Ice-sheet grounding-zone wedges (GZWs) on high-latitude continental margins
Grounding-zone wedges (GZWs) are asymmetric sedimentary depocentres which form
through the rapid accumulation of glacigenic debris along a line-source at the grounding …
through the rapid accumulation of glacigenic debris along a line-source at the grounding …
[HTML][HTML] Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM
Onshore and offshore studies show that an expanded, grounded ice sheet occupied the
Ross Sea Embayment during the Last Glacial Maximum (LGM). Results from studies of till …
Ross Sea Embayment during the Last Glacial Maximum (LGM). Results from studies of till …
Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model
A new model of the last deglaciation event of the Late Quaternary ice age is here described
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …
[BOEK][B] Reconstructing quaternary environments
This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …
and updated to provide a new account of the history and scale of environmental changes …
Obliquity-paced Pliocene West Antarctic ice sheet oscillations
Thirty years after oxygen isotope records from microfossils deposited in ocean sediments
confirmed the hypothesis that variations in the Earth's orbital geometry control the ice ages …
confirmed the hypothesis that variations in the Earth's orbital geometry control the ice ages …
Submarine landforms and the reconstruction of fast-flowing ice streams within a large Quaternary ice sheet: The 2500-km-long Norwegian-Svalbard margin (57–80 N)
Morphological interpretation of regional and detailed bathymetric data sets on the 2500-km-
long Norwegian shelf from the North Sea (57° N) to Svalbard (80° N) has revealed a …
long Norwegian shelf from the North Sea (57° N) to Svalbard (80° N) has revealed a …
Holocene climate variability in Antarctica based on 11 ice-core isotopic records
V Masson, F Vimeux, J Jouzel, V Morgan… - Quaternary …, 2000 - cambridge.org
A comparison is made of the Holocene records obtained from water isotope measurements
along 11 ice cores from coastal and central sites in east Antarctica (Vostok, Dome B, Plateau …
along 11 ice cores from coastal and central sites in east Antarctica (Vostok, Dome B, Plateau …
Stability of the Larsen B ice shelf on the Antarctic Peninsula during the Holocene epoch
E Domack, D Duran, A Leventer, S Ishman, S Doane… - Nature, 2005 - nature.com
The stability of the Antarctic ice shelves in a warming climate has long been discussed, and
the recent collapse of a significant part, over 12,500 km2 in area, of the Larsen ice shelf off …
the recent collapse of a significant part, over 12,500 km2 in area, of the Larsen ice shelf off …
Ice sheet sources of sea level rise and freshwater discharge during the last deglaciation
We review and synthesize the geologic record that constrains the sources of sea level rise
and freshwater discharge to the global oceans associated with retreat of ice sheets during …
and freshwater discharge to the global oceans associated with retreat of ice sheets during …
The marine geological imprint of Antarctic ice shelves
Reductions in the thickness and extent of Antarctic ice shelves are triggering increased
discharge of marine-terminating glaciers. While the impacts of recent changes are well …
discharge of marine-terminating glaciers. While the impacts of recent changes are well …