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.

Data and resources

ANU_Bostock_GC13_1_data.xls

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aodn: bluenet_datasets_capricorn_channel

Core data - Capricorn Channel

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License Graphic

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Additional information

Date (publication)	2007-06-25
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