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. 2012 Dec 3;109(51):20998–21003. doi: 10.1073/pnas.1214398110

Fig. 3.

Fig. 3.

Calibrated COI phylogenetic tree for European Oxyrrhis isolates based on a sequence substitution rate of 0.01 substitutions per million years. Errors for each dated node are upper and lower 95% posterior densities. MSC, Messinian Salinity Crisis; LP, Late Pleistocene glaciations; LGM, Last Glacial Maximum.