Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma

Paleogeographic maps are essential tools for understanding Earth system dynamics. They provide boundary conditions climate and geodynamic modelling, analysing surface processes biotic interactions. However, the temporal spatial distribution of key features such as seaways mountain belts that govern changes interchange differ between various paleogeographies require regular updates with new data models. We developed a reproducible systematic approach to paleogeographic reconstruction set worldwide Cenozoic at 60, 40 20 Ma. followed six-stage methodology integrates an extensive review geological into coherent plate tectonic model using open source software GPlates. (1) generated global kinematic model, reconstructed intensely-deformed boundaries structural, paleomagnetic other geologic in six regions: Andes, North American Cordillera, Scotia Arc, Africa, Mediterranean region Tibetan-Himalayan collision zone. (2) modified previously published paleobathymetry several regions where continental oceanic crust overlap due differences (3) then defined paleoshorelines updated fossil databases locate terrestrial marine transition. (4) applied isostatic compensation polar eustatic sea level adjustments. (5) Paleoelevations were estimated broad range including thermochronology stable isotopes, combined paleobotanical (mostly pollen leaf physiognomy), structural geomorphological data. address ongoing controversies on mechanisms chronology India-Asia by providing alternate reconstructions each time slice. finally discuss implications our evolution weatherability methodological limitations potential improvements. Future addition data, can be accommodated through dedicated interactive website tool (https://map.paleoenvironment.eu/) enables users interactively upload download compare models, generate their own plots. Our aim is regularly update models presented here they become available.