Ancient sediments have recorded the cooling of the solid Earth. This is shown by the analysis of oxygen isotopes. According to this, the early oceans were not as hot as previously thought.
New DFG Research Unit “Clock Metrology: A Novel Approach to TIME in Geodesy” with GFZ participation
Looking back 550 million years: How did the oldest animals feed? Researchers used biomarkers to study the gut contents of Ediacara communities.
The Alps are not yet fully grown. But what is driving them further upwards: Crustal or mantle dynamics? GFZ researchers are now making a new contribution to the discussion.
In the beginning of November, the joint colloquium of the "International Ocean Discovery Program" (IODP) and the "International Continental Scientific Drilling Progr
The 20th autumn school "System Earth" of GFZ and DMG offers further training for teachers on extreme events in the Earth system.
![[Translate to English:] Profilfoto mit schwarzem Rahmen von Henning Francke](/fileadmin/_processed_/f/6/csm_20221026_Henning-Francke_3e299a36a1.webp)
The GFZ German Research Center for Geosciences mourns the passing of Henning Francke.
Making geodata interoperable and suited for curiosity driven research: GEO-INQUIRE project launched.
European Geothermal Congress from 17 to 21 October 2022 in Berlin
Contributions at the International Conference on Polar and Alpine Microbiology confirm: "The effects of climate change are particularly evident in these ecosystems."