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  • 1
    Online Resource
    Online Resource
    Proceedings of the National Academy of Sciences ; 2021
    In:  Proceedings of the National Academy of Sciences Vol. 118, No. 12 ( 2021-03-23)
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 118, No. 12 ( 2021-03-23)
    Abstract: The ocean is a reservoir for CFC-11, a major ozone-depleting chemical. Anthropogenic production of CFC-11 dramatically decreased in the 1990s under the Montreal Protocol, which stipulated a global phase out of production by 2010. However, studies raise questions about current overall emission levels and indicate unexpected increases of CFC-11 emissions of about 10 Gg ⋅ yr −1 after 2013 (based upon measured atmospheric concentrations and an assumed atmospheric lifetime). These findings heighten the need to understand processes that could affect the CFC-11 lifetime, including ocean fluxes. We evaluate how ocean uptake and release through 2300 affects CFC-11 lifetimes, emission estimates, and the long-term return of CFC-11 from the ocean reservoir. We show that ocean uptake yields a shorter total lifetime and larger inferred emission of atmospheric CFC-11 from 1930 to 2075 compared to estimates using only atmospheric processes. Ocean flux changes over time result in small but not completely negligible effects on the calculated unexpected emissions change (decreasing it by 0.4 ± 0.3 Gg ⋅ yr −1 ). Moreover, it is expected that the ocean will eventually become a source of CFC-11, increasing its total lifetime thereafter. Ocean outgassing should produce detectable increases in global atmospheric CFC-11 abundances by the mid-2100s, with emission of around 0.5 Gg ⋅ yr −1 ; this should not be confused with illicit production at that time. An illustrative model projection suggests that climate change is expected to make the ocean a weaker reservoir for CFC-11, advancing the detectable change in the global atmospheric mixing ratio by about 5 yr.
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
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    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2021
    detail.hit.zdb_id: 209104-5
    detail.hit.zdb_id: 1461794-8
    SSG: 11
    SSG: 12
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2019
    In:  Geochemistry, Geophysics, Geosystems Vol. 20, No. 4 ( 2019-04), p. 2021-2039
    In: Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 20, No. 4 ( 2019-04), p. 2021-2039
    Abstract: Nitrate and nitrite ( ) are relevant to prebiotic chemistry; past work has argued these molecules were abundant in the early ocean Fe 2+ and UV suppress [ ] to much lower concentrations than previously thought in the ocean; [ ] could have been higher in ponds Most should have been nitrate; prebiotic chemistries that use nitrate are more plausible than those that use nitrite
    Type of Medium: Online Resource
    ISSN: 1525-2027 , 1525-2027
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2019
    detail.hit.zdb_id: 2027201-7
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  • 3
    Online Resource
    Online Resource
    American Society for Microbiology ; 2023
    In:  Applied and Environmental Microbiology Vol. 89, No. 8 ( 2023-08-30)
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 89, No. 8 ( 2023-08-30)
    Abstract: Bacteria specialized in anaerobic ammonium oxidation (anammox) are widespread in many anoxic habitats and form an important functional guild in the global nitrogen cycle by consuming bio-available nitrogen for energy rather than biomass production. Due to their slow growth rates, cultivation-independent approaches have been used to decipher their diversity across environments. However, their full diversity has not been well recognized. Here, we report a new family of putative anammox bacteria, “ Candidatus Subterrananammoxibiaceae,” existing in the globally distributed terrestrial and marine subsurface (groundwater and sediments of estuary, deep-sea, and hadal trenches). We recovered a high-quality metagenome-assembled genome of this family, tentatively named “ Candidatus Subterrananammoxibius californiae,” from a California groundwater site. The “ Ca. Subterrananammoxibius californiae” genome not only contains genes for all essential components of anammox metabolism (e.g., hydrazine synthase, hydrazine oxidoreductase, nitrite reductase, and nitrite oxidoreductase) but also has the capacity for urea hydrolysis. In an Arctic ridge sediment core where redox zonation is well resolved, “ Ca. Subterrananammoxibiaceae” is confined within the nitrate-ammonium transition zone where the anammox rate maximum occurs, providing environmental proof of the anammox activity of this new family. Phylogenetic analysis of nitrite oxidoreductase suggests that a horizontal transfer facilitated the spreading of the nitrite oxidation capacity between anammox bacteria (in the Planctomycetota phylum) and nitrite-oxidizing bacteria from Nitrospirota and Nitrospinota . By recognizing this new anammox family, we propose that all lineages within the “ Ca. Brocadiales” order have anammox capacity. IMPORTANCE Microorganisms called anammox bacteria are efficient in removing bioavailable nitrogen from many natural and human-made environments. They exist in almost every anoxic habitat where both ammonium and nitrate/nitrite are present. However, only a few anammox bacteria have been cultured in laboratory settings, and their full phylogenetic diversity has not been recognized. Here, we present a new bacterial family whose members are present across both the terrestrial and marine subsurface. By reconstructing a high-quality genome from the groundwater environment, we demonstrate that this family has all critical enzymes of anammox metabolism and, notably, also urea utilization. This bacterium family in marine sediments is also preferably present in the niche where the anammox process occurs. These findings suggest that this novel family, named “ Candidatus Subterrananammoxibiaceae,” is an overlooked group of anammox bacteria, which should have impacts on nitrogen cycling in a range of environments.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
