Depth Distribution of Ammonia Oxidation Rates and Ammonia-Oxidizer Community Composition in the Sargasso Sea
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ABSTRACT:
ORGANISM(S): synthetic construct
SUBMITTER: Silvia Newell
PROVIDER: E-GEOD-42287 | biostudies-arrayexpress |
REPOSITORIES: biostudies-arrayexpress
Similar Datasets
Project description:The Baltic Sea is one of the largest brackish water bodies in the world. Redoxclines that form between oxic and anoxic layers in the deepest sub-basins are a semi-permanent character of the pelagic Baltic Sea. The microbially mediated nitrogen removal processes in these redoxclines have been recognized as important ecosystem service that removes large proportion of the nitrogen load originating from the drainage basin. However, nitrification, which links mineralization of organic nitrogen and nitrogen removal processes, has remained poorly understood. To gain better understanding of the nitrogen cycling in the Baltic Sea, we analyzed the assemblage of ammonia oxidizing bacteria and archaea in the central Baltic Sea using functional gene microarrays and measured the biogeochemical properties along with potential nitrification rates. Overall, the ammonia oxidizer communities in the Baltic Sea redoxcline were very evenly distributed. However, the communities were clearly different between the eastern and western Gotland Basin and the correlations between different components of the ammonia oxidizer assemblages and environmental variables suggest ecological basis for the community composition. The more even community ammonia oxidizer composition in the eastern Gotland Basin may be related to the constantly oscillating redoxcline that does not allow domination of single archetype. The oscillating redoxcline also creates long depth range of optimal nitrification conditions. The rate measurements suggest that nitrification in the central Baltic Sea is able to produce all nitrate required by denitrification occurring below the nitrification zone. Two color array (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5. Three replicate probes were printed for each archetype. Two replicate arrays were run on duplicate targets.
2013-08-24 | E-GEOD-50164 | biostudies-arrayexpress
Project description:Ammonia-oxidizing archaeal (AOA) amoA diversity and relative abundance in Gulf of Mexico sediments (0-2 cm) were investigated using a functional gene microarray; a two color array with a universal internal standard Two color array (cy3 and cy5): the universal standard 20 bp oligo (fluoresced with cy5) is printed to the slide with a 70-mer. Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer will bind to it. Signal is the cy3/cy5. Up to four arrays per sample, with two biological replicates made into two targets, each run on duplicate arrays.
2013-03-01 | E-GEOD-42286 | biostudies-arrayexpress
Project description:Increasing atmospheric CO2 concentrations are causing decreased pH over vast expanses of the ocean. This decreasing pH may alter biogeochemical cycling of carbon and nitrogen via the microbial process of nitrification, a key process that couples these cycles in the ocean, but which is often sensitive to acidic conditions. Recent reports indicate a decrease in oceanic nitrification rates under experimentally lowered pH. How composition and abundance of ammonia oxidizing bacteria (AOB) and archaea (AOA) assemblages respond to decreasing oceanic pH, however, is unknown. We sampled microbes from two different acidification experiments and used a combination of qPCR and functional gene microarrays for the ammonia monooxygenase gene (amoA) to assess how acidification alters the structure of ammonia oxidizer assemblages. We show that despite widely different experimental conditions, acidification consistently altered the community composition of AOB by increasing the relative abundance of taxa related to the Nitrosomonas ureae clade. In one experiment this increase was sufficient to cause an increase in the overall abundance of AOB. There were no systematic shifts in the community structure or abundance of AOA in either experiment. These different responses to acidification underscore the important role of microbial community structure in the resiliency of marine ecosystems. amoA gene diversity from two ocean acidification experiments, Monterey Bay experiment (two time points, ambient and acidified) and Vineyard Sound experiment (ambient and acifidied, with and without nutrients) examined with 2 two-color arrays (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5.
2013-08-27 | E-GEOD-49956 | biostudies-arrayexpress
Project description:The abundance of bacterial (AOB) and archaeal (AOA) ammonia oxidisers, assessed using quantitative PCR measurements of their respective a-subunit of the ammonia monooxygenase (amoA) genes, and ammonia oxidation rates were measured in four contrasting coastal sediments in the Western English Channel. Sediment was sampled bimonthly from July 2008 to May 2011, and measurements of ammonia oxidiser abundance and activity compared to a range of environmental variables including salinity, temperature, water column nutrients and sediment carbon and nitrogen content. Despite a higher abundance of AOA amoA genes within all sediments, and at all time-points, rates of ammonia oxidation correlated with AOB and not AOA amoA gene abundance. Other than ammonia oxidation rate, sediment particle size was the only variable that correlated with the spatial and temporal patterns of AOB amoA gene abundance, implying a preference of the AOB for larger sediment particles. This is possibly due to deeper oxygen penetration into the sandier sediments, increasing the area available for ammonia oxidation to occur, higher concentrations of inhibitory sulphide with pore waters of muddier sediments or a combination of both oxygen and sulphide concentrations. Similar to many other temporal studies of nitrification within estuarine and coastal sediments, decreases in AOB amoA gene abundance were evident during summer and autumn, with maximum abundance and ammonia oxidation rates occurring in winter and early spring. The lack of correlation between AOA amoA gene abundance and ammonium oxidation rate suggests an alternative role for amoAÂ-carrying AOA within these sediments. Two color array (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5. Three replicate probes were printed for each archetype. Two replicate arrays were run on duplicate targets.
