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The western edge of the Mediterranean Pelagian Platform: A Messinian mixed siliciclastic–carbonate ramp in northern Tunisia
- Source :
- Palaeogeography, Palaeoclimatology, Palaeoecology, Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 285 (1-2), pp.85-103. ⟨10.1016/j.palaeo.2009.10.028⟩, Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2010, 285 (1-2), pp.85-103. ⟨10.1016/j.palaeo.2009.10.028⟩
- Publication Year :
- 2010
- Publisher :
- Elsevier BV, 2010.
-
Abstract
- International audience; The marine Messinian deposits of Tunisia cover a narrow littoral strip some 300 km long between the northern Bizerte and Cap Bon areas and the central-eastern Sahel region. Litho- and biofacies analysis of six stratigraphic sections reveals the distinctive features of these deposits.;The lower Messinian deposits are characterized by ubiquitous siliciclastics and abundant oolitic/bioclastic limestones organized in an eastward facing ramp. Westward (landward), this ramp changes into coastal lagoons, sometimes containing evaporites. Eastward, the ramp passes to the reefal Pelagian Platform extending as far as Lampedusa.;Two main sedimentary cycles are distinguished: 1) an early Messinian siliciclastic retrogradational then oolitic/bioclastic progradational cycle (Beni Khiar Formation and lower Oued bel Khedim Formation): 2) a late Messinian brackish to continental cycle that probably accumulated in rapidly subsiding lagoons (Cued el Bir Formation and upper Oued bel Khedim Formation). The Tunisian early Messinian cycle is partly eustatically controlled, but the late Messinian cycle cannot be confidently correlated to other well-known Messinian series because of tectonic movements.;The lower Messinian deposits of Tunisia are also characterized by abundant suspension-feeding organisms (molluscs and bryozoans) and rare corals, calcareous algae, echinoids, and larger benthic foraminifers. The proposed palaeoenvironmental model shows that the lower Messinian ramp of Tunisia was located on a current-protected margin and subjected to continent-derived sediment and nutrient supply. Eastward, nutrient influx diminished and a shallow-water isolated carbonate platform with coralgal facies developed between the western and the eastern Mediterranean basins. The main hydrological connection between these two basins occurred through a narrow seaway situated to the northeast of the Pelagian Platform, south of Sicily and Malta.
- Subjects :
- 010506 paleontology
Tunisia
Evaporite
Carbonate platform
[SDE.MCG]Environmental Sciences/Global Changes
Pelagian Platform
Mediterranean
010502 geochemistry & geophysics
Oceanography
01 natural sciences
Paleontology
chemistry.chemical_compound
14. Life underwater
Northern Africa
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment
Ecology, Evolution, Behavior and Systematics
0105 earth and related environmental sciences
Earth-Surface Processes
Ramp system
Miocene
Tectonics
chemistry
Benthic zone
Facies
Carbonate
Siliciclastic
Sedimentary rock
Geology
Subjects
Details
- ISSN :
- 00310182
- Volume :
- 285
- Database :
- OpenAIRE
- Journal :
- Palaeogeography, Palaeoclimatology, Palaeoecology
- Accession number :
- edsair.doi.dedup.....d60a8499e8c0887a2571421379935679