Nile floods recorded in deep Mediterranean sediments
Datos Bibliográficos
| ID | 24088409 |
|---|---|
| Autores | Emmanuelle Ducassou (Université de Bordeaux, autor de correspondencia), Thierry Mulder (Université de Bordeaux), Sébastien Migeon, Eliane Gonthier, Anne Murat (0000-0002-8666-9607, Conservatoire National des Arts et Métiers), Marie Revel, Lucilla Capotondi (0000-0003-3282-7910, Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche), Stefano M Bernasconi (0000-0001-7672-8856, ETH Zurich), Jean Mascle, Sébastien Zaragosi (0000-0002-1456-8129, Université de Bordeaux) |
| Año | 2008 |
| Volumen | 70 |
| Número | 3 |
| Páginas | 382-391 |
| Fecha de publicación | 2008-11-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Quaternary Research (JOURNAL) |
| Identificadores de la revista | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editorial | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1016/j.yqres.2008.02.011 |
| OpenAlex | W2049870640 |
| Idioma | EN |
| Citas recibidas | 4 |
| Referencias citadas | 54 |
Clastic mud beds rich in continental organic matter are observed recurrently in the Nile deep-sea turbidite system. They formed during flooding periods of the river similar to those that induce sapropel formation and occurred during periods of increased density stratification of the eastern Mediterranean. The very fine-grained flood deposits are intercalated within pelagic sediments, sapropels and Bouma-type turbidites. These flood deposits form by the successive reconcentrations of surface (hypopycnal) plumes by convective sedimentation, which in turn generate a fine-grained low-energy hyperpycnal flow. Sea-level high stands seem also to favor hypopycnal plume formation and increase clastic mud bed formation. Consequently, these muddy clastic beds provide a direct link between deep-marine sedimentary records and continental climatic change through flood frequency and magnitude.
Clastic rock · Deep sea · Geochemistry · Geomorphology · Mediterranean climate · Mediterranean sea · Sapropel · Sedimentary depositional environment · Sedimentary rock · Turbidite · Turbidity current · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Hydrocarbon exploration and reservoir analysis · Oceanography · Paleontology
Late Quaternary Sapropel Sediments in the Eastern Mediterranean Sea
Paleoclimatic Record of a Long Deep Sea Core from the Eastern Mediterranean
The Limnology, Climatology and Paleoclimatology of the East African Lakes
The Holocene climatic optimum and pollen records of sapropel 1 in the eastern Mediterranean, 9000–6000BP
Hydrological changes in the African tropics since the Last Glacial Maximum
Abrupt post-glacial climate events in West Asia and North Africa monsoon domains
Geomorphic/Tectonic Control of Sediment Discharge to the Ocean
The intercept is a poor estimate of a calibrated radiocarbon age
The Sahara and the Nile
Marine04 Marine Radiocarbon Age Calibration, 0–26 Cal Kyr Bp
Extended 14 C Data Base and Revised Calib 3.0 14 C Age Calibration Program
| Obras citantes distintas | 4 |
|---|---|
| Citas por año | 0,24 |
| Intervalo de citas | 2009 - 2018 (10) |
| Velocidad de citación | historical |
| Altamente citado | No |
| Tipos de cita | Neutras: 4 |