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Weekly fast-ice and snow thicknesses from an ongoing long-term time-series together with meteorological data will be used to analyse ice-atmosphere interactions. Interannual changes will be studied for climate effects.
To effectively monitor human imapcts on subantarctic ecosystems, in particular the introduction of new ‘pest’ species, long-term monitoring programs must be set in place.
This is a cooperative project with the Ohio State University (OSU) and the United States Geological Survey (USGS).The project will establish a GPS deformation network along the Transantarctic Mountains in the eastern sector of the AAT.
The aim of this project is to determine the biodiversity of Antarctica microorganisms. Environmental samples will be used to grow microbes which will then be tested for their nitrogen fixation capability and other growth characteristics involved in adaptation.
Although oceanic crust covers about 60% of the Earth, relatively little is known of its geology and the processes that have created it. Macquarie Island represents a unique subaerial exposure of the seafloor, and an exceptional environment for active study and research into the ocean crust.
Marine Plain at Vestfold Hills, contains a unique record of sea level, climate and glacial history within its sediments and microfossils. Coring of the deeper sediments will reveal how this part of coastal east Antarctica changed during the Neogene (26 million years-the present).
Plants from herbarium collections dating back to the 19th century will be compared with recent collections to gain an understanding of ecosystems responses to global change.
Three soil animals, a land shrimp, a slater and a flat worm, were all introduced to Macquarie Island early last century. The three species were probably imported accidentally with sealers and their supplies from New Zealand.
Heard Island offers scientists a unique subantarctic laboratory for investigating climate change.
This project seeks to monitor Holocene-Quaternary variability of Antarctic bottom water outflow at a known deep pathway (east flank of Kerguelen Plateau) into a major ocean basin.