Author:
Bouabid Najia,Srarfi Feyda,Tagorti Mohamed Ali
Publisher
Springer Science and Business Media LLC
Reference41 articles.
1. Abbes C, Zargouni F (1986) Anatomie d’un couloir de decrochements: le couloir de Hadifa (Chaine Nord des Chotts—Tunisie). Rev Sci Terre 4:31–37
2. Azuara J (2017) L’influence du climat et des activités humaines sur l’histoire holocène de la végétation du nord-ouest de la Méditerranée (Doctoral dissertation, Museum national d’histoire naturelle-MNHN PARIS)
3. Ben Ameur M, Masmoudi S, Omar H, Ouameni I, Medhioub M, Yaich C (2022) Middle to late Holocene sedimentary filling history of the Sebkha el Melah in south-eastern Tunisia. Sedimentol 69(5):2348–2366
4. Bond G, Kromer B, Beer J, Muscheler R, Evans MN, Showers W, Hoffmann S, Lotti-Bond R, Hajdas I, Bonani G (2001) Persistent solar influence on north Atlantic climate during the Holocene. Science 294:2130–2136
5. Boukhalfa K, Li G, Ben Ali W, Soussi M (2015) Early Cretaceous spinicaudatans (“conchostracans”) from lacustrine strata of the sidi aich formation in the northern chotts range, southern Tunisia: taxonomy, biostratigraphy and stratigraphic implication. Cretac Res 56:482–490. https://doi.org/10.1016/j.cretres.2015.06.006