paleoclimate

The pulsed rise of the Nahuelbuta Range: How glaciers indirectly built a mountain in Patagonia

Ambrosio Vega-Ruiz, edited by Lorenzo Mantiloni and edited by Michaël Pons July 29, 2026

Mapuche creational myth of the struggle between Caicai Vilu (water snake) and Trentren Vilu (earth snake), which shaped the Patagonian forearc. Credit: Ambrosio Vega-Ruiz.

Forearc ranges are a striking example of how tectonic processes shape our planet. The Nahuelbuta Range in southern Chile is one of such settings. This week, Ambrosio Vega-Ruiz from the GFZ Helmholtz Centre for Geosciences, Germany, is telling us the story of this remarkable range, exploring how climate feedback can influence tectonic uplift across coastal forearcs. Tectonic uplift before tectonic ...[Read More]

Destruction of the North China Craton and its global impact

Jyotirmoy Paul and edited by Lorenzo Mantiloni November 12, 2025

Left: Location of the North China Craton (modified from Wikipedia image). Right: Schematic diagram of the North China Craton destruction (Figure taken from Paul et al., 2025).

Cratons are forever, until they are not. These long-lived portions of lithosphere are known for being remarkably stable. However, if the conditions are right, even cratons can be ripped apart by geological forces, with far-reaching impacts on Earth’s systems. This week, Jyotirmoy Paul from the University of Oslo, Norway will tell us the downfall of the North China Craton, using numerical sim ...[Read More]

Paleogeography and the Northern Hemisphere Oceanic Gateways

Eivind Straume and edited by Antoniette G. Grima March 2, 2022

Eivind Straume a Postdoctoral fellow at the Department of Geological Sciences within the Jackson School of Geosciences explores how the opening and closing ocean gateways have influenced the Earth’s climate in the past. Changes in Earth’s geography due to tectonic plate motions and mantle convection influence climate evolution on geological timescales. Over millions of years, continen ...[Read More]