Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Effect of eastern oysters (Crassostrea virginica) on sediment carbon and nitrogen dynamics in an urban estuary
Oyster reefs have declined globally. Interest in their restoration has motivated research into oyster‐mediated ecosystem services including effects on biodiversity, filtration, and nitrogen (N) cycling. Recent evidence suggests oysters may promote denitrification, or anaerobic respiration of nitrate (NO3−) into di‐nitrogen gas, via benthic deposition of carbon (C) and N‐rich biodeposits. However, the mechanisms whereby biodeposits promote N transformations prerequisite to denitrification (e.g., mineralization and nitrification) are unclear. Previous research has also not measured oysters' influence on N cycling in urbanized areas. In May 2010 we deployed eastern oysters (Crassostrea virginica) in mesh cages above sand‐filled boxes at four sites across a nutrient gradient in Jamaica Bay, New York City (New York, USA). Oysters were arranged at four densities: 0, 40, 85, and 150 oysters/m2. For 17 months we measured water‐column nutrients and chlorophyll a, every two weeks to monthly. Every two months we measured sediment ash‐free dry mass (AFDM), exchangeable ammonium (NH4+), ammonification, nitrification, denitrification potential (DNP), and NO3− and C limitation of DNP. Oysters increased sediment AFDM at three of four sites, with the greatest increase at high density. Oysters did not affect any N pools or transformations. However, variation among sites and dates illustrated environmental drivers of C and N biogeochemistry in this urban estuary. Overall, nitrification was positively related to net ammonification, water column NH4+, and sediment NH4+, but was not correlated with DNP. Denitrification was consistently and strongly NO3− limited, while C was not limiting or secondarily limiting. Therefore, the oyster‐mediated increase in AFDM did not affect DNP because C was not its primary driver. Also, because DNP was unrelated to nitrification, it is unlikely that biodeposit N was converted to NO3− for use as a denitrification substrate. Predicting times or sites where denitrification is driven by the C and N species originating from oyster biodeposits remains a challenge under eutrophic conditions. Towards this goal, we synthesized our conclusions with literature predictions in a conceptual model for pathways whereby oysters might influence C and N dynamics differently in oligotrophic relative to eutrophic ecosystems.
Effect of eastern oysters (Crassostrea virginica) on sediment carbon and nitrogen dynamics in an urban estuary
Oyster reefs have declined globally. Interest in their restoration has motivated research into oyster‐mediated ecosystem services including effects on biodiversity, filtration, and nitrogen (N) cycling. Recent evidence suggests oysters may promote denitrification, or anaerobic respiration of nitrate (NO3−) into di‐nitrogen gas, via benthic deposition of carbon (C) and N‐rich biodeposits. However, the mechanisms whereby biodeposits promote N transformations prerequisite to denitrification (e.g., mineralization and nitrification) are unclear. Previous research has also not measured oysters' influence on N cycling in urbanized areas. In May 2010 we deployed eastern oysters (Crassostrea virginica) in mesh cages above sand‐filled boxes at four sites across a nutrient gradient in Jamaica Bay, New York City (New York, USA). Oysters were arranged at four densities: 0, 40, 85, and 150 oysters/m2. For 17 months we measured water‐column nutrients and chlorophyll a, every two weeks to monthly. Every two months we measured sediment ash‐free dry mass (AFDM), exchangeable ammonium (NH4+), ammonification, nitrification, denitrification potential (DNP), and NO3− and C limitation of DNP. Oysters increased sediment AFDM at three of four sites, with the greatest increase at high density. Oysters did not affect any N pools or transformations. However, variation among sites and dates illustrated environmental drivers of C and N biogeochemistry in this urban estuary. Overall, nitrification was positively related to net ammonification, water column NH4+, and sediment NH4+, but was not correlated with DNP. Denitrification was consistently and strongly NO3− limited, while C was not limiting or secondarily limiting. Therefore, the oyster‐mediated increase in AFDM did not affect DNP because C was not its primary driver. Also, because DNP was unrelated to nitrification, it is unlikely that biodeposit N was converted to NO3− for use as a denitrification substrate. Predicting times or sites where denitrification is driven by the C and N species originating from oyster biodeposits remains a challenge under eutrophic conditions. Towards this goal, we synthesized our conclusions with literature predictions in a conceptual model for pathways whereby oysters might influence C and N dynamics differently in oligotrophic relative to eutrophic ecosystems.
Effect of eastern oysters (Crassostrea virginica) on sediment carbon and nitrogen dynamics in an urban estuary
Hoellein, Timothy J. (Autor:in) / Zarnoch, Chester B. (Autor:in)
Ecological Applications ; 24 ; 271-286
01.03.2014
16 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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