Relevance of soil-speleothem relationships for paleoenvironmental reconstructions: Example from a Holocene deposit in SW Romania
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Abstract
We present a multi-proxy study of a colluvium-derived soil (2.5-m deep) developed above Ascunsă Cave, in the Mehedinți Mountains, SW Romania, presumably in depositional connection with a coeval stalagmite (Faur et al., 2021). Soil samples, contiguously taken every 5 cm, were analyzed for clay mineralogy, grain size, chemical composition, magnetic susceptibility, and stable carbon isotopes.
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