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

Created 23/06/2025

Updated 23/06/2025

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.

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Field Value
Title Age vs Depth profile of core GC14, collected from the Capricorn Channel off the Eastern Australian Coast
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/dataset/12e82573-3045-4338-8f5b-20d1bdd19818
Contact Point
Australian Ocean Data Network
h.bostock@niwa.co.nz
Reference Period 01/01/1997 - 01/01/1997
Geospatial Coverage
Map data © OpenStreetMap contributors
{
  "coordinates": [
    [
      [
        154.0,
        -24.0
      ],
      [
        154.5,
        -24.0
      ],
      [
        154.5,
        -23.5
      ],
      [
        154.0,
        -23.5
      ],
      [
        154.0,
        -24.0
      ]
    ]
  ],
  "type": "Polygon"
}
Data Portal Australian Oceans Data Network

Data Source

This dataset was originally found on Australian Oceans Data Network "Age vs Depth profile of core GC14, collected from the Capricorn Channel off the Eastern Australian Coast". Please visit the source to access the original metadata of the dataset:
https://catalogue.aodn.org.au/geonetwork/srv/eng/csw/dataset/age-vs-depth-profile-of-core-gc14-collected-from-the-capricorn-channel-off-the-eastern-australi1