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1

Morzadec-Kerfourn, Marie Thérèse. "L'évolution des Sebkhas du golf de Gabès (Tunisie) à la transition Pléistocène supérieur-Holocène." Quaternaire 13, no. 2 (2002): 111–23. http://dx.doi.org/10.3406/quate.2002.2185.

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ZAIBI, CHAHIRA, BURKHARD SCHARF, FINN ANDREAS VIEHBERG, DIETMAR KEYSER, and FEKRI KAMOUN. "Preliminary report on the living non-marine Ostracoda (Crustacea) from Tunisia with the description of a new Psychrodromus species." Zootaxa 3626, no. 4 (2013): 499–516. http://dx.doi.org/10.11646/zootaxa.3626.4.5.

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Since 1928, Henri Gauthier has been the only zoologist to describe the extant non-marine ostracod fauna of Tunisia. In 2010, new samples of living non-marine ostracods were collected from central and southern Tunisia. A complete list of the 41 non-marine ostracods of Tunisiais presented, including the species of Gauthier’s work, published Holocene records, and new results from our field study. Historical faunal variations (El Melah Lagoon, Lac de Tunis, Sebkhas El- Guettiate and Dreîaa, and Lac Ichkeul) are briefly discussed and related to recent environmental changes. In 2006, El Melah Lagoon
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Marquer, L., S. Pomel, A. Abichou, E. Schulz, D. Kaniewski, and E. Van Campo. "Late Holocene high resolution palaeoclimatic reconstruction inferred from Sebkha Mhabeul, southeast Tunisia." Quaternary Research 70, no. 2 (2008): 240–50. http://dx.doi.org/10.1016/j.yqres.2008.06.002.

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AbstractRelations between climate change and landscape evolution during the last two millennia in southeastern coastal Tunisia have been documented using high-resolution reconstruction of flood history and fire activity in the Sebkha Mhabeul core. The age model, based on tephrochronology, indicates that the core extends from Roman to modern times and encompasses the well-defined climatic periods of the last two millennia. This record provides a first palaeoecological/palaeoclimatic high resolution reconstruction in North Africa using a cross-disciplinary approach with both physical (grey-scale
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Essefi, Elhoucine, Samir Mefteh, Mounir Medhioub, and Chokri Yaich. "Magnetic Study of the Heated and Unheated Sedimentary Fillings of Sebkha Mhabeul, Southeast Tunisia: A Geophysical Method for Paleoclimatic Investigation and Tephrochronological Dating." International Journal of Geophysics 2014 (2014): 1–7. http://dx.doi.org/10.1155/2014/908395.

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This paper is meant to investigate the climatic and volcanic signals within the sedimentary filling of sebkha Mhabeul through a thermomagnetic study of a 37 cm length core. Values of the magnetic susceptibility at ambient temperature show that the core encompasses four climatic stages: the Warming Present (WP), the Little Ice Age (Late LIA), Early Little Ice Age (ELIA), and the Medieval Climate Anomalies (MCA). Added to the subcycles, the spectral analysis shows the individualization of an 888 yr cycle probably related to solar activity. The heating at 250°C is good-for-nothing since it was us
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Brahim, Fawzi. "Évolution de la paléolagune-sebkha d’Ennjila et de ses environs (Sahel tunisien – Tunisie orientale)." Méditerranée, no. 125 (November 1, 2015): 51–62. http://dx.doi.org/10.4000/mediterranee.7928.

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Chaggar, Meriem, and Mohsen Boubaker. "IDENTIFICATION OF NEW ICONIC OBJECTS FOR THE SUSTAINABLE DEVELOPMENT OF HERGLA (TUNISIA)." International Journal of Engineering Technologies and Management Research 5, no. 12 (2020): 101–13. http://dx.doi.org/10.29121/ijetmr.v5.i12.2018.332.

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This paper discusses the issue of territorial identity by facing globalization in Hergla's delegation. In order to requalify the “image of the city”, amulticriteria analysis of the landscape units ofthe “El Medfoun” forest and the Sebkha “Halk El Menjel” has been developed to detect symbol indices of change for a new “territorial landscaping”. These natural areas were identified as new iconic objects. Indeed, the Sebkha and the forest, carrying ecological, patrimonial, social and economic values, may be integrated into a territorial project, through of landscape geomediation practices. These v
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Essefi, Elhoucine, and Mohamed Ali Tagorti. "Geoeconomic interest of minerals assemblage of sebkha El Melah, southeastern Tunisia." Water Practice and Technology 16, no. 2 (2021): 633–47. http://dx.doi.org/10.2166/wpt.2021.004.

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Abstract This work aimed to study the formation of salt through a progressive evaporation of sebkha El Melah brine. The precipitated salt in the case of sebkha El Melah is variable along the progressive evaporation. Weights of salt after each phase of precipitation indicate a heterogeneous evaporation process cumulating at 315 g L−1. With an increasing evaporation of El Melah brine, the number of precipitated mineral species increased. The cumulative number of species along the evaporation process reached 20, including principally: Halite (NaCl) (73–95%), epsomite (MgSO4·7H2O) (7–14%), bischof
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Najjari, Afef, Mostafa S. Elshahed, Ameur Cherif, and Noha H. Youssef. "Patterns and Determinants of Halophilic Archaea (Class Halobacteria) Diversity in Tunisian Endorheic Salt Lakes and Sebkhet Systems." Applied and Environmental Microbiology 81, no. 13 (2015): 4432–41. http://dx.doi.org/10.1128/aem.01097-15.

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ABSTRACTWe examined the diversity and community structure of members of the halophilicArchaea(classHalobacteria) in samples from central and southern Tunisian endorheic salt lakes and sebkhet (also known as sebkha) systems using targeted 16S rRNA gene diversity survey and quantitative PCR (qPCR) approaches. Twenty-three different samples from four distinct locations exhibiting a wide range of salinities (2% to 37%) and physical characteristics (water, salt crust, sediment, and biofilm) were examined. A total of 4,759 operational taxonomic units at the 0.03 (species-level) cutoff (OTU0.03s) bel
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Boujelben, Abdelkarim, Vincent Lebreton, and Mohamed Raouf Karray. "Dynamique lacustre Holocène dans la sebkha al Kalbiyya(Tunisie centre orientale)." Quaternaire, no. 28/2 (May 29, 2017): 239–45. http://dx.doi.org/10.4000/quaternaire.8138.

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Kbir-Ariguib, Najia, Dalila Ben Hassan Chehimi, and Lotfi Zayani. "Treatment of Tunisian salt lakes using solubility phase diagrams." Pure and Applied Chemistry 73, no. 5 (2001): 761–70. http://dx.doi.org/10.1351/pac200173050761.

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The Tunisian salt lakes are considered as an important materials resource useful for industry and agriculture. They are called sebkhat or chott, and they cover a large part of Tunisian land. Their brines correspond to the quinary system: Na+, K+, Mg2+ / Cl­, SO42­­H2O. In the first part of this paper, a short description and abstracted geochemical and economical data about some Tunisian salt lakes are given. In the second part, the fitting equations used for modeling the quinary system are established and applied to the subsystems NaCl­KCl­H2O, NaCl­MgCl2­H2O, KCl­MgCl2­H2O, and to NaCl­Na2SO4
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Jaouadi, Sahbi, Vincent Lebreton, Viviane Bout-Roumazeilles, et al. "Environmental changes, climate and anthropogenic impact in south-east Tunisia during the last 8 kyr." Climate of the Past 12, no. 6 (2016): 1339–59. http://dx.doi.org/10.5194/cp-12-1339-2016.

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Abstract. Pollen and clay mineralogical analyses of a Holocene sequence from Sebkha Boujmel (southern Tunisia) trace the climatic and environmental dynamics in the lower arid bioclimatic zone over the last 8000 years. During the mid- to late Holocene transition, between ca. 8 and 3 ka BP, a succession of five wet–dry oscillations is recorded. An intense arid event occurs between ca. 5.7 and 4.6 ka BP. This episode marks the onset of a long-term aridification trend with a progressive retreat of Mediterranean woody xerophytic vegetation and of grass steppes. It ends with the establishment of pre
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Chabbi, Iness, Moez Bahloul, Rim Dammak, and Chafai Azri. "DUST PARTICLE DEPOSITION QUALITY ASSESSMENT IN RURAL AREAS LOCATED NOT FAR FROM A CONGESTED HIGHWAY AND SEVERAL SEBKHAS: CASE OF MONASTIR REGION, EASTERN TUNISIA." Journal of Environmental Engineering and Landscape Management 26, no. 2 (2018): 141–57. http://dx.doi.org/10.3846/16486897.2017.1378221.

