Quantifying the isotopic composition of oxygen and carbon through time in the core GC04, located off the coast of New Caledonia
Core GC04 was collected from the southeastern side of the New Caledonian Basin. In relation to isotopic composition there appears to be a correlation between 13C and 18O measurements. The results also highlight a definite change in average 13C at isotopic stage 5e.
Data and resources
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XLS Open
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Core data - New Caledonian BasinWMS Open
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HTML Open
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HTML Open
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License GraphicPNG Open
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HTML Open
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HTML Open
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HTML Open
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HTML Open
Additional information
| Date (publication) | 2007-06-19 |
|---|---|
| Status | completed |
| Update frequency | notPlanned |
| Metadata language | en |
| License | Creative Commons Attribution 4.0 |
| Source metadata | ISO 19115 XML |
| Last updated | 2026-11-05 |
| Created | 2026-11-05 |
| API | package_show |