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2013 | 20 |

Tytuł artykułu

Variability to sedimentary dynamics and climatic conditions during the last two millennia at sebkha Souassi in eastern Tunisia

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Języki publikacji

EN

Abstrakty

EN
This 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 WP stretches across the uppermost 3 cm, with a high grey scale indicating a dry climate. The Late LIA is located between 3 and 7 cm, and the ELIA between 7 and 28 cm. Intermediate values for GS indicate that this stage may be classified as moderate. The MCA spanning from 28 to 40 cm is marked by a sharp decrease in GS indicative of a wet period. The DA appear along the part between 40 and 79 cm, a shift from light to dark sediments being recorded. The RWP in turn appears between 79 and 114 cm. Based on the grain-size distribution, two low-frequency cycles were identified, indicating radical global changes in climatic conditions, differential tectonics and groundwater fluctuations. High-frequency cycles in turn attest to local modifications of climatic conditions.

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-

Rocznik

Numer

20

Opis fizyczny

p.29-45,fig.,ref.

Twórcy

autor
  • National Engineering School of Sfax, Road of Soukra, km 4 Zip code 3038, University of Sfax, Road of the Airport km 0.5, Zip code: 3029, Tunisia
  • RE: Sedimentary Dynamics and Environment (DSE) (Code 03/UR/10-03), National Engineering School of Sfax, University of Sfax, Tunisia
autor
  • Faculty of Arts and Humanities of Sfax, Road of the Airport 5, Zip code 3023, University of Sfax, Tunisia
  • Laboratory of Geomorphologic Cartography of Fields, Environments, and Dynamics, Tunisia
autor
  • Laboratory of Water Energy and Environment, National Engineering School of Sfax, University of Sfax, Tunisia
  • Faculty of Sciences of Sfax, Road of Soukra km 4, Zip code 3038 Sfax, University of Sfax, Tunisia
  • Higher Institute of Biotechnology of Monastir, Tahar Haded A venue, Zip code 5000, Monastir; University of Monastir. Road Sallem Bechir ‒ B.P. n° 56 ‒ 5000 Monastir, Tunisia
autor
  • National Engineering School of Sfax, Road of Soukra, km 4 Zip code 3038, University of Sfax, Road of the Airport km 0.5, Zip code: 3029, Tunisia
  • RU: Sedimentary Dynamics and Environment (DSE) (Code 03/UR/10-03), National Engineering School of Sfax, University of Sfax, Tunisia

