Meghalayen Climate and Environment Changes Inferred from Geochemical, Paleontological, and Sedimentological Proxies of Lagoonal Sediment Sequences of the Thapsus Coast (Eastern Tunisia)

Author:

Kamoun Mohamed,Langer Martin R.,Zaibi Chahira,Ben Youssef Mohamed,Kallel Amjad,Kamoun Fekri

Publisher

Springer Nature Switzerland

Reference12 articles.

1. Anzidei, M., Antonioli, F., Lambeck, K., Benini, A., Soussi, M., & Lakhdar, R. (2011). New insights on the relative sea level change during Holocene along the coasts of Tunisia and western Libya from archaeological and geomorphological markers. Quaternary International, 232, 5–12.

2. Ben Khalifa, K., Zaïbi, C., Bonnin, J., Carbonel, P., Zouari, K., Mnif, T. & Kamoun, F. (2019). Holocene environment changes in the Hachichina wetland (Gulf of Gabes, Tunisia) evidenced by foraminifera and ostracods, geochemical proxies and sedimentological analysis. RivistaItaliana di Paleontologia e Stratigrafia, 125, 517–549.

3. Ben Hamad, A., Viehberg, F., Khadraoui, A., Zaïbi, C., Trabelsi, Y., Mouanga, G. H., Langer, M. R, Abida, H., & Kamoun, F. (2018). Water level and atmospheric humidity history of lake Ichkeul (northern Tunisia) during the last 3000 years. Arabian Journal Geosciences, 11(12), 316

4. Cimerman, F. & Langer, M. R. (1991). Mediterranean foraminifera—Academia Scientarium et Artium Slovenica, Dela, Opera 30, Classis IV: Historia Naturalis( p. 1–119, pl. 1–93). Ljubljana.

5. Jedoui, Y., Kallel, N., Fontugne, M., Ben Ismail, M. H., M'Rabet, A., & Montacer, M. (1998). A high relative sea level stand in the middle Holocene of Southeastern Tunisia. Marine Geology, 147, 123–130.

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