A team of French, American and Turkish palaeontologists and geologists led by CNRS researchers (note 1) has discovered the existence of a forgotten continent they have dubbed Balkanatolia, which today covers the present-day Balkans and Anatolia. Formerly inhabited by a highly specific fauna, they believe that it enabled mammals from Asia to colonise Europe 34 million years ago. Their findings are published in the March 2022 volume of Earth Science Reviews.
For millions of years during the Eocene Epoch (55 to 34 million years ago), Western Europe and Eastern Asia formed two distinct land masses with very different mammalian faunas: European forests were home to endemic fauna such as Palaeotheres (an extinct group distantly related to present-day horses, but more like today’s tapirs), whereas Asia was populated by a more diverse fauna including the mammal families found today on both continents.
We know that, around 34 million years ago, Western Europe was colonised by Asian species, leading to a major renewal of vertebrate fauna and the extinction of its endemic mammals, a sudden event called the ‘Grande Coupure’. Surprisingly, fossils found in the Balkans point to the presence of Asian mammals in southern Europe long before the Grande Coupure, suggesting earlier colonisation.
Now, a team led by CNRS researchers has come up with an explanation for this paradox. To do this, they reviewed earlier palaeontological discoveries, some of which date back to the 19th century, sometimes reassessing their dating in the light of current geological data. The review revealed that, for much of the Eocene, the region corresponding to the present-day Balkans and Anatolia was home to a terrestrial fauna that was homogeneous, but distinct from those of Europe and eastern Asia. This exotic fauna included, for example, marsupials of South American affinity and Embrithopoda (large herbivorous mammals resembling hippopotamuses) formerly found in Africa. The region must therefore have made up a single land mass, separated from the neighbouring continents.
The team also discovered a new fossil deposit in Turkey (Büyükteflek) dating from 38 to 35 million years ago, which yielded mammals whose affinity was clearly Asian, and are the earliest discovered in Anatolia until now. They found jaw fragments belonging to Brontotheres, animals resembling large rhinoceroses that died out at the end of the Eocene.
All this information enabled the team to outline the history of this third Eurasian continent, wedged between Europe, Africa and Asia, which they dubbed Balkanatolia. The continent, already in existence 50 million years ago (note 2) and home to a unique fauna, was colonised 40 million years ago by Asian mammals as a result of geographical changes that have yet to be fully understood. It seems likely that a major glaciation 34 million years ago, leading to the formation of the Antarctic ice sheet and lowering sea levels, connected Balkanatolia to Western Europe, giving rise to the ‘Grande Coupure’.
1 Working at the Centre for Research and Teaching in Environmental Geoscience (CNRS/Aix-Marseille Université/IRD/INRAE) and at the Centre for Research on Palaeontology – Paris (CNRS/Museum national d’Histoire naturelle/Sorbonne Université). Another French laboratory, Geosciences Rennes (CNRS/Université Rennes 1) also contributed to this study, along with Kütahya Dumlupınar and Eskişehir Osmangazi Universities (Turkey) and the universities of Washington, Connecticut, Kansas and Chicago (USA).
2 Balkanatolia may be a relic of Greater Adria, another of the Mediterranean region’s ‘forgotten continents’, formed over 200 million years ago, and brought to light by reconstructions of the location of tectonic plates carried out by Douwe van Hinsbergen et al. and published in a 2019 paper.