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Helmholtz Centre for Ocean Research Kiel (GEOMAR)


Conundrum of missing iron in oxygen minimum zones solved

A international research team has discovered a new biogeochemical process that explains the removal of dissolved iron from seawater in oxygen minimum zones. This process, which involves the reaction of iron with nitrate instead of oxygen, is essential for understanding nutrient availability and carbon fixation in the oceans.

SourceHelmholtz Centre for Ocean Research Kiel (GEOMAR)·JournalEarth and Planetary Science Letters·DateOct 28, 2016

Sensitive youngsters

A long-term laboratory experiment showed that young sea stars grow more slowly and eat less in acidic conditions, even after a prolonged acclimation period. The study suggests that young sea stars may not adapt to the effects of ocean acidification, potentially affecting entire ecosystems.

SourceHelmholtz Centre for Ocean Research Kiel (GEOMAR)·JournalMarine Ecology Progress Series·DateSep 26, 2014

The fate of the eels

Researchers used a new ocean model to simulate the migration of eel larvae from the Sargasso Sea to Europe. The study found that small-scale ocean currents play a crucial role in determining eel population fluctuations and that eels return to specific locations within the Sargasso Sea where their mother spawned.