4.7 Article

High metabolism and periodic hypoxia associated with drifting macrophyte detritus in the shallow subtidal Baltic Sea

Journal

BIOGEOSCIENCES
Volume 20, Issue 9, Pages 1713-1724

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/bg-20-1713-2023

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This study investigates the dynamics of dissolved oxygen (O2) and macrobenthic biodiversity in a shallow macrophyte detritus field in the northern Baltic Sea. The results show that hypoxia is prevalent in the detritus field and negatively affects macrobenthic abundance.
Macrophytes form highly productive habitats that export a substantial proportion of their primary production as particulate organic matter. As the detritus drifts with currents and accumulates in seafloor depressions, it constitutes organic enrichment and can deteriorate O-2 conditions on the seafloor. In this study, we investigate the O-2 dynamics and macrobenthic biodiversity associated with a shallow similar to 2300 m(2) macrophyte detritus field in the northern Baltic Sea. The detritus, primarily Fucus vesiculosus fragments, had a biomass of similar to 1700 g dry weight m(-2), approximately 1.5 times larger than nearby intact F. vesiculosus canopies. A vertical array of O-2 sensors placed within the detritus documented that hypoxia ([O-2] < 63 mu mol L-1) occurred for 23 % of the time and terminated at the onset of wave-driven hydrodynamic mixing. Measurements in five other habitats nearby, spanning bare sediments, seagrass, and macroalgae, indicate that hypoxic conditions were unique to detritus canopies. Fast-response O-2 sensors placed above the detritus documented pulses of hypoxic waters originating from within the canopy. These pulses triggered a rapid short-term (similar to 5 min) deterioration of O-2 conditions within the water column. Eddy covariance measurements of O-2 fluxes indicated high metabolic rates, with daily photosynthetic production offsetting up to 81 % of the respiratory demands of the detritus canopy, prolonging its persistence within the coastal zone. The detritus site had a low abundance of crustaceans, bivalves, and polychaetes when compared to other habitats nearby, likely because their low O-2 tolerance thresholds were often exceeded.

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