Articles | Volume 41, issue 2
https://doi.org/10.5194/jm-41-129-2022
https://doi.org/10.5194/jm-41-129-2022
Research article
 | 
13 Sep 2022
Research article |  | 13 Sep 2022

Meghalayan environmental evolution of the Thapsus coast (Tunisia) as inferred from sedimentological and micropaleontological proxies

Mohamed Kamoun, Martin R. Langer, Chahira Zaibi, and Mohamed Ben Youssef

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Cited articles

Anzidei, M., Antonioli, F., Lambeck, K., Benini, A., Soussi, M., and Lakhdar, R.: New insights on the relative sea level change during Holocene along the coasts of Tunisia and western Libya from archaeological and geomorphological markers, Quaternary Int., 232, 5–12, 2011. 
Armynot du Châtelet, E., Francescangeli, F., and Frontalini, F.: Definition of benthic foraminiferal bioprovinces in transitional environments of the Eastern English Channel and the Southern North Sea, Rev. Micropal., 61, 223-234, 2018. 
Avnaim-Katav, S., Hyams-Kaphzan, O., Milker, Y., and Almogi-Labin, A.: Bathymetric zonation of modern shelf benthic foraminifera in the Levantine Basin, eastern Mediterranean Sea, J. Sea Res., 99, 97–106, 2015. 
Bahrouni, N., Bouaziz, S., Soumaya, A., Ben Ayed, N., Attafi, K., Houla, Y., El Ghali, A., and Rebai, N.: Neotectonic and seismotectonic investigation of seismically active regions in Tunisia: a multidisciplinary approach, J. Seismol., 18, 235–256, 2014. 
Ben Khalifa, K., Zaïbi, C., Bonnin, J., Carbonel, P., Zouari, K., Mnif, T., and Kamoun, F.: Holocene environment changes in the Hachichina wetland (Gulf of Gabes, Tunisia) evidenced by foraminifera and ostracods, geochemical proxies and sedimentological analysis, Riv. Ital. Paleontol. S., 125, 517–549, 2019. 
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Short summary
Sedimentology and micropaleontology analyses provide the dynamic processes that shaped the environmental evolution of the Thapsus coastline (Tunisia) including its lagoon and Roman harbor. The highlights are paleoenvironmental change records from the coast of Thapsus for the last 4000 years, benthic foraminiferal biota recording the dynamic coastal processes, two transgressive events being recognized, and a presented model for the paleoenvironmental evolution.
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