Origines du peuplement mammalien en Afrique du Nord durant le miocène terminal

The late Miocene North African mammalianassemblage is considered here from three viewpoints: survivals, extinctions, and immigrations. The Eurasiatic affinities of the large mammals slightly prevail over the Ethiopian affinities. Amongst the North African large mammals, 4 to 8 taxa are Eurasiatic immigrants, while 4 to 6 are of Subsaharian origin. Contrarily, the micromammalian fauna is highly endemic, with only one species, a murid (Paraethomys miocaenicus), considered here as being related to an Asiatic form (Karnimata darwini). Our study of Eurasian and African Miocene faunas reveals that during the late Astaracian-early Turolian interval, the Saharo-Arabic belt permitted very little latitudinal faunal exchanges. However, during the middle and late Turolian such faunal exchanges became frequent. The micromammal record unequivocally indicates that a brief period of faunal exchange occurred between Africa and western Europe at the end of the Miocene, corresponding with the Messinian Salinity Crisis. The increased intercontinental faunal exchange between Africa and Eurasia during the late Miocene coincides with, and counterbalances the extinction of more than 10 taxa at the Mio/Pliocene boundary.     

Revision du genre LycopodiopsisB. Renault, 1890

The study of imprints of Lycopsida from Permianof the Gondwana has permitted to specify the organisation of the leaf cushions and their variation in the genus LycopodiopsisB. Renault. The presence of a ligula is showed off. The invalidity of the genera Cyclodendron and Lycopodiophloios is demonstrated, and the species refered to these genera must be refered to the genus Lycopodiopsis for which an emended diagnosis is proposed.     

Le Middle Stone Age de la grotte du Porc-Épic (Dire Dawa, Éthiopie) : gestion des matières premières et comportements techniques

With the emergence of Modern Humans in Africa a new post-Acheulean culture seems to take form: the Middle Stone Age. Although the geo-chronological limits of this period remain unclear, it may however be characterised by behavioural modifications, in particular an important change in the relationship between humans and their environment. Theses changes may partially result from the diversification of stone-tool production techniques, as well as socio-economical conditions. Sites dating of this period show that flake types are more abundant and result from exploitation methods that become gradually more sophisticated from about 300ka.In this context, study of the lithic assemblage from Porc-Epic Cave in Ethiopia contributes to the knowledge about operative methods used during the Middle Stone Age. The combined production of flakes, blades, bladelets and points using various methods, a differential economy towards raw materials and the diversity of tool types produced, underline the large extent of technological variability that the Porc-Epic tool-makers were capable of. We may conclude that, in spite of certain differences concerning raw material acquisition, a chronological homogeneity exists in the production modes and their variability. This apparent homogeneity throughout the stratigraphical sequence underlines the difficulty of attributing a cultural characteristic to stone assemblages of this period.     

Étude craniométrique du complexe d’espèces Meriones shawii–grandis (Mammalia : Rodentia) au Maroc,en Algérie et en Tunisie

In North Africa, the rodents of the species complex Meriones shawii–grandis have a considerable ecological, economic and epidemiological importance. Until now, the systematics of these species was subject to discussion due to the presence of populations displaying high morphological variability. By means of an approach of traditional morphometrics based on cranial distances and by using the method of the log shape-ratio, we attempt to characterize morphologically these two taxa. The results show significant differences in size and shape between the specimens of Morocco, on the one hand, and those of Algeria and Tunisia, on the other hand. The samples of Morocco that have been molecularly typed and attributed to M. grandis have larger tooth rows and narrower skulls, as well as relatively small tympanic bullae. On the other hand, those of Algeria and Tunisia assigned to M. shawii are characterized by small tooth rows and wide skulls with well-developed tympanic bullae. The morphological distance is relatively strong between both clades (79.5%), which corresponds to the molecular distance. However, the discriminant analysis performed after molecularly-typed specimens allows the correct classification of only 91.8% of the individuals.     

Les premières étapes de la colonisation de l’Europe et l’arrivée de l’Homme sur les rives de la Méditerranée

Over recent years, many discoveries have renewed our knowledge about the oldest stone industries and also about the behaviour and lifestyle of the hominids that made them, not only in East Africa, but also in the Near East, in Trans Caucasia and in southern Europe. If the first tools making hominids appear in East Africa as early as 2.55 million years ago, they are present in the Levant a little over 2 million years ago, as early as 1.81 million years ago at the gates of Europe in Trans-Caucasia, and a little over 1.4 million years ago on the Mediterranean coasts of Europe.     

