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Penguin populations are sensitive indicators of climate change and have fluctuated through time. Coastal Antarctic lakes near penguin rookeries contain a record of the adjacent rookery activity, locked away in the lake sediments.
This project will contribute to a revolution in our understanding of the Southern Ocean.
Global climate change will lead to a reduction in the duration and thickness of sea ice in coastal areas. We will determine whether this will lead to a decrease in primary production and food value to higher predators.
Measuring present-day glacial isostatic rebound in Antarctica will provide new observations to help constrain ice models that seek to quantify the effect on present-day sea-level rise of changes in the Antarctic Ice Sheet since the Last Glacial Maximum.
Macquarie Island represents a globally unique opportunity to examine in situ oceanic crust as it is the only subaerial exposure of non-plume-related oceanic crust that still lies within the basin in which it formed.
Pfiesteria is an unusual fish-killing dinoflagellate, best known from eutrophic North Carolina estuaries. Preliminary molecular evidence has demonstrated the presence of this organism in Ace Lake, Antarctica, which has no resident fish population.
This project will study the limnology of lakes in the Framnes Mountains near Mawson Station.
When skin is exposed to sunlight, vitamin D is produced, which is needed to maintain proper bone health. Therefore long periods of sun deprivation can have a negative effect on bone.
In this project a sea-ice model for application in Southern Ocean climate and forecasting studies will be developed to amend identified deficiencies in numerical models (i.e. unaccounted short-term dynamics; or non-suitable ice rheology).
Dating of glacial moraines in the Lambert Glacier region, East Antarctica, will reveal changes in ice thickness since about 18,000 years ago.