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• W2810161570 abstract "Abstract Late Pleistocene to Holocene evolution of the Northern coast of Sfax (Gulf of Gabes, Tunisia) is deduced on the basis of the analyses of sediment cores and coastal outcrops. The environmental changes are established by means of microfauna and mollusk assemblages and biocenotic parameters complemented by geochemical, sedimentological and correspondence analysis (CA). An opened embayment, rich in warm Senegalese fauna, allowed the deposition of quartz-rich sands Late Pleistocene in age. During the Late Holocene, a major modification of the environmental characters is recognized. The dominance of marine ostracod and coastal foraminifera coupled with high values of species richness characterize a widely opened lagoon. This lagoon is subjected to the action of the alongshore drifts which are responsible for the build-up of sand spits and the genesis of the present sebkhas. Two transgressive events, overlying the marine Late Pleistocene quartz-rich sands, are dated at 2018–2419 and 1001–1804 a cal BP. The dominance of marine and coastal foraminifera, the recurrence of ostracods and the high values of biocenotic parameters testify these two events. Sudden changes, toward 0–502 a cal BP, in the structure of populations, geochemical element concentrations and sedimentological trend argue in favor of a tsunami event and the settlement of peculiar environment. The latter records (1) the reworking of Holocene microfauna and Tyrrhenian sands rich in mollusks eroded from the marine substrata; (2) the high concentration of poorly stratified and poorly sorted shells; (3) fining-upward and thinning landward sequences; (4) the dominance of articulated bivalves and sharpened shells; and (5) the locally extensive deposits up to 160 m inland rising in altitude of about 0.75 m. This extreme event can be correlated with the tsunami generated by the strong earthquake, 1908 AD in age, in Eastern Sicily or by one of the earthquakes recorded during the 18th Century around the Mediterranean basin such as Sfax earthquake of 1750 AD." @default.
• W2810161570 created "2018-07-10" @default.
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• W2810161570 date "2018-11-01" @default.
• W2810161570 modified "2023-10-18" @default.
• W2810161570 title "New insights from microfauna associations characterizing palaeoenvironments, sea level fluctuations and a tsunami event along Sfax Northern coast (Gulf of Gabes, Tunisia) during the Late Pleistocene-Holocene" @default.
• W2810161570 cites W1884987214 @default.
• W2810161570 cites W1964173380 @default.
• W2810161570 cites W1964577047 @default.
• W2810161570 cites W1966801905 @default.
• W2810161570 cites W1968428502 @default.
• W2810161570 cites W1969536777 @default.
• W2810161570 cites W1976783623 @default.
• W2810161570 cites W1977534850 @default.
• W2810161570 cites W1977844210 @default.
• W2810161570 cites W1978118135 @default.
• W2810161570 cites W1978808232 @default.
• W2810161570 cites W1982823243 @default.
• W2810161570 cites W1984526242 @default.
• W2810161570 cites W1988040128 @default.
• W2810161570 cites W1988338845 @default.
• W2810161570 cites W1996270672 @default.
• W2810161570 cites W1997068715 @default.
• W2810161570 cites W2002821853 @default.
• W2810161570 cites W2004295589 @default.
• W2810161570 cites W2005633815 @default.
• W2810161570 cites W2006476283 @default.
• W2810161570 cites W2009348157 @default.
• W2810161570 cites W2012183191 @default.
• W2810161570 cites W2013139856 @default.
• W2810161570 cites W2016225258 @default.
• W2810161570 cites W2019268850 @default.
• W2810161570 cites W2023317688 @default.
• W2810161570 cites W2029969075 @default.
• W2810161570 cites W2030913689 @default.
• W2810161570 cites W2032767344 @default.
• W2810161570 cites W2035460512 @default.
• W2810161570 cites W2042194141 @default.
• W2810161570 cites W2043408732 @default.
• W2810161570 cites W2047417954 @default.
• W2810161570 cites W2047590352 @default.
• W2810161570 cites W2048522333 @default.
• W2810161570 cites W2048895120 @default.
• W2810161570 cites W2052994917 @default.
• W2810161570 cites W2053187508 @default.
• W2810161570 cites W2053229117 @default.
• W2810161570 cites W2053870388 @default.
• W2810161570 cites W2054839152 @default.
• W2810161570 cites W2055544523 @default.
• W2810161570 cites W2063728274 @default.
• W2810161570 cites W2066362794 @default.
• W2810161570 cites W2068558878 @default.
• W2810161570 cites W2072065433 @default.
• W2810161570 cites W2072986148 @default.
• W2810161570 cites W2074537988 @default.
• W2810161570 cites W2074580567 @default.
• W2810161570 cites W2079956254 @default.
• W2810161570 cites W2080464240 @default.
• W2810161570 cites W2082947006 @default.
• W2810161570 cites W2093443145 @default.
• W2810161570 cites W2094794354 @default.
• W2810161570 cites W2098333110 @default.
• W2810161570 cites W2098945937 @default.
• W2810161570 cites W2099458900 @default.
• W2810161570 cites W2103543262 @default.
• W2810161570 cites W2117308691 @default.
• W2810161570 cites W2123647041 @default.
• W2810161570 cites W2136759598 @default.
• W2810161570 cites W2138003993 @default.
• W2810161570 cites W2152211452 @default.
• W2810161570 cites W2158686645 @default.
• W2810161570 cites W2159454800 @default.
• W2810161570 cites W2162888074 @default.
• W2810161570 cites W2184631047 @default.
• W2810161570 cites W2239972880 @default.
• W2810161570 cites W2274493790 @default.
• W2810161570 cites W2280624662 @default.
• W2810161570 cites W2325292866 @default.
• W2810161570 cites W2336183815 @default.
• W2810161570 cites W2472719849 @default.
• W2810161570 cites W2508537769 @default.
• W2810161570 cites W2546004951 @default.
• W2810161570 cites W2562503751 @default.
• W2810161570 cites W2576256935 @default.
• W2810161570 cites W2582227996 @default.
• W2810161570 cites W2589738239 @default.
• W2810161570 cites W2595072387 @default.
• W2810161570 cites W2614135944 @default.
• W2810161570 cites W2991571263 @default.

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