). Whether Nitrosospira cluster 1 is able to compete for ammonium with high‐affinity AOA, whose K m is in the nM range, cannot be resolved on the basis of our data.…”
Section: Resultsmentioning
confidence: 97%
“…In the Mai Po mangrove wetland, Li et al (2011) suggested that it was AOB not AOA communities that were grouped by distances between sampling sites and mangrove trees, which indicated the effect of mangrove trees on AOA and AOB community structures. In a black mangrove in the USA, Laanbroek et al (2012) showed that AOB community structures were shaped by vegetation coverage with which different mangrove habitats were formed. Furthermore, the plant species effect on ammonia-oxidizing community structures was observed in grassland soils as well (Patra et al 2006).…”
Section: Community Structures Of Ammonia Oxidizers Shaped By Plantsmentioning
confidence: 98%
“…A case study in mangrove sediments revealed that the effect of mangrove plants on abundances and community structures of AOA and AOB is species dependent . Moreover, Laanbroek et al (2012) showed that soil chemical properties associated with vegetation densities affected community structures of AOB, while an earlier study suggested that variations of nitrification potential between different soils were related to vegetation type rather than the soil physiochemical properties (Wedin and Tilman 1990).…”
Section: Introductionmentioning
confidence: 96%
“…Finally, the paper of Laanbroek et al (2012) introduces the Black mangrove wetlands as a microbial habitat to the reader. The specific focus in this study is on diversity of ammonia-oxidizing Betaproteobacteria , which reflects the changes in hydrology in three different Black mangrove habitats, i.e., locations with dwarf, sparse, and dense trees.…”
Section: Microbial Abundance Diversity and Spatial Distributionmentioning
confidence: 99%
“…Notably, these studies address a wide variety of wetland types including rice paddies (Alam and Jia, 2012; Conrad et al, 2012), acidic Sphagnum -dominated peatlands (Bragina et al, 2011; Ivanova and Dedysh, 2012; Kolb and Horn, 2012; Preston et al, 2012; Putkinen et al, 2012; Sun et al, 2012), riparian wetlands (Wang et al, 2012), black mangroves (Laanbroek et al, 2012), superficial aquatic sediments (Gu et al, 2012), salt marshes (Irvine et al, 2012; Lovell and Davis, 2012), and littoral boreal wetlands (Siljanen et al, 2012). …”
Section: Introductionmentioning
confidence: 99%