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Transient fertilization of a post-Sturtian Snowball ocean margin with dissolved phosphate by clay minerals

Earth Sciences

Transient fertilization of a post-Sturtian Snowball ocean margin with dissolved phosphate by clay minerals

E. C. Fru, J. A. Bahri, et al.

Explore how the melting of Sturtian Snowball ice sheets drastically increased phosphate levels in seawater, igniting a surge in marine primary production and enhancing ocean-atmosphere oxygenation. This groundbreaking research conducted by Ernest Chi Fru and colleagues uncovers the vital role of clay minerals in this transformative ecological event.

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