Ocean Science

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New research from Rutgers University reveals that meltwater from Antarctic ice shelves contributes far less iron to surrounding ocean waters than scientists had assumed. Instead, most iron originates from deep ocean water and continental sediments. The findings challenge expectations about iron fertilization and its role in carbon absorption.

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An international team of researchers has developed a new system to identify and compare episodes of sudden underwater darkness, known as marine darkwaves, which threaten light-dependent marine ecosystems. These events, triggered by storms, sediment runoff, and algae blooms, can drastically reduce light to the seafloor for days or months. The framework aims to standardize monitoring of these disruptions worldwide.

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