2013-08-24 | E-GEOD-50163 | biostudies-arrayexpress
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. Two-color array (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5. Three replicate probes were printed for each archetype. Two replicate arrays were run on duplicate targets.
2013-06-20 | E-GEOD-46851 | biostudies-arrayexpress
Project description:Coastal marine sediments, as locations of substantial fixed nitrogen loss, are very important to the nitrogen budget and to the primary productivity of the oceans. Coastal sediment systems are also highly dynamic and subject to periodic natural and anthropogenic organic substrate additions. The response to organic matter by the microbial community involved in nitrogen loss processes was evaluated using mesocosms of Chesapeake Bay sediments. Over the course of a 50-day incubation, rates of anammox and denitrification were measured weekly using 15N tracer incubations, and samples were collected for genetic analysis. Rates of both nitrogen loss processes and gene abundances associated with them corresponded loosely, probably because heterogeneities in sediments obscured a clear relationship. The rates of denitrification were stimulated more by the higher organic matter addition, and the fraction of nitrogen loss attributed to anammox slightly reduced. Furthermore, the large organic matter pulse drove a significant and rapid shift in the denitrifier community as determined using a nirS microarray, indicating the diversity of these organisms plays an essential role in responding to anthropogenic inputs. We also suggest that the proportion of nitrogen loss due to anammox in these coastal estuarine sediments may be underestimated due to temporal dynamics as well as from methodological artifacts related to conventional sediment slurry incubation approaches. Two color array (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5. Three replicate probes were printed for each archetype. Two replicate arrays were run on duplicate targets.
2015-01-30 | E-GEOD-65430 | biostudies-arrayexpress
Project description:The community composition (in terms of abundance, distribution and contribution of diverse clades) of bacteria involved in nitrogen transformations in the oxygen minimum zones may be related to the rates of fixed N loss in these systems. The abundance of both denirifying and anammox bacteria, and the assemblage composition of denitrifying bacteria were investigated in the Eastern Tropical South Pacific and the Arabian Sea using assays based on molecular markers for the two groups of bacteria. The abundance and distribution of bacteria associated with the fixed N removal processes denitrification and anammox were investigated using quantitative PCR for genes encoding nitrite reductase (nirK and nirS) in denitrifying bacteria and hydrazine oxidase(hzo) and 16S rRNA genesin anammox bacteria. All of these genes had depth distributions with maxima associated with the secondary nitrite maximum in low oxygen waters. NirS was mch more abundant than nirK, and much more abundant than the 16S rRNA gene from anammox bacteria. The ratio of hzo:16S rRNA for anammox was low and variable implying greater unexplored diversity in the the hzo gene. Assemblage composition of the abundant nirS-type denitrifiers was evaluated using a funcitonal gene microarray. Of the nirS archetypes represented on the microarray, very few occurred speficically in one region or depth interval, but the assemblages varied significantly. Community composition of denitrifiers based on microarray analysis of the nirS gene was most different between geographical regions. Within each region, the surface layer and OMZ assemblages clustered distinctly. Thus, in addition to spatial and temporal variation in denitrificaiton and anammox rates, both microbial abundance and community composition also vary between OMZ regions and depths. Two color array (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5. Three replicate probes were printed for each archetype. Two replicate arrays were run on duplicate targets.
