Ash-Mor et al. (2017) described Event E in R/V Mediterranean Explorer Canyon Core P22 as a 10 cm thick Mass Transport Deposit. They provided an unmodeled ¹⁴C age of 7416 ± 42 cal years BP, which is slightly younger than the event and corresponds to approximately 5466 BCE.

Left - Fig. 1a - Location Map - Right - Figure 5 - Core P22 3D grain size distribution up to 2 mm (left) and radiocarbon dating results (right) along the slope core MG10P22. Color bar represent % of grain size differential distribution by volume. Black dots represent the chronological age of the pelagic sediments, whereas diamonds represent the different color groups of LBF shells from within the MTDs - click on either image to open in a new tab - left image from Kanari et al. (2020) - right image from Ash-Mor et al. (2017)