Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …

Future sea-level rise generates hazards for coastal populations, economies, infrastructure,
and ecosystems around the world. The projection of future sea-level rise relies on an …

We present a glacial isostatic adjustment (GIA) model for Antarctica. This is driven by a new
deglaciation history that has been developed using a numerical ice-sheet model, and is …

Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …

The rate and magnitude of the Antarctic Ice Sheet (AIS) contribution to global sea-level rise
beyond 2100 ce remains highly uncertain. Past changes of the AIS, however, offer …

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 …

Global mean sea level (GMSL) has risen by about 7–8 inches (about 16–21 cm) since 1900,
with about 3 of those inches (about 7 cm) occurring since 1993 (very high confidence) …

Abstract Knowledge about biodiversity changes during transitions from glacial landscape to
lake formation is limited to contemporary studies. Here, we combined analyses of lithology …

Widespread existing geological records from above the modern ice-sheet surface and
outboard of the current ice margin show that the Antarctic Ice Sheet (AIS) was much more …

Introduction Eukaryotic algae in the top few centimeters of fellfield soils of ice-free Maritime
Antarctica have many important effects on their habitat, such as being significant drivers of …