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Moreover, the ages obtained for this study give us the opportunity to compare the timing of the sea-level fluctuations inferred from the stratigraphic record and that provided by the astrochronologic calibration of the Oxygen isotopic curves, and to assess the calibrations of Assessing ages of sedimentary successions deposited in near-coastal environments in response to sea-level fluctuations is a straightforward mean to investigate the timing of glacio-eustatic cycles and provide insights on their forcing mechanisms.In this light, the coastal plain of the Tiber River near Rome (Fig.The new geochronologic constraints suggest a long duration for the period of sea-level rise (533 ± 2 through 498 ± 2 ka) encompassing two consecutive positive peaks of the δO curve (substages 13.3 and 13.1).Consistently, the litho-stratigraphic features of the sedimentary record account for two aggradational phases separated by an intervening erosional phase.Moreover, the newly provided ages and those of the Paleo-Tiber River dataset give us the opportunity to compare the match between the timing of the sea-level fluctuations inferred from the stratigraphic record and that provided by the astrocalibration of the isotopic curves, and to assess the calibrations of the The Valle Giulia Formation (hereby VGF) was introduced by (ref.23) to designate the fluvial deposits of the Paleo-Tiber River in Rome emplaced during sea-level rise of MIS 13. 2) provided geologic constraints on the VGF through Ar dating of several tephra layers, allowing (ref.8) used the ages of the gravel-clay transitions in the older aggradational successions of the Paleo-Tiber River, determined through .

16), provided constraints on the late aggradational phase during the high stand of MIS 13.(a) composite N-S cross-section, correlating different outcrops and borehole logs along the Tiber valley (see Fig.1 for location), showing the stratigraphic position of the pyroclastic-flow deposits of Tufo del Palatino (TP), Tufo Giallo di Prima Porta (TGPP) and Grottarossa Pyroclastic Sequence (GRPS), and of Tufo Lionato (TL).(b) Reconstruction of the erosional/depositional phases during aggradation of the VGF, showing the occurrence of an early aggradational phase coeval with emplacement of TP (I-II-III), followed by a regression coeval with emplacement of TGPP (IV-V) and by a new aggradational phase (VI); reported ages according to this study (see text for detail).Supplementary Figure 1 shows the Zr/Y vs Nb/Y composition of the analysed samples of volcanic deposit and their correlation with known eruptive units.(a) Cross-section showing the stratigraphic relationships among the VGF and the previous (Santa Cecilia Formation -SC, MIS 15 (ref.3)) and the following (San Paolo Formation -SP, MIS 11 (ref.

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