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
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Astrophysique [astro-ph]Kazuyo Tachikawa : Connectez-vous pour contacter le contributeur
https://hal.science/hal-01463312
Soumis le : jeudi 9 février 2017-14:53:39
Dernière modification le : jeudi 28 mars 2024-09:24:15
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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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