GeologyBiology
J. Rage
tlooto Summary
The Oligocene fauna was transitional between the ‘old’ Eocene and the modern Miocene faunas, and markedly changed when an important wave of dispersals entered Europe during a climatic optimum.
Abstract
Abstract is not available.
Citation format
RAGE, J. Mesozoic and cenozoic squamates of europe. Palaeobiodiversity and Palaeoenvironments, 2013, 93: 517–534.