Quantifying the isotopic composition of oxygen and carbon through time in the core GC04, located off the coast of New Caledonia

Oxygène

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.

Données et ressources

ANU_Gretton_GC04_2_data.xls

XLS Ouvrir
aodn:bluenet_datasets_new_caledonian_basin

Core data - New Caledonian Basin

WMS Ouvrir
Unnamed resource

HTML Ouvrir
Unnamed resource

HTML Ouvrir
Unnamed resource

License Graphic

PNG Ouvrir
Unnamed resource

HTML Ouvrir
Unnamed resource

HTML Ouvrir
Unnamed resource

HTML Ouvrir
Unnamed resource

HTML Ouvrir

Informations supplémentaires

Date (publication)	2007-06-19
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