2013-09-12 | E-GEOD-50787 | biostudies-arrayexpress
Project description:P. aeruginosa PAO wildtype Cy3 PA3898 mutant Cy5
| PRJNA491282 | ENA
Project description:Ammonia oxidizer community structure were examined in a depth profile from 20 to 2000 m at the Bermuda Atlantic Time-series Study using a functional gene microarray to look at amoA diversity
2012-11-15 | GSE42287 | GEO
Project description:Sample groupings for this project are as follows: Cauline leaf vs Cultured Cell : - Cauline leaf, p1; Exp:Red; Ref: Green (Cy5:Cy3) - Cauline leaf, p2; Exp:Red; Ref: Green (Cy5:Cy3) - Cauline leaf, p3; Exp:Red; Ref: Green (Cy5:Cy3) Cotyledon light vs Cotyledon dark : - Cotyledon, CP1; Exp:Red; Ref: Green (Cy5:Cy3) - Cotyledon, CP2; Exp:Red; Ref: Green (Cy5:Cy3) Cotyledon light vs Cultured cell : - Cotyledon, cn1; Exp:Green; Ref: Red (Cy3:Cy5) - Cotyledon, cn2; Exp:Green; Ref: Red (Cy3:Cy5) Cotyledon dark vs Cultured cell : - Cotyledon dark, n1; Exp:Green; Ref: Red (Cy3:Cy5) - Cotyledon dark, n2; Exp:Green; Ref: Red (Cy3:Cy5) - Cotyledon dark, n3; Exp:Green; Ref: Red (Cy3:Cy5) Germinating seed vs Cultured cell : - Germinating seed, gn1; Exp:Green; Ref: Red (Cy3:Cy5) - Germinating seed, gn2; Exp:Green; Ref: Red (Cy3:Cy5) - Germinating seed, gn3; Exp:Green; Ref: Red (Cy3:Cy5) Hypocotyl light vs Hypocotyl dark : - Hypocotyl, hldn1; Exp:Red; Ref: Green (Cy5:Cy3) - Hypocotyl, hldn2; Exp:Red; Ref: Green (Cy5:Cy3) Hypocotyl light vs Cultured cell : - Hypocotyl light, hln1; Exp:Green; Ref: Red (Cy3:Cy5) - Hypocotyl light, hln2; Exp:Green; Ref: Red (Cy3:Cy5) Petal vs Cultured cell : - Petal, pn1; Exp:Green; Ref: Red (Cy3:Cy5) - Petal, pn2; Exp:Green; Ref: Red (Cy3:Cy5) - Petal, pn3; Exp:Green; Ref: Red (Cy3:Cy5) 1DBP vs Cultured cell : - Pistil 1DBP, pin1; Exp:Green; Ref: Red (Cy3:Cy5) - Pistil 1DBP, pin2; Exp:Green; Ref: Red (Cy3:Cy5) - Pistil 1DBP, pin3; Exp:Green; Ref: Red (Cy3:Cy5) Pistil 1DPP vs Cultured cell : - Pistil 1DPP, psn1; Exp:Green; Ref: Red (Cy3:Cy5) - Pistil 1DPP, psn2; Exp:Green; Ref: Red (Cy3:Cy5) - Pistil 1DPP, psn3; Exp:Green; Ref: Red (Cy3:Cy5) - Pistil 1DPP, psn4; Exp:Green; Ref: Red (Cy3:Cy5) Root dark vs Cultured cell : - Root dark, rdn1; Exp:Green; Ref: Red (Cy3:Cy5) - Root dark, rdn2; Exp:Green; Ref: Red (Cy3:Cy5) Root light vs Cultured cell : - Root light, rln1; Exp:Green; Ref: Red (Cy3:Cy5) - Root light, rlp1; Exp:Red; Ref: Green (Cy5:Cy3) Root light vs Root dark : - Root light vs dark, rldp1; Exp:Red; Ref: Green (Cy5:Cy3) - Root light vs dark, rldp2; Exp:Red; Ref: Green (Cy5:Cy3) Rosette leaf vs Cultured cell : - Rosette leaf, rfp1; Exp:Red; Ref: Green (Cy5:Cy3) - Rosette leaf, rfp2; Exp:Red; Ref: Green (Cy5:Cy3) - Rosette leaf, rfp3; Exp:Red; Ref: Green (Cy5:Cy3) Sepal vs Cultured cell : - Sepal, sn1; Exp:Green; Ref: Red (Cy3:Cy5) - Sepal, sn2; Exp:Green; Ref: Red (Cy3:Cy5) Silique 3DPP vs Cultured cell : - Silique 3DPP, s3n1; Exp:Green; Ref: Red (Cy3:Cy5) - Silique 3DPP, s3n2; Exp:Green; Ref: Red (Cy3:Cy5) - Silique 3DPP, s3n3; Exp:Green; Ref: Red (Cy3:Cy5) Silique 8DPP vs Cultured cell : - Silique 8DPP, s8n1; Exp:Green; Ref: Red (Cy3:Cy5) - Silique 8DPP, s8n2; Exp:Green; Ref: Red (Cy3:Cy5) - Silique 8DPP, s8n3; Exp:Green; Ref: Red (Cy3:Cy5) Stamen vs Cultured cell : - Stamen, smn1; Exp:Green; Ref: Red (Cy3:Cy5) - Stamen, smn2; Exp:Green; Ref: Red (Cy3:Cy5) - Stamen, smn3; Exp:Green; Ref: Red (Cy3:Cy5) Hypocotyl dark vs Cultured cell : - Hypocotyl dark, hn1; Exp:Green; Ref: Red (Cy3:Cy5) - Hypocotyl dark, hn2; Exp:Green; Ref: Red (Cy3:Cy5) Stem vs Cultured cell : - Stem, stp1; Exp:Red; Ref: Green (Cy5:Cy3) - Stem, stp2; Exp:Red; Ref: Green (Cy5:Cy3) - Stem, stp3; Exp:Red; Ref: Green (Cy5:Cy3) Keywords: other
2004-10-24 | GSE1599 | GEO