Procatopodidae

Bragança, Pedro H. N. & Costa, Wilson J. E. M., 2019, Multigene fossil-calibrated analysis of the African lampeyes (Cyprinodontoidei: Procatopodidae) reveals an early Oligocene origin and Neogene diversification driven by palaeogeographic and palaeoclimatic events, Organisms Diversity & Evolution (New York, N. Y.) 19 (2), pp. 303-320 : 312

publication ID

https://doi.org/ 10.1007/s13127-019-00396-1

persistent identifier

https://treatment.plazi.org/id/03D187A0-FF9E-FFE9-08D4-FA41FC506AAB

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Felipe

scientific name

Procatopodidae
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Procatopodidae diversification

Procatopodidae basal lineages and the early and middle Miocene moist-wet climate

Plataplochilus lineage originated in the early Oligocene, but subsequent species diversification started only in the Pliocene (3.2 Mya, 95% HDP 1.7–5.6 Mya), whereas Aplocheilichthys spilauchen , a salt-brackish water tolerant species, distributed over Africa west coast ( Fig. 4 View Fig ), diverged in the early Miocene (23.1 Mya, 95% HDP 19.1–27.2 Mya). Despite all, Plataplochilus species are strictly freshwater; it is not possible to conclude if during the Procatopodidae evolution, two independent freshwater invasions occurred, one with Plataplochilus and the other with the remaining African lampeyes except A. spilauchen , or if the latter species represents a reversal to the salt-brackish water tolerant plesiomorphic condition.

Genera representing lineages that diversified during a moist-wet stable climate phase between the early and middle Miocene are today restricted to rainforests ( Procatopus , B Hypsopanchax ,^ Hypsopanchax , and Hylopanchax ) or swampy humid areas ( Congopanchax and Lacustricola ), and all genera except Lacustricola , Lamprichthys , and one species of Hypsopanchax occur only in the Lower Guinean and Congo river ichthyological provinces ( Figs. 1 View Fig and 4 View Fig ) (Wildekamp et al. 1986). During this warm time, rainforests were broadly distributed in Africa, forming a continuous area, extending to the present East African coast and to the Sahara, in the north ( Lovett 1993; Maley 1996; Plana 2004; Stanley et al. 2005).

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