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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,... -
Quantifying the isotopic composition of oxygen and carbon through time in the core GC04, located off the coast of New Caledonia
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 the core BAR 9403, located off the coast of Sumatra
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... -
Quantifying colour patterns on the black carapace of the fiddler crab Uca capricornis
Fiddler crabs are often spectacularly coloured and capable of dramatic colour changes. While the adaptive significance of variation resulting from short- or long-term colour... -
Preliminary log of core GC04, collected from the southeastern side of the New Caledonian Basin
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... -
Phytoplankton Ecology in the Upper Swan River Estuary, Western Australia - Summary
The aim of the study was to determine the extent to which phytoplankton population in the upper Swan River Estuary, W.A. (see thumbnail) are controlled by physico-chemical... -
Phytoplankton Ecology in the Upper Swan River Estuary, Western Australia - Species composition and distribution patterns
This study correlated temporal and depth differences in phytoplankton species distribution with various physical and chemical parameters in the upper Swan River Estuary between... -
Phytoplankton Ecology in the Upper Swan River Estuary, Western Australia - Seasonal nitrogen uptake rates and preferential uptake of inorganic and organic nitrogen and comparison of C:N ratios
The major aim of the study was to determine monthly and seasonal nitrogen uptake by phytoplankton communities of the three nitrogen species NO3-, NH4+ and urea from 1998 to 1999... -
Phytoplankton Ecology in the Upper Swan River Estuary, Western Australia - Nitrogen uptake for inorganic and organic nitrogen sources
The main aim of this study was to detemine seasonal uptake kinetics for the different nitrogen species; two inorganic sources (NO3- and NH4+), and an organic source (urea) in... -
Phytoplankton Ecology in the Upper Swan River Estuary, Western Australia - Microheterotroph grazers and their impact on phytoplankton biomass
Species composition trends for the microheterotrophic grazing community (<300 um) over an annual period (1998-1999) were determined for the upper Swan River estuary. Also... -
Phytoplankton Ecology in the Upper Swan River Estuary, Western Australia - A comparison of nitrogen uptake by seasonal bloom assemblages
Maximum nitrogen uptake rates (Vmax) and preferential nitrogen sources were determined for the different major bloom types between November 1995 and May 1996 in the upper Swan... -
Phytolith recovery from core MD88-779
Core MD88-779 was taken during the 1988 French APSARA IV cruise in the South East Indian Ocean. The core was situated on the South Tasman Rise (47º50.690S, 146º32.750E) at a... -
Physical and biological factors influencing larval supply of reef fish to the lagoon of Lord Howe Island
Abundances of reef fish larvae, conspecific adults and habitat type were measured at 5 sites in the Lord Howe Island lagoon. Light traps were deployed daily over a 28 day period... -
Percentage of variance in radiolarian correspondence analysis scores explained by various oceanic parameters
Percentage of the variance in correspondence scores for radiolarian abundance counts for sites in the eastern & southern Indian Ocean explained by environmental variables...