Diatoms of Dindifelou fall (upper Basin of the Gambia River,Senegal): floristic inventory

The Dindifelou fall, located in south‐eastern Senegal, receives its water from discharging springs located in Dande plate‐land. These waters form, at the foot of the cliff, a pond that drains into the Thiokoye, a tributary of the Gambia River. The water quality of the pond and the stream is very good based on physicochemical analyses. Around the pond region, a microclimate characterized by a higher humidity and a lower temperature compared with the surrounding area is present. Diatoms study is carried out in different habitat types associated with this fall. The samples were taken by scraping the surface of rocks and rinsing fern leaves with sparkling water. Dande plate‐land is made of Upper Proterozoic sandstones whose gravity accumulations litter the bottom of the pond and the stream. This study allowed us to inventory 61 species and varieties of diatoms belonging to 28 genera. The most represented genera are Achnanthidium (ten species), Eunotia and Pinnularia (eight species each). Twelve species and varieties are reported for the first time in Senegambia including five of the genera Achnanthidium. The microflora is dominated by Achnantidium minutissimum and Achnanthidium catenatum, followed by Ulnaria ulna and various species of the genera Eunotia and Brachysira. Aerial habitats are more diversified here than the epilithic samples.     

Présence de Pleurothyrella knodi (Brachiopoda,Terebratulida dévoniens) en Guinée-bissau. Implications paléogéographiques

Pleurothyrella knodi, known only from Bolivia and Argentina, is recorded from Guinea-Bissau (West Africa). It represents a new and sure point of the faunistic Malvinokaffric Realm extension during the Early Devonian.     

Elephas reckiDietrich,, 1915 (Proboscidea,Elephantidae)). Évolution au cours du Plio-pléistocène en Afrique orientale

A revision of the presently available materialrefered to the species Elephas reckiDietrich.. 1915, collected in East african plio-pleistocene levels, leads up to distinguish a succession of five subspecies within the species: E. r. brumpti n. subsp.; E. r. shungurensis n. subsp.; E. r. atavusArambourg 1947; E. r. ileretensis n. subsp. and E. r. reckiDietrich,, 1915.The five subspecies diagnosis are proposed here. They together represent a monophyletic lineage, the study of which allows to propose new interpretations regarding the history and evolutionary trends of the genus in Africa.     

Dental remains of Lower Miocene small rodents from Napak (Uganda): Afrocricetodontidae,Myophiomyidae, Kenyamyidae and Sciuridae

The Early Miocene sites of Napak (Uganda), which have been prospected by the Uganda Palaeontology Expedition since 1985, have yielded abundant fossil remains, including a rich and diverse rodent fauna. Ever since the work of Lavocat (1973) on the East African Miocene rodents, which focused mainly on the Kenyan remains (but included some material from Napak discovered by Bishop during the 1950s and 1960s), few studies have been made on the Ugandan specimens. This lack provides motivation for further study of Napak micro-mammals, especially the abundant rodents, which were collected at five sites, Napak IV, V, XV, XXX and XXXI. The fossils described here are attributed to six species representing four families: Afrocricetodontidae (Afrocricetodon songhori, Protarsomys macinnesi), Myophiomyidae (Myophiomys arambourgi), Kenyamyidae (Simonimys genovefae, Kenyamys mariae) and Sciuridae (Vulcanisciurus africanus). Comparison of the dentition of extant and extinct taxa allows us to propose dietary hypotheses (granivory, herbivory and omnivory) for these rodents. In addition, the fossil rodents associated with other fauna from the same localities suggest a more-or-less dense forest environment with clearings, and the probable presence of a humid climate at the time of deposition.     

Civettictis braini nov. sp. (Mammalia: Carnivora), a new viverrid from the hominin-bearing site of Kromdraai (Gauteng,South Africa)

A new Plio-Pleistocene viverrid species is described based on two newly discovered maxillae (KW 10141 and KW 10383) from the recent excavations at the hominin-bearing site of Kromdraai (Gauteng, South Africa). This major site allows us to address the conundrum of Paranthropus and Homo origins in South Africa and presents a highly diverse carnivore spectrum (at least 22 species) including herpestids and viverrids. Civettictis braini nov. sp. is a viverrid species comparable in size to the extant African civet Civettictis civetta (Schreber, 1776). However C. braini nov. sp. differs significantly from the extant species in its dental proportions. Its canine and three premolars (P1–P3) are relatively robust, while its carnassials (P4) and two molars (M1, M2) are extremely reduced. This new species supplements our knowledge on carnivore taxonomic diversity and paleoecology in Southern Africa about 2 millions of years ago.