20
th
century, was wiped out by an abrupt event which occurred at that time in the
Central Mediterranean Sea.
This region actually experienced a catastrophic earthquake in 1908, with an epicentre
off the coast of Messina (northeastern Sicily). This event is known to have generated
tsunami waves that reached the coast of Malta (Mottershead et al., 2017).
The consequent shift in sediments grain size and the sudden burial of Posidonia
oceanica, as observed in our cores, likely created an unsuitable habitat for A. lobifera
that is known to prefer vegetated bottoms with coarser substrata (Guastella et al., 2019).
The reappearance of the species in Marsamxett samples can be dated around the 1940s,
hence after a considerable lag-time after the first failed invasion.
In conclusion, the analysis of historical records preserved in sediment cores
radiometrically dated allows to reconstruct the invasion dynamics of alien species and
to detect possible early failed invasions, leading to a better understanding of biological
invasion mechanisms.
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