User:Hzara002/Neanderthal extinction

Interbreeding
Infectious illness interactions may express the prolonged period of stagnation before the modification, as per disease ecology. Utilizing mathematical modeling, we've made forecasts for future investigations. Researchers argue that this technique gives information into inter-species interactions during the shift between of Middle and Upper Paleolithic eras, given the sparse material record from this time and the potential of DNA sequencing and dating technology. Such modeling, together with modern technology and prehistoric archeological methodologies, may provide a fresh understanding of this time in human origins.

New evidence discovered at Grotte Mandrin in Malataverne, France,  dating back by 10,000 years. Six of the individuals were recognized as Neanderthal, but a modern human upper molar was recovered in between Neanderthal sections. At Grotte Mandrin, the existence of  modern human molar inside the Neronian layer prompted researchers to connect this stone tool manufacturing to Homo sapiens. The existence of the homo sapiens molar beside the Neronian solidifies the narrative: Neanderthals and modern humans replaced each other multiple times in same area. Finds at Grotte Mandrin imply the Mediterranean region had a crucial importance in shaping humans' spread into Western Eurasia.

Recent research in northern Spain suggests that Neanderthals vanished earlier in Vasco-Cantabrian eastern and southern Iberia. The projected outcome will assist assess the consequences for region systems of resource extraction, subsistence techniques, and environmental–human connections in the Neanderthals' death and modern humans' evolutionary progress.

Climate
The data reveal that sudden climatic change, although crucial locally, had a limited effect on the worldwide Neanderthal population. Interbreeding and assimilation, which were hypothesized as causes in the death of European Neanderthal populations are successful only for low levels of food competition. More specific genes calculations of the total amount of interbreeding individuals during the last glacial epoch are needed to restrict the influence of interbreeding in my model. These figures are questionable. To simulate numerous interbreeding occurrences, start the model early (125 ka). Future research will examine. models of interbreeding and hybridization may be evaluated using genomic records from last ice age (Fu et al., 2016).