Fig. 7

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Curve of the D/P ratio of the Carmona series with respect to its chronostratigraphy correlated with the Montemayor-1 oxygen isotope curve. Comparison with the D/P curve and the foraminifer-based paleobathymetric curve (Pérez-Asensio, 2021) from the Montemayor-1 hole and proposed relationships with the global sea level and Mediterranean events, all calibrated with ATNTS2012 as the oxygen isotope curve. D/P curves are drawn according to a semi-logarithmic scale.
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