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| Giresse, P; Buscail, R; Charriere, B. |
| The upper similar to50 cm sediments in the deep-sea Aegean Sea were generally deposited through hemipelagic rain as indicated by paucity of terrigenous sand-sized particles, abundance of clay-sized materials and lack of turbiditic beds. However, quartz sand-sized grains, black debris, higher C org content and ON ratio attest to a significant river-borne supply in the North Aegean Trough. Recurrent gravity-induced transfers from the shelf break are evidenced through various markers of coastal deposition dating back the last low-stand (Characea oogons, Elphidium crispum, Ammonia beccarii, glauconitic grains, evolved organic matter). Especially, this deposition induced significant rise of the C/N ratio of successive layers. The top of ash layers of the Minoan... |
| Tipo: Text |
Palavras-chave: Halocène tardif; Dépôt; Mer Egée; Late Holocene; Deposit; Aegean Sea. |
| Ano: 2003 |
URL: http://archimer.ifremer.fr/doc/00321/43256/42987.pdf |
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