A solitary hydroid drifts in currents at approximately 380 m deep in an area of the seabed that was very recently covered by the George VI Ice Shelf, a floating glacier in Antarctica. Image courtesy of ROV SuBastian / Schmidt Ocean Institute.
This week: New research exploring carbon sequestration in the deep ocean, predicting hard substrate availability in the abyss, & microplastic fluxes!
CLICK FOR YOUR DEEP-SEA ROUND-UP – 2 October 2025
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