Full description
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.Lineage
Maintenance and Update Frequency: notPlannedNotes
CreditFunded by The Australian Research Council (ARC)
Funded by The Australian National University (ANU) Faculties Research Grant Scheme
To determine the sedimentological variations with sea-level over the last glacial/ interglacial cycle in the Capricorn Channel. Very little previous work has been undertaken within this area.
Issued: 04 07 2007
Data time period: 1997 to 1997
text: westlimit=154; southlimit=-24; eastlimit=154.5; northlimit=-23.5
text: uplimit=2004; downlimit=2004
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(ANU_Bostock_GC14_1_data.xls)
Core data - Capricorn Channel (aodn: bluenet_datasets_capricorn_channel)
url :
http://geoserver-123.aodn.org.au/geoserver/wms![]()
global : 13f86210-29ca-11dc-b961-00188b4c0af8
- global : 33089890-29d0-11dc-b961-00188b4c0af8
