PhysOrg: Earth Sciences - 2010 March 02
Quarternary International 207, 137-144. doi:10.1016/j.quaint.2009.05.006At the end of the last interglacial epoch, around 115,000 years ago, there were significant climate fluctuations. In Central and Eastern Europe, the slow transition from the Eemian Interglacial to the Weichselian Glacial was marked by a growing instability in vegetation trends with possibly at least two warming events.