-
Carbon isotope (13-C) values for 5 different foraminiferal species down the...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). 13-C values were recorded for 5 foraminiferal... -
A survey of limpets on an intertidal rocky shore in Western Port Bay, Victoria
School of BioSciences, The University of Melbourne
This data set is from a survey comparing the size and shape of limpets in the high intertidal zone compared to the low intertidal zone on a rocky shore in Western Port Bay,... -
Age vs Depth profile of core GC14, collected from the Capricorn Channel off...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18-O and 13-C were obtained... -
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... -
ASGS SA1 2021 by GP Catchments 2023
Department of Health and Aged Care
General Practitioner Catchment (GPC) Developed by the Australian Government Department of Health and Aged Care as custom aggregations of the Australian Bureau of Statistics... -
Water levels in the Gippsland Lakes; 1998 to 2002.
The Centre for Environmental Applied Hydrology (CEAH) at the University of Melbourne, with funding from the Gippsland Ports Authority (GPA) established a water level monitoring... -
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 percentage of CaCO3 in samples taken from various depths in core GC12,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The percentage of CaCO3 in samples collected from... -
Spatially variable effects of copper on sessile invertebrates across a marina
School of BioSciences, The University of Melbourne
A manipulative field experiment was used to assess the spatial variation in the effect of copper on sessile invertebrates within a marina in Port Phillip Bay, Victoria. Sessile... -
Recovery of the encrusting bryozoan, Parasmittina delicatula, from damage at...
School of BioSciences, The University of Melbourne
Parasmittina delicatula colonies were located on the Flinders pier in early 1999 and assigned to a small size class (10-15mm) or large size class (30mm or more). Each colony was... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
National Institute of Water and Atmosphere (NIWA)
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 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
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... -
Physical and biological factors influencing larval supply of reef fish to...
School of BioSciences, The University of Melbourne
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... -
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 GC-12, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC12 (23o34' 37S 153o49' 94E) was collected from the Capricorn Channel at a depth of 990.5 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-10, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC10 (22o59 76S 152o48' 00E) was collected from the Capricorn Channel at a depth of 335 mbsl (metres below sea level). By investigating the properties and components of... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-787
Department of Biological Sciences, Macquarie University
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,... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-784
Department of Biological Sciences, Macquarie University
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,...