The important role of macroalgal canopies in the oceanic carbon (C) cycle is increasingly being recognized, but direct assessments of community productivity remain scarce. We conducted a seasonal study on a sublittoral Baltic Sea canopy of the brown alga Fucus vesiculosus, a prominent species in temperate and Arctic waters. We investigated community production on hourly, daily, and seasonal timescales. Aquatic eddy covariance (AEC) oxygen flux measurements integrated ~ 40 m2 of the seabed surface area and documented considerable oxygen production by the canopy year‐round. High net oxygen production rates of up to 35 ± 9 mmol m-2 h-1 were measured under peak irradiance of ~ 1200 µmol photosynthetically active radiation (PAR) m-2 s-1 in summ...
Eutrophication combined with climate change has caused ephemeral filamentous macroalgae to increase ...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Warming and acidification of the oceans as a consequence of increasing CO2-concentrations occur at l...
The important role of macroalgal canopies in the oceanic carbon (C) cycle is increasingly being reco...
The brown macroalga Fucus vesiculosus is a foundation species in temperate rocky shores, subjected t...
Stochastic upwelling of seawater in the Baltic Sea from the deep, anoxic bottoms may bring low-pH wa...
Stochastic upwelling of seawater in the Baltic Sea from the deep, anoxic bottoms may bring low-pH wa...
Shallow benthic habitats are hotspots for carbon cycling and energy flow, but metabolism (primary pr...
International audienceThe photosynthetic activity and productivity of four dominant canopy intertida...
Warming is one of the most dramatic aspects of climate change and threatens future ecosystem functio...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Ocean warming and acidification may substantially affect the photophysiological performance of keyst...
Carbon content, nitrogen content, carbon:nitrogen ratio, chlorophyll a and chlorophyll fluorescence ...
Seaweeds provide important ecosystem services in coastal areas, and loss of these macrophytes due to...
Eutrophication combined with climate change has caused ephemeral filamentous macroalgae to increase ...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Warming and acidification of the oceans as a consequence of increasing CO2-concentrations occur at l...
The important role of macroalgal canopies in the oceanic carbon (C) cycle is increasingly being reco...
The brown macroalga Fucus vesiculosus is a foundation species in temperate rocky shores, subjected t...
Stochastic upwelling of seawater in the Baltic Sea from the deep, anoxic bottoms may bring low-pH wa...
Stochastic upwelling of seawater in the Baltic Sea from the deep, anoxic bottoms may bring low-pH wa...
Shallow benthic habitats are hotspots for carbon cycling and energy flow, but metabolism (primary pr...
International audienceThe photosynthetic activity and productivity of four dominant canopy intertida...
Warming is one of the most dramatic aspects of climate change and threatens future ecosystem functio...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Ocean warming and acidification may substantially affect the photophysiological performance of keyst...
Carbon content, nitrogen content, carbon:nitrogen ratio, chlorophyll a and chlorophyll fluorescence ...
Seaweeds provide important ecosystem services in coastal areas, and loss of these macrophytes due to...
Eutrophication combined with climate change has caused ephemeral filamentous macroalgae to increase ...
Shallow coastal marine ecosystems are exposed to intensive warming events in the last decade, threat...
Warming and acidification of the oceans as a consequence of increasing CO2-concentrations occur at l...