Abstract:Intense annual spring phytoplankton blooms and thermohaline stratification lead to anoxia in Chesapeake Bay bottom waters. Once oxygen becomes depleted in the system, microbial communities use energetically favourable alternative electron acceptors for respiration. The extent to which changes in respiration are reflected in community gene expression have only recently been investigated. Metatranscriptomes prepared from near-bottom water plankton over a 4-month time series in central Chesapeake Bay demonstrated… Show more
“…This pattern is consistent with a metatranscriptome analysis that showed lowest transcript ratios for denitrification in June before the onset of hypoxia and highest ratios in August when anoxia was most pronounced (Eggleston et al, 2015 Denitrification, as a major pathway of fixed nitrogen removal, is critical to mitigating eutrophication in natural waters.…”
Section: Active N2o Production By Denitrificationsupporting
Abstract. Nitrous oxide (N2O) is a greenhouse gas and an ozone depletion agent. One of the major uncertainties in the global N2O budget is the contribution of the coastal region, including estuaries, which can be sites of intense N2O efflux.Incubation experiments with nitrogen stable isotope tracer ( 15 N) enabled the investigation of the environmental controls of 10 N2O production in the water column of Chesapeake Bay, the largest estuary in North America. The highest potential rates of N2O production (7.5±1.2 nmol-N L -1 hr -1 ) were detected during summer anoxia, during which oxidized nitrogen species (nitrate and nitrite) were absent from the water column. At the top of the anoxic layer, N2O production from denitrification was stimulated by addition of nitrate and nitrite. The relative contribution of nitrate and nitrite to N2O production was positively correlated with the ratio of nitrate to nitrite concentrations. Increased oxygen availability, up to 7 µM oxygen 15 inhibited both N2O production and the reduction of nitrate to nitrite. Therefore, reducing the nitrogen input into the Chesapeake Bay has two potential impacts on the N2O efflux: In the short-term, N2O emission will be mitigated due to nitrogen deficiency. In the long-run, eutrophication will be alleviated and subsequent re-oxygenation of the bay will further inhibit N2O production.
“…This pattern is consistent with a metatranscriptome analysis that showed lowest transcript ratios for denitrification in June before the onset of hypoxia and highest ratios in August when anoxia was most pronounced (Eggleston et al, 2015 Denitrification, as a major pathway of fixed nitrogen removal, is critical to mitigating eutrophication in natural waters.…”
Section: Active N2o Production By Denitrificationsupporting
Abstract. Nitrous oxide (N2O) is a greenhouse gas and an ozone depletion agent. One of the major uncertainties in the global N2O budget is the contribution of the coastal region, including estuaries, which can be sites of intense N2O efflux.Incubation experiments with nitrogen stable isotope tracer ( 15 N) enabled the investigation of the environmental controls of 10 N2O production in the water column of Chesapeake Bay, the largest estuary in North America. The highest potential rates of N2O production (7.5±1.2 nmol-N L -1 hr -1 ) were detected during summer anoxia, during which oxidized nitrogen species (nitrate and nitrite) were absent from the water column. At the top of the anoxic layer, N2O production from denitrification was stimulated by addition of nitrate and nitrite. The relative contribution of nitrate and nitrite to N2O production was positively correlated with the ratio of nitrate to nitrite concentrations. Increased oxygen availability, up to 7 µM oxygen 15 inhibited both N2O production and the reduction of nitrate to nitrite. Therefore, reducing the nitrogen input into the Chesapeake Bay has two potential impacts on the N2O efflux: In the short-term, N2O emission will be mitigated due to nitrogen deficiency. In the long-run, eutrophication will be alleviated and subsequent re-oxygenation of the bay will further inhibit N2O production.
“…This contrasts with other environmental studies, where switches in expression of low-and high-affinity terminal oxidases have been observed over oxic-anoxic gradients. However, in other studies, the changes in O 2 concentration occurred at time scales of weeks, or over spatial scales of meters (Schunck et al, 2013;Hewson et al, 2014;Eggleston et al, 2015;Kalvelage et al, 2015). In permeable sediments, changes in O 2 concentration happen over minutes and hours and at spatial scales of millimeters to centimeters.…”
Section: Adaptations In the Microbial Community Leading To Aerobic Dementioning
Nitrogen (N) input to the coastal oceans has increased considerably because of anthropogenic activities, however, concurrent increases have not occurred in open oceans. It has been suggested that benthic denitrification in sandy coastal sediments is a sink for this N. Sandy sediments are dynamic permeable environments, where electron acceptor and donor concentrations fluctuate over short temporal and spatial scales. The response of denitrifiers to these fluctuations are largely unknown, although previous observations suggest they may denitrify under aerobic conditions. We examined the response of benthic denitrification to fluctuating oxygen concentrations, finding that denitrification not only occurred at high O concentrations but was stimulated by frequent switches between oxic and anoxic conditions. Throughout a tidal cycle, in situtranscription of genes for aerobic respiration and denitrification were positively correlated within diverse bacterial classes, regardless of O concentrations, indicating that denitrification gene transcription is not strongly regulated by O in sandy sediments. This allows microbes to respond rapidly to changing environmental conditions, but also means that denitrification is utilized as an auxiliary respiration under aerobic conditions when imbalances occur in electron donor and acceptor supply. Aerobic denitrification therefore contributes significantly to N-loss in permeable sediments making the process an important sink for anthropogenic N-inputs.
“…In stark contrast to higher organisms such as plants and animals, bacteria and archaea employ diverse and complex energy metabolic pathways (Kolber, 2007), which are adapted to and effective in diverse environments. Microbial communities select energetically favorable electron donors and acceptors from their environment for energy transduction (Bar-Even et al, 2012; Eggleston et al, 2015). Even so, energy may be a limited resource for certain marine ecosystems (Burgin et al, 2011; Moore et al, 2013; Vallino and Algar, 2016).…”
Transformation and mobilization of bioessential elements in the biosphere, lithosphere, atmosphere, and hydrosphere constitute the Earth's biogeochemical cycles, which are driven mainly by microorganisms through their energy and material metabolic processes. Without microbial energy harvesting from sources of light and inorganic chemical bonds for autotrophic fixation of inorganic carbon, there would not be sustainable ecosystems in the vast ocean. Although ecological energetics (eco-energetics) has been emphasized as a core aspect of ecosystem analyses and microorganisms largely control the flow of matter and energy in marine ecosystems, marine microbial communities are rarely studied from the eco-energetic perspective. The diverse bioenergetic pathways and eco-energetic strategies of the microorganisms are essentially the outcome of biosphere-geosphere interactions over evolutionary times. The biogeochemical cycles are intimately interconnected with energy fluxes across the biosphere and the capacity of the ocean to fix inorganic carbon is generally constrained by the availability of nutrients and energy. The understanding of how microbial eco-energetic processes influence the structure and function of marine ecosystems and how they interact with the changing environment is thus fundamental to a mechanistic and predictive understanding of the marine carbon and nitrogen cycles and the trends in global change. By using major groups of chemolithoautotrophic microorganisms that participate in the marine nitrogen cycle as examples, this article examines their eco-energetic strategies, contributions to carbon cycling, and putative responses to and impacts on the various global change processes associated with global warming, ocean acidification, eutrophication, deoxygenation, and pollution. We conclude that knowledge gaps remain despite decades of tremendous research efforts. The advent of new techniques may bring the dawn to scientific breakthroughs that necessitate the multidisciplinary combination of eco-energetic, biogeochemical and "omics" studies in this field.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.