Mantle evolution and the origin of Earth's atmosphere. This project aims to investigate Earth’s early evolution and the origin of our atmosphere. Using state-of-the-art instrumentation the project will measure noble gas and tungsten isotopes in unique volcanic glasses that record the composition of the Earth’s mantle. These measurements are expected to clarify the relationship between the formation of Earth’s atmosphere, mantle and core, and to generate new knowledge about convective currents ....Mantle evolution and the origin of Earth's atmosphere. This project aims to investigate Earth’s early evolution and the origin of our atmosphere. Using state-of-the-art instrumentation the project will measure noble gas and tungsten isotopes in unique volcanic glasses that record the composition of the Earth’s mantle. These measurements are expected to clarify the relationship between the formation of Earth’s atmosphere, mantle and core, and to generate new knowledge about convective currents in the modern mantle. The project aims to train the next generation of Earth scientists and to provide new knowledge to assist in overcoming the challenges in mitigating climate change and sustaining a resource-based economy.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE220101017
Funder
Australian Research Council
Funding Amount
$456,000.00
Summary
Assessing the vulnerability of East Antarctica to future warming. This DECRA aims to address major gaps in our understanding of how the Antarctic Ice Sheet will respond to climate change, by enabling critical insights on its sensitivity to past climate warming. The project will apply a suite of geochemical approaches to determine – for East Antarctica’s most vulnerable basin – the extent of ice-sheet loss during past warming, and the impact of glacial meltwater on biological productivity and Sou ....Assessing the vulnerability of East Antarctica to future warming. This DECRA aims to address major gaps in our understanding of how the Antarctic Ice Sheet will respond to climate change, by enabling critical insights on its sensitivity to past climate warming. The project will apply a suite of geochemical approaches to determine – for East Antarctica’s most vulnerable basin – the extent of ice-sheet loss during past warming, and the impact of glacial meltwater on biological productivity and Southern Ocean circulation. New knowledge of how the ice sheet and ocean respond to climate warming, will lead to more reliable projections of future sea-level rise and climate. The DECRA will benefit Australia by providing a strong evidence base for policy decision-making to manage the impact of sea-level rise.Read moreRead less
Novel dating methods for marine sediments of relevance to determining past climate changes. Future climate change is a subject of enormous contemporary interest with economic and social implications for much of humanity. Accurate knowledge of past climates is, however, crucial to understanding how the global climate will evolve into the future. This proposal aims to develop novel methods for dating marine sediments using cosmogenic isotopes, in order to extract the palaeoclimatic signals that ar ....Novel dating methods for marine sediments of relevance to determining past climate changes. Future climate change is a subject of enormous contemporary interest with economic and social implications for much of humanity. Accurate knowledge of past climates is, however, crucial to understanding how the global climate will evolve into the future. This proposal aims to develop novel methods for dating marine sediments using cosmogenic isotopes, in order to extract the palaeoclimatic signals that are locked into these sediments. We will concentrate on the Southern Ocean which plays a crucial role in the world's climate. This proposal will also contribute to Australia's international obligation to conduct research in this critical area.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE160100443
Funder
Australian Research Council
Funding Amount
$393,434.00
Summary
Resolving nutrient groundwater exports versus soil burial in mangroves. This project aims to examine the role of mangroves in the sequestration and burial of nutrients. Coastal areas increasingly receive enriched nutrient loads, driving anthropogenic eutrophication. Mangrove wetlands naturally filter and bury large quantities of nutrients through soil accretion. This project aims to quantify nutrient groundwater export as related to mangrove soil nutrient retention and determine if these wetland ....Resolving nutrient groundwater exports versus soil burial in mangroves. This project aims to examine the role of mangroves in the sequestration and burial of nutrients. Coastal areas increasingly receive enriched nutrient loads, driving anthropogenic eutrophication. Mangrove wetlands naturally filter and bury large quantities of nutrients through soil accretion. This project aims to quantify nutrient groundwater export as related to mangrove soil nutrient retention and determine if these wetlands have the potential to provide negative feedback to coastal eutrophication. The project plans to use state-of-the-art radionuclide tracer technology to quantify the relationship between groundwater discharge and historical soil nutrient retention.Read moreRead less
Holding coral reefs together with soluble cement. This project aims to characterise and understand cement formation in coral reefs. Coral reefs are constructed by cementing together aragonite building blocks made by corals. The main cementing agent is high-magnesium calcite, the most soluble carbonate mineral and susceptible to ocean acidification. High-magnesium calcite cements are best developed on the high energy margins of coral reefs. This project will quantify how crustose coralline algae ....Holding coral reefs together with soluble cement. This project aims to characterise and understand cement formation in coral reefs. Coral reefs are constructed by cementing together aragonite building blocks made by corals. The main cementing agent is high-magnesium calcite, the most soluble carbonate mineral and susceptible to ocean acidification. High-magnesium calcite cements are best developed on the high energy margins of coral reefs. This project will quantify how crustose coralline algae produces high-magnesium calcite and controls the dissolution and reprecipitation of high-magnesium cements. This project intends to quantify rates of reef cementation, susceptibility to ocean acidification and warming, and possible mitigating effects of alkalinity addition.Read moreRead less
The recovery of seagrass beds: the role of catchments and options for management responses. Seagrass beds once dominated tidal flats but are disappearing at an increasing rate due to human actions, both in Australia and around the world. This project will develop an understanding of the processes that cause these losses, the factors that prevent seagrass-bed re-establishment, and provide a framework for evaluating alternative management options.
