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  • 1
    Publication Date: 2024-03-15
    Description: Research so far has provided little evidence that benthic biogeochemical cycling is affected by ocean acidification under realistic climate change scenarios. We measured nutrient exchange and sediment community oxygen consumption (SCOC) rates to estimate nitrification in natural coastal permeable and fine sandy sediments under pre-phytoplankton bloom and bloom conditions. Ocean acidification, as mimicked in the laboratory by a realistic pH decrease of 0.3, significantly reduced SCOC on average by 60% and benthic nitrification rates on average by 94% in both sediment types in February (pre-bloom period), but not in April (bloom period). No changes in macrofauna functional community (density, structural and functional diversity) were observed between ambient and acidified conditions, suggesting that changes in benthic biogeochemical cycling were predominantly mediated by changes in the activity of the microbial community during the short-term incubations (14 days), rather than by changes in engineering effects of bioturbating and bio-irrigating macrofauna. As benthic nitrification makes up the gross of ocean nitrification, a slowdown of this nitrogen cycling pathway in both permeable and fine sediments in winter, could therefore have global impacts on coupled nitrification-denitrification and hence eventually on pelagic nutrient availability.
    Keywords: 115bis; 330; Abra alba; Abundance per area; Alkalinity, total; Alkalinity, total, standard error; Ammonium, flux; Aragonite saturation state; Aragonite saturation state, standard error; Bathyporeia elegans; Benthos; Bicarbonate ion; Biomass, wet mass; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calcite saturation state, standard error; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard error; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyll a; Coast and continental shelf; Community, oxygen consumption; Community composition and diversity; Date; Date/time end; Date/time start; Diameter; Entire community; Estimated from mass budget; Event label; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Genus; Glycera alba; Individuals; Laboratory experiment; Macoma balthica; Magelona johnstoni; Magelona mirabilis; Nephtys cirrosa; Nephtys hombergii; Nitrate, flux; Nitrification, oxygen consumption; Nitrogen mineralization; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Oligochaeta sp.; Other metabolic rates; Oxygen; Oxygen, standard error; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard error; pH; pH, standard error; Potentiometric; Potentiometric titration; Replicate; Respiration; Salinity; Salinity, standard error; Sample ID; Scoloplos armiger; Sigalion mathildae; Soft-bottom community; Species; Spionida sp.; Tellina fabula; Temperate; Temperature, water; Temperature, water, standard error; Treatment; Urothoe brevicornis
    Type: Dataset
    Format: text/tab-separated-values, 3558 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Vopel, Kay; Del-Río, Vopel; Pilditch, Conrad A (2018): Effects of CO2 enrichment on benthic primary production and inorganic nitrogen fluxes in two coastal sediments. Scientific Reports, 8(1), https://doi.org/10.1038/s41598-017-19051-w
    Publication Date: 2024-03-15
    Description: Ocean acidification may alter the cycling of nitrogen in coastal sediment and so the sediment-seawater nitrogen flux, an important driver of pelagic productivity. To investigate how this perturbation affects the fluxes of NOX- (nitrite/nitrate), NH4+ and O2, we incubated estuarine sand and subtidal silt in recirculating seawater with a CO2-adjusted pH of 8.1 and 7.9. During a 41-day incubation, the seawater kept at pH 8.1 lost 97% of its NOX- content but the seawater kept at pH 7.9 lost only 18%. Excess CO2 increased benthic photosynthesis. In the silt, this was accompanied by a reversal of the initial NOX- efflux into influx. The estuarine sand sustained its initial NOX- influx but, by the end of the incubation, released more NH4+ at pH 7.9 than at pH 8.1. We hypothesise that these effects share a common cause; excess CO2 increased the growth of benthic microalgae and so nutrient competition with ammonia oxidising bacteria (AOB). In the silt, diatoms likely outcompeted AOB for NH4+ and photosynthesis increased the dark/light fluctuations in the pore water oxygenation inhibiting nitrification and coupled nitrification/denitrification. If this is correct, then excess CO2 may lead to retention of inorganic nitrogen adding to the pressures of increasing coastal eutrophication.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Ammonium; Ammonium, flux; Ammonium, standard deviation; Aragonite saturation state; Benthos; Bicarbonate ion; Calcite saturation state; Calculated using CO2calc; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Containers and aquaria (20-1000 L or 〈 1 m**2); Difference; Entire community; Event label; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Hauraki_Gulf; Identification; Laboratory experiment; Light mode; Nitrate and Nitrite; Nitrate and Nitrite, standard deviation; Nitrite and nitrate, flux; OA-ICC; Ocean Acidification International Coordination Centre; Other studied parameter or process; Oxygen uptake, total; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Potentiometric; Salinity; Salinity, standard deviation; Sediment type; Soft-bottom community; South Pacific; Tauranga_Harbour; Temperate; Temperature, water; Temperature, water, standard deviation; Time point, descriptive; Treatment; Type
    Type: Dataset
    Format: text/tab-separated-values, 2627 data points
    Location Call Number Limitation Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Klages, Michael; Vopel, Kay; Bluhm, Hartmut; Brey, M; Soltwedel, Thomas; Arntz, Wolf E (2001): Deep-sea food falls: first observation of a natural event in the Arctic Ocean. Polar Biology, 24(4), 292-295, https://doi.org/10.1007/s003000000199
    Publication Date: 2024-03-01
    Description: Concentrations of scavengers attracted by bait in the deep sea are documented by time-lapse photography and results of baited traps. During a remotely operated vehicle deployment in the Molloy Deep, the deepest depression of the Fram Strait, the carcass of a natant decapod, Pasiphaea tarda Krøyer, 1845, was discovered at 79°08.4'N and 002°49.85'E in a depth of 5,551 m. The carcass was covered by hundreds of individuals of Uristes sp., a scavenging lysianassoid amphipod. After documentation of this event, both the carcass and the majority of amphipods were collected. This is the first reported observation and sampling of an ongoing feeding process of scavengers on a natural food fall in the deep sea.
    Keywords: ARK-XV/1; AWI_BPP; Bentho-Pelagic Processes @ AWI; Image analysis; MUC; MultiCorer; Polarstern; PS55; PS55/003; Uristes sp., length
    Type: Dataset
    Format: text/tab-separated-values, 693 data points
    Location Call Number Limitation Availability
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