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In order to better understand the processes of removing atmospheric particles to the surface, dry particle deposition in Monastir region (eastern Tunisia) has been studied. As a first step, a biweekly monitoring of the particulate deposits was carried out in 26 sites from January to August, 2012. Secondly, two particular sites were investigated from October, 2014 to August, 2015. A very high fluctuation in those particle fluxes, ranging from 0.560 to 2.210 g/m2/14days, was clearly observed. The spatial distribution of particulate deposits shows a growing trend from rural to urban (coastal) are
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13

Ayache, F., A. M. Gammar, and M. Chaouach. "Environmental dynamics and conservation of the flamingo in the vicinity of Greater Tunis, Tunisia: the case study of Sebkha Essijoumi." Earth Surface Processes and Landforms 31, no. 13 (2006): 1674–84. http://dx.doi.org/10.1002/esp.1438.

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Abdeljabbar, HEDI, ESSGHAIER Badiaa, CAYOL Jean-Luc, FARDEAU Marie-Laure, and SADFI Najla. "Prokaryotic biodiversity of halophilic microorganisms isolated from Sehline Sebkha Salt Lake (Tunisia)." African Journal of Microbiology Research 8, no. 4 (2014): 355–67. http://dx.doi.org/10.5897/ajmr12.1087.

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Essefi, Elhoucine. "Geochemistry and mineralogy of the sebkha Oum El Khialate evaporites mixtures, southeastern Tunisia." Resource Geology 71, no. 3 (2021): 242–49. http://dx.doi.org/10.1111/rge.12264.

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16

Hollis, G. E., and M. R. Kallel. "Modelling Natural and Man-Induced Hydrological Changes on Sebkhet Kelbia, Tunisia." Transactions of the Institute of British Geographers 11, no. 1 (1986): 86. http://dx.doi.org/10.2307/622073.

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DUPLAY, JOËLLE, SLIM KHEDHIRI, KHADIJA SEMHI, and FADILA DARRAGI. "Water quality in a protected natural wetland: El Kelbia sebkhet, Tunisia." International Journal of Environmental Studies 70, no. 1 (2013): 33–48. http://dx.doi.org/10.1080/00207233.2012.747249.

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18

Schulz, E., A. Abichou, T. Hachicha, S. Pomel, U. Salzmann, and K. Zouari. "Sebkhas as ecological archives and the vegetation and landscape history of southeastern Tunisia during the last two millennia." Journal of African Earth Sciences 34, no. 3-4 (2002): 223–29. http://dx.doi.org/10.1016/s0899-5362(02)00021-0.

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Turki, Souad, Abderrazak Mastouri, Fourat Akrout, Noura Balti, Intissar Baouech, and Ridha M’rabet. "Potential impacts of sebkhet Ariana rainfall discharges on the trophic state of the coastal zone of Raoued (Gulf of Tunis, Tunisia)." Desalination 246, no. 1-3 (2009): 337–43. http://dx.doi.org/10.1016/j.desal.2008.03.058.

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Ben Ameur, Mariem, Sameh Masmoudi, Abdelhakim Abichou, Mounir Medhioub, and Chokri Yaich. "Use of the magnetic, geochemical, and sedimentary records in establishing paleoclimate change in the environment of Sebkha: Case of the Sebkha Mhabeul in southeastern Tunisia." Comptes Rendus Geoscience 351, no. 7 (2019): 487–97. http://dx.doi.org/10.1016/j.crte.2019.10.003.

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Chouari, Walid. "Spatialisation et Analyse du Risque d’Inondation dans le Bassin versant de la Sebkha de l’Ariana (Tunisie Nord-orientale)." Bulletin de la Société de Géographie d'Egypte 89, no. 1 (2016): 123–54. http://dx.doi.org/10.21608/bsge.2016.90344.

