Millennial climate oscillations of the glacial interval are interrupted by extreme events, the so‐
called Heinrich events of the North Atlantic. Their near‐global footprint is a testament to …

A prominent, abrupt climate event about 8200 years ago brought generally cold and dry
conditions to broad northern-hemisphere regions especially in wintertime, in response to a …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

The evidence for the Little Ice Age, the most important fluctuation in global climate in
historical times, is most dramatically represented by the advance of mountain glaciers in the …

High-resolution studies of North Atlantic deep sea cores demonstrate that prominent
increases in iceberg calving recurred at intervals of 2000 to 3000 years, much more …

Observations of large and abrupt climate changes recorded in Greenland ice cores have
spurred a search for clues to their cause. This search has revealed that at six times during …

Increasingly, environmental scientists, palaeoceanographers and geologists are collecting
quantitative records of environmental changes (time series) from sediments, ice cores, cave …

This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new mapping inventory that includes previously hypothesised ice …

Heinrich events are well documented for the last glaciation, but little is known about their
occurrence in older glacial periods of the Pleistocene. Here we report scanning XRF and …

X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …