Quantifying the isotopic composition of oxygen and carbon with increasing depth in core GC13, located in the Capricorn Channel
A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides ruber were analysed to allow a preliminary understanding of the hemipelagic sedimentary environment over the last glacial / interglacial cycle. The results suggest that the core reaches the Last Glacial Maximum (LGM) at ~90cm depth and MIS 6 at ~340cm corresponding to heavier 18-O values and other measured parameters.
Données et ressources
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Core data - Capricorn ChannelWMS Ouvrir
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License GraphicPNG Ouvrir
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Informations supplémentaires
| Date (publication) | 2007-06-25 |
|---|---|
| Statut | completed |
| Fréquence de mise à jour | notPlanned |
| Langue des métadonnées | en |
| Licence | Creative Commons Attribution 4.0 |
| Métadonnées sources | ISO 19115 XML |
| Dernière mise à jour | 2026-11-05 |
| Créé | 2026-11-05 |
| API | package_show |