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Chairi, Raja. "Etude du remplissage sédimentaire d’un système hypersalin de la Tunisie orientale au cours du Quaternaire récent : la sebkha de Moknine." Quaternaire, no. 16/2 (August 1, 2005): 107–17. http://dx.doi.org/10.4000/quaternaire.328.

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Fezei, Radouanne, Halim Hammi, and Adel M’nif. "Extractive process for preparing high purity magnesium chloride hexahydrate." Chemical Industry and Chemical Engineering Quarterly 18, no. 1 (2012): 83–88. http://dx.doi.org/10.2298/ciceq110815049f.

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This paper refers a method for the preparation of magnesium chloride hexahydrate (bischofite) from Sebkha el Melah of Zarzis Tunisian natural brine. It is a five-stage process essentially based on crystallization by isothermal evaporation and chemical precipitation. The two first steps were dedicated to the crystallization of sodium chloride and potassiummagnesium double salts, respectively. Then, the resulting liquor was desulfated using calcium chloride solution. After that another isothermal evaporation stage was implemented in order to eliminate potassium ions in the form of carnallite, KC
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Jaouani, Atef, Mohamed Neifar, Valeria Prigione, et al. "Diversity and Enzymatic Profiling of Halotolerant Micromycetes from Sebkha El Melah, a Saharan Salt Flat in Southern Tunisia." BioMed Research International 2014 (2014): 1–11. http://dx.doi.org/10.1155/2014/439197.

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Twenty-one moderately halotolerant fungi have been isolated from sample ashes collected from Sebkha El Melah, a Saharan salt flat located in southern Tunisia. Based on morphology and sequence inference from the internal transcribed spacer regions, 28S rRNA gene and other specific genes such asβ-tubulin, actin, calmodulin, and glyceraldehyde-3-phosphate dehydrogenase, the isolates were found to be distributed over 15 taxa belonging to 6 genera of Ascomycetes:Cladosporium(n=3),Alternaria(n=4),Aspergillus(n=3),Penicillium(n=5),Ulocladium(n=2), andEngyodontium(n=2). Their tolerance to different co
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Essefi, Elhoucine. "Geoeconomic Interest Versus Environmental and Health Issues of the Mineralogical Assemblage of Sebkha Oum El Khialate, Southeastern Tunisia." Arabian Journal for Science and Engineering 46, no. 6 (2021): 5835–45. http://dx.doi.org/10.1007/s13369-020-05244-5.

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Essefi, Elhoucine, Jamel Touir, Mohamed Ali Tagorti, and Chokri Yaich. "Record of the Climatic Variability and the Sedimentary Dynamics during the Last Two Millennia at Sebkha Dkhila, Eastern Tunisia." ISRN Geology 2013 (July 15, 2013): 1–9. http://dx.doi.org/10.1155/2013/936198.

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This paper aimed to study the record of the climatic variability during the last two millennia within the sebkha of Dkhila. Six climatic stages were recognized along the 104 cm core: the Warming Present (WP), the Late Little Ice Age (Late LIA), the Early Little Ice Age (ELIA), the Medieval Climatic Anomaly (MCA), the Dark Age (DA), and the Roman Warm Period (RWP). The WP stretches along the uppermost 1 cm with a high grey scale as sign of a dry climate. The Late LIA is located between 1 cm and 6 cm. The ELIA is located between 6 cm and 40 cm. The MCA spanning from 40 cm to 72 cm is marked by a
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Zaïbi, Chahira, Pierre Carbonel, Fekri Kamoun, et al. "Evolution of the sebkha Dreîaa (South-Eastern Tunisia, Gulf of Gabes) during the Late Holocene: Response of ostracod assemblages." Revue de Micropaléontologie 55, no. 3 (2012): 83–97. http://dx.doi.org/10.1016/j.revmic.2012.03.003.

