: 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
The Auel records highlight how vegetation cover dictates landscape stability.
: 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.
: 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.
: Large mammals (megafauna) actually reached higher numbers during colder stadial climates, likely because the shift from dense forest to open steppe provided more grazing material.
In scientific and paleoclimatic research, the "AUEL - Frozen Forests" typically refers to the (a volcanic crater lake) located in the Eifel region of Germany. This site has become a cornerstone of the ELSA-Project (Eifel Laminated Sediment Archive) , providing a high-resolution window into the climatic and ecological history of Central Europe over the last 60,000 years. The Auel Archive: A Paleoclimatic Deep-Dive