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The relative abundance (%) of planktonic foraminifera over time in core...
Australian National University
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 MD...
Australian National University
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...
Australian National University
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 percentage breakdown of carbonate/non-carbonate fractions in core GC04,...
Australian National University
Core GC04, was collected from the southeastern side of the New Caledonian Basin (22.99965 S, 166.150716 E). Carbonate percent in the curve has an average value of ~79% and... -
The age versus depth profile for core GC04, located off the coast of New Caledonia
Australian National University
Core GC04, was collected from the southeastern side of the New Caledonian Basin (22.99965 S, 166.150716 E). The age of the sediment at each sample depth was determined by... -
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... -
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. -
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... -
Preliminary log of core GC04, collected from the southeastern side of the...
Australian National University
Core GC04 was collected from the southeastern side of the New Caledonian Basin. The upper 140cm of the core was used in this study and was composed of very fine yellow-brown... -
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... -
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 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... -
Ocean temperatures over time estimated from planktonic foraminifera...
Australian National University
In recent years the term 'enhanced greenhouse effect' has become well known in modern society and yet aspects of this possible 'future climate' are poorly understood. The... -
Ocean temperatures over time estimated from planktonic foraminifera...
Australian National University
In recent years the term 'enhanced greenhouse effect' has become well known in modern society and yet aspects of this possible 'future climate' are poorly understood. The... -
Ocean temperatures over time estimated from planktonic foraminifera...
Australian National University
In recent years the term 'enhanced greenhouse effect' has become well known in modern society and yet aspects of this possible 'future climate' are poorly understood. The... -
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...