Discovering climate signals in the archives: how using a common language for data deposition ensures your data are found, understood and cited.
Paleoceanography and Paleoclimatology
Posted inResearch Spotlights
Simulating 195 Million Years of Global Climate in the Mesozoic
An ensemble of climate simulations identifies factors that drove long-term trends of a prehistoric greenhouse climate.
Posted inResearch Spotlights
A 50,000-Year History of Current Flow Yields New Climate Clues
The first high-resolution historical record of Europe’s Glacial Eastern Boundary Current sheds new light on ocean circulation, ice sheet dynamics, and climate change.
Posted inResearch Spotlights
Los océanos liberaron dióxido de carbono durante la última deglaciación
Un nuevo registro de isótopos de boro proveniente de sedimentos marinos del Pacifico Sur, ofrece una imagen más completa del intercambio de dióxido de carbono entre el océano y la atmósfera durante el Pleistoceno tardío.
Posted inResearch Spotlights
Ancient Sea Levels in South Africa May Offer Modern Analogues
Largely spared from disruptive tectonic activity, the South African coastline offers a natural setting to study sea levels from when Earth’s atmospheric carbon dioxide last reached today’s levels.
Posted inResearch Spotlights
Chinese Swamp Core Reveals 47,000 Years of Monsoon History
Magnetic analysis of mineral composition supports the importance of tropical climate processes in shaping long-term monsoon patterns.
Posted inEditors' Vox
New Editor in Chief of Paleoceanography and Paleoclimatology
Find out about the person taking the helm of Paleoceanography and Paleoclimatology and his vision for the coming years.
Posted inEditors' Vox
Between Past and Future
The outgoing Editor in Chief of Paleoceanography and Paleoclimatology reflects on her tenure and changes in the journal over those years.
Posted inResearch Spotlights
Southern California Climate Change over 100,000 Years
Researchers used a sediment core from a lake in California’s San Bernardino Mountains to track the effect of climate on vegetation, fire, and erosion between about 120,000 and 15,000 years ago.