Auel - Frozen Forests -

: During warmer, wet interstadials, the expansion of trees promoted landscape stability and active soil development.

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. AUEL - Frozen Forests

: 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. : During warmer, wet interstadials, the expansion of

: 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 : Research indicates that from roughly 60,000 to

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

: 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.