And a response about the future of the science journalism field.

New evidence suggests Gondwana was far larger than previously thought, challenging models of continental cycling

High sea surface temperatures are expected to weaken ocean carbon sinks and damage coral reefs.

A “start button” for the formation of giant gold deposits on Earth is the subduction of plume-related seamounts.

Ancient Teghaza meteorite hints at granitelike crust and shows Mars was already losing its water 4.1 billion years ago

A rift event set off a domino effect of geologic processes that created conditions ripe for Antarctica’s glaciation, a new study suggests.

Mantle waves and tectonic stretching lofted polar mountains into a deep freeze

Mantle waves and tectonic stretching lofted polar mountains into a deep freeze

Die durch Gesteins-Tropfen an der Unterseite der antarktischen Platte verursachte Kontinentalhebung hob die Landmasse über einen Kipppunkt hinaus, ab dem Eis wachsen und bestehen bleiben konnte.

Why Antarctica became glaciated ∼34 million years ago (Ma) remains debated, as relatively warm climates and sea temperatures appear inconsistent with ice sheet formation. Although a critical decline i...

Continental uplift, caused by drips at the underside of the Antarctic plate, elevated the landmass above a tipping point where ice could grow and remain.

New solutions to two interlinked mysteries reveal how and why the Antarctic’s enormous ice sheet formed.

As his new novel is published, the US author talks about nurturing the next generation of creatives, debating Sam Altman – and why he writes on a boat in San Francisco Bay

Researchers exhume fossilized corals to predict the fate of a key climate pacemaker in a warmer world

The burial of terrestrially derived organic carbon in coastal marine sediments greatly increased during the Palaeocene–Eocene Thermal Maximum, probably helping to draw down a large portion of carbon r...

The US president accuses Leo of being

The US was founded on a pledge to limit the damages of war, even if it has often failed to uphold its commitment

Sediments from Scotland hint that ocean-atmosphere interactions continued more than 600 million years ago despite widespread ice.

Sediments from Scotland hint that ocean-atmosphere interactions continued more than 600 million years ago despite widespread ice.

During the two Cryogenian snowball Earth glaciations, the Sturtian (ca. 717–658 Ma) and Marinoan (ca. 639–635 Ma), ice persisted in the tropics for mi…