Discovery Early Career Researcher Award - Grant ID: DE210101395
Funder
Australian Research Council
Funding Amount
$447,627.00
Summary
Linking continental emergence and climatic evolution on the Early Earth. This project will use a range of innovative geochemical techniques to constrain the timing and extent to which the continents were emergent (above sea-level) throughout Earth’s history and its impact on climatic evolution. Continental emergence was pivotal to the development of our habitable planet, as it controlled the influx of bioessential elements, like phosphorus, to the oceans. Expected outcomes include a detailed rec ....Linking continental emergence and climatic evolution on the Early Earth. This project will use a range of innovative geochemical techniques to constrain the timing and extent to which the continents were emergent (above sea-level) throughout Earth’s history and its impact on climatic evolution. Continental emergence was pivotal to the development of our habitable planet, as it controlled the influx of bioessential elements, like phosphorus, to the oceans. Expected outcomes include a detailed record of changes in ocean chemistry, and a time integrated model for the emergence of continents on the early Earth. Documenting the impact of changes in the solid Earth on evolution is not only of interest to society in general, but also contributes to understanding the formation of Australia’s vast iron ore deposits.Read moreRead less
ARC Centre of Excellence for Core to Crust Fluid Systems. Water is essential for human existence, indeed for life's beginning. The circulation of water between the surface and the deep interior lubricates the internal dynamics that keep Earth geologically alive; it is crucial to most Earth systems, including the evolution of the hydrospher/atmosphere/biosphere, and the development of giant ore deposits. However, the origin, abundance, speciation and movements of fluids inside Earth are largely u ....ARC Centre of Excellence for Core to Crust Fluid Systems. Water is essential for human existence, indeed for life's beginning. The circulation of water between the surface and the deep interior lubricates the internal dynamics that keep Earth geologically alive; it is crucial to most Earth systems, including the evolution of the hydrospher/atmosphere/biosphere, and the development of giant ore deposits. However, the origin, abundance, speciation and movements of fluids inside Earth are largely unknown, and represent key issues in modern geoscience. This CoE will integrate previously disparate fields - geology, tectonics, geochemistry, petrophysics, geophysics and dynamic modelling - to understand the workings of Earth's deep plumbing system.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE130100099
Funder
Australian Research Council
Funding Amount
$390,000.00
Summary
New horizons in geochemical isotopic analysis with a new-generation multicollector plasma mass spectrometer: towards unravelling the deep earth system. A new-generation plasma mass spectrometer will let us develop novel applications in geochemistry to better understand Earth processes. This will enhance Australian Geosciences’ high international profile, and help attract high-quality researchers to attack problems relevant to the Deep Earth Resources National Priority and mineral exploration.
Discovery Early Career Researcher Award - Grant ID: DE140100553
Funder
Australian Research Council
Funding Amount
$392,570.00
Summary
Exploring links between climate change, ocean chemistry, and the rise of multicellular life: The Ediacaran sedimentary record of central Australia. For most of Earth’s history, single-celled organisms were the only forms of life on the planet. Not until roughly 600 million years ago do fossils of multicellular animals appear in the rock record. Explanations for the Ediacaran rise of multicellularity include extreme climate change, meteorite impact and oxygenation of the global ocean. Evaluation ....Exploring links between climate change, ocean chemistry, and the rise of multicellular life: The Ediacaran sedimentary record of central Australia. For most of Earth’s history, single-celled organisms were the only forms of life on the planet. Not until roughly 600 million years ago do fossils of multicellular animals appear in the rock record. Explanations for the Ediacaran rise of multicellularity include extreme climate change, meteorite impact and oxygenation of the global ocean. Evaluation of these hypotheses is complicated by the fact that stratigraphic records that span the appropriate time interval are rare. This project is focused on the carbon, oxygen, and zinc isotopic records preserved by Ediacaran marine rocks in the Amadeus Basin of central Australia. Results will contribute to a more complete record of fluctuations in ocean chemistry during a key interval of Earth history.Read moreRead less
Four dimensional lithospheric evolution and controls on mineral system distribution in Neoarchean to Paleoproterozoic terranes. This project will resolve important questions about the links between the evolution and preservation of continents and important mineral deposits in Australia and West Africa between 2.7 and 1.8 billion years ago. The results will improve the understanding of a key period of Earth history and make a major contribution to mineral exploration.