Southern gateways - the icehouse cometh: Eocene to Oligocene evolution of southeast Australia. The 50 to 30 million years old strata of southeastern Australia have great economic importance for Australia. Most of the gas and oil extracted in the region comes from strata of this age. The research will lead to better age constraints on these reserves, thus enhancing petroleum prospectivity in the area. The global environment changes from 50 to 30 million years charted in this project will lead ....Southern gateways - the icehouse cometh: Eocene to Oligocene evolution of southeast Australia. The 50 to 30 million years old strata of southeastern Australia have great economic importance for Australia. Most of the gas and oil extracted in the region comes from strata of this age. The research will lead to better age constraints on these reserves, thus enhancing petroleum prospectivity in the area. The global environment changes from 50 to 30 million years charted in this project will lead to a better understanding of the geological record of greenhouse-icehouse change. Knowledge of the nature of this change in the past is critical to predicting how our climate is going to behave in the future.Read moreRead less
PAST EAST ANTARCTIC ICE SHEET AND GLOBAL SEA-LEVEL VARIATIONS. Unique fossil-bearing, open marine sediments occur inland from the modern Antarctic coastline. These were deposited when a now-glaciated Antarctic basin became a marine embayment, during intervals of significantly reduced ice sheet volume and elevated global sea-level in the past. Urgent palaeontological, sedimentological and geochemical research on these sediments are vital to provide: directly datable in situ evidence for major i ....PAST EAST ANTARCTIC ICE SHEET AND GLOBAL SEA-LEVEL VARIATIONS. Unique fossil-bearing, open marine sediments occur inland from the modern Antarctic coastline. These were deposited when a now-glaciated Antarctic basin became a marine embayment, during intervals of significantly reduced ice sheet volume and elevated global sea-level in the past. Urgent palaeontological, sedimentological and geochemical research on these sediments are vital to provide: directly datable in situ evidence for major ice sheet retreat and global sea-level rise in the past; and quantifiable data concerning the environment during such events; an innovative opportunity to improve predictions of Antarctica's response to global warming and answer international debate about past Antarctic Ice Sheet stability.Read moreRead less
Seismic velocity problems associated with Cretaceous-Tertiary carbonate sediments that overlie oil and gas fields of the North West Shelf. The major aim of this collaborative study between Partner Oil Companies and The University of Melbourne is to understand seismic velocity problems associated with tropical carbonate sediments on Australias? North West Shelf. These problems can hinder the hydrocarbon exploration efforts below these carbonates. The project is a multi faceted study and will invo ....Seismic velocity problems associated with Cretaceous-Tertiary carbonate sediments that overlie oil and gas fields of the North West Shelf. The major aim of this collaborative study between Partner Oil Companies and The University of Melbourne is to understand seismic velocity problems associated with tropical carbonate sediments on Australias? North West Shelf. These problems can hinder the hydrocarbon exploration efforts below these carbonates. The project is a multi faceted study and will involve integration of seismic stratigraphy with sedimentological, micropaleontological, and geophysical data. The methods outlined below would underpin any seismic depth migration applications, thereby assisting with the delineation of new gas and oil fields, and help with the estimation of reserves in existing fields.
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Oxygenation of the oceans and the origin of animals. This research project will investigate newly discovered ancient reefs and fossils from the Flinders Ranges that may represent the oldest known animals on Earth. Results from the project will help understand the early evolution of animal life on Earth and will contribute to a greater appreciation of Australia's geological heritage.
Discovery Early Career Researcher Award - Grant ID: DE140100376
Funder
Australian Research Council
Funding Amount
$389,339.00
Summary
The role of mantle plumes in driving plate tectonics and continental margin evolution. Plumes of molten rock rise from deep within the Earth resulting in massive surface eruptions that can lead to global mass extinction events. Despite their size, the role plumes play in driving movements of the continents is poorly understood. This project combines independent global and Australian geological and geophysical data with open software systems to link deep Earth and surface geological processes. Th ....The role of mantle plumes in driving plate tectonics and continental margin evolution. Plumes of molten rock rise from deep within the Earth resulting in massive surface eruptions that can lead to global mass extinction events. Despite their size, the role plumes play in driving movements of the continents is poorly understood. This project combines independent global and Australian geological and geophysical data with open software systems to link deep Earth and surface geological processes. This approach will result in a clearer understanding of how the internal workings of our planet drive, and interact with, surface geological processes. The project will also show how these interactions shape the environmentally important, and resources rich, continental margins and ocean basins.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE120102245
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
Comparison of early mesozoic sedimentary provenances of both sides of the YarlungTsangpo suture zone and the evolution of the neotethys. This project aims to develop a new, more geologically-consistent evolution of the Neotethys and test the affinity of southern Lhasa terrane with Australian terranes. The work will provide new constraints on the early evolution of the Himalayan-Tibetan continental collision.
