Earliest occurrence of Hydrocynus (Characiformes, Alestidae) from Eocene continental deposits of Méridja Hamada, northwestern Sahara, Algeria

Author:

Hammouda Sid-Ahmed1,Murray Alison M.2,Divay Julien D.3,Mebrouk Fateh4,Adaci Mohammed1,Bensalah Mustapha1

Affiliation:

1. Research Laboratory No. 25, PWSMR-ELTC, Department of Earth Sciences and the Universe, University of Tlemcen, Tlemcen 13000, Algeria.

2. Department of Biological Sciences, University of Alberta, Edmonton, AB T6G 2E9, Canada.

3. Royal Tyrrell Museum of Palaeontology, P.O. Box 7500, Drumheller, AB T0J 0Y0, Canada.

4. Department of Earth Sciences and the Universe, Faculty of Life and Natural Sciences, University of Jijel, Jijel 18000, Algeria.

Abstract

We here report the oldest remains (teeth) of the African tigerfish (Hydrocynus) from the Oued Méridja and Garet Dermchane sections, Hamada of Méridja deposits, in southwestern Algeria. The tigerfish, a large carnivorous fish today represented by several species in the freshwaters of Africa, was previously found in upper middle to upper Eocene deposits in Egypt and Libya. The remains described here are several million years older, being early to middle Eocene in age, and are associated with other fish elements including lungfish, polypterid, amiiform, possible cichlid, and Alestes and Brycinus material, along with several fish elements that cannot be associated with a specific taxon and some fragmentary amphibian bones. This represents the first detailed description of a freshwater fish assemblage from the Eocene of Algeria, although a short list of fish taxa from Eocene Algerian deposits was previously reported. Furthermore, these new Algerian fossils allow us to assess the hypothesized existence of an east–west or west–east hydrological connection between eastern and western parts of northern Africa. We suggest that the shared presence of tigerfish in the Eocene deposits of Algeria, Libya, and Egypt does not necessarily indicate a permanent (i.e., nonseasonal) connection east–west or west–east among these areas. Rather, the observed faunal similarities could have been the result of seasonal flooding that caused the dispersal of Hydrocynus and associated taxa across coastal flood plains.

Publisher

Canadian Science Publishing

Subject

General Earth and Planetary Sciences

Reference52 articles.

1. Adaci, M. 2012. Le Paléogène continental du Sud-Ouest Algérien (Lithostratigraphie, paléontologie et sédimentologie), Vol. 1. Ph.D. thesis, Department of Earth Sciences and the Universe, Tlemcen University, Tlemcen, Algeria.

2. Nouveaux sites à vertébrés paléogènes dans la région des Gour Lazib (Sahara nord-occidental, Algérie)

3. Anonymous. 1952. Carte géologique au 1:2 000 000 du Nord-Ouest de l’Afrique (feuille “Maroc-Algérie Ouest”). Comité d’organisation du XIXe Congrès Géologique International, Alger.

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