This paper reports stratigraphically extensive ice-rafted debris, including macroscopic dropstones, in late Eocene to early Oligocene sediments from Norwegian-Greenland Sea, that were deposited between ∼ 38 and 30 million years ago. The data suggest the existence of at least isolated glaciers on Greenland about 20 million years earlier than previously documented, at a time when temperatures and atmospheric carbon dioxide concentrations were substantially higher.
- James S. Eldrett
- Ian C. Harding
- Andrew P. Roberts