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.

: 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 AUEL - Frozen Forests

The Auel sediment cores are vital for reconstructing "frozen" or glacial-era landscapes. Unlike many other sites, the Auel maar contains laminated (layered) sediments that acted as a natural trap, preserving pollen, spores, and chemical proxies of the surrounding environment. : 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 Unlike many other sites, the Auel maar contains

: 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.

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