Stratigraphy and chronology of the Cala Mosca site, SW Sardinia (Italy)
Autor: | Daniele Sechi, Stefano Andreucci, Fabrizio Cocco, Vincenzo Pascucci |
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Rok vydání: | 2022 |
Předmět: | |
Zdroj: | Quaternary Research. 112:160-179 |
ISSN: | 1096-0287 0033-5894 |
DOI: | 10.1017/qua.2022.45 |
Popis: | The relict beach deposit of the Cala Mosca marine terrace is considered an important section of Marine Isotopic Stage (MIS) 5e (ca. 125 ka) sea-level highstands. Analysis of the stratigraphy and sediments of the deposit indicates the presence of a composite marine terrace comprising two superimposed marine units, luminescence dated to the MIS 5e (137 ± 7, 134 ± 7 ka) and MIS 5c (92 ± 6 ka) substages. The stratigraphic superimposition of the two highstands, both placed ~5 m above present sea level, agrees with other areas along the Sardinia coasts. The evident superimposition of two sea-level highstands and development of the composite terrace cannot be accounted solely by high-frequency sea-level oscillation that occurred within MIS 5 for the Mediterranean Sea. This suggests controversial, but significant, regional versus local tectonic activity occurred during the Late Pleistocene. |
Databáze: | OpenAIRE |
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