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Quantifying the isotopic composition of oxygen and carbon with increasing depth in core GC14, located in the Capricorn Channel

Created 24/06/2017

Updated 24/06/2017

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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). 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 ~80cm depth corresponding to heavier 18-O values and other measured parameters.

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Title Quantifying the isotopic composition of oxygen and carbon with increasing depth in core GC14, located in the Capricorn Channel
Language English
Licence Creative Commons Attribution 2.5 Australia
Landing Page https://devweb.dga.links.com.au/data/dataset/c3fabf24-7666-4d82-8a42-6dedacc26e21
Contact Point
National Institute of Water and Atmosphere (NIWA)
h.bostock@niwa.co.nz
Geospatial Coverage {"type": "Polygon", "coordinates": [[[154.0, -24.0], [154.5, -24.0], [154.5, -23.5], [154.0, -23.5], [154.0, -24.0]]]}
Data Portal data.gov.au