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Abdeljabbar, Hedi, Jean-Luc Cayol, Wajdi Ben Hania, Abdellatif Boudabous, Najla Sadfi, and Marie-Laure Fardeau. "Halanaerobium sehlinense sp. nov., an extremely halophilic, fermentative, strictly anaerobic bacterium from sediments of the hypersaline lake Sehline Sebkha." International Journal of Systematic and Evolutionary Microbiology 63, Pt_6 (2013): 2069–74. http://dx.doi.org/10.1099/ijs.0.040139-0.

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A strictly anaerobic, extremely halophilic, Gram-positive, rod-shaped bacterium was isolated from the hypersaline (>20 % NaCl) surface sediments of Sehline Sebkha in Tunisia. The strain, designated 1SehelT, was strictly halophilic and proliferated at NaCl concentrations of between 5 % and 30 % (saturation), with optimal growth at 20 % NaCl. Strain 1SehelT was non-spore-forming, non-motile, appearing singly or in pairs, or occasionally as long chains and measured 0.5–0.8 µm by 3–10 µm. Strain 1SehelT grew optimally at pH values of 7.4 but had a very broad pH range for growth (pH 5.2–9.4). It
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Essefi, Elhoucine, Mohamed Ali Tagorti, Jamel Touir, and Chokri Yaich. "Hydrocarbons Migration through Groundwater Convergence toward Saline Depressions: A Case Study, Sidi El Hani Discharge Playa, Tunisian Sahel." ISRN Environmental Chemistry 2013 (October 30, 2013): 1–14. http://dx.doi.org/10.1155/2013/709190.

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This paper aims to provide proofs of hydrocarbons migration from petroleum reservoirs towards the surface of discharge playas. This is a case study of the discharge playa of Sidi El Hani, eastern Tunisia. The geochemistry of water of some hydrological drills in the Sahel area and of water from the discharge playa proves relatedness between the deep aquifer and the water of the discharge playa. Thus, the hydrology is now more than likely converging from the subsurface. This convergence may be an agent of transport of hydrocarbons. Concerning the organic matter within the discharge playa, high p
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Lebreton, Vincent, Sahbi Jaouadi, Simone Mulazzani, et al. "Early oleiculture or native wildOleain eastern Maghreb: new pollen data from the sebkha-lagoon Halk el Menjel (Hergla, Central Tunisia)." Environmental Archaeology 20, no. 3 (2014): 265–73. http://dx.doi.org/10.1179/1749631414y.0000000046.

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Wali, Ahmed, Atsushi Kawachi, Mohamed Seddik Mahmoud Bougi, et al. "Effects of Metal Pollution on Sediments in a Highly Saline Aquatic Ecosystem: Case of the Moknine Continental Sebkha (Eastern Tunisia)." Bulletin of Environmental Contamination and Toxicology 94, no. 4 (2015): 511–18. http://dx.doi.org/10.1007/s00128-015-1469-9.

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Sellami, Imene, Guy Charmantier, Hachem B. Naceur, Adnane Kacem, and Catherine Lorin-Nebel. "Osmoregulatory performance and immunolocalization of Na+/K+-ATPase in the branchiopod Artemia salina from the Sebkha of Sidi El Hani (Tunisia)." Tissue and Cell 63 (April 2020): 101340. http://dx.doi.org/10.1016/j.tice.2020.101340.

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Sellami, Imene, Hachem Ben Naceur, and Adnane Kacem. "Reproductive performance in successive generations of the brine shrimp Artemia salina (Crustacea: Anostraca) from the Sebkha of Sidi El Hani (Tunisia)." Animal Reproduction Science 225 (February 2021): 106692. http://dx.doi.org/10.1016/j.anireprosci.2021.106692.

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Sellami, Imene, Hachem Ben Naceur, and Adnane Kacem. "Study of Cysts Biometry and Hatching Percentage of the Brine Shrimp Artemia salina (Linnaeus, 1758) from the Sebkha of Sidi El Hani (Tunisia) According to Successive Generations." Aquaculture Studies 21, no. 1 (2020): 41–46. http://dx.doi.org/10.4194/2618-6381-v21_1_05.

