: Insights from these ancient forests are often used in modern ecological research to understand the resilience of coppice forests and other European woodland types in the face of modern climate change. Coppice Forests in Europe
: As the climate cooled toward the Last Glacial Maximum (LGM) , the landscape underwent a "stepwise" change from these dense forests toward a "glacial desert" after 26,000 years ago. AUEL - Frozen Forests
: High concentrations of quartz-bound Si in Auel sediments reveal the intensification of eolian (wind-blown) dust during colder stadial periods, marking the transition from stable, forested land to exposed, wind-swept tundras. Megafauna and Human Coexistence : Insights from these ancient forests are often
One of the most significant findings from the Auel site involves the presence of (spores that grow on animal dung like Sordaria and Sporormiella ). These markers prove that the "frozen forests" of the Eifel were never empty. Megafauna and Human Coexistence One of the most
: During warmer, wet interstadials, the expansion of trees promoted landscape stability and active soil development.
: The data suggests that Neanderthals and later Anatomically Modern Humans were attracted to these areas by the abundant food supply. Crucially, researchers from the Nature journal study conclude that megafauna were not "overkilled" by humans but were instead victims of the drastic vegetation shifts caused by climate change. Ecological Resilience
: Research indicates that from roughly 60,000 to 48,000 years ago , the landscape was dominated by a boreal forest featuring cold-temperate wood taxa and steppe components.