A new perspective on the δ13C signal preserved in speleothems using LC–IRMS analysis of bulk organic matter and compound specific stable isotope analysis
The analysis of δ13C in speleothem calcite is established as a palaeoenvironmental proxy, but records can often be complex to interpret due to multiple controls on the signal. Here we present a novel palaeoenvironmental application of non-purgeable organic carbon (NPOC) δ13C analysis and compound-sp...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Pergamon
2013
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/29100 |