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Research Topic : variability
Field of Research : Geochemistry
Field of Research : Palaeoclimatology
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Geochemistry (7)
Palaeoclimatology (7)
Isotope Geochemistry (5)
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Inorganic Geochemistry (1)
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Effects of Climate Change and Variability on Australia (excl. Social Impacts) (4)
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  • Researchers (51)
  • Funded Activities (7)
  • Organisations (26)
  • Funded Activity

    Discovery Projects - Grant ID: DP110105419

    Funder
    Australian Research Council
    Funding Amount
    $540,000.00
    Summary
    Australian dust: its response to, and role in, climate change. Atmospheric dust plumes can affect global climate, but the impact of Australian dust on climate is poorly known even though it is a major dust source. This project will study the magnetism of dust deposits in marine sediments to understand how Australian dust influences climate in order to better predict the influence of humans on future climate.
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    Funded Activity

    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.
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    Funded Activity

    ARC Future Fellowships - Grant ID: FT160100259

    Funder
    Australian Research Council
    Funding Amount
    $776,000.00
    Summary
    Deep-sea coral ocean-climate records of the last glacial and recent eras. The project aims to predict the ocean carbon dioxide sink’s long-term capacity and future trajectories of global warming and increasing carbon dioxide. This project will use geochemical proxies encoded in the skeletons of deep-sea corals in the Perth Canyon, Tasman seas, and Antarctica, in the heart of the ocean-climate system, to reveal continuous long-term records of environmental change at annual-decadal resolution for .... Deep-sea coral ocean-climate records of the last glacial and recent eras. The project aims to predict the ocean carbon dioxide sink’s long-term capacity and future trajectories of global warming and increasing carbon dioxide. This project will use geochemical proxies encoded in the skeletons of deep-sea corals in the Perth Canyon, Tasman seas, and Antarctica, in the heart of the ocean-climate system, to reveal continuous long-term records of environmental change at annual-decadal resolution for our recent past (hundreds to thousands of years) and the Last Glacial Maximum. These records are expected to provide a more accurate understanding of Earth’s long-term responses to anthropogenic carbon dioxide emissions and global warming.
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    Funded Activity

    ARC Future Fellowships - Grant ID: FT110100793

    Funder
    Australian Research Council
    Funding Amount
    $714,418.00
    Summary
    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.
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    Active Funded Activity

    Discovery Projects - Grant ID: DP210100508

    Funder
    Australian Research Council
    Funding Amount
    $476,000.00
    Summary
    Fire and rain: Drivers of deep-time ecosystem assembly in Australia. This project aims to investigate the influence of bushfires and shifting rainfall patterns on the development of Australia’s dominant ecosystems. By combining a range of novel geochemical, isotopic and palaeontological techniques, this research seeks to reveal the causes and consequences of Australia’s transformation from a forested to mainly open landscape of grassland, shrubland and savannah. The expected outcome is detailed .... Fire and rain: Drivers of deep-time ecosystem assembly in Australia. This project aims to investigate the influence of bushfires and shifting rainfall patterns on the development of Australia’s dominant ecosystems. By combining a range of novel geochemical, isotopic and palaeontological techniques, this research seeks to reveal the causes and consequences of Australia’s transformation from a forested to mainly open landscape of grassland, shrubland and savannah. The expected outcome is detailed knowledge of how changes in fire and rain shaped the ecology and evolution of plants and animals. This knowledge is key to understanding how Australian ecosystems function and to protecting their cultural, economic and environmental values, especially as climate and fire regimes continue to change into the future.
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    Funded Activity

    Discovery Early Career Researcher Award - Grant ID: DE120102504

    Funder
    Australian Research Council
    Funding Amount
    $375,000.00
    Summary
    Old stalagmites, new techniques: South African palaeoclimate records linked to early human evolution. Caves in South Africa preserve a rich hominin (early human) fossil and archaeological record dating back over two million years. This project uses stalagmites from various South African caves to provide a new, detailed record of the palaeoclimate, forming the backdrop to the evolutionary changes that took place during this period.
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    Funded Activity

    Discovery Projects - Grant ID: DP120100104

    Funder
    Australian Research Council
    Funding Amount
    $270,000.00
    Summary
    Were abrupt changes in the Precambrian global carbon cycle the trigger for animal appearance and radiation on Earth? The origin of complex life and the properties that allow that life to be sustained on this planet are recorded within the geologic record. This project will reveal the role that severe perturbations of the global carbon cycle and climate had in triggering the step-wise change to animal life after billions of years of only single cell organisms.
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