Omz_coassembly
Ontology highlight
ABSTRACT:
PROVIDER: PRJEB19326 | ENA |
REPOSITORIES: ENA
Similar Datasets
Project description:Nitrite oxidizing bacteria in oxygen minimum zones
| PRJNA1003508 | ENA
Project description:Metal availability predicts community metallogenomes in marine oxygen minimum zones
| PRJNA254808 | ENA
Project description:Foraminiferal nitrate respiration in oxygen minimum zones - past and present - Metagenomics
| PRJNA503328 | ENA
Project description:Ammonia-oxidizing archaea (AOA) have been reported at high abundance in much of the global ocean, even in environments such as pelagic oxygen minimum zones (OMZs), where conditions seem unlikely to support aerobic ammonium oxidation. Due to the lack of information on any potential alternative metabolism of AOA, the AOA community composition might be expected to differ between oxic and anoxic environments, indicating some difference in ecology and/or physiology of the AOA assemblage. This hypothesis was tested by evaluating AOA community composition using a functional gene microarray that targets the ammonia monooxygenase gene subunit A (amoA). The relationship between environmental parameters and the biogeography of the Arabian Sea and the Eastern Tropical South Pacific (ETSP) AOA assemblages was investigated using principal component analysis (PCA) and redundancy analysis (RDA). In both the Arabian Sea and the ETSP, AOA communities within the core of the OMZ were not significantly different from those inhabiting the oxygenated surface waters above the OMZ. The AOA communities in the Arabian Sea were significantly different from those in the ETSP. In both oceans, the abundance of archaeal amoA gene in the core of the OMZ was higher than that in the surface waters. Our results indicate that AOA communities are distinguished by their geographic origin. RDA suggested that temperature was the main factor that correlated with the differences between the AOA communities from the Arabian Sea and those from the ETSP. Physicochemical properties that characterized the different environments of the OMZ and surface waters played a less important role than did geography in shaping the AOA community composition.
2013-06-20 | GSE46851 | GEO
Project description:Chemoautotrophic bacteria from the SUP05 clade often dominate anoxic waters in marine oxygen minimum zones (OMZs) where reduced sulfur can fuel carbon fixation and denitrification. Some members of the SUP05 clade are facultative aerobes that thrive at the boundaries of OMZs where they experience fluctuations in dissolved oxygen (DO). The degree to which SUP05 contribute to nitrate reduction in these regions depends on their sensitivity to oxygen. We evaluated growth and quantified differences in gene expression in Ca. T. autotrophicus strain EF1 from the SUP05 clade under high DO (22 μM), anoxic, and low DO (3.8 μM) concentrations. We show that strain EF1 cells respire oxygen and nitrate and that cells have higher growth rates, express more genes, and fix more carbon when oxygen becomes available for aerobic respiration. Evidence that facultatively aerobic SUP05 are more active and respire nitrate when oxygen becomes available at low concentrations suggests that they are an important source of nitrite across marine OMZ boundary layers.
2020-06-01 | GSE144480 | GEO
Project description:Cryptic Oxygen Cycle in the Oxygen Minimum Zones: the role of the Secondary Chlorophyll Maximum
| PRJNA305951 | ENA
Project description:marine oxygen minimum zones single-cell and community genomes Raw sequence reads
| PRJNA393056 | ENA
Project description:Marine microbial communities from expanding oxygen minimum zones in the Saanich Inlet - SI047_10m_RNA
| PRJNA324862 | ENA
Project description:Marine microbial communities from expanding oxygen minimum zones in the Saanich Inlet - SI047_100m_RNA
| PRJNA324863 | ENA