Fig. 10

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Compared summary pollen diagrams from Montemayor-1 well (correlated with ATNTS2012 reversals and some key isotope stages), Carmona A and D sections, and reference sections from the Sicilian succession (Capodarso Tripoli, Realmonte clay layer within halite, Racalmuto clay layers within halite, Eraclea Minoa marly levels intercalated with gypsum beds, Eraclea Minoa Lago Mare Formation, Eraclea Minoa Arenazzolo Formation, Capo Rossello Trubi). Compared climatic quantification (MAT and MAP) of the Carmona with those of Sicily (pre-MC, 1st step MC, post-MC) and a part of Montemayor-1 (MC paroxysm), which are climatostratigraphically correlated with the Montemayor-1 oxygen isotopic curve. Three Sicilian sections, Capodarso (Tripoli), Racalmuto (halite) and Capo Rossello (Trubi) are also correlated with ATNTS2012 (Hilgen, 1991; Gautier et al., 1994). Legend of pollen groups, see Figure 6.

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