Linkage Infrastructure, Equipment And Facilities - Grant ID: LE120100180
Funder
Australian Research Council
Funding Amount
$150,000.00
Summary
An Australian fluid-inclusion facility for climate-change science. Understanding past temperature and rainfall changes is essential for improving climate projections. The proposed facility will generate new palaeotemperature and palaeorainfall information from cave deposits, leading to a better understanding of natural climate variability and change.
Palaeoclimate reconstructions from the isotopic signatures of fossilised leaf waxes. This project develops a method for using the chemical signature of fossilised leaf waxes to reconstruct hydrologic change in south-eastern Australia during the Holocene (last 10,000 years) and Eocene (56-34 million years ago). Understanding climate in the geologic past is essential for testing models and projecting future climate with rising carbon dioxide.
Are subterranean estuaries a source or sink of greenhouse gases? The aim of this project is to investigate the role of subterranean estuaries and submarine groundwater discharge on the marine cycle of the greenhouse gases carbon dioxide, methane, and nitrous oxide. The expected outcome of this project is a better understanding of the role of coastal environments as a net source or sink of greenhouse gases.
The application of clumped isotope thermometry to the terrestrial environment. Clumped-isotope geochemistry, a novel method for measuring the temperature of formation of carbonate minerals, will be applied to terrestrial materials (soil carbonates, lake deposits and speleothems) from Australia and New Zealand. The method relates the abundance or 'clumping' of rare isotopes (for example, carbon dioxide of mass 47 as carbon-13, oxygen-18, oxygen-16) extracted from carbonates to their formation tem ....The application of clumped isotope thermometry to the terrestrial environment. Clumped-isotope geochemistry, a novel method for measuring the temperature of formation of carbonate minerals, will be applied to terrestrial materials (soil carbonates, lake deposits and speleothems) from Australia and New Zealand. The method relates the abundance or 'clumping' of rare isotopes (for example, carbon dioxide of mass 47 as carbon-13, oxygen-18, oxygen-16) extracted from carbonates to their formation temperature and is independent of the oxygen-18:oxygen-16 value of the host water from which the mineral precipitated. The materials to be investigated span the Last Glacial-Interglacial Transition and will provide robust past temperature estimates and the delta-oxygen-18 values of waters, thereby permitting hydrological balances (for example, precipitation/evaporation) to be constructed. Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE150100139
Funder
Australian Research Council
Funding Amount
$160,000.00
Summary
Isotope analyser with delta17O capability to examine water fluxes. Isotope analyser with delta-17-O capability to examine water fluxes: This project aims to investigate a range of processes, including quantifying evaporative losses, moisture recycling, groundwater-surface water interactions, and records of past climate in ice cores using novel capabilities for continuous measurement of triple oxygen isotopes (16-O, 17-O, 18-O) in water vapour. Enhanced understanding of water cycles is critical f ....Isotope analyser with delta17O capability to examine water fluxes. Isotope analyser with delta-17-O capability to examine water fluxes: This project aims to investigate a range of processes, including quantifying evaporative losses, moisture recycling, groundwater-surface water interactions, and records of past climate in ice cores using novel capabilities for continuous measurement of triple oxygen isotopes (16-O, 17-O, 18-O) in water vapour. Enhanced understanding of water cycles is critical for understanding the discrete changes occurring in water regimes under changing climates and land use to efficiently manage our limited freshwater resources. The instrumentation is intended to put Australia at the forefront of new and emerging research in d17O analysis of water, an area that has potential to greatly improve our understanding of the water cycle within arid climates including Antarctica.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE180100185
Funder
Australian Research Council
Funding Amount
$464,531.00
Summary
Mass spectrometry for next generation isotope analysis of silicate minerals. This project aims to establish a facility for mass spectrometry and sample preparation to enhance Australian capacity to analyse the stable isotope composition of silicate minerals. The project seeks to implement innovations that will greatly enhance the use of stable isotopes in silicate minerals by increasing analytical throughput and reducing cost. This will provide better understanding of the trajectories of environ ....Mass spectrometry for next generation isotope analysis of silicate minerals. This project aims to establish a facility for mass spectrometry and sample preparation to enhance Australian capacity to analyse the stable isotope composition of silicate minerals. The project seeks to implement innovations that will greatly enhance the use of stable isotopes in silicate minerals by increasing analytical throughput and reducing cost. This will provide better understanding of the trajectories of environmental change, formation of mineral deposits and identifying trade networks in prehistoric societies.Read moreRead less
Southern Ocean oxygen variability since the last glacial maximum. Recently observed decreases in ocean oxygen concentration could decrease ocean biodiversity and accelerate climate change. This project will determine the links between climate change and ocean oxygenation since the last ice age, and provide a way to predict future oxygen concentrations.
Discovery Early Career Researcher Award - Grant ID: DE140101733
Funder
Australian Research Council
Funding Amount
$395,220.00
Summary
The mangrove carbon pump: Resolving the contribution of underground respiration to mangrove greenhouse gas and carbon budgets. Mangroves are considered an important global carbon sink. However, there is an imbalance of about 50 per cent in mangrove carbon budgets. This project will resolve whether advective pore water exchange and associated underground respiration represents the missing component of mangrove carbon and greenhouse gas budgets. This innovative project will examine the previously ....The mangrove carbon pump: Resolving the contribution of underground respiration to mangrove greenhouse gas and carbon budgets. Mangroves are considered an important global carbon sink. However, there is an imbalance of about 50 per cent in mangrove carbon budgets. This project will resolve whether advective pore water exchange and associated underground respiration represents the missing component of mangrove carbon and greenhouse gas budgets. This innovative project will examine the previously overlooked concept that crab burrow flushing is a major driver of biogeochemical reactions in mangroves. It will use a combination of new experimental and modelling approaches and will contribute to closing a significant gap in our understanding of the coastal carbon cycle.Read moreRead less
Australia as the world warmed: our regional response to rapid global warming events in the geological past. Projections of global climate change over the next century are so negative we must look to the Pliocene Epoch, more than 2.5 million years ago, for past analogues. Nonetheless, more recent episodes of rapid global warming during the late Pleistocene might approximate those expected for coming decades. This project will study past Australian regional temperature and rainfall responses to th ....Australia as the world warmed: our regional response to rapid global warming events in the geological past. Projections of global climate change over the next century are so negative we must look to the Pliocene Epoch, more than 2.5 million years ago, for past analogues. Nonetheless, more recent episodes of rapid global warming during the late Pleistocene might approximate those expected for coming decades. This project will study past Australian regional temperature and rainfall responses to these events, on a high-resolution absolute timescale. The necessary analytical technologies are new, meaning a study of this scope could not previously be attempted, and they will be further developed under this project. Outputs will include spatial patterns and lead/lag relationships which can be used to supplement climate model predictions for Australia.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