Australian Laureate Fellowships - Grant ID: FL120100050
Funder
Australian Research Council
Funding Amount
$3,079,069.00
Summary
Sea level change and climate sensitivity. This project will aim to improve understanding of climate and sea-level change on timescales relevant to longer-term planning, by characterising the relationship between past sea-level/ice-volume change and other key climate factors such as temperature and greenhouse gases, and by quantifying how rapidly sea level may adjust to climate change.
Dissolution of CaCO3 in sediments in an acidifying ocean. Dissolution of calcium carbonate (CaCO3) in sediments in the context of ocean acidification is poorly understood. This project will use in situ advective benthic chamber incubations and experimental manipulations under future ocean acidification scenarios to determine the controls on the dissolution of CaCO3 in sediments. This project is significant because changes in the dissolution of CaCO3 in sediments in an acidifying ocean are at lea ....Dissolution of CaCO3 in sediments in an acidifying ocean. Dissolution of calcium carbonate (CaCO3) in sediments in the context of ocean acidification is poorly understood. This project will use in situ advective benthic chamber incubations and experimental manipulations under future ocean acidification scenarios to determine the controls on the dissolution of CaCO3 in sediments. This project is significant because changes in the dissolution of CaCO3 in sediments in an acidifying ocean are at least as important, and potentially more important, than calcification to the future accretion and survival of carbonate ecosystems. It is expected that outcomes of this project will significantly advance our understanding of the drivers of the dissolution of CaCO3 in sediments and the functioning of globally important carbonate ecosystems.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE140100141
Funder
Australian Research Council
Funding Amount
$360,000.00
Summary
High sensitivity and precision mass spectrometry for tracing Australia's ancient evolution and securing our future groundwater resources. High sensitivity and precision mass spectrometry for tracing Australia’s ancient evolution and securing our future groundwater resources: Micro-sampling thermal ionisation mass spectrometry (TIMS) provides the ability to undertake ultra low-level isotope analysis of earth and environmental samples. Analysis of radiogenic (for example, Neodymium, Strontium and ....High sensitivity and precision mass spectrometry for tracing Australia's ancient evolution and securing our future groundwater resources. High sensitivity and precision mass spectrometry for tracing Australia’s ancient evolution and securing our future groundwater resources: Micro-sampling thermal ionisation mass spectrometry (TIMS) provides the ability to undertake ultra low-level isotope analysis of earth and environmental samples. Analysis of radiogenic (for example, Neodymium, Strontium and Lead) and stable (for example, Boron) isotopes allows researchers to trace the evolution of the Australian continent from its beginnings in the Precambrian through to the impacts of climate change in the Quaternary period (the last 2.6 million years). The proposed micro-sampling TIMS facility will give researchers the opportunity to characterise mineral deposit formation, paleoclimate records and groundwater sources with new levels of accuracy and precision. This will help secure the economic and environmental future of Australia.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE110100045
Funder
Australian Research Council
Funding Amount
$370,000.00
Summary
A mass spectrometer to analyse carbonate isotope records of Australia's climate, soil and groundwater history. Water is a critical resource in Australia, yet there is a fundamental lack of knowledge about the causes and timing of groundwater recharge in the past. This facility will allow researchers to better understand climate and groundwater interactions through high resolution isotope analysis of deposits, such as cave stalagmites and marine corals.