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
MACQUARIE ISLAND: A UNIQUE WINDOW INTO THE OCEAN BASEMENT AND THE LINK BETWEEN OCEAN RIDGES AND OPHIOLITES. Knowledge about the composition and structure of the oceanic crust is limited due to the inaccessibility of the deep-ocean floor. Macquarie Island is the only fragment of ocean crust and mantle exposed above sea-level in the world, providing a unique opportunity to study processes of oceanic floor generation in-situ. Our project will carry out detailed mapping of the lower crust and mantle ....MACQUARIE ISLAND: A UNIQUE WINDOW INTO THE OCEAN BASEMENT AND THE LINK BETWEEN OCEAN RIDGES AND OPHIOLITES. Knowledge about the composition and structure of the oceanic crust is limited due to the inaccessibility of the deep-ocean floor. Macquarie Island is the only fragment of ocean crust and mantle exposed above sea-level in the world, providing a unique opportunity to study processes of oceanic floor generation in-situ. Our project will carry out detailed mapping of the lower crust and mantle sections on the island, followed by an integrated microstructural, petrological, and geochronological analysis of samples. Such investigations may lead to fundamental advances in the understanding of formation, deformation, and emplacement of oceanic crust at mid-ocean ridge spreading centres.Read moreRead less
Crustal Stress Field of SE Asia. The key project benefit is to advance our fundamental understanding of tectonic processes such as sedimentary basin development and continental collision. It has major implications for natural hazard assessment and resources exploration in SE Asia, consistent with Australia's participation in the APEC Energy Working Group. The project has major ancillary benefits. It will strengthen international links between Australia, SE Asia, the UK, USA and Germany. It will ....Crustal Stress Field of SE Asia. The key project benefit is to advance our fundamental understanding of tectonic processes such as sedimentary basin development and continental collision. It has major implications for natural hazard assessment and resources exploration in SE Asia, consistent with Australia's participation in the APEC Energy Working Group. The project has major ancillary benefits. It will strengthen international links between Australia, SE Asia, the UK, USA and Germany. It will provide high-quality research and training experience for the APD and PhD student involved, whom will spend time with research groups and oil companies in Australia, UK, USA and SE Asia. Finally, the project will increase the institutional capacity for contract research in SE Asia.Read moreRead less
Neoproterozoic global geodynamic and climatic events: were they linked? This project will study a unique cluster of global geodynamic and climatic events 850-700 million years ago that will help us to understand the interactions between the Earth's deep mantle, its crust, and its atmospheric climate. Academic values aside, the work will bring direct benefit to the Australian industry. Knowledge on the distribution of the Neoproterozoic plume events will provide new exploration targets for Ni-Cu- ....Neoproterozoic global geodynamic and climatic events: were they linked? This project will study a unique cluster of global geodynamic and climatic events 850-700 million years ago that will help us to understand the interactions between the Earth's deep mantle, its crust, and its atmospheric climate. Academic values aside, the work will bring direct benefit to the Australian industry. Knowledge on the distribution of the Neoproterozoic plume events will provide new exploration targets for Ni-Cu-PGE and V-Ti deposits. Better constrained palaeogeography will help to locate mineral-rich crustal provinces that were once connected. Understanding climatic consequences of global geodynamic events will help to better understand and respond to climate changes. Read moreRead less
Defects and Deformation in Olivine: From Molecules to Mantle. This project establishes the role of hydrogen in controlling olivine deformation, plate tectonics and mantle geodynamics. The unique application of innovative nanoscale simulation, microscale observation and geophysical characterisation ensures that results will have far-reaching impact in the Australian and International Earth Science community. In particular, our results will enable greater understanding of water migration in the m ....Defects and Deformation in Olivine: From Molecules to Mantle. This project establishes the role of hydrogen in controlling olivine deformation, plate tectonics and mantle geodynamics. The unique application of innovative nanoscale simulation, microscale observation and geophysical characterisation ensures that results will have far-reaching impact in the Australian and International Earth Science community. In particular, our results will enable greater understanding of water migration in the mantle, the formation of deep Earth mineral resources and lead to significant improvements in the interpretation of geophysical variations in Earth's lithosphere.Read moreRead less
The Early Stages of Granite Evolution: Extraction and Transport Through Ductile Crust . This research is aimed at understanding how the continents develop through several stages of rock melting. Rock melts deep in the continents to form granite magmas which rise, transporting to the upper crust important metals, such as gold, copper and tin, and heat producing elements such as uranium, thorium and potassium. This research proposal seeks to understand how granite melts form and rise transporting ....The Early Stages of Granite Evolution: Extraction and Transport Through Ductile Crust . This research is aimed at understanding how the continents develop through several stages of rock melting. Rock melts deep in the continents to form granite magmas which rise, transporting to the upper crust important metals, such as gold, copper and tin, and heat producing elements such as uranium, thorium and potassium. This research proposal seeks to understand how granite melts form and rise transporting these all important elements, which control not only our wealth but also the stability of the continents we live in.Read moreRead less
