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Byrd ice core debris constrains the sediment provenance signature of central West Antarctica
Provenance records from sediments deposited offshore of the West Antarctic Ice Sheet
(WAIS) can help identify past major ice retreat, thus constraining ice‐sheet models …
(WAIS) can help identify past major ice retreat, thus constraining ice‐sheet models …
A large-scale transcontinental river system crossed West Antarctica during the Eocene
Extensive ice coverage largely prevents investigations of Antarctica's unglaciated past.
Knowledge about environmental and tectonic development before large-scale glaciation …
Knowledge about environmental and tectonic development before large-scale glaciation …
Return to the Ross Ice Shelf Project (RISP), Site J-9 (1977–1979): perspectives of West Antarctic Ice Sheet history from Miocene and Holocene benthic foraminifera
Abstract In 1977–1978 and 1978–1979, the Ross Ice Shelf Project (RISP) recovered
sediments from beneath the largest ice shelf in Antarctica at Site J-9 (∼ 82° S, 168° W),∼ …
sediments from beneath the largest ice shelf in Antarctica at Site J-9 (∼ 82° S, 168° W),∼ …
[HTML][HTML] A multi-proxy detrital study from Permian-Triassic fluvial sequences of Victoria Land (Antarctica): Implications for the Gondwanan basin evolution
One of the most complete Permian-Triassic fluvial sequences of the Beacon Supergroup,
characterizing the infilling of the Transantarctic Basin, is recorded in the Allan Hills in …
characterizing the infilling of the Transantarctic Basin, is recorded in the Allan Hills in …
[HTML][HTML] Dynamic collapse and regrowth of the Antarctic Ice Sheet in the Weddell Sea sector during the middle Miocene: A novel multi-proxy sedimentary provenance …
The latest generation of Antarctic paleo-ice sheet models, incorporating bedrock paleo-
topography, reconstruct the development of substantial ice-sheet embayments during the …
topography, reconstruct the development of substantial ice-sheet embayments during the …
Recurrent EW oscillations of the ice flow confluence of the East and West Antarctic ice sheets in the central Ross Sea, Antarctica, from the Middle Miocene to the …
We present a multidisciplinary provenance study on legacy cores drilled in the 1970s during
DSDP Leg 28 at sites 271 and 272, in the central Ross Sea, Antarctica. The two sites …
DSDP Leg 28 at sites 271 and 272, in the central Ross Sea, Antarctica. The two sites …
[HTML][HTML] Miocene climate cooling and aridification of Antarctica may have enhanced syn-extensional magmatism in the western Ross Sea
Continental rift systems are commonly characterized by volcanism with parental basaltic
magmas sourced from the mantle. Erosion of the rift shoulders and sedimentation in the …
magmas sourced from the mantle. Erosion of the rift shoulders and sedimentation in the …
[HTML][HTML] Petrographic signature of the gravel fraction from late Quaternary glacigenic sediments in the Ross Sea (Antarctica): Implications for source terranes and …
Abstract The Ross Embayment is a key region to study the dynamics of the ice sheets during
colder and warmer than present climatic conditions, because both the East and West …
colder and warmer than present climatic conditions, because both the East and West …
Sourcing of the Oligocene to Pliocene sediments of the Ningnan Basin: Evidence for Tibetan Plateau growth and local faulting unravelled by detrital apatite fission …
The Cenozoic topographic growth of the Tibetan Plateau is a pulsed, polyphase process that
still requires more constraints. The Cenozoic sedimentary record of the Ningnan Basin, a …
still requires more constraints. The Cenozoic sedimentary record of the Ningnan Basin, a …