-
The Australian Marine Quaternary Program
The Australian Marine Quaternary Program is a loose association of researchers who visited the Geology Department (now called Department of Earth and Marine Sciences) at the... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
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... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides... -
The relative abundance (%) of planktonic foraminifera over time in core...
The advent of deep-sea drilling in the 1950's prompted the use of planktonic foraminifera (unicellular protozans) as palaeoceanographic indicators. They provide a natural... -
The relative abundance (%) of planktonic foraminifera over time in core BAR...
The advent of deep-sea drilling in the 1950's prompted the use of planktonic foraminifera (unicellular protozans) as palaeoceanographic indicators. They provide a natural... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-779
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... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-787
Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The data from stable isotopes of Globigerinoides... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
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... -
The relative abundance (%) of planktonic foraminifera over time in core MD...
The advent of deep-sea drilling in the 1950's prompted the use of planktonic foraminifera (unicellular protozans) as palaeoceanographic indicators. They provide a natural... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-784
Core MD88-784 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,...
1 - 13 of 13 results