New study explains how winter sea ice and melting ice shelves control the formation of deep ocean water in Antarctica.

As the last Ice Age waned and the Holocene dawned, deep-ocean circulation around Antarctica underwent dramatic shifts that helped release long-stored carbon back into the atmosphere. Deep-sea ...

In the far North Atlantic, a rapid and little‑noticed rise in sea level is sending signals that reach all the way to American ...

The story of how the last Ice Age ended is being rewritten from the bottom up, as new records etched into the sea floor ...

Ancient Antarctic Bottom Water expansion triggered carbon release and ended the last Ice Age, offering critical insight into ocean circulation’s role in global climate change.

A groundbreaking study in the journal Science, has unveiled how deep ocean currents—known as global overturning circulation—play a pivotal role in shaping the diversity and function of microbial life ...

New findings challenge climate models by revealing the Southern Ocean's unexpected, but also transient, resilience as a carbon sink.

India's deep-ocean exploration has taken a monumental leap forward with a 15-year agreement to explore for precious metals in ...

Earth's deep mantle stored enough water in rocks to equal one ocean during our planet's early molten days, helping explain ...