The convergence of biological and sedimentary data, supported by five new radiocarbon dates, allows to describe the Holocene relative rise in sea level along the banks of a Mediterranean lagoon. The marine transgression interfers with uplift and pulses of terrigenous deposition in the evolution of the coastline.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.