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Figure 4 | BMC Evolutionary Biology

Figure 4

From: When environmental changes do not cause geographic separation of fauna: differential responses of Baikalian invertebrates

Figure 4

Calibrated demographic histories of G. fasciatus and M. herderiana and reconstructed paleoclimatic history. (a) Inferred lake water level (relative to present) based on seismic survey of the delta of the Selenga River. The two lines (NW and SE) represent results obtained using the northwestern and southeastern (respectively) blocks of the delta (see reference [32] for details); adapted from reference [32], (b) changes in population size in G. fasciatus and M. herderiana (mean estimates; obtained in this study) and (c) diatom abundance inferred from sedimentary drill core BDP-93-2 (redrawn from [21]). In (c), solid triangles are the radiocarbon dates for the core BDP-93-1 [82, 83] and squares are for core BDP-93-2; the arrow indicates the 50.3 Kyr BP correlation tie point for BDP-93 record [29]. The shaded areas correspond to Marine Isotope Stage 3.

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