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Circulation and ocean–ice shelf interaction beneath the Denman and Shackleton Ice Shelves Science Advances, 2025 (Ref: 17478)
Category 1: Peer-reviewed literature

Ocean-driven basal melt can thin and weaken ice shelves, reducing buttressing and causing sea level rise. However, the processes driving melt in ice shelf cavities are challenging to observe. Here we report float observations spanning the ocean cavity beneath Shackleton Ice Shelf.

Predicting trends in atmospheric CO2 across the Mid-Pleistocene Transition using existing climate archives Climate of the Past, 2024 (Ref: 17203)
Category 1: Peer-reviewed literature

During the Mid-Pleistocene Transition (MPT), ca. 1200–800?000 years ago (ka), the Earth's glacial cycles changed from 41 to 100?kyr periodicity.

Thrusting in the lower crust: evidence from the Oygarden Islands, Kemp Land, East Antarctica Geological Magazine, 2000 (Ref: 9368)
Category 1: Peer-reviewed literature

Layered orthogneisses of the Oygarden Islands preserve evidence for four high-grade deformation events (D1 to D4). Archaean D1 and D2 structures are only patchily preserved due to extensive recrystallization during D3 and D4, which represent effects of the c.1000 Ma Rayner Structural Episode (RSE).

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