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    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 2023
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    detail.hit.zdb_id: 1478346-0
    SSG: 12
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  • 4
    Online Resource
    Online Resource
    Journal of Marine Research/Yale ; 2015
    In:  Journal of Marine Research Vol. 73, No. 3 ( 2015-05-01), p. 71-92
    In: Journal of Marine Research, Journal of Marine Research/Yale, Vol. 73, No. 3 ( 2015-05-01), p. 71-92
    Abstract: Nitrous oxide (N 2 O) is important to Earth's climate because it is a strong absorber of radiation and an important ozone depletion agent. Increasing anthropogenic nitrogen input into the marine environment, especially to coastal waters, has led to increasing N 2 O emissions. Identifying the nitrogen compounds that serve as substrates for N 2 O production in coastal waters reveals important pathways and helps us understand their control by environmental factors. In this study, sediments were collected from a long-term fertilization site in Great Sippewissett Marsh, Falmouth, Massachusetts. The 15 N tracer incubation time course experiments were conducted and analyzed for potential N 2 O production and consumption rates. The two nitrogen substrates of N 2 O production, ammonium and nitrate, correspond to the two production pathways, nitrification and denitrification, respectively. When measurable nitrate was present, despite ambient high ammonium concentrations, denitrification was the major N 2 O production pathway. When nitrate was absent, ammonium became the dominant substrate for N 2 O production, via nitrification and coupled nitrification-denitrification. Net N 2 O consumption was enhanced under low oxygen and nitrate conditions. N 2 O production and consumption rates increased with increasing levels of nitrogen fertilization in long-term experimental plots. These results indicate that increasing anthropogenic nitrogen input to salt marshes can stimulate sedimentary N 2 O production via both nitrification and denitrification, whereas episodic oxygen depletion results in net N 2 O consumption.
    Type of Medium: Online Resource
    ISSN: 0022-2402
    Language: English
    Publisher: Journal of Marine Research/Yale
    Publication Date: 2015
    detail.hit.zdb_id: 410655-6
    detail.hit.zdb_id: 2066603-2
    SSG: 12
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  • 5
    Online Resource
    Online Resource
    American Association for the Advancement of Science (AAAS) ; 2015
    In:  Science Vol. 348, No. 6239 ( 2015-06-05), p. 1127-1129
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 348, No. 6239 ( 2015-06-05), p. 1127-1129
    Abstract: Nitrous oxide (N 2 O) is a powerful greenhouse gas and a major cause of stratospheric ozone depletion, yet its sources and sinks remain poorly quantified in the oceans. We used isotope tracers to directly measure N 2 O reduction rates in the eastern tropical North Pacific. Because of incomplete denitrification, N 2 O cycling rates are an order of magnitude higher than predicted by current models in suboxic regions, and the spatial distribution suggests strong dependence on both organic carbon and dissolved oxygen concentrations. Furthermore, N 2 O turnover is 20 times higher than the net atmospheric efflux. The rapid rate of this cycling coupled to an expected expansion of suboxic ocean waters implies future increases in N 2 O emissions.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2015
    detail.hit.zdb_id: 128410-1
    detail.hit.zdb_id: 2066996-3
    detail.hit.zdb_id: 2060783-0
    SSG: 11
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2017
    In:  Global Biogeochemical Cycles Vol. 31, No. 2 ( 2017-02), p. 258-271
    In: Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 31, No. 2 ( 2017-02), p. 258-271
    Abstract: Directly measured in situ rates produce the broad nitrogen profiles in ODZs assuming contributions from both anammox and denitrification Nitrite and nitrate are rapidly cycled in ODZs, and iodate stimulates nitrite oxidation in the upper ODZ Cyanate can act as a reduced nitrogen source for anammox, while urea is not directly used
    Type of Medium: Online Resource
    ISSN: 0886-6236 , 1944-9224
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2017
    detail.hit.zdb_id: 2021601-4
    SSG: 12
    SSG: 13
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  • 7
    Online Resource
    Online Resource
    Oxford University Press (OUP) ; 2023
    In:  PNAS Nexus Vol. 2, No. 2 ( 2023-02-03)
    In: PNAS Nexus, Oxford University Press (OUP), Vol. 2, No. 2 ( 2023-02-03)
    Abstract: Particulate organic carbon settling through the marine water column is a key process that regulates the global climate by sequestering atmospheric carbon. The initial colonization of marine particles by heterotrophic bacteria represents the first step in recycling this carbon back to inorganic constituents—setting the magnitude of vertical carbon transport to the abyss. Here, we demonstrate experimentally using millifluidic devices that, although bacterial motility is essential for effective colonization of a particle leaking organic nutrients into the water column, chemotaxis specifically benefits at intermediate and higher settling velocities to navigate the particle boundary layer during the brief window of opportunity provided by a passing particle. We develop an individual-based model that simulates the encounter and attachment of bacterial cells with leaking marine particles to systematically evaluate the role of different parameters associated with bacterial run-and-tumble motility. We further use this model to explore the role of particle microstructure on the colonization efficiency of bacteria with different motility traits. We find that the porous microstructure facilitates additional colonization by chemotactic and motile bacteria, and fundamentally alters the way nonmotile cells interact with particles due to streamlines intersecting with the particle surface.
