Abstract
Past hydrological interactions between the Mediterranean Sea and Black Sea are poorly resolved due to complications in establishing a high-resolution time frame for the Black Sea. We present a new greigite-based magnetostratigraphic age model for the Mio-Pliocene deposits of DSDP Hole 380/380A, drilled in the southwestern Black Sea. This age model is complemented by
| Original language | English |
|---|---|
| Pages (from-to) | 433-441 |
| Journal | Terra Nova |
| Volume | 27 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - 2015 |