2014
DOI: 10.1016/j.geobios.2014.06.006
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Organic-walled dinoflagellate cysts from the Upper Cretaceous–lower Paleocene succession in the western External Rif, Morocco: New species and new biostratigraphic results

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Cited by 29 publications
(10 citation statements)
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“…Among the spe cies iden ti fied in this for ma tion, an im por tant marker taxon is Pterodinum cretaceum, which has been named dif fer ently (see Slimani et al, 2010: pp. 104), having the LAD in the lat est Maastrichtian (Schirler and Wil son, 1993;Roncaglia and Corradini, 1997a, b;Slimani, 2001;Torricelli and Amore, 2003;Slimani et al, 2008Slimani et al, , 2010Slimani et al, , 2011Slimani et al, , 2016Slimani and Toufiq, 2013;M'Hamdi et al, 2013;Guédé et al, 2014). This spe cies is re corded in a sin gle sam ple (P140).…”
Section: Dinoflagellate Cyst Biostratigraphymentioning
confidence: 92%
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“…Among the spe cies iden ti fied in this for ma tion, an im por tant marker taxon is Pterodinum cretaceum, which has been named dif fer ently (see Slimani et al, 2010: pp. 104), having the LAD in the lat est Maastrichtian (Schirler and Wil son, 1993;Roncaglia and Corradini, 1997a, b;Slimani, 2001;Torricelli and Amore, 2003;Slimani et al, 2008Slimani et al, , 2010Slimani et al, , 2011Slimani et al, , 2016Slimani and Toufiq, 2013;M'Hamdi et al, 2013;Guédé et al, 2014). This spe cies is re corded in a sin gle sam ple (P140).…”
Section: Dinoflagellate Cyst Biostratigraphymentioning
confidence: 92%
“…Manumiella seelandica, Deflandrea galeata and Muratodinium fimbriatum have been iden ti fied in the top of the Lepºa For ma tion (P141 sam ple). These spe cies have their FAD's in the Up per Maastrichtian, but may per sist up to the Danian in Mo rocco (Slimani et al, 2010, Guédé et al, 2014, Tu ni sia (M'Hamdi et al, 2013), the Czech Carpathians (Gedl, 2004) and else where. An other spe cies, such as Rottnestia wetzelii subsp.…”
Section: Dinoflagellate Cyst Biostratigraphymentioning
confidence: 99%
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“…En revanche, les études fondées sur la palynologie sont rares et demeurent encore insuffisantes. En effet, les études palynologiques des gisements phosphatés des Plateaux de Phosphates (Prévôt et al, 1979 ;Rauscher et Doubinger, 1982 ;Rauscher, 1985 ;Soncini et Rauscher, 1988 ;Soncini, 1990) et des dépôts du Rif Externe (Slimani et al, 2008(Slimani et al, , 2010(Slimani et al, , 2012Slimani et Toufiq, 2013 ;Guédé et al, 2014 ;Slimani et al, 2016), fondées sur les kystes de dinoflagellés, sont parmi des rares études palynologiques qui ont été réalisées sur le Paléocène et l'Eocène du Maroc. La présente étude est menée dans le Rif Externe occidental où les affleurements de l'Eocène sont, en général, rares et discontinus.…”
Section: Introductionunclassified