| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 7452392 | Quaternary International | 2014 | 10 Pages |
Abstract
Similar measurements in a pelecypod valve (Cerastoderma sp.) and a vermetid colony at San Marco yielded much younger apparent ages, tentatively attributed to late “diagenetic” U-uptake processes. Both the first minor pulses and the most important “eustatic” pulse recorded at San Giovanni di Sinis cannot be assigned unequivocally to one of the MIS 5e sea-level oscillations proposed in the recent literature, due to dating inaccuracies and uncertainties, but it seems probable that it occurred during an early part of the interval.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Salvatore Carboni, Luciano Lecca, Claude Hillaire-Marcel, Bassam Ghaleb,