Distinguishing the combined vegetation and soil component of δ 13 C variation in speleothem records...
Distinguishing the combined vegetation and soil component of δ 13 C variation in speleothem records from subsequent degassing and prior calcite precipitation effects
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English
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The carbon isotopic signature inherited from soil and epikarst processes may be modified by degassing and prior calcite precipitation (PCP) before its imprint on speleothem calcite. Despite laboratory demonstration of PCP effects on carbon isotopes and increasingly sophisticated models of the governing processes, to date, there has been limited eff...
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Distinguishing the combined vegetation and soil component of δ 13 C variation in speleothem records from subsequent degassing and prior calcite precipitation effects
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TN_cdi_crossref_primary_10_5194_cp_19_2423_2023
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_crossref_primary_10_5194_cp_19_2423_2023
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ISSN
1814-9332
E-ISSN
1814-9332
DOI
10.5194/cp-19-2423-2023