Luminescence Dating of Sediments from the Luthern Valley, Central Switzerland, and Implications for the Chronology of the Last Glacial Cycle

Luminescence chronology of non-glacial s

Luminescence chronology of non-glacial sediments in Changeable Lake, Russian High Arctic, and implications for limited Eurasian ice-sheet extent during the LGM

✍ Glenn W. Berger; Martin Melles; Debabrata Banerjee; Andrew S. Murray; Alexandra 📂 Article 📅 2004 🏛 John Wiley and Sons 🌐 English ⚖ 315 KB

## Abstract A 10.5 m core from Changeable Lake in the Severnaya Zemlya Archipelago just north of the Taymyr Peninsula intersects ca. 30 cm of diamicton at its base, interpreted as a basal till. Because the upper 10.13 m of this core consists of non‐glacial sediments, a maximum numeric age for these