... Michelle A Alting-mees, Eddy P Risseeuw, Enwu Liu, Michel Desautels, William A Crosby, Sean M... more ... Michelle A Alting-mees, Eddy P Risseeuw, Enwu Liu, Michel Desautels, William A Crosby, Sean M Hemmingsen in Yeast (2005). Save ... traditional pairwise analysis using tools such as the Basic Local Alignment Search Tool (BLAST) (6) and analysis using hidden Markov model ...
Philosophical Transactions of the Royal Society B: Biological Sciences, 2013
Ocean acidification (OA), caused by the dissolution of increasing concentrations of atmospheric c... more Ocean acidification (OA), caused by the dissolution of increasing concentrations of atmospheric carbon dioxide (CO 2 ) in seawater, is projected to cause significant changes to marine ecology and biogeochemistry. Potential impacts on the microbially driven cycling of nitrogen are of particular concern. Specifically, under seawater pH levels approximating future OA scenarios, rates of ammonia oxidation (the rate-limiting first step of the nitrification pathway) have been shown to dramatically decrease in seawater, but not in underlying sediments. However, no prior study has considered the interactive effects of microbial ammonia oxidation and macrofaunal bioturbation activity, which can enhance nitrogen transformation rates. Using experimental mesocosms, we investigated the responses to OA of ammonia oxidizing microorganisms inhabiting surface sediments and sediments within burrow walls of the mud shrimp Upogebia deltaura . Seawater was acidified to one of four target pH values (pH T...
Ocean acidification influences sediment/water nitrogen fluxes, possibly by impacting on the micro... more Ocean acidification influences sediment/water nitrogen fluxes, possibly by impacting on the microbial process of ammonia oxidation. To investigate this further, undisturbed sediment cores collected from Ny Alesund harbour (Svalbard) were incubated with seawater adjusted to CO2 concentrations of 380, 540, 760, 1,120 and 3,000 µatm. DNA and RNA were extracted from the sediment surface after 14 days' exposure and the abundance of bacterial and archaeal ammonia oxidising (amoA) genes and transcripts quantified using quantitative polymerase chain reaction. While there was no change to the abundance of bacterial amoA genes, an increase to 760 µatm pCO2 reduced the abundance of bacterial amoA transcripts by 65 %, and this was accompanied by a shift in the composition of the active community. In contrast, archaeal amoA gene and transcript abundance both doubled at 3,000 µatm, with an increase in species richness also apparent. This suggests that ammonia oxidising bacteria and archaea in marine sediments have different pH optima, and the impact of elevated CO2 on N cycling may be dependent on the relative abundances of these two major microbial groups. Further evidence of a shift in the balance of key N cycling groups was also evident: the abundance of nirS-type denitrifier transcripts decreased alongside bacterial amoA transcripts, indicating that NO3− produced by bacterial nitrification fuelled denitrification. An increase in the abundance of Planctomycete-specific 16S rRNA, the vast majority of which grouped with known anammox bacteria, was also apparent at 3,000 µatm pCO2. This could indicate a possible shift from coupled nitrification–denitrification to anammox activity at elevated CO2.
Effects of ocean acidification on the composition of the active bacterial and archaeal community ... more Effects of ocean acidification on the composition of the active bacterial and archaeal community within Arctic surface sediment was analysed in detail using 16S rRNA 454 pyrosequencing. Intact sediment cores were collected and exposed to one of five different pCO(2) concentrations [380 (present day), 540, 750, 1120 and 3000 μatm] and RNA extracted after a period of 14 days exposure. Measurements of diversity and multivariate similarity indicated very little difference between pCO(2) treatments. Only when the highest and lowest pCO(2) treatments were compared were significant differences evident, namely increases in the abundance of operational taxonomic units most closely related to the Halobacteria and differences to the presence/absence structure of the Planctomycetes. The relative abundance of members of the classes Planctomycetacia and Nitrospira increased with increasing pCO(2) concentration, indicating that these groups may be able to take advantage of changing pH or pCO(2) conditions. The modest response of the active microbial communities associated with these sediments may be due to the low and fluctuating pore-water pH already experienced by sediment microbes, a result of the pH buffering capacity of marine sediments, or due to currently unknown factors. Further research is required to fully understand the impact of elevated CO(2) on sediment physicochemical parameters, biogeochemistry and microbial community dynamics.
Sediments play a key role in the marine nitrogen cycle and can act either as a source or a sink o... more Sediments play a key role in the marine nitrogen cycle and can act either as a source or a sink of biologically available (fixed) nitrogen. This cycling is driven by a number of microbial remineralization reactions, many of which occur across the oxic/anoxic interface near the sediment surface. The presence and activity of large burrowing macrofauna (bioturbators) in the sediment can significantly affect these microbial processes by altering the physicochemical properties of the sediment. For example, the building and irrigation of burrows by bioturbators introduces fresh oxygenated water into deeper sediment layers and allows the exchange of solutes between the sediment and water column. Burrows can effectively extend the oxic/anoxic interface into deeper sediment layers, thus providing a unique environment for nitrogen-cycling microbial communities. Recent studies have shown that the abundance and diversity of micro-organisms can be far greater in burrow wall sediment than in the ...
