Figure 5: Hypothesis of the Biogeography of the Genus Moricandia Coupled to the Geological Events at the End of the Miocene (A: Middle Tortonian; B: Early Messinian) and Early Pliocene (C: Late Zanclean) in the Betic-Rifean Arch, the Strait of Gibraltar at Current Times.
doi 10.7717/peerj.3964/fig-5