Évolution du trait de côte à l’Holocène supérieur dans la Sebkha El-Guettiate de Skhira (Golfe de Gabès, Tunisie) à travers sa faune d’ostracodes et de foraminifères

Zaïbi, Chahira; Carbonel, Pierre; Kamoun, Fékri; Azri, Chafai; Kharroubi, Amira; Kallel, Néjib; Jedoui, Younes; Montacer, Mabrouk; Fontugne, Michel

doi:10.1016/j.geobios.2010.11.002

Cited by 17 publications

(2 citation statements)

References 46 publications

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“…The Gulf of Gabes and its associated coastal wetlands are considered highly productive areas, contributing about 40 percent of Tunisia's total fish production (DGPA 2015). Numerous recent studies on modern shallow-water benthic foraminifera have provided essential contributions and information on the species richness, habitat structures, and evolution coastal environments along the coast of Tunisia Zaïbi et al 2011;Zaïbi et al 2016;Ben Khalifa et al 2019;Kamoun et al 2019;Kamoun et al 2022a;Kamoun et al 2022b). This work has contributed to a better understanding of the evolution of the Tunisian coast, a coastal environment that has undergone significant changes over the last 6000 years due to tectonic, climatic, and anthropogenic forcing (Jedoui et al 1998;Anzidei et al 2011;Zaïbi et al 2016;.…”

Section: Discussionmentioning

confidence: 97%

Lower Paleocene foraminiferal assemblages from the Tibeisale Formation in the Arctic region of Western Siberia

Trubin¹,

Marinov²,

Smirnov³

et al. 2022

njgpa

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Bioerosion structures, such as holes, pits, and grooves, found on the surface of benthic foraminiferal tests from the Upper Cretaceous and Paleogene of Western Siberia have been analysed. The morphology is examined, their potential origin and the paleogeographic and stratigraphic distribution within sections illustrating marine basins of Western Siberia are discussed. The assemblage of ichnospecies under examination comprises Oichnus simplex

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Section: Discussionmentioning

confidence: 97%

Lower Paleocene foraminiferal assemblages from the Tibeisale Formation in the Arctic region of Western Siberia

Trubin¹,

Marinov²,

Smirnov³

et al. 2022

njgpa

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“…Other studies have focused on foraminifera as proxies to trace the evolution of coastal systems. There are numerous examples only in the Mediterranean area, such as the Elx lagoon (Blázquez and Usera, 2010), the Ebro delta (Cearreta et al, 2016), the plain and delta of the Po River (Fiorini, 2004; Rossi and Horton, 2009; Rossi and Vaiani, 2008), and the Venice lagoon (Serandrei Barbero et al, 1997), together with other coastal areas in Italy (Carboni et al, 2010; Di Bella et al, 2014; Ricci et al, 2006), in sebkhas in Northern Africa (Zaibi et al, 2011), in littoral and marginal marine environments in the coasts of Greece (Avramidis et al, 2013; Drinia and Anastasakis, 2012; Drinia et al, 2014; Hageman, 1979; Koukousioura et al, 2012; Nixon et al, 2009), or in coastal and athalassic basins in Israel (Avnaim-Katav et al, 2013), among many others.…”

Section: Introductionmentioning

confidence: 99%

Maximum flood area during MIS 1 in the Almenara marshland (Western Mediterranean): Benthic foraminifera and sedimentary record

et al. 2018

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The sedimentological and micropaleontological analysis of three mechanical cores in the marshland of Almenara (Valencian Community, Spain) has allowed the reconstruction of the Holocene evolution of this wetland. The cold and dry 8.2-ka event might be represented in Almenara by a massive carbonate precipitation bed, upon which mid- and late-Holocene sediments were subsequently deposited. The direct influence of sea-level changes has been recorded in the two cores (S-4 and S-5) located near the marsh barrier, at 400–450 m from the current coastline. The maximum flood area during MIS 1 (last 11,600 years) is represented in these cores by sediments indicative of different littoral subenvironments (shoreface, foreshore, backshore). These sediments contain typically littoral marine foraminiferal species such as Ammonia beccarii, Rosalina globularis, Asterigerinata mamilla, Adelosina longirostra, Cibicidoides lobatulus, Elphidium macellum, and Bolivina pseudoplicata. The base of these littoral sedimentary materials has been dated as 5480 and 5580 cal. yr BP. At this moment, the inner area (core S-7) was occupied by a restricted oligohaline marsh subject to water-table fluctuations and with scarce individuals of brackish water foraminifera, such as Ammonia tepida, Haynesina germanica, or Cribroelphidium excavatum, that in more recent times (since at least 1700 cal. yr BP) gradually evolved to a palustrine area.

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Paleoenvironment Evolution of a Paralic System, El Guettiate and Dreïaa Sebkhas (Gulf of Gabès, Tunisia)

Gargouri

Zouari

2019

Patterns and Mechanisms of Climate, Paleoclimate and Paleoenvironmental Changes From Low-Latitude Regions

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Évolution du trait de côte à l’Holocène supérieur dans la Sebkha El-Guettiate de Skhira (Golfe de Gabès, Tunisie) à travers sa faune d’ostracodes et de foraminifères

Cited by 17 publications

References 46 publications

Lower Paleocene foraminiferal assemblages from the Tibeisale Formation in the Arctic region of Western Siberia

Lower Paleocene foraminiferal assemblages from the Tibeisale Formation in the Arctic region of Western Siberia

Maximum flood area during MIS 1 in the Almenara marshland (Western Mediterranean): Benthic foraminifera and sedimentary record

Paleoenvironment Evolution of a Paralic System, El Guettiate and Dreïaa Sebkhas (Gulf of Gabès, Tunisia)

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