Full description
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18O and 13C were obtained from Gs. ruber and correlated with the SPECMAP age-model. The results highlight 4 glacial cycles, incorporating Marine Isotope Stage (MIS) 1 through to MIS 11. Isotopically heavier 18O values at ~460cm, ~345cm, 150cm, and 30cm correspond respectively to MIS 10 (359 kyr BP), MIS 8 (260 kyr BP), MIS 6 (140 kyr BP) and the LGM (20 kyr BP). Sedimentation rates are typically low, <1 cm/kyr to ~4 cm/kyr. The higher sedimentation rates are evident at glacial / interglacial terminations, but then drop off rapidly in the interglacials.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: 27 06 2007
Data time period: 1997 to 1997
text: westlimit=151.5; southlimit=-24.5; eastlimit=153; northlimit=-23
text: uplimit=502; downlimit=502
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(ANU_Bostock_GC11_2_data.xls)
Core data - Capricorn Channel (aodn: bluenet_datasets_capricorn_channel)
url :
http://geoserver-123.aodn.org.au/geoserver/wms![]()
global : 2b6c31c0-2465-11dc-95fb-00188b4c0af8
- global : be8d3fd0-246f-11dc-95fb-00188b4c0af8