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Artemia salina cysts harvested from the Sebkha of Sidi El Hani were hatched and cultivated in the laboratory. The obtained nauplii were acclimated at 90 ppt and fed with Dunaliella salina microalgae until the adult stage called generation 1 (G1) was reached. Ten couples were isolated and acclimated in the same conditions. Observations of the offspring lasted for a maximum of 60 days. Cysts obtained from G1 were collected and counted. Cyst diameter, chorion thickness and hatching percentage were established. Nauplii obtained from G1 were labelled G2. The third (G3) and the fourth (G4) generatio
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Hmidi, Dorsaf, Dorsaf Messedi, Claire Corratg�-Faillie, et al. "Investigation of Na+ and K+ Transport in Halophytes: Functional Analysis of the HmHKT2;1 Transporter from Hordeum maritimum and Expression under Saline Conditions." Plant and Cell Physiology 60, no. 11 (2019): 2423–35. http://dx.doi.org/10.1093/pcp/pcz136.

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Abstract Control of K+ and Na+ transport plays a central role in plant adaptation to salinity. In the halophyte Hordeum maritimum, we have characterized a transporter gene, named HmHKT2;1, whose homolog HvHKT2;1 in cultivated barley, Hordeum vulgare, was known to give rise to increased salt tolerance when overexpressed. The encoded protein is strictly identical in two H. maritimum ecotypes, from two biotopes (Tunisian sebkhas) affected by different levels of salinity. These two ecotypes were found to display distinctive responses to salt stress in terms of biomass production, Na+ contents, K+
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Ferchichi, Selma, Kamel Hessini, Emilia Dell'Aversana, et al. "Hordeum vulgare and Hordeum maritimum respond to extended salinity stress displaying different temporal accumulation pattern of metabolites." Functional Plant Biology 45, no. 11 (2018): 1096. http://dx.doi.org/10.1071/fp18046.

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Hordeum maritimum With. (= H. marinum Huds. subsp. marinum, 2n = 14) is a wild cereal present in the saline depressions of the Soliman and Kelbia Sebkhas, which contributes significantly to annual biomass production in Tunisia. This species is able to tolerate high NaCl concentrations at the seedling stage without showing symptoms of toxicity; however, the tolerance strategy mechanisms of this plant have not yet been unravelled. Our metabolite analysis, performed on leaves of H. maritimum during extended stress in comparison with Hordeum vulgare L. cv. Lamsi, has revealed an adaptive response
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Jaouadi, Sahbi, Vincent Lebreton, Beya Mannai-Tayech, Rached Lakhdar, and Mohamed Soussi. "Apport de l’analyse pollinique des sédiments de la sebkha Boujmel (Sud-Est tunisien) à la reconstitution des paléopaysages et paléoclimats holocènes en milieu aride." Méditerranée, no. 125 (November 1, 2015): 39–49. http://dx.doi.org/10.4000/mediterranee.7891.

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Zaîbi, Chahira, Pierre Carbonel, Fekri Kamoun, et al. "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." Geobios 44, no. 1 (2011): 101–15. http://dx.doi.org/10.1016/j.geobios.2010.11.002.

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Perthuisot, J. P., S. Castanier, and A. Maurin. "La huntite (CaMg <sub>3</sub> (CO <sub>3</sub> ) <sub>4</sub> ) de la Sebkha el Melah (Zarzis, Tunisie); un exemple de microbiodiagenese carbonatogene." Bulletin de la Société Géologique de France VI, no. 4 (1990): 657–66. http://dx.doi.org/10.2113/gssgfbull.vi.4.657.

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Chairi, Raja, and Saadi Abdeljaouad. "Étude environnementale et géomorphologique des Sebkhas de Gotaia et Eliane en relation avec l’évolution de la Sebkha de Moknine (Tunisie orientale)." Géomorphologie : relief, processus, environnement 25, no. 2 (2019). http://dx.doi.org/10.4000/geomorphologie.13086.

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Mahdhi, Abdelkarim, Concetta Messina, Fathi Kamoun, Andrea Santulli, and Amina Bakhrouf. "Determination of biological characteristics of Tunisian Artemia salina populations." Biologia 67, no. 1 (2012). http://dx.doi.org/10.2478/s11756-011-0149-4.