Like both terrestrial plants and other benthic marine organisms, seagrasses host abundant and div... more Like both terrestrial plants and other benthic marine organisms, seagrasses host abundant and diverse communities of microorganisms. These microbes fundamentally influence seagrass physiology and health, while also regulating the biogeochemical dynamics of entire seagrass meadows. Discrete populations of bacteria, fungi, microalgae, archaea and viruses inhabit seagrass leaves, roots and rhizomes and the surrounding sediments. The plethora of ecological interactions taking place between seagrasses and this microbiome span the continuum of symbiotic relationships from mutualism to parasitism. Indeed, the metabolic activities of some seagrass associated microbes, such as diazotrophic and sulphur oxidizing bacteria, govern the local chemical environment in ways that facilitate seagrass survival. On the other hand, pathogens, such as the protozoan parasite Labyrinthula cause disease outbreaks that can lead to mass seagrass die offs. While the role of the seagrass microbiome in defining the success of seagrass habitats is becoming increasingly apparent, there is still much to be learnt. For instance, the development of an understanding of how seagrass associated microbes may buffer or augment the negative impacts of growing environmental pressures will be valuable for informing decisions regarding the management and conservation of threatened seagrass habitats. In this chapter we will synthesise the current state of knowledge on the microbiology of seagrasses, with a goal of conveying the often overlooked importance of the seagrass microbiome in governing seagrass health and the biogeochemical stability of seagrass ecosystems.
Sustained observations of microbial dynamics are rare, especially in southern hemisphere waters. ... more Sustained observations of microbial dynamics are rare, especially in southern hemisphere waters. The Australian Marine Microbial Biodiversity Initiative (AMMBI) provides methodologically standardized, continental scale, temporal phylogenetic amplicon sequencing data describing Bacteria, Archaea and microbial Eukarya assemblages. Sequence data is linked to extensive physical, biological and chemical oceanographic contextual information. Samples are collected monthly to seasonally from multiple depths at seven sites: Darwin Harbour (Northern Territory), Yongala (Queensland), North Stradbroke Island (Queensland), Port Hacking (New South Wales), Maria Island (Tasmania), Kangaroo Island (South Australia), Rottnest Island (Western Australia). These sites span ~30° of latitude and ~38° longitude, range from tropical to cold temperate zones, and are influenced by both local and globally significant oceanographic and climatic features. All sequence datasets are provided in both raw and proce...
... Michelle A Alting-mees, Eddy P Risseeuw, Enwu Liu, Michel Desautels, William A Crosby, Sean M... more ... Michelle A Alting-mees, Eddy P Risseeuw, Enwu Liu, Michel Desautels, William A Crosby, Sean M Hemmingsen in Yeast (2005). Save ... traditional pairwise analysis using tools such as the Basic Local Alignment Search Tool (BLAST) (6) and analysis using hidden Markov model ...
Philosophical Transactions of the Royal Society B: Biological Sciences, 2013
Ocean acidification (OA), caused by the dissolution of increasing concentrations of atmospheric c... more Ocean acidification (OA), caused by the dissolution of increasing concentrations of atmospheric carbon dioxide (CO 2 ) in seawater, is projected to cause significant changes to marine ecology and biogeochemistry. Potential impacts on the microbially driven cycling of nitrogen are of particular concern. Specifically, under seawater pH levels approximating future OA scenarios, rates of ammonia oxidation (the rate-limiting first step of the nitrification pathway) have been shown to dramatically decrease in seawater, but not in underlying sediments. However, no prior study has considered the interactive effects of microbial ammonia oxidation and macrofaunal bioturbation activity, which can enhance nitrogen transformation rates. Using experimental mesocosms, we investigated the responses to OA of ammonia oxidizing microorganisms inhabiting surface sediments and sediments within burrow walls of the mud shrimp Upogebia deltaura . Seawater was acidified to one of four target pH values (pH T...
Ocean acidification influences sediment/water nitrogen fluxes, possibly by impacting on the micro... more Ocean acidification influences sediment/water nitrogen fluxes, possibly by impacting on the microbial process of ammonia oxidation. To investigate this further, undisturbed sediment cores collected from Ny Alesund harbour (Svalbard) were incubated with seawater adjusted to CO2 concentrations of 380, 540, 760, 1,120 and 3,000 µatm. DNA and RNA were extracted from the sediment surface after 14 days' exposure and the abundance of bacterial and archaeal ammonia oxidising (amoA) genes and transcripts quantified using quantitative polymerase chain reaction. While there was no change to the abundance of bacterial amoA genes, an increase to 760 µatm pCO2 reduced the abundance of bacterial amoA transcripts by 65 %, and this was accompanied by a shift in the composition of the active community. In contrast, archaeal amoA gene and transcript abundance both doubled at 3,000 µatm, with an increase in species richness also apparent. This suggests that ammonia oxidising bacteria and archaea in marine sediments have different pH optima, and the impact of elevated CO2 on N cycling may be dependent on the relative abundances of these two major microbial groups. Further evidence of a shift in the balance of key N cycling groups was also evident: the abundance of nirS-type denitrifier transcripts decreased alongside bacterial amoA transcripts, indicating that NO3− produced by bacterial nitrification fuelled denitrification. An increase in the abundance of Planctomycete-specific 16S rRNA, the vast majority of which grouped with known anammox bacteria, was also apparent at 3,000 µatm pCO2. This could indicate a possible shift from coupled nitrification–denitrification to anammox activity at elevated CO2.
