Latest Quaternary glaciation Stories
Atmospheric carbon dioxide (CO2) is one of the most important greenhouse gases and the increase of its abundance in the atmosphere by fossil fuel burning is the main cause of future global warming.
At the end of the last Ice Age, atmospheric carbon dioxide levels rose rapidly as the planet warmed; scientists have long hypothesized that the source was CO2 released from the deep ocean.
Scientists at the University of York, using an 'amino acid time capsule', have led the largest ever program to date the British Quaternary period, stretching back nearly three million years.
Fresh research into glaciers could help scientists better predict the impact of changing climates on global sea levels.
A set of maps created by the University of Sheffield have illustrated, for the first time, how our last British ice sheet shrunk during the Ice Age.
Russian scientists are set to pierce through Antarctica's frozen surface to reveal the secrets of an icebound lake that has been sealed deep there for the past 15 million years.
Researchers at the California Institute of Technology have discovered new details supporting the idea that mass extinction is linked to a cooling climate.
Southampton researchers have estimated that sea-level rose by an average of about 1 meter per century at the end of the last Ice Age, interrupted by rapid â€˜jumpsâ€™ during which it rose by up to 2 and a half meters per century.
The landform known as a drumlin, created when the ice advanced during the Ice Age, can also be produced by today's glaciers.
NASA and European researchers have conducted a novel study to simultaneously measure, for the first time, trends in how water is transported across Earth's surface and how the solid Earth responds to the retreat of glaciers following the last major Ice Age, including the shifting of Earth's center of mass.
- To swell, as grain or wood with water.