Figure from Neogene paleosols of the Sirius Group, Dominion Range, Antarctica

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Figure 3. A reconstruction of soils and vegetation in Meyer Desert during deposition of the Sirius Group. Peligro and Viento pedotypes are presumed precursors in development toward the Siesta pedotype, but the type Peligro and Viento pedotypes are in the upper Oliver Platform. The South Pole is 500 kilometers south in the direction of the Beardmore Glacier.