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Survey data collected from Core E53-10, located on the edge of the South Tasman rise
Most globally linked climatic records dealing with continuous longterm change are derived from the ocean sea-floors where sedimentation of microplankton is accumulated on a time... -
Shell cross sections of the bivalve Saccostrea glomerata collected from Pambula Lake, NSW
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... -
Shell cross sections of the bivalve Saccostrea glomerata collected from Moreton Bay
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... -
Shell cross sections of the bivalve Pinctada imbricata collected from Moreton Bay
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... -
Shell cross sections of the bivalve Ostrea angasi collected from Severs Beach, NSW
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... -
Shell cross sections of the bivalve Ostrea angasi collected from Pambula Lake, NSW
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... -
Shell cross sections of the bivalve Ostrea angasi collected from Little Swanport, Tasmania
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... -
Shell cross sections of the bivalve Mytilus galloprovincialis collected from Pambula Lake, NSW
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... -
Shell cross sections of the bivalve Mytilus galloprovincialis collected from Little Swanport, Tasmania
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... -
Shell cross sections of the bivalve Crassostrea gigas collected from Little Swanport, Tasmania
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 on Last Glacial Maximum core samples
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
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 with increasing depth in core GC14, located in the Capricorn Channel
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 depth in core GC13, located in the Capricorn Channel
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... -
Quantifying the isotopic composition of oxygen and carbon with increasing depth in core GC12, located in the Capricorn Channel
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 depth in core GC11, located in the Capricorn Channel
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 depth in core GC10, located in the Capricorn Channel
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 depth in core GC09, located in the Capricorn Channel
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 the core MD032607, located off South Australia
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 the core MD002361, located on the shelf edge offshore Western Australia
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,...