The sediment record from Rodderberg potentially provides a climate and environmental record spanning at least the last ca 130 ka. Results from a low resolution pilot study reveal characteristic fluctuations that can be related to global climate variability as reflected in marine isotope stages and document the potential of this site for continuous and high-resolution investigations of the Middle to Late Pleistocene. Here we document the tentative lithology drilled, and show how the elemental composition can be interpreted with regard to lake level fluctuations, related redox conditions, but also to grain-size distribution and changes in lacustrine productivity. Finally, based on major lithological changes, a preliminary depth/age model is suggested that allows reassessing published luminescence ages from the same site.

Supplement to: Zolitschka, Bernd; Rolf, Christian; Bittmann, Felix; Binot, Franz; Frechen, Manfred; Wonik, Thomas; Froitzheim, Nikolaus; Ohlendorf, Christian (2014): Pleistocene climatic and environmental variations inferred from a terrestrial sediment record - the Rodderberg Volcanic Complex near Bonn, Germany. Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 165, 407-427