Abstract
The so-called Blake Event, an event of the geomagnetic fi eld,
was identifi ed in the Middle Palaeolithic Neumark-Nord 2
(NN2) site in Germany by Sier et al. (2o11). These authors discussed
the implications for the positioning of the Eemian in
the Marine isotope stage (MIS) scale in northern-central
Europe. The NN2 data showed a
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