    Type of Medium: Online Resource
    ISSN: 2752-6542
    Language: English
    Publisher: Oxford University Press (OUP)
    Publication Date: 2023
    detail.hit.zdb_id: 3120703-0
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  • 8
    In: The ISME Journal, Springer Science and Business Media LLC, Vol. 15, No. 4 ( 2021-04), p. 1222-1235
    Abstract: Coral reef health depends on an intricate relationship among the coral animal, photosynthetic algae, and a complex microbial community. The holobiont can impact the nutrient balance of their hosts amid an otherwise oligotrophic environment, including by cycling physiologically important nitrogen compounds. Here we use 15 N-tracer experiments to produce the first simultaneous measurements of ammonium oxidation, nitrate reduction, and nitrous oxide (N 2 O) production among five iconic species of reef-building corals ( Acropora palmata , Diploria labyrinthiformis , Orbicella faveolata , Porites astreoides , and Porites porites ) in the highly protected Jardines de la Reina reefs of Cuba. Nitrate reduction is present in most species, but ammonium oxidation is low potentially due to photoinhibition and assimilatory competition. Coral-associated rates of N 2 O production indicate a widespread potential for denitrification, especially among D. labyrinthiformis , at rates of ~1 nmol cm −2  d −1 . In contrast, A. palmata displays minimal active nitrogen metabolism. Enhanced rates of nitrate reduction and N 2 O production are observed coincident with dark net respiration periods. Genomes of bacterial cultures isolated from multiple coral species confirm that microorganisms with the ability to respire nitrate anaerobically to either dinitrogen gas or ammonium exist within the holobiont. This confirmation of anaerobic nitrogen metabolisms by coral-associated microorganisms sheds new light on coral and reef productivity.
    Type of Medium: Online Resource
    ISSN: 1751-7362 , 1751-7370
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2021
    detail.hit.zdb_id: 2299378-2
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  • 9
    In: The ISME Journal, Springer Science and Business Media LLC, Vol. 17, No. 8 ( 2023-08), p. 1167-1183
    Abstract: Microbial interactions govern marine biogeochemistry. These interactions are generally considered to rely on exchange of organic molecules. Here we report on a novel inorganic route of microbial communication, showing that algal-bacterial interactions between Phaeobacter inhibens bacteria and Gephyrocapsa huxleyi algae are mediated through inorganic nitrogen exchange. Under oxygen-rich conditions, aerobic bacteria reduce algal-secreted nitrite to nitric oxide (NO) through denitrification, a well-studied anaerobic respiratory mechanism. The bacterial NO is involved in triggering a cascade in algae akin to programmed cell death. During death, algae further generate NO, thereby propagating the signal in the algal population. Eventually, the algal population collapses, similar to the sudden demise of oceanic algal blooms. Our study suggests that the exchange of inorganic nitrogen species in oxygenated environments is a potentially significant route of microbial communication within and across kingdoms.
    Type of Medium: Online Resource
    ISSN: 1751-7362 , 1751-7370
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2023
    detail.hit.zdb_id: 2299378-2
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  • 10
    Online Resource
    Online Resource
    American Chemical Society (ACS) ; 2013
    In:  Environmental Science & Technology Vol. 47, No. 9 ( 2013-05-07), p. 4189-4196
    In: Environmental Science & Technology, American Chemical Society (ACS), Vol. 47, No. 9 ( 2013-05-07), p. 4189-4196
    Type of Medium: Online Resource
    ISSN: 0013-936X , 1520-5851
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    Language: English
    Publisher: American Chemical Society (ACS)
    Publication Date: 2013
    detail.hit.zdb_id: 280653-8
    detail.hit.zdb_id: 1465132-4
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