Sedimentary phosphorites as geochemical sponges: trace element scavenging, the chemical evolution of seawater and an innovative method for dating sediments. Ancient sedimentary phosphorite is the major source of commercial phosphate in Australia and East Asia. This project will lead to economic and environmental benefits to Australia by providing the minerals industry with the tools to target purer phosphate, thus improving resource estimations and minimising the environmental impact of trace me ....Sedimentary phosphorites as geochemical sponges: trace element scavenging, the chemical evolution of seawater and an innovative method for dating sediments. Ancient sedimentary phosphorite is the major source of commercial phosphate in Australia and East Asia. This project will lead to economic and environmental benefits to Australia by providing the minerals industry with the tools to target purer phosphate, thus improving resource estimations and minimising the environmental impact of trace metal burdened fertiliser. The study will enhance our understanding of the nature and timing of key moments in Earth history and could serve as a launchpad for future studies on the use of phosphate for environmental remediation. We hope to provide exciting opportunities for Australian postgraduates through cutting edge research in partnership with both homespun and international academic collaborators.Read moreRead less
Crustal-Scale Fluid Flow in Deep Intracontinental Settings: Conditions, Sources and Deformational Responses. Fluids are important agents of heat and mass transport in the Earth's crust. They play a key role in the mobilisation of metals and as such play a crucial role in the generation of ore deposits. The outcomes of this project will result in a greater understanding of the mechanisms and sources of fluid generation and mobilisation in deep-crustal settings. These outcomes can be related direc ....Crustal-Scale Fluid Flow in Deep Intracontinental Settings: Conditions, Sources and Deformational Responses. Fluids are important agents of heat and mass transport in the Earth's crust. They play a key role in the mobilisation of metals and as such play a crucial role in the generation of ore deposits. The outcomes of this project will result in a greater understanding of the mechanisms and sources of fluid generation and mobilisation in deep-crustal settings. These outcomes can be related directly to the understanding of the controls on the transport and deposition of metals and hence the formation of mineral resources which are vital to maintaining a strong Australian economy.Read moreRead less
Biogeochemical characterisation of Archaean microfossils, biomarkers and organic matter: Probing the nature and diversity of early life on Earth. Recognizing biological signatures in ancient rocks poses the single greatest challenge to our understanding of the origin and evolution of life. This Project will use new advanced technology to reveal when and where life first appeared and assess its impact on the environment, atmosphere and climate. Results are essential for understanding the transfor ....Biogeochemical characterisation of Archaean microfossils, biomarkers and organic matter: Probing the nature and diversity of early life on Earth. Recognizing biological signatures in ancient rocks poses the single greatest challenge to our understanding of the origin and evolution of life. This Project will use new advanced technology to reveal when and where life first appeared and assess its impact on the environment, atmosphere and climate. Results are essential for understanding the transformation of our planet into a suitable habitat for humankind. The work will place Australia among world leaders in one of the most exciting topics of current scientific research, raising Australia's reputation in this high profile and competitive field. The Project tackles profound questions and seeks to attract, inspire and train future scientists in an ideal location and research environment.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE0560725
Funder
Australian Research Council
Funding Amount
$127,042.00
Summary
Enhancing the Monash-VIEPS Stable Isotope Facility. This proposal is to enhance the Monash-Victorian Institute of Earth and Planetary Sciences (VIEPS) Stable Isotope Facility to expand our capacity for state-of-the-art research in hydrogeology, hydrology, aqueous chemistry, modern and palaeoclimatology, sedimentology, geochemistry, economic geology, and biological sciences. This facility will then have an analytical capability that is at least the equal of those elsewhere in Australia and which ....Enhancing the Monash-VIEPS Stable Isotope Facility. This proposal is to enhance the Monash-Victorian Institute of Earth and Planetary Sciences (VIEPS) Stable Isotope Facility to expand our capacity for state-of-the-art research in hydrogeology, hydrology, aqueous chemistry, modern and palaeoclimatology, sedimentology, geochemistry, economic geology, and biological sciences. This facility will then have an analytical capability that is at least the equal of those elsewhere in Australia and which will maintain our position as a World Class stable isotope research facility. The enhanced facility will permit new research to be carried out that will lead to new collaborations both within the traditional Earth Sciences and across disciplines.Read moreRead less
Stable isotopic studies and isotopic dating, Woodleigh Impact Structure, Western Australia: implications for the Late Devonian mass extinction. The 120 km diameter Woodleigh impact structure in the Carnarvon Basin, Western Australia is the third largest Phanerozoic impact structure. K-Ar dating of impact-induced alteration minerals indicates a Late Devonian age for Woodleigh. The precise timing of impact, nature of the impacting body and processes responsible for redistribution of meteoritic com ....Stable isotopic studies and isotopic dating, Woodleigh Impact Structure, Western Australia: implications for the Late Devonian mass extinction. The 120 km diameter Woodleigh impact structure in the Carnarvon Basin, Western Australia is the third largest Phanerozoic impact structure. K-Ar dating of impact-induced alteration minerals indicates a Late Devonian age for Woodleigh. The precise timing of impact, nature of the impacting body and processes responsible for redistribution of meteoritic components will be investigated using a range of analytical methodologies. A search will be made for impact-related sedimentary deposits to see if an extraterrestrial component can be identified and correlated with Woodleigh. The expected outcome is proof of an impact-extinction connection for the Late Devonian mass extinction, one of the largest in Earth history.Read moreRead less
