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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. -
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... -
Age vs. Depth of core MD032607 (off South Australia). Age has been...
Australian National University
The age with depth of core MD032607 is calculated through 18O values, which are then correlated with the SPECMAP age-model. Based upon these measurements the age at the deepest... -
Age vs. depth of core MD002361 (shelf edge offshore Western Australia). Age...
Australian National University
Radiocarbon dating was used to construct an age model for the upper sections of core MD002361 to a depth of 205cm, after which the age-model was based on the chronology of... -
Age vs. Depth of core BAR 9403 (located off the coast of Sumatra). Age has...
Australian National University
The age with depth of core BAR9403 is calculated through 18O values, which are then correlated with the SPECMAP age-model. Based upon these measurements the age at the deepest...
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