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Deep-sea coral ocean-climate records of the last glacial and recent eras. The project aims to predict the ocean carbon dioxide sink’s long-term capacity and future trajectories of global warming and increasing carbon dioxide. This project will use geochemical proxies encoded in the skeletons of deep-sea corals in the Perth Canyon, Tasman seas, and Antarctica, in the heart of the ocean-climate system, to reveal continuous long-term records of environmental change at annual-decadal resolution for ....Deep-sea coral ocean-climate records of the last glacial and recent eras. The project aims to predict the ocean carbon dioxide sink’s long-term capacity and future trajectories of global warming and increasing carbon dioxide. This project will use geochemical proxies encoded in the skeletons of deep-sea corals in the Perth Canyon, Tasman seas, and Antarctica, in the heart of the ocean-climate system, to reveal continuous long-term records of environmental change at annual-decadal resolution for our recent past (hundreds to thousands of years) and the Last Glacial Maximum. These records are expected to provide a more accurate understanding of Earth’s long-term responses to anthropogenic carbon dioxide emissions and global warming.Read moreRead less
Roles of deep-Earth fluid cycling in the generation of intra-continental magmatism. This project aims to test a provocative and potentially ground-breaking hypothesis that fluid released from subducted oceanic slabs and stored in the mantle transition zone, may trigger or control some major intra-plate geotectonic phenomena. It aims to provide a self-consistent model that links geological processes occurring at plate boundaries with those far-field effects well away from plate boundaries via dee ....Roles of deep-Earth fluid cycling in the generation of intra-continental magmatism. This project aims to test a provocative and potentially ground-breaking hypothesis that fluid released from subducted oceanic slabs and stored in the mantle transition zone, may trigger or control some major intra-plate geotectonic phenomena. It aims to provide a self-consistent model that links geological processes occurring at plate boundaries with those far-field effects well away from plate boundaries via deep-Earth fluid cycling. The outcomes of this project aim to help to better understand links between plume and plate tectonic processes in the first-order dynamic system of Earth, and identify ways to improve success in future mineral exploration.Read moreRead less
Linking the deep carbon cycle with critical mineral deposits. This project aims to determine how the global carbon cycle controlled the occurrence of carbonatites, which provide most of the world’s rare earth elements, using novel methods to improve our understanding of carbonatites and carbon-rich mantle rocks. This project expects to generate new knowledge on how global geodynamic processes, including the supercontinent cycle, influenced carbon recycling and mantle enrichments. This project wi ....Linking the deep carbon cycle with critical mineral deposits. This project aims to determine how the global carbon cycle controlled the occurrence of carbonatites, which provide most of the world’s rare earth elements, using novel methods to improve our understanding of carbonatites and carbon-rich mantle rocks. This project expects to generate new knowledge on how global geodynamic processes, including the supercontinent cycle, influenced carbon recycling and mantle enrichments. This project will have significant economic benefits for targeting economically critical mineral deposits required to transition to a decarbonized world and placing the carbon cycle in a paleogeographic context to understand the climate in deep time.Read moreRead less
Subduction of elements with variable oxidation state: effects on the source of arc magmatism. This project will use studies of elements with variable oxidation state: iron; carbon and sulphur, to resolve key geological questions, enable better targeting of ore deposits and develop ways to aid the practicality of mineral sequestration of carbon dioxide.
From core to ore: emplacement dynamics of deep-seated nickel sulphide systems. This project will investigate the genesis of ore deposits containing nickel, copper and the immensely valuable platinum group elements. These systems provide insights into fundamental questions regarding the evolution and dynamics of the Earth system, because these ore deposits are windows into the deep mantle of our planet.
How warm and how wet? New perspectives on paleoclimate records and hydrological regimes in arid zones of Australia. This project will develop a new and precise palaeotemperature record for southern Australia, and will investigate the hydrologic dynamics of inland Australia. Together, this research will lead to new discoveries in the way Australian ecosystems respond to climate variability and will enable better understanding of its impacts.