Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for ^1^3C variations in speleothems

Details Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for ^1^3C variations in speleothems Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for ^1^3C variations in speleothems

Oct 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001gecoa..65.3443h&link_type=openurl

Geochimica et Cosmochimica Acta, v. 65, iss. 20, p. 3443-3457.

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