An interdisciplinary study confirms, for the first time, the oceanographic pathways that transport floating macroalgae from the coastal waters of Southwest Greenland to deep-sea carbon reservoirs, potentially playing a previously underappreciated role
An interdisciplinary study confirms, for the first time, the oceanographic pathways that transport floating macroalgae from the coastal waters of Southwest Greenland to deep-sea carbon reservoirs, potentially playing a previously underappreciated role in global carbon storage.
Macroalgae, or seaweeds (including kelp), are highly productive coastal habitats capable of absorbing significant quantities of atmospheric carbon (CO₂). Previous studies have estimated that globally, 4–44 teragrams (1Tg = one million metric tons) per year of macroalgal-derived carbon may reach depths of 200m, where it may be sequestered for at least 100 years.
However, macroalgae’s contribution to long-term carbon storage has been challenging to quantify with any certainty due to issues including: the wide range of macroalgae properties that need to be considered; the complexity of interactions with physical oceanographic transport processes, and a lack of scientific evidence about the travels and transformations of detached macroalgae after leaving coastal rocky shores.
To address this knowledge gap, the study team, co-led by the Leibniz Institute for Baltic Sea Research Warnemünde and Helmholtz-Zentrum Hereon in Germany and involving scientists from Plymouth Marine Laboratory, University of Exeter, Portugal, Saudi Arabia and Denmark, used a combination of satellite imagery, ocean drifter tracking, numerical modelling and advanced turbulence
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