Figure 4. Graph and maps of ice-sheet growth, showing ice-sheet size and location at mean sea
level temperatures 5, 9, 10, 15, 19, and 20 Kelvin (K) above present. The maps indicate where
margin sedimentation might be sensitive to particular stages of ice-sheet growth. Antarctic
Peninsula glaciation appears to have developed during the last 5-9 K of cooling (from Huybrechts,
1993).
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