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Ar ages of tephra layers from an aggradational succession (Valle Giulia Formation) near the mouth of the Tiber Valley in Rome that was deposited in response to sea-level rise during Marine Isotopic Stage (MIS) 13.
The sole purpose of the UCCJEA is to ensure that states honor the child custody orders of other states, in order to prevent parental abduction or other custody problems.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.
Ar ages of the primary pyroclastic deposits of Tufo Giallo di Prima Porta (TGPP) and Fall A1 occurring at the base and in the middle of the fluvial-lacustrine succession (sample NCR4, NCR1, Table 1, Fig. In order to provide further constraints on the deposition of the VGF, two samples of pyroclastic-fall deposits (sample C2-SC, C5-SC, Table 1) at the proximal section of Santa Cecilia (Figs 1 and 3) also have been dated and correlated with Fall A1 and Fall C, respectively.