Fossil pollen records indicate that Patagonian desertification was not solely a consequence of Andean uplift

The Patagonian steppe-a massive rain-shadow on the lee side of the southern Andes-is assumed to have evolved similar to 15-12 Myr as a consequence of the southern Andean uplift. However, fossil evidence supporting this assumption is limited. Here we quantitatively estimate climatic conditions and plant richness for the interval similar to 10-6 Myr based on the study and bioclimatic analysis of terrestrially derived spore-pollen assemblages preserved in well-constrained Patagonian marine deposits. Our analyses indicate a mesothermal climate, with mean temperatures of the coldest quarter between 11.4 degrees C and 16.9 degrees C (presently similar to 3.5 degrees C) and annual precipitation rarely below 661mm (presently similar to 200 mm). Rarefied richness reveals a significantly more diverse flora during the late Miocene than today at the same latitude but comparable with that approximately 2,000 km further northeast at mid-latitudes on the Brazilian coast. We infer that the Patagonian desertification was not solely a consequence of the Andean uplift as previously insinuated.