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| Dimitrov, P; Ryan, W; Ballard, R; Haarmann, H; Dimitrov, D; Solakov, D; Slavova, K; Peev, P; Peychev, V; Petrov, P; Lericolais, Gilles. |
| The most recent geological history of the Black Sea, which covers the last 25 thousand years, is a subject of special attention today. This interest is due mainly to the hypothesis we have launched about the early Holocene flood in the Black Sea. This hypothesis was a real shock to the scientific community, among whom the Bulgarian geologists and archaeologists received it with great hostility. The anathematization was accompanied by a fierce media campaign, as a result of which Prof. Robert Ballard, the discoverer of Titanic, left Bulgaria disappointed. |
| Tipo: Text |
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| Ano: 2006 |
URL: http://archimer.ifremer.fr/doc/2006/acte-4934.pdf |
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| Eris, K; Ryan, W; Cagatay, M; Sancar, U; Lericolais, Gilles; Menot, G; Bard, E. |
| High-resolution reflection seismic profiles with core analyses of sedimentary sequence near the Sea of Marmara (SoM) entrance to the Strait of İstanbul (SoI, Bosphorus) provide detailed record of sealevel changes since the Late Glacial Maximum (LGM). The sequence is deposited over the LGM erosional surface at a maximum depth of -105 m. It includes seven seismic units that can be confidently correlated with 14C-dated sedimentary units in the cores. Unit 6 represents levee deposits of the paleo-SoI channel that was deposited by a Black Sea outflow during 11.2-10.6 kyr BP. The reflection surfaces at base of Unit 5 and 4 correspond to wave-cut terraces at -71and -63 m, respectively, and are estimated to be 10.6 and 9.8 kyr BP. The seismic Unit 2, overlaying a... |
| Tipo: Text |
Palavras-chave: Sapropel; Delta; Marmara Sea; Holocene; Sea level; Seismic stratigraphy. |
| Ano: 2007 |
URL: http://archimer.ifremer.fr/doc/2007/publication-3574.pdf |
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