The mammal localities of Grand Daoui Quarries, Ouled Abdoun Basin, Morocco, Ypresian:: a first survey

被引:58
作者
Gheerbrant, E
Sudre, J
Cappetta, H
Mourer-Chauviré, C
Bourdon, E
Iarochene, M
Amaghzaz, M
Bouya, B
机构
[1] Museum Natl Hist Nat, Lab Paleontol, UMR 8569, CNRS, F-75005 Paris, France
[2] Univ Montpellier 2, Lab Paleontol, ISEM, UMR 5554 CNRS, F-34095 Montpellier 05, France
[3] Univ Lyon 1, UMR 5125, F-69622 Villeurbanne, France
[4] Rabat Inst, Direct Geol, Minist Energie & Mines, Rabat, Morocco
[5] Ctr Minier Khouribga, Serv Geolog & Direct Dev, Grp Off Cherifien Phosphates, Khouribga, Morocco
来源
BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE | 2003年 / 174卷 / 03期
关键词
Africa; Ouled Abdoun Basin; phosphates; mammals; birds; Selachians; early Eocene;
D O I
10.2113/174.3.279
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The unexpected discovery of mammals such as the earliest known proboscidean Phosphatherium escuilliei in the Ouled Abdoun phosphate Basin (Morocco), which is otherwise renowned for its very rich marine vertebrate fauna, has opened major new perspectives on the early African placental fauna. It was the impetus for several field parties by us between 1997 and 2001 which has allowed this survey of the geological, stratigraphic and paleontological context of Phosphatherium localities. This is the first important paleontological field work dealing with higher vertebrates in the Ouled Abdoun Basin since the work of C. Arambourg. Most of the material of Phosphatherium and other Ouled Abdoun mammals was found by local people searching for fossils for dealing, in an area where the economy is widely dominated by the mining development, in addition to more traditional but very poor agricultural resources. All Phosphatherium remains were found in the northeasternmost quarries of the Ouled Abdoun Basin, from a restricted quarrying area called Grand Daoui (fig. 3). In all Grand Daoui recognized localities (8), the mammals come from the lowermost Eocene level. The stratigraphically re-situated mammalian material was found in a bone-bed of the level called "Intercalaire Couches II/I" which is dated as early(iest) Ypresian on the basis of its relative stratigraphic position and its selachian fauna. At present, the occurrence of several mammal horizons in the "Intercalaire Couches II/I" (and Couche I ?) cannot be excluded, but their age difference seems not significant according to both the associated selachi.an taxa and the mammalian material, in present data. The bone-bed is very rich in macro-vertebrates. It includes especially large teeth of the shark Otodus obliquus which are the subject of very active research for dealing, and which explains the recent discovery of mammals such as Phosphatherium.
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页码:279 / 293
页数:15
相关论文
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