Lancaster EPrints
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Late Holocene climate reconstructions for the Russian steppe, based on mineralogical and magnetic properties of buried palaeosols.
Insights into past climate changes, and corresponding evolution of soils and the environment, can be gained by multidisciplinary studies of palaeosols. Here, we focus on palaeosols buried beneath archaeological monuments, specifically, funerary mounds (kurgans), in the Russian steppe. The kurgans we
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