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Parent record: Datasets relating to core MD032607 (off South Australia)
Australian National University
We must understand the natural cycles of the oceans to understand the evolution of our climate through geological time. Core MD 032607 was obtained in 2003 off the coast of... -
Carbon isotope (13-C) values for 5 different foraminiferal species down the...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). 13-C values were recorded for 5 foraminiferal... -
Quantifying the isotopic composition of oxygen and carbon through time in...
Australian National University
Core GC04 was collected from the southeastern side of the New Caledonian Basin. In relation to isotopic composition there appears to be a correlation between 13C and 18O... -
Radiolarian abundance counts on Last Glacial Maximum core samples
Australian National University
Abundance counts by taxon of radiolaria from six Eastern Indian Ocean core samples dated to the last glacial maximum. The samples were selected because they were also used for... -
Shell cross sections of the bivalve Saccostrea glomerata collected from...
Australian National University
Petrological and some geochemical analysis methods require the sample to be made into a thin or thick section. This record provides a series of shell cross-sectional images and... -
Age vs Depth profile of core GC12, collected from the Capricorn Channel off...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18-O and 13-C were obtained... -
Parent record: Datasets relating to core GC-12, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC12 (23o34' 37S 153o49' 94E) was collected from the Capricorn Channel at a depth of 990.5 mbsl (metres below sea level). By investigating the properties and components of... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides... -
Shell cross sections of the bivalve Ostrea angasi collected from Pambula Lake, NSW
Australian National University
Petrological and some geochemical analysis methods require the sample to be made into a thin or thick section. This record provides a series of shell cross-sectional images and... -
Radiolarian abundance counts from the eastern and southern Indian Ocean
Australian National University
Abundance counts by taxon of radiolaria from ~100 surface sediment gravity cores from the Southern and Eastern Indian Ocean collected between 1988 and 2004. -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Datasets relating to five cores taken from different locations on Wistari Reef
Wistari Reef is a lagoonal platform reef, situated on the Tropic of Capricorn, within the Capricorn and Bunker region of the southern Great Barrier Reef. Fives cores were... -
Percentage of variance in radiolarian correspondence analysis scores...
Australian National University
Percentage of the variance in correspondence scores for radiolarian abundance counts for sites in the eastern & southern Indian Ocean explained by environmental variables... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
A visual summary and annotation of the stratification in core MD002361,...
Australian National University
The core description highlights the stark contrast been glacial and interglacial periods. 1-1.5m bands of red/brown clay indicate interglacial periods, which then alternate with... -
Parent record: Datasets relating to core GC-11, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC11 (23o23' 07S 153o22' 00E) was collected from the Capricorn Channel at a depth of 502 mbsl (metres below sea level). By investigating the properties and components of... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Shell cross sections of the bivalve Ostrea angasi collected from Little...
Australian National University
Petrological and some geochemical analysis methods require the sample to be made into a thin or thick section. This record provides a series of shell cross-sectional images and... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-779
Department of Biological Sciences, Macquarie University
Core MD88-779 was taken during the 1988 French ASPARA IV cruise in the South East Indian Ocean aboard the Marion DuFresne. The core was situated on the South Tasman Rise...