Rates of metamorphic processes - correlating U-Pb ages with the pressure-temperature conditions of mineral growth. To determine the speed of metamorphic processes, the age obtained from accessory uranium-bearing minerals will be correlated to pressure and temperature obtained from major rock forming minerals. I will develop a new and innovative technique that uses trace element geochemistry to provide this link. The trace element partitioning between datable minerals (zircon, monazite and titani ....Rates of metamorphic processes - correlating U-Pb ages with the pressure-temperature conditions of mineral growth. To determine the speed of metamorphic processes, the age obtained from accessory uranium-bearing minerals will be correlated to pressure and temperature obtained from major rock forming minerals. I will develop a new and innovative technique that uses trace element geochemistry to provide this link. The trace element partitioning between datable minerals (zircon, monazite and titanite) and key metamorphic minerals will be investigated in natural samples and in piston cylinder experiments. I will apply this technique to the study of processes such as the exhumation of eclogites in subduction zones and the duration of granulite-facies metamorphism in lower crustal rocks.Read moreRead less
Continental temperature and rainfall change during past global warming - a multiproxy approach involving clumped isotopes in speleothems. Global climate simulation and prediction models depend on accurate and quantitative measurements of key climatic parameters such as temperature and rainfall, and their temporal changes and spatial distributions. Our research will combine the revolutionary clumped isotope thermometry with other climatic proxies archived in stalagmites to quantify temperature an ....Continental temperature and rainfall change during past global warming - a multiproxy approach involving clumped isotopes in speleothems. Global climate simulation and prediction models depend on accurate and quantitative measurements of key climatic parameters such as temperature and rainfall, and their temporal changes and spatial distributions. Our research will combine the revolutionary clumped isotope thermometry with other climatic proxies archived in stalagmites to quantify temperature and rainfall changes in Australia and China during the past two major episodes of global warming (Terminations I and II). This pilot project directly addresses national research priority goals 'Water - a critical resource', 'Responding to climate change and variability', provide an excellent platform for cross-institutional research training and enhance scientific exchange with China.Read moreRead less
Proterozoic crustal evolution of the Northern Australian Craton revealed from hafnium-oxygen isotope systematics of granite-hosted and detrital zircons. This project will provide an detailed view of continental crust formation during a key period of Earth's history. Through an innovative approach and the use of sophisticated micro-analytical techniques, it will enhance the profile and global competitiveness of Australian research. The project is an integral part of a national collaboration on Pr ....Proterozoic crustal evolution of the Northern Australian Craton revealed from hafnium-oxygen isotope systematics of granite-hosted and detrital zircons. This project will provide an detailed view of continental crust formation during a key period of Earth's history. Through an innovative approach and the use of sophisticated micro-analytical techniques, it will enhance the profile and global competitiveness of Australian research. The project is an integral part of a national collaboration on Proterozoic terranes involving universities, Geoscience Australia and state geological surveys, and datasets generated by this study can potentially lead to refined mineral exploration strategies. The project is linked to the development of a major new analytical facility at James Cook University that will support local and international research and research training.Read moreRead less
Sources and processes in the early solar system - an isotopic study. Our solar system formed over 4.5 billion years ago. We aim to develop techniques that will allow us to determine the sequence of events that led to our planetary system with unprecedented detail. The same techniques can be applied to dating geological events, for example, correlating ore-forming events and dating opal formation. This project utilizes new Australian technologies that will have potential economic benefits both ....Sources and processes in the early solar system - an isotopic study. Our solar system formed over 4.5 billion years ago. We aim to develop techniques that will allow us to determine the sequence of events that led to our planetary system with unprecedented detail. The same techniques can be applied to dating geological events, for example, correlating ore-forming events and dating opal formation. This project utilizes new Australian technologies that will have potential economic benefits both in instrument sales and applications.Read moreRead less
Improving climate models through new insights on long-term inter-hemispheric climate synchronicity from speleothems. It is important that palaeoclimatologists continue to improve understanding of how the Earth responds to climate forcing, so that climate models can be rigorously validated and refined. Since the Earth responds to most of this forcing over time scales that exceed the length of instrumental weather measurements, the recovery of datable palaeoclimate archives that are highly sensiti ....Improving climate models through new insights on long-term inter-hemispheric climate synchronicity from speleothems. It is important that palaeoclimatologists continue to improve understanding of how the Earth responds to climate forcing, so that climate models can be rigorously validated and refined. Since the Earth responds to most of this forcing over time scales that exceed the length of instrumental weather measurements, the recovery of datable palaeoclimate archives that are highly sensitive to past climate changes is essential. Our project will provide important new palaeoclimate data from both hemispheres on how key regions of the Earth responded to past climate changes. This will bring improved understanding of past oceanic-atmospheric processes that can be fed into climate models, ultimately producing better forecasts to the benefit of all Australians.Read moreRead less