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Late Miocene vegetation and palaeoenvironments of the Drygalski Formation, Heard Island, Indian Ocean: evidence from palynology. Antarctic Science, 2005 (Ref: 12168)
Category 1: Peer-reviewed literature

Abstract : Well sorted, fine lithic sandstone within the Drygalski Formation at Cape Lockyer on the … southern tip of Heard Island, preserves a diverse terrestrial palynoflora as well as marine diatoms and a few … foraminifera. A combination of these elements suggests a Late Miocene age (10–5 Ma).

A review of the Cenozoic stratigraphy and glacial history of the Lambert Graben-Prydz Bay region, East Antarctica. Antarctic Science, 2006 (Ref: 12660)
Category 1: Peer-reviewed literature

The Cenozoic glacial history of East Antarctica is recorded in part by the stratigraphy of the Prydz … Bay–Lambert Graben region. The glacigene strata and associated erosion surfaces record at least 10 intervals … of glacial advance (with accompanying erosion and sediment compaction)…

Landform evolution in the Marine Plain region, Vestfold Hills, East Antarctica. Antarctic Science, 2006 (Ref: 12661)
Authors:
Category 1: Peer-reviewed literature

Landforms of Marine Plain in the Vestfold Hills contrast with those of most in the Vestfold Hills. They include consistent land surfaces at 40+ m and 25 m, characteristics controlled by orientation of rock … features, and imprints of phases of glaciation…

Austrochlamys heardensis (Fleming, 1957) (Bivalvia:Pectinidae) from Central Kerguelen Plateau, Indian Ocean: palaeontology and possible tectonic significance. Antarctic Science, 2004 (Ref: 12167)
Category 1: Peer-reviewed literature

Abstract: Austrochlamys heardensis (Fleming) is recorded from a boulder of Late Pliocene (3.62–2.5 Ma) volcaniclastic sandstone dredged 70 km east-north-east of Heard Island, the third record of the species.

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