Empirical Evidence Reveals Seasonally Dependent Reduction in Nitrification in Coastal Sediments Subjected to Near Future Ocean Acidification

• Main Authors: Braeckman, Ulrike, Van Colen, Carl, Guilini, Katja, Van Gansbeke, D, Soetaert, Karline, Vincx, Magda, Vanaverbeke, Jan, Vopel, Kay
• Format: Dataset
• Language: English
• Published: PANGAEA 2014
• Subjects: 115bis; 330; Abra alba; Abundance per area; Alkalinity; total; standard error; Ammonium; flux; Aragonite saturation state; Bathyporeia elegans; Benthos; Bicarbonate ion; Biomass; wet mass; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (<20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon; inorganic; dissolved; 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; Ocean acidification
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.840479; https://doi.org/10.1594/PANGAEA.840479

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.