Cores acquired by the ANDRILL McMurdo Ice Shelf Project (AND-1B) provide the basis for a
new sedimentation model for glacimarine depositional sequences that reflect cyclic glacial …

Geological records from the Antarctic margin offer direct evidence of environmental
variability at high southern latitudes and provide insight regarding ice sheet sensitivity to …

Cenozoic evolution of the Antarctic ice sheets is thought to be driven primarily by long-term
changes in radiative forcing, but the tectonic evolution of Antarctica may also have played a …

A newly constructed composite oxygen isotope record is a proxy for eustasy that extends
back to the Cretaceous-Tertiary boundary and provides an independent test of sequence …

Abstract Early to Middle Miocene sea-level oscillations of approximately 40–60 m estimated
from far-field records,–are interpreted to reflect the loss of virtually all East Antarctic ice …

This book is a comprehensive overview of the ever-captivating field of glaciation from the
perspective of glacial landsystems. This approach models the many processes, forms and …

Abstract A 1284.87-m-long sediment core (AND-1B) from beneath the McMurdo sector of the
Ross Ice Shelf provides the most complete single section record to date of fluctuations of the …

Although hundreds of cores have been collected on the Antarctic continental shelf over the
past five decades, definitive interpretations of depositional environments associated with …

On the basis of geomorphic mapping, we reconstruct the landscape evolution of the Convoy
Range to Mackay Glacier area of the rifted margin of the Transantarctic Mountains and …

Seismic stratigraphic and drill data from Antarctic continental margins have provided much
direct evidence concerning ice sheet evolution as Earth's climate cooled from the warmth of …