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Quantifying the isotopic composition of oxygen and carbon with increasing...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC09) was collected from a depth of 166m within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides ruber... -
Quantifying the isotopic composition of oxygen and carbon through time in...
Australian National University
The calcareous tests of Globigerina bulloides are analysed to quantify the isotopic composition of oxygen and carbon through time at core site MD032607 (137.4065 E, 36.9606... -
Quantifying the isotopic composition of oxygen and carbon through time in...
Australian National University
The calcareous tests of Globigerinoides ruber are analysed to quantify the isotopic composition of oxygen and carbon through time at core site MD002361 (113o28.63'E,... -
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... -
Quantifying the isotopic composition of oxygen and carbon through time in...
Australian National University
This short core obtained off Sumatra (BAR9403, 5.82 S, 104.0316 E) records the palaeoceanography from the Last Glacial Maximum (LGM) to the present day. The lightest 18O value... -
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... -
Parent record: Datasets relating to core MD002361 (shelf edge offshore...
Australian National University
We must understand the natural cycles of the oceans to understand the evolution of our climate through geological time. Core MD 002361 was obtained in 2000 off the coast of... -
Parent record: Datasets relating to core GC-14, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC14 (23o49' 52S 154o21' 67E) was collected from the Capricorn Channel at a depth of 2004 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC13, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC13 (23o47' 30S 154o13' 56E) was collected from the Capricorn Channel at a depth of 1482 mbsl (metres below sea level). By investigating the properties and components of... -
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... -
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... -
Parent record: Datasets relating to core GC-10, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC10 (22o59 76S 152o48' 00E) was collected from the Capricorn Channel at a depth of 335 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-09, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC09 (22o53' 70S 152o38' 10E) was collected from the Capricorn Channel at a depth of 166 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core BAR9403 (off the coast of Sumatra)
Australian National University
We must understand the natural cycles of the oceans to understand the evolution of our climate through geological time. Core BAR 9403 was obtained in 1994 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... -
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...