Effects of ocean acidification on the composition of the active bacterial and archaeal community ... more Effects of ocean acidification on the composition of the active bacterial and archaeal community within Arctic surface sediment was analysed in detail using 16S rRNA 454 pyrosequencing. Intact sediment cores were collected and exposed to one of five different pCO(2) concentrations [380 (present day), 540, 750, 1120 and 3000 μatm] and RNA extracted after a period of 14 days exposure. Measurements of diversity and multivariate similarity indicated very little difference between pCO(2) treatments. Only when the highest and lowest pCO(2) treatments were compared were significant differences evident, namely increases in the abundance of operational taxonomic units most closely related to the Halobacteria and differences to the presence/absence structure of the Planctomycetes. The relative abundance of members of the classes Planctomycetacia and Nitrospira increased with increasing pCO(2) concentration, indicating that these groups may be able to take advantage of changing pH or pCO(2) conditions. The modest response of the active microbial communities associated with these sediments may be due to the low and fluctuating pore-water pH already experienced by sediment microbes, a result of the pH buffering capacity of marine sediments, or due to currently unknown factors. Further research is required to fully understand the impact of elevated CO(2) on sediment physicochemical parameters, biogeochemistry and microbial community dynamics.
Sediments play a key role in the marine nitrogen cycle and can act either as a source or a sink o... more Sediments play a key role in the marine nitrogen cycle and can act either as a source or a sink of biologically available (fixed) nitrogen. This cycling is driven by a number of microbial remineralization reactions, many of which occur across the oxic/anoxic interface near the sediment surface. The presence and activity of large burrowing macrofauna (bioturbators) in the sediment can significantly affect these microbial processes by altering the physicochemical properties of the sediment. For example, the building and irrigation of burrows by bioturbators introduces fresh oxygenated water into deeper sediment layers and allows the exchange of solutes between the sediment and water column. Burrows can effectively extend the oxic/anoxic interface into deeper sediment layers, thus providing a unique environment for nitrogen-cycling microbial communities. Recent studies have shown that the abundance and diversity of micro-organisms can be far greater in burrow wall sediment than in the ...
Like both terrestrial plants and other benthic marine organisms, seagrasses host abundant and div... more Like both terrestrial plants and other benthic marine organisms, seagrasses host abundant and diverse communities of microorganisms. These microbes fundamentally influence seagrass physiology and health, while also regulating the biogeochemical dynamics of entire seagrass meadows. Discrete populations of bacteria, fungi, microalgae, archaea and viruses inhabit seagrass leaves, roots and rhizomes and the surrounding sediments. The plethora of ecological interactions taking place between seagrasses and this microbiome span the continuum of symbiotic relationships from mutualism to parasitism. Indeed, the metabolic activities of some seagrass associated microbes, such as diazotrophic and sulphur oxidizing bacteria, govern the local chemical environment in ways that facilitate seagrass survival. On the other hand, pathogens, such as the protozoan parasite Labyrinthula cause disease outbreaks that can lead to mass seagrass die offs. While the role of the seagrass microbiome in defining the success of seagrass habitats is becoming increasingly apparent, there is still much to be learnt. For instance, the development of an understanding of how seagrass associated microbes may buffer or augment the negative impacts of growing environmental pressures will be valuable for informing decisions regarding the management and conservation of threatened seagrass habitats. In this chapter we will synthesise the current state of knowledge on the microbiology of seagrasses, with a goal of conveying the often overlooked importance of the seagrass microbiome in governing seagrass health and the biogeochemical stability of seagrass ecosystems.
Sustained observations of microbial dynamics are rare, especially in southern hemisphere waters. ... more Sustained observations of microbial dynamics are rare, especially in southern hemisphere waters. The Australian Marine Microbial Biodiversity Initiative (AMMBI) provides methodologically standardized, continental scale, temporal phylogenetic amplicon sequencing data describing Bacteria, Archaea and microbial Eukarya assemblages. Sequence data is linked to extensive physical, biological and chemical oceanographic contextual information. Samples are collected monthly to seasonally from multiple depths at seven sites: Darwin Harbour (Northern Territory), Yongala (Queensland), North Stradbroke Island (Queensland), Port Hacking (New South Wales), Maria Island (Tasmania), Kangaroo Island (South Australia), Rottnest Island (Western Australia). These sites span ~30° of latitude and ~38° longitude, range from tropical to cold temperate zones, and are influenced by both local and globally significant oceanographic and climatic features. All sequence datasets are provided in both raw and proce...
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