Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution
Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution
Authors
Keywords
Speleothem, Dead carbon proportion (DCP), Stable isotope ratios of carbon (δ, C), Sulfuric acid dissolution, Corchia Cave
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