Carbon Isotope Analysis of Ouled Abdoun Basin, Morocco Has Implications for Africa's Earliest Placentals

First carbon isotope chemostratigraphy of the Ouled Abdoun phosphate Basin, Morocco; implications for dating and evolution of earliest African placental mammals

Authors:

1. Johan Yans (a)
2. M’Barek Amaghzaz (b)
3. Baadi Bouya (b)
4. Henri Cappetta (c)
5. Paola Iacumin (d)
6. László Kocsis (e)
7. Mustapha Mouflih (f)
8. Omar Selloum (b)
9. Sevket Sen (g)
10. Jean-Yves Storme (a)
11. Emmanuel Gheerbrant (g)

Affiliations:

a. University of Namur, Department of Geology, NaGRIDD, 61 rue de Bruxelles, 5000 Namur, Belgium

b. Groupe Office Chérifien des Phosphates (OCP), Centre Minier de Khouribga, Service Géologique, Khouribga, Morocco

c. Université Montpellier II, UMR 5554, France

d. Parma University, Earth Sciences, Parco Area delle Scienze, 157, 43100 Parma, Italy

e. University of Lausanne, Faculty of Geoscience and Environment, Institute of Earth Sciences, UNIL - Geopolis, CH-1015 Lausanne, Switzerland

f. University Hassan II-Mohammedia, Faculty of Sciences Ben M'sik, Casablanca, Morocco

g. UMR-CNRS 7207, CR2P Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements, Muséum National d'Histoire Naturelle, Département Histoire de la Terre, CP38, 8 rue Buffon, 75005 Paris, France

Abstracts:

The well-known Maastrichtian-Ypresian vertebrate-bearing phosphate series, in the Ouled Abdoun Basin, Morocco, is classically dated using regional selachian biostratigraphic zonation. These marine sediments yielded Paleocene and Eocene mammals comprising the earliest known placentals from Africa. This study provides the first insight into the organic carbon isotope chemostratigraphy (δ¹³C_org) of the Moroccan phosphate series and a refined dating of its vertebrate-bearing levels. Four Paleocene-Eocene sections in the NE Ouled Abdoun quarries show consistent δ¹³C_org long term evolutions, from the base to the top: 1) positive trend in phosphorite Bed IIa, beginning with the lower Bone Bed yielding mammals such as Eritherium, Ocepeia, Abdounodus, Lahimia, of early Thanetian and Selandian age; 2) transitional negative trend in the Intercalary phosphorite Beds II/I that includes the Otodus obliquus and Phosphatherium escuilliei Bone Bed of earliest Ypresian age; 3) negative trend to the lowermost δ¹³C_org values that are correlative to the early-middle Ypresian interval including ETM 2 and ETM 3 hyperthermal events in the global record; 4) positive trend in chert-enriched facies containing the middle Ypresian EECO global climatic event. Our chemostratigraphic study of the Ouled Abdoun phosphate series provides a new chronostratigraphic framework for calibrating the beginning of the evolution of placental mammals in Africa. The lower Bone Bed level from the Paleocene phosphorite Bed IIa yielding Eritherium is not younger than early Thanetian, and is most likely Selandian. The Phosphatherium Bone Bed in the Intercalary Beds II/I is earliest Ypresian. The phosphorite Bed 0, from which Daouitherium probably came, is early-middle Ypresian, just below the EECO. This suggests that the first large proboscideans evolved after the PETM, during mid-Ypresian warming events. The δ¹³C_org study does not support the presence of Lutetian in the NE Ouled Abdoun phosphate series and suggests that a noticeable part of the upper Thanetian is absent.