Abstract:
During the past 2 million years, mass dispersal
events of mammals from Africa into Eurasia possibly
triggered the arrival of early hominins (Bar-Yosef
and Belfer-Cohen, 2001; Abbate and Sagri,
2012; Koufos and Kostopoulos, 2016; Muttoni et
al., 2018). At Early Pleistocene sites, where rich
fauna complements the presence of carnivore and
hominin activity, important taphonomic processes
further complicate the recovery and interpretation
of early human behaviors and remains. Evidence
of hominins from this period is sparse and is found
at only a handful of locations outside of Africa
(Garcia et al., 2013). Even though an obvious gap
continues to exist in Greece and the Balkans, this
region of Europe is located in the direct path of
human migrations out of Africa and Asia. For the
Middle Pleistocene, the paleoanthropological, archaeological,
and paleontological records of Greece
are currently improving, in large part through the
efforts of the ERC projects PaGE and CROSSROADS
and the associated MegaPal survey (e.g.,
Panagopoulou et al., 2015; Harvati et al., 2018;
Karkanas et al., this volume; Tourloukis et al., this
volume; Athanassiou et al., this volume; Konidaris
et al., this volume; Thompson et al., this volume),
therefore starting to fill this research gap of Eastern
Europe during this crucial period of hominin
migrations.
CROSSROADS aimed to continue to fill this
gap in the Early to Middle Pleistocene record by
conducting multidisciplinary systematic fieldwork
to locate stratified dateable contexts that promote
the construction of a chronostratigraphic framework
for this region of Eurasia. The Mygdonian
Basin archaeological survey was therefore part of
this effort and was conducted in 2019, 2021 and
2022 by the Aristotle University of Thessaloniki,
in collaboration with the University of Tübingen
Paleoanthropology team, in the framework
of CROSSROADS. The survey was a direct target-oriented double-intensive archaeological investigation
of Pleistocene sediments, aiming to
identify traces of human activity by systematically
surveying exposed section profiles and by collecting
lithic artifacts from stratified dateable contexts.