Full description
A gravity core (GC13) was collected from a depth of 1482 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. The age-model that was produced plausibly extends back to Marine Isotope Stage (MIS) 6, with approximate sedimentation rates calculated according to this model. Sedimentation rates fluctuate from 5cm/kyr during the last transition and interglacial, to 1cm/kyr during the glacial maximum.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: 25 06 2007
Data time period: 1997 to 1997
text: westlimit=154; southlimit=-24; eastlimit=154.5; northlimit=-23.5
text: uplimit=1482; downlimit=1482
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(ANU_Bostock_GC13_2_data.xls)
Core data - Capricorn Channel (aodn: bluenet_datasets_capricorn_channel)
url :
http://geoserver-123.aodn.org.au/geoserver/wms![]()
global : e231da30-2533-11dc-aba4-00188b4c0af8
- global : 19a86b60-2533-11dc-aba4-00188b4c0af8
