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Article Reference A phylogeny of Cichlidogyrus species (Monogenea, Dactylogyridea) clarifies a host switch between fish families and reveals an adaptive component to attachment organ morphology of this parasite genus
Background: Parasite switches to new host species are of fundamental scientific interest and may be considered an important speciation mechanism. For numerous monogenean fish parasites, infecting different hosts is associated with morphological adaptations, in particular of the attachment organ (haptor). However, haptoral morphology in Cichlidogyrus spp. (Monogenea, Dactylogyridea), parasites of African cichlids, has been mainly linked to phylogenetic rather than to host constraints. Here we determined the position of Cichlidogyrus amieti, a parasite of species of Aphyosemion (Cyprinodontiformes, Nothobranchiidae) in the phylogeny of its congeners in order to infer its origin and assess the morphological changes associated with host-switching events. Methods: The DNA of specimens of C. amieti isolated from Aphyosemion cameronense in Cameroon was sequenced and analyzed together with that of Cichlidogyrus spp. from cichlid hosts. In order to highlight the influence of the lateral transfer of C. amieti on the haptoral sclerotised parts we performed a Principal Component Analysis (PCA) to compare the attachment organ structure of C. amieti to that of congeners infecting cichlids. Results: Cichlidogyrus amieti was found to be nested within a strongly supported clade of species described from Hemichromis spp. (i.e. C. longicirrus and C. dracolemma). This clade is located at a derived position of the tree, suggesting that C. amieti transferred from cichlids to Cyprinodontiformes and not inversely. The morphological similarity between features of their copulatory organs suggested that C. amieti shares a recent ancestor with C. dracolemma. It also indicates that in this case, these organs do not seem subjected to strong divergent selection pressure. On the other hand, there are substantial differences in haptoral morphology between C. amieti and all of its closely related congeners described from Hemichromis spp.. Conclusions: Our study provides new evidence supporting the hypothesis of the adaptive nature of haptor morphology. It demonstrates this adaptive component for the first time within Cichlidogyrus, the attachment organs of which were usually considered to be mainly phylogenetically constrained.
Located in Library / RBINS Staff Publications
Article Reference The Oued Belif hematite-rich breccia (Nefza Mining District, NW Tunisia): a potential candidate for a Miocene small-scale iron oxide copper gold (IOCG) deposit in Northern Tunisia
Located in Library / No RBINS Staff publications
Article Reference SIMS U–Pb dating of uranium mineralization in the Katanga Copperbelt: Constraints for the geodynamic context
Located in Library / No RBINS Staff publications
Article Reference Geodynamic and climate controls in the formation of Mio–Pliocene world-class oxidized cobalt and manganese ores in the Katanga province, DR Congo
Located in Library / No RBINS Staff publications
Article Reference Mn oxides as efficient traps for metal pollutants in a polyphase low-temperature Pliocene environment: A case study in the Tamra iron mine, Nefza mining district, Tunisia
Located in Library / No RBINS Staff publications
Article Reference Geochemical signatures of uraninite: From unconformity to syn-metamorphic uranium deposits in the Panafrican Lufilian Copperbelt
Located in Library / No RBINS Staff publications
Article Reference Malachite, an indicator of major Pliocene Cu remobilization in a karstic environment (Katanga, Democratic Republic of Congo)
Located in Library / No RBINS Staff publications
Article Reference Iron mineralization in a volcanic and sedimentary Mio-Pliocene complex (Tamra mine, Northern Tunisia): the influence of diagenesis and pedogenesis
Located in Library / No RBINS Staff publications
Article Reference Pb-Zn mineralizations in a Miocene regional extensional context: the case of the Sidi Driss and the Douahria ore deposits (Nefza mining district, N. Tunisia)
Located in Library / No RBINS Staff publications
Article Reference Poly-phased alteration history in the “Cava di Caolino” kaolinite profile (Lipari Island, Southern Italy)
Located in Library / No RBINS Staff publications