Longshore Sediment Supply to the Deep Ocean. The current model to supply sand to deep water off continental margins is that provided by rivers operating at low sea level. We propose an alternative model in which sand is provided by longshore transport to deep water at high sea level north of Fraser Island, SE Queensland. Here we will test the validity of our new model by site studies of sea bottom morphology, composition and dynamics. If the model proves true, we will have: 1) generated an entir ....Longshore Sediment Supply to the Deep Ocean. The current model to supply sand to deep water off continental margins is that provided by rivers operating at low sea level. We propose an alternative model in which sand is provided by longshore transport to deep water at high sea level north of Fraser Island, SE Queensland. Here we will test the validity of our new model by site studies of sea bottom morphology, composition and dynamics. If the model proves true, we will have: 1) generated an entirely new exploration model for deepwater hydrocarbons, 2) provided new expertise and seabed maps for generating a superior marine naval defence capability.Read moreRead less
Understanding the Sibao Orogenic Belt in South China: A Part of the Rodinian Supercontinent Assembly Adjacent to Australia. The Sibao Orogenic Belt (SOB) in South China is regarded as one of the worldwide 1300-1000 Ma mountain belts that record the assembly of the supercontinent Rodinia. However, recent work suggests that some of these mountain belts, including the SOB, were probably active until 900 Ma, thus questioning parts of the early Rodinia reconstructions. In this study we aim to deter ....Understanding the Sibao Orogenic Belt in South China: A Part of the Rodinian Supercontinent Assembly Adjacent to Australia. The Sibao Orogenic Belt (SOB) in South China is regarded as one of the worldwide 1300-1000 Ma mountain belts that record the assembly of the supercontinent Rodinia. However, recent work suggests that some of these mountain belts, including the SOB, were probably active until 900 Ma, thus questioning parts of the early Rodinia reconstructions. In this study we aim to determine the ages, and geochemical and structural characteristics of key tectonic units in the SOB. This will lead to a better understanding of the assembly process of Rodinia, and events occurring in continental blocks adjacent to Australia at that time.Read moreRead less
Reconstruction of marine ecosystems following the greatest mass extinction during the Phanerozoic history of Earth life: Lessons for the present. Frequent defaunation events strongly threaten sustainable development of marine resources and human environments especially in countries that are surrounded by oceans such as Australia. By analysing recovery mechanisms of marine ecosystems following the Permian-Triassic mass extinction, the greatest crisis of Earth life, we will develop predictive tool ....Reconstruction of marine ecosystems following the greatest mass extinction during the Phanerozoic history of Earth life: Lessons for the present. Frequent defaunation events strongly threaten sustainable development of marine resources and human environments especially in countries that are surrounded by oceans such as Australia. By analysing recovery mechanisms of marine ecosystems following the Permian-Triassic mass extinction, the greatest crisis of Earth life, we will develop predictive tools for analysing restoration of modern marine defaunated ecosystems. Understanding biotic extinction and recovery is crucial to understanding the evolution of the Earth's biosphere. This study increases Australia's research profile on this global issue. The target strata are quality oil source rocks in Perth Basin, and thus this project is beneficial to the Australian petroleum industry.Read moreRead less
Extinction and survival: biotic responses to environmental change in Late Devonian oceans during a greenhouse-icehouse transition. This project represents an important opportunity to answer fundamental questions about the role of environmental changes in major mass extinction events in the geological past and to provide insight into the survival of modern marine species in response to climate change (National Research Priority 1). It will enhance Australia's global research profile in biostratig ....Extinction and survival: biotic responses to environmental change in Late Devonian oceans during a greenhouse-icehouse transition. This project represents an important opportunity to answer fundamental questions about the role of environmental changes in major mass extinction events in the geological past and to provide insight into the survival of modern marine species in response to climate change (National Research Priority 1). It will enhance Australia's global research profile in biostratigraphical and palaeontological research through contribution to the development of biozonations, correlation and global debate on extinction mechanisms. It will also strengthen international collaboration, and, importantly, provide crucial research training to young researchers in these fields.Read moreRead less