Age vs Depth profile of core GC14, collected from the Capricorn Channel off the Eastern Australian Coast

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A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18-O and 13-C were obtained from : Globigerinoides ruber and correlated with the SPECMAP age-model. It appears that the core extends back to MIS 3 (Marine Isotope Stage). From limited depth matching with the Martinson et al. (1987) SPECMAP age-model it is extremely difficult to determine a sedimentation rate, however, it exhibits a relatively uniform rate throughout the core of ~4cm/kyr. This is a fairly high sedimentation rate for a core this distal and abyssal.

Data and resources

ANU_Bostock_GC14_2_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