Submarine landslides unravel the dynamics of the past East Antarctic Ice Sheet
Póster presentado en EGU General Assembly (2024), Vienna, Austria & Online | 14–19 April 2024 A giant submarine landslide in front of the Wilkes subglacial basin along the Cook continental margin one of the least explored areas on Earth¿has been documented for the first time. This area is critic...
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| Format: | Still Image |
| Language: | unknown |
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European Geosciences Union
2024
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| Online Access: | http://hdl.handle.net/10261/365912 https://doi.org/10.5194/egusphere-egu24-7756 |
| Summary: | Póster presentado en EGU General Assembly (2024), Vienna, Austria & Online | 14–19 April 2024 A giant submarine landslide in front of the Wilkes subglacial basin along the Cook continental margin one of the least explored areas on Earth¿has been documented for the first time. This area is critical to understanding the stability of one among the most vulnerable sectors of the Antarctic Ice sheet to climate and ocean warming. It is named as Cook mega-slide complex (CMSC), which occurred in the early Pliocene according to the seismic interpretation correlated to the IODP Exp 318 sites. The giant submarine landslide is well imaged on the seismic profiles and exhibits various kinematic indicators with the basal glide planes and original headwall scarps. It affected the area of c. 22, 686.5 km2, approximately 3399 km3 of sediments evacuated from the continental margin. With a scale similar to Storegga Slide on the Norway margin, the size of the CMSC is mostly likely the largest submarine landslide ever discovered around the Antarctic margin. We propose that glacial isostatic adjustment and glacial outburst floods caused by the East Antarctic Ice Sheet (EAIS) retreat lead to the formation of the large slides and create the condition for slope instability and erosion. The development and collapse of peripheral bulge has been firstly observed from Antarctic margin, associated with the glaciation and subsequent deglaciation of the EAIS, led to a distinct spatial variation in sea level changes and further affected the deposition on the slope. Our results yield intriguing insights into the relationship of stratigraphic evolution, submarine landslides, and past EAIS instabilities throughout the warm periods of the late Miocene-Pliocene, and thereby provide important constraints for ice sheet modeling and sea level prediction. |
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