Discovery Early Career Researcher Award - Grant ID: DE120100030
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
The role of Antarctic sea ice as a natural ocean fertiliser. This project will assess the importance of sea ice as a natural fertiliser in the climatically important polar region. The knowledge gained will aid climate modellers and Governmental policy-makers concerned with the commercial use of ocean iron fertilisation as an attempt to reduce human-induced atmospheric carbon dioxide and gain carbon credits.
Ocean fertilisation: a positive effect from Antarctica’s great thaw? This project will evaluate how the Antarctica's great thaw may fertilise the Southern Ocean with iron and help mitigate carbon dioxide emissions now and in the future. The Southern Ocean is anaemic, meaning that the iron levels are too low to sustain photosynthesis, a pathway by which the oceans transform carbon dioxide into carbon-rich sediments. There is evidence that melting ice may supply substantial amount of iron, capable ....Ocean fertilisation: a positive effect from Antarctica’s great thaw? This project will evaluate how the Antarctica's great thaw may fertilise the Southern Ocean with iron and help mitigate carbon dioxide emissions now and in the future. The Southern Ocean is anaemic, meaning that the iron levels are too low to sustain photosynthesis, a pathway by which the oceans transform carbon dioxide into carbon-rich sediments. There is evidence that melting ice may supply substantial amount of iron, capable of boosting marine life and removing carbon dioxide. As polar regions show the earliest and most severe impacts of anthropogenic activity, studying ice-ocean interactions is central to supporting national and international policy development that can effectively limit the worst impacts of climate change globally. Read moreRead less
Dating West Antarctic ice sheet collapse using molecular sequence data. This project aims to investigate the past stability and configuration of the West Antarctic Ice Sheet by examining genomic signatures in present day bottom-dwelling Antarctic marine animals. By employing this novel biological approach this project will provide an independent test of the hypothesis that the West Antarctic Ice Sheet collapsed during the most recent interglacial period and formed a trans-Antarctic seaway. Expec ....Dating West Antarctic ice sheet collapse using molecular sequence data. This project aims to investigate the past stability and configuration of the West Antarctic Ice Sheet by examining genomic signatures in present day bottom-dwelling Antarctic marine animals. By employing this novel biological approach this project will provide an independent test of the hypothesis that the West Antarctic Ice Sheet collapsed during the most recent interglacial period and formed a trans-Antarctic seaway. Expected project outcomes include increased resolution of the most recent collapse of the West Antarctic Ice Sheet. This project should provide benefits in predicting future ice sheet collapse and its impact on sea level rise, which is a key uncertainty resulting from climate change.Read moreRead less