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Environmental controls on growth of massive Porites corals from the Great...
Australian Institute of Marine Science
Massive Porites colonies were collected from 29 reefs, located along the length and across the width of the Great Barrier Reef (GBR) between November 1987 and May 1992. The... -
Coral calcification in massive Porites in the nearshore region of the...
Australian Institute of Marine Science
Ten massive Porites colonies were collected from the fringing reefs of each of 4 inshore islands of the Great Barrier Reef in January 2004. Two reefs were located in the Far... -
Rainfall variability over northeastern Australia derived from coral luminescence data
Australian Institute of Marine Science
Twenty coral cores from the Australian Institute of Marine Science's archive of long Porites spp. coral cores from the Great Barrier Reef were chosen for this study. The cores... -
Growth of Western Australian corals in the Anthropocene
Australian Institute of Marine Science
Twenty-seven long cores were collected between October 2008 and September 2010 from massive Porites sp. colonies at six locations covering approximately 1000 km of the coast of... -
Luminescent lines in massive Porites corals from the Great Barrier Reef as...
Australian Institute of Marine Science
Massive Porites colonies were collected from 1 reef in the Coral Sea and 29 reefs located along the length and across the width of the Great Barrier Reef (GBR), between November... -
Weather records in corals from northern Australia (CCEP Project)
Australian Institute of Marine Science
A large scale coral core drilling program was undertaken between March 1986 and April 1987. Coral cores were collected from Porites spp. bommies on reefs between Darwin and... -
Age vs Depth profile of core GC10, collected from the Capricorn Channel off...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18O and 13C were obtained from... -
Oxygen isotope (18-O) 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). The 18-O values of the different foraminiferal... -
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... -
Parent record: Datasets relating to core GC13, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC13 (23o47' 30S 154o13' 56E) was collected from the Capricorn Channel at a depth of 1482 mbsl (metres below sea level). By investigating the properties and components of... -
Radiometrically determined 14C dates obtained for 4 sediment cores on Wistari Reef
Wistari Reef is a lagoonal platform reef, situated on the Tropic of Capricorn, within the Capricorn and Bunker region of the southern Great Barrier Reef. In this dataset seven... -
Shell cross sections of the bivalve Crassostrea gigas collected from Little...
Australian National University
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... -
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... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
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 data from stable isotopes of Globigerinoides... -
Parent record: Datasets relating to core GC-14, located in the Capricorn...
National Institute of Water and Atmosphere (NIWA)
Core GC14 (23o49' 52S 154o21' 67E) was collected from the Capricorn Channel at a depth of 2004 mbsl (metres below sea level). By investigating the properties and components 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... -
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... -
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... -
Quantifying the isotopic composition of oxygen and carbon with increasing...
National Institute of Water and Atmosphere (NIWA)
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...
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). The data from stable isotopes of Globigerinoides...