Unraveling North-African riverine and eolian contributions to central Mediterranean sediments during Holocene sapropel S1 formation
Résumé
Hydroclimate variability has exerted a fundamental control on the alternating deposition of organic-lean marl and organic-rich sapropel sediments in the eastern Mediterranean Sea (EMS). However, the exact mechanisms regarding the freshwater sources and related changes are still debated. Here, Sr and Nd isotopes and high-resolution elemental data are used to constrain different riverine and eolian supplies to the central Mediterranean over the past 9.8 l
Domaines
Astrophysique [astro-ph]Origine | Fichiers produits par l'(les) auteur(s) |
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https://hal.science/hal-01463312
Soumis le : jeudi 17 octobre 2024-17:29:17
Dernière modification le : vendredi 18 octobre 2024-03:05:42
Dates et versions
Identifiants
- HAL Id : hal-01463312 , version 1
- DOI : 10.1016/j.quascirev.2016.09.029
Citer
Jiawang Wu, Philipp Boening, Katharina Pahnke, K. Tachikawa, Gert J. De Lange. Unraveling North-African riverine and eolian contributions to central Mediterranean sediments during Holocene sapropel S1 formation. Quaternary Science Reviews, 2016, 152, pp.31-48. ⟨10.1016/j.quascirev.2016.09.029⟩. ⟨hal-01463312⟩
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