Skip to main content
. 2019 Jan 15;9(3):1041–1060. doi: 10.1002/ece3.4745

Figure 7.

Figure 7

Coalescence trees of the ten major clusters of Rana pipiens in North Dakota based on the Beaumont (a) and Cornuet–Miller (b) models. Both models show the major split between the populations east and west of the Missouri River occurred during the late Pleistocene (18–13 kya), while most of the subdivision within these major populations occurring during the dry period of the Holocene (11–7 kya)