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AbstractIn this study, Artemia salina cysts collected from four Tunisian hypersaline environments were characterized using biometrical, biological and biochemical descriptors. Biometrical analysis revealed that the mean diameter value ranged from 220.25 to 237.76 μm, for the untreated cysts, from 199 to 224.52 μm for decapsulated cysts and that the chorion thickness ranged from 6.62 to 10.58 μm. 48 h after hatching, Artemia from Sebkha El Meleh, Sebha Moknine, Sfax saltworks and Sahline saltworks presented a hatching percentage of 52.7%, 53.75%, 70.16% and 43.74%, respectively. The length of t
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Essefi, Elhoucine, Hayet Ben Jmaa, Jamel Touir, Mohamed Ali Tagortig, and Chokri Yaicha. "Variability to sedimentary dynamics and climatic conditions during the last two millennia at sebkha Souassi in eastern Tunisia." Papers on Global Change IGBP 20, no. 1 (2013). http://dx.doi.org/10.2478/igbp-2013-0001.

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AbstractThis paper covers work intended to study the interplay of sedimentary dynamics and climatic variability over the last two millennia within Tunisia’s sebkha Souassi. Based on the Visual Core Description, and magnetic susceptibility, we date the core from sebkha Souassi to the last two millennia. Genetic grain-size distribution then provided a basis for the identification of six climatic stages, i.e. the Warming Present (WP), the Late Little Ice Age (Late LIA), the Early Little Ice Age (ELIA), the Medieval Climatic Anomaly (MCA), the Dark Ages (DA), and the Roman Warm Period (RWP). The W
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Chaieb, Ghassen, Chedly Abdelly, and Richard Michalet. "A Regional Assessment of Changes in Plant–Plant Interactions Along Topography Gradients in Tunisian Sebkhas." Ecosystems, October 6, 2020. http://dx.doi.org/10.1007/s10021-020-00567-8.

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"Évolution morphologique quaternaire d'un bassin fermé en milieu continental (Sebkhet Mechiguig, Tunisie centrale)." Zeitschrift für Geomorphologie 53, no. 1 (2009): 81–108. http://dx.doi.org/10.1127/0372-8854/2009/0053-0081.

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Chouari, Walid. "Occupation des sols et morphodynamique récente dans le bassin versant de la sebkha de l’Ariana (Tunisie Nord-orientale)." Confins, no. 24 (July 21, 2015). http://dx.doi.org/10.4000/confins.10269.

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B, Elhoucine Essefia. "Spectral Analysis of a Core from the Sebkha of Sidi Mansour, Southern Tunisia: The Holocene Cyclostratigraphy." Journal of Geophysics & Remote Sensing 04, no. 02 (2015). http://dx.doi.org/10.4172/2169-0049.1000141.

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Essefia B, Elhoucine, Najoua Gharsallia B, and Sabrine Kalabi AB. "Spectral Analysis of a Core from the Sebkha of Sidi Mansour, Southern Tunisia: The Holocene Cyclostratigraphy." Journal of Remote Sensing & GIS 4, no. 2 (2016). http://dx.doi.org/10.4172/2469-4134.1000141.

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Chairi, Raja. "Biomarkers on Sediments in a Highly Saline Aquatic Ecosystem: Case of the Moknine Continental Sebkha (Eastern Tunisia)." Journal of Coastal Zone Management 21, no. 2 (2018). http://dx.doi.org/10.4172/2473-3350.1000463.

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Ben Ameur, Mariem, Sameh Masmoudi, and Chokri Yaich. "Flood and sandstorm events recorded in holocene sebkha deposits in Southeastern Tunisia: Evidence from magnetic and geochemical properties." Quaternary International, September 2020. http://dx.doi.org/10.1016/j.quaint.2020.09.006.

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Essefi, Elhoucine, Narjes Ben Smida, Ibtissem Jandoubi, Mohamed Ali Othmani, and Mohamed Ali Tagorti. "Progressive evaporation of brine of sebkha Mchiguig, central Tunisia: a geo-economical comparative study of salt and brine." Carbonates and Evaporites 35, no. 2 (2020). http://dx.doi.org/10.1007/s13146-020-00592-7.

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