The Marine Isotopic Stage 3 (MIS3- 57,000 to 27,000 cal. BP [before present]) is characterised by abrupt and rapid climatic oscillations between glacial and interglacial phases. The Middle-Upper Paleolithic (MP-UP) transition, occurring during the MIS3, is one of the key periods for human evolution, as it corresponds to the time when the last Homo neanderthalensis (Neanderthal) were replaced by Homo sapiens (our species) after both species co-occurred in Europe for less than 7,000 years. It is now accepted that it was a multifactor event happening at different spatial and temporal scales across Europe. For example, in north Iberia, there is a temporal difference in Neanderthal decline, with the late evidence in the North-West Iberia at 48-45,000 cal. BP and around 42,000 year cal. BP in North-East Iberia. There is currently no consensus regarding the impact of global climatic oscillations on this disappearance.
Could climate-induced local environmental differences, by modifying the ecology of these human species' herbivore preys, have led to changes in their subsistence strategies in response? Could this explain the asynchronous timing of Neanderthal disappearance across Europe?
Therefore, EnvINExt's main goal was to investigate the impact of climatic factors on Neanderthal and Sapiens ecosystems and subsistence strategies and on their disappearance at the Middle-Upper Paleolithic transition. To do this, the spatial and temporal variations in the ecology of ungulates (which account for over 50% of these humans' daily food intake) were explored using a combination of cutting-edge methods.
Due to a long history of Paleolithic Archeology in the north of the Iberian Peninsula, this area is rich in well-documented and dated sites covering the period of interest. For these reasons, EnvINExt focused on northern Iberia, a unique framework to explore these questions.