Age vs Depth profile of core GC13, collected from the Capricorn Channel off the Eastern Australian Coast

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. Files (slice {"file": url}): - ANU_Bostock_GC13_2_data.xls (excel): http://catalogue.aodn.org.au/geonetwork/srv/en/file.disclaimer?uuid=19a86b60-2533-11dc-aba4-00188b4c0af8&fname=ANU_Bostock_GC13_2_data.xls&access=private

Cite as: National Institute of Water and Atmosphere (NIWA). Age vs Depth profile of core GC13, collected from the Capricorn Channel off the Eastern Australian Coast. https://data.gov.au/data/dataset/age-vs-depth-profile-of-core-gc13-collected-from-the-capricorn-channel-off-the-eastern-australi