Abstract Otavi Group is a 1.5–3.5-km-thick epicontinental marine carbonate succession of
Neoproterozoic age, exposed in an 800-km-long Ediacaran− Cambrian fold belt that rims …

The Antarctic Peninsula region is currently undergoing rapid environmental change,
resulting in the thinning, acceleration and recession of glaciers and the sequential collapse …

The reliability of Arctic climate predictions is currently hampered by insufficient knowledge of
natural climate variability in the past. A sediment core from Lake El'gygytgyn in northeastern …

The influence of Antarctica and the Southern Ocean on Late Pliocene global climate
reconstructions has remained ambiguous due to a lack of well-dated Antarctic-proximal …

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 …

Deep sea geological records indicate that Antarctic ice-sheet growth and decay is strongly
influenced by the Earth's astronomical variations (known as Milankovitch cycles), and that …

Abstract The Otavi Group is a Neoproterozoic carbonate‐dominated succession up to 4 km
thick, which blankets the southern promontory of the Congo craton in northern Namibia. This …

The Quaternary Period, comprising the Holocene and Pleistocene Epochs, encompasses
the last~ 2.6 Ma during which time Earth's climate was strongly influenced by bipolar …

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