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Accounting for an approximate tenth of the Earth’s land surface, Antarctica stores about 70% of the world’s freshwater (29.46 million km) in the form of ice which covers 90% of its continental surface (Fretwell et al. 2013; Kennicut et al., 2014). During climatic transitions, mechanisms related to melting or fracturing destabilize the voluminous Western/ Eastern Antarctic Ice-sheets (WAIS/EAIS) and their freshwater stores are released, further increasing sea-level and destabilizing ice-sheets (Bamber et al., 2013; Favier et al., 2014).

SEDIMENT RECORDS OF ICE-SHEET INSTABILITY AT ODP SITE 697 (JANE BASIN), NW WEDDELL SEA, SOUTH ORKNEY MICROCONTINENT