Bibliografia

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  • Ben Jmaa H., 2008, The endorheic system of Sidi El Hani, Chrita and Mechertate: Paleoenvironment and recent dynamics, PhD Thesis, University of Tunis.
  • Bridge J.S., 1981, Hydraulic interpretation of grain-size distributions using a physical model for bedload transport, Journal of Sedimentary Petrology, 51, 1109−1124.
  • Essefi E., 2009, Multidisciplinary study of Sidi El Hani Saline Environment: the History and the Climatic Variability, Master thesis, Faculty of sciences of Sfax, University of Sfax.
  • Essefi E., 2013, Wet Aeolian Sedimentology and Sequence Stratigraphy in Eastern Tunisia: Implications for Wet Aeolian Sedimentology and Sequence Stratigraphy on Mars, Ph.D,thesis, National Engineering School of Sfax.
  • Essefi E., Fairén A. G., Komatsu G., Rekhiss F., Yaich C., 2012a, Study of cores from a spring mound at the mars analog of Boujmal, eastern Tunisia: coring martian spring moundsas potential efficient tool for a geologic exploration of early Mars, Third Conference onEarly Mars, 7029 (abstracts).
  • Essefi E., Komatsu G., Fairén A.G., Rekhiss F., Yaich C., 2012b, Identification of tephra layers in spring mounds at the terrestrial analog of Boujmal, eastern Tunisia: repercussions and limits of tephrostratigraphy application on martian stratigraphy and paleoclimatology,Third Conference on Early Mars, 7034 (abstracts).
  • Essefi E., Komatsu G., Fairén A.G., Chan M. A., Yaich, C., 2013, Groundwater influence on the aeolian sequence stratigraphy of the Mechertate-Chrita-Sidi El Hani system, TunisianSahel: Analogies to the wet-dry aeolian sequence stratigraphy at Meridiani Planum, Terbycrater, and Gale crater, Mars, Accepted manuscript, Planetary and Space Science, DOI:10.1016/j.pss.2013.05.010.
  • Essefi E., Touir J., Tagorti M.A., Bouri S., Essefi H., Ouali J., Ben Jmaa H., 2009, Modeling of the chaotic behavior of Sidi El Hani discharge playa, Tunisian Sahel: which exogenousfactor commands this saline environment? The subsurface flow or the climatic variability?International Congress Geotunis, 4th edition.
  • Essefi E., Touir J., Tagorti M.A., Yaich C., 2012c, Effect of the groundwater contribution, the climatic change, and the human induced activities on the hydrological behavior ofdischarge playas: a case study Sidi El Hani discharge playa, Tunisian Sahel, ArabianJournal of Geoscience, DOI: 10.1007/s12517-012-0659-6.
  • Essefi E., Touir J., Tagorti M.A., Yaich C., 2013, Magnetic Study of the Sedimentary Filling of Sebkha Boujmal, (eastern Tunisia): the Sedimentary Dynamics and the Climatic Variability,International Conference on Natural Hazard and Geomatics (ICNHC ), 17−20 May,Hammamet, Tunisia.
  • Flemming B.W., 2000, A revised textural classification of gravel-free muddy sediments on the basis of ternary diagrams, Continental Shelf Research, 20, 1125−1137.
  • Manté C., Yao A.F., Degiovanni C., 2007, Principal component analysis of measures, with special emphasis on grain-size curves, Computational Statistics & Data Analysis, 51,4969−4983.
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  • Mefteh S., Essefi E., Medhioub M., Yaich C., Jamoussi F., 2012, Correlation between clay minerals, organic matter, and magnetic susceptibility along NWA-1 well (southern Tunisia): paleo-environmental indications, 4th Magrebian Symposium on Clays, 21−23 March, Hammamet, Tunisia, Abstract book, pp. 78.
  • Pye K., 1987, Aeolian dust and dust deposits, Academic Press, London, 29−62.
  • Rodbell D.T., Seltzer G.O., Anderson D.M., Abbott M.B., Enfield D.B., Newman J.H., 1999, An 15,000-year record of El Niño-driven alluviation in southwestern Ecuador, Science283, 516−520.
  • Sun D., Bloemendal J., Rea D.K., Vandenberghe J., Jiang F., An Z., Su R., 2002, Grainsize distribution function of polymodal sediments in hydraulic and aeolian environments,and numerical partitioning of the sedimentary components, Sedimentary Geology, 152,263−277.
  • Tagorti M. A., Essefi E., Touir J., Guellala R., Yaich C., 2013, Geochemical controls of groundwaters upwelling in saline environments: Case study the discharge playa of Sidi El Hani (Sahel, Tunisia), Accepted manuscript, African Earth Science Journal. Tricart J., Cailleux A., 1962, Le modèle glaciaire et nival, SEDES, Paris.
  • Tricart J., Cailleux A., 1967, Le modelé des régions périglaciaires, SEDES, Paris.
  • Tsoar H., Pye K., 1987, Dust transport and the question of desert loess formation, Sedimentology, 3 4, 139−153, doi:10.1111/j.1365-3091.1987.tb00566.x.
  • Wiles, G.C., Barclay, D.J., Calkin, P.E., Lowell, T.V., 2008, Century to millennial-scale temperature variations for the last two thousand years indicated from glacial geologic records of Southern Alaska, Global and Planetary Change, 60, 115−125.

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Bibliografia

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