Magnetic paleointensity stratigraphy is used to detect variations in the strength of Earth's
ancient magnetic field. Paleointensity studies have demonstrated that a dominantly dipolar …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

The Antarctic Peninsula is one of the three fastest warming regions on Earth. Here we
review Holocene proxy records of marine and terrestrial palaeoclimate in the region, and …

Silicon (Si) is a pivotal element in the biogeochemical and ecological functioning of the
ocean. The marine Si cycle is thought to be in internal equilibrium, but the recent discovery …

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

We present marine sedimentologic and radiocarbon data for the timing of retreat of the
largely marine-based Antarctic Peninsula Ice Sheet since the Last Glacial Maximum (LGM) …

A Holocene palaeomagnetic secular variation master curve (FENNOSTACK) and a relative
palaeointensity curve (FENNORPIS) for Fennoscandia are presented. These curves were …

Abstract Changes in penguin populations on the Antarctic Peninsula have been linked to
several environmental factors, but the potentially devastating impact of volcanic activity has …

The marine geological record of the glacial-retreat history of the South Shetland Islands is
derived from the integration of seismic data, core lithofacies, radiocarbon ages and …

The Antarctic Peninsula is one of the most rapidly warming regions on Earth, as evidenced
by a recent increase in the intensity and duration of summer melting, the recession of …