Examining hypotheses regarding Mediterranean geology
According to the expert Leticia Bidegaray-Batista, paperʼs first author, «so far it was assumed that the tectonic collision of the African and Eurasian plates originated the diversification of the fauna endemic to the Western Mediterranean. Nonetheless, no scientific study had confirmed that possibility. With this research, we prove for the first time that the distribution of the genus Parachtes is linked to the tectonic events that occurred in the Mediterranean more than 25 million years ago».
Spiders provide an interesting model for the study of biological and evolutionary processes, which allows for examining hypotheses not yet contrasted, within a temporal context well supported by geological studies. Utilizing molecular techniques to elucidate phylogenetic relationships (three nuclear and five mitochondrial genes), and with biogeographic and fossil points of external calibration, the experts have confirmed that the origin of the spiders diversification matches the geological changes undergone by the Mediterranean basin, an area particularly active during the Oligocene.
Following the shifting of the tectonic plates
«Most likely, the ancestor of the genus Parachtes —explains Miquel A. Arnedo— arrived to the Iberian Peninsula from the Middle East via Europe. From this point, the diversification of the different lineages in the Mediterranean can be followed through the movement of the tectonic plates, as a conveyor belt. However the temporal framework for the observed separation between Corsica and Sardinia was unexpected: according to the study, there was a quite early differentiation between the lineages of these islands, in spite of their geographic proximity».
Characterizing the factors that drive biodiversity is key to identify and understand the natural richness of the Mediterranean, a biogeographic region characterized by a high number of endemism. According to Leticia Bidegaray-Batista, «several alternative hypotheses could explain the distribution of the genus Parachtes in the Mediterranea. In this specific case, the tectonic dynamic of the Mediterranean was singled out as the main factor driving species diversification».
Moreover, this study also provides information regarding the rate of substitution in genetic markers commonly used in phylogenetic studies, which allows absolute time inferences using molecular clocks. The conclusions of this research contrast with other phylogenetic studies conducted in Mediterranean islands, where the dynamics of the colonization and diversification of the fauna are associated with the Messinian salinity crisis, a dramatic event that caused the drying of the Mediterranean Sea at the end of the Miocene.
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