The Continental intercalaire, sometimes referred to as the Continental intercalaire Formation, is a term applied to Cretaceous strata in NorthernAfrica. It is the largest single stratum found in Africa to date, being between 30 and 800 metres (98 and 2,625 ft) thick in some places. Fossils, including dinosaurs, have been recovered from this formation.[1] The Continental intercalaire stretches from Algeria, Tunisia and Niger in the west to Egypt and Sudan in the east.[2][3]
History
The Continental intercalaire was first identified during the course of several expeditions to the Sahara from 1946 to 1959 which were led by the French paleontologist Albert-Félix de Lapparent.[4]
Description
The Continental intercalaire is most often likened to the Kem Kem Group.[5]
^Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Africa)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 571-573. ISBN0-520-24209-2.
^Paul E. Anderson, Michael J. Benton,⁎ Clive N. Trueman, Bruce A. Paterson, Gilles Cuny (2007). "Palaeoenvironments of vertebrates on the southern shore of Tethys: The nonmarine Early Cretaceous of Tunisia". Palaeogeography, Palaeoclimatology, Palaeoecology. 243 (1–2). Elsevier: 118–131. Bibcode:2007PPP...243..118A. doi:10.1016/j.palaeo.2006.07.015.{{cite journal}}: CS1 maint: multiple names: authors list (link)[dead link]
^Federico Fanti, Michela Contessi, Fulvio Franchi (2012). "The Continental Intercalaire of southern Tunisia: Stratigraphy, paleontology, and paleoecology". Journal of African Earth Sciences. 73 (73–74). Elsevier: 1–23. Bibcode:2012JAfES..73....1F. doi:10.1016/j.jafrearsci.2012.07.006.{{cite journal}}: CS1 maint: multiple names: authors list (link)[dead link]
^ abDe Broin, France; Taquet, Philippe (1966). "Découverte d'un Crocodilien nouveau dans le Crétacé inférieur du Sahara". C. R. Acad. Sci. Paris (in French). 262 (D).
^ abcdefghijklmno"Continental intercalaire." Weishampel, et al. (2004). Pg. 571-572.