Discovery Early Career Researcher Award - Grant ID: DE160101020
Funder
Australian Research Council
Funding Amount
$350,821.00
Summary
The geodynamics of past sea level changes. This project is designed to quantify the effect of flow deep within Earth’s interior on past sea-level changes and on the flooding history of Australia over the last 550 million years. The rise and fall of sea level has shaped our planet over time. This project plans to combine recent advances in tectonic reconstructions and dynamic Earth models with the global and Australian rock record. The intended outcome is to understand how the Earth’s surface is ....The geodynamics of past sea level changes. This project is designed to quantify the effect of flow deep within Earth’s interior on past sea-level changes and on the flooding history of Australia over the last 550 million years. The rise and fall of sea level has shaped our planet over time. This project plans to combine recent advances in tectonic reconstructions and dynamic Earth models with the global and Australian rock record. The intended outcome is to understand how the Earth’s surface is shaped by flow within its interior, and how these processes explain the sedimentary record. Project results have the potential to be used as an exploration tool to maximise Australia’s competitive advantage in exploring onshore sedimentary basins.Read moreRead less
Oxygenation history of the Earth and the evolution of complex life. This project will investigate how and when the atmosphere became oxygen-rich by analyzing ancient barrier reefs and other rocks that formed between 1000 to 300 million years ago, spanning the appearance and diversification of animals and plants. The project is significant because the buildup of oxygen in the atmosphere was arguably the most important chemical process ever to have occurred on Earth and controlled the evolution of ....Oxygenation history of the Earth and the evolution of complex life. This project will investigate how and when the atmosphere became oxygen-rich by analyzing ancient barrier reefs and other rocks that formed between 1000 to 300 million years ago, spanning the appearance and diversification of animals and plants. The project is significant because the buildup of oxygen in the atmosphere was arguably the most important chemical process ever to have occurred on Earth and controlled the evolution of environments, climate and life. A major outcome will be an improved understanding of how the Earth's atmosphere and climate are regulated by geological processes. This project will generate new knowledge about how sedimentary zinc, lead and copper ore deposits form, which may guide exploration for these commodities.Read moreRead less
The early history of atmospheric oxygen. Atmospheric oxygen is essential for advanced life and its accumulation on the ancient Earth was accompanied by profound environmental, climatic and biological change. This project will clarify the complex interactions between the rise in atmospheric oxygen and changes in the Earth's surface environment, extreme climate change and biospheric evolution.
Precise global time scale for the oxidation of Earth's atmosphere between 2.6 and 2.0 billion years ago. The rock record from 2600 to 2000 million years ago preserves evidence for dramatically fluctuating greenhouse and icehouse climates at the same time as, and possibly caused by, change from an oxygen-deficient to an oxygen-rich atmosphere. Although the global changes are well-documented, correlation of their timing and duration between continents is poorly constrained. This project aims to re ....Precise global time scale for the oxidation of Earth's atmosphere between 2.6 and 2.0 billion years ago. The rock record from 2600 to 2000 million years ago preserves evidence for dramatically fluctuating greenhouse and icehouse climates at the same time as, and possibly caused by, change from an oxygen-deficient to an oxygen-rich atmosphere. Although the global changes are well-documented, correlation of their timing and duration between continents is poorly constrained. This project aims to redress that problem by producing a precise calibration of the global changes by analysis of the rock records in Australia, Canada and South Africa. It will provide a much needed time framework within which long-term feedback between atmospheric composition and climate can be understood.Read moreRead less