We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …

Two fundamental questions about the ice-age climate system await satisfactory resolution.
First, if summer solar radiation intensity truly controls the orbital signature of the last glacial …

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 …

On-line analysis of split sediment cores by XRF core scanners has become increasingly
popular in the past decade, because it allows nondestructive extraction of near-continuous …

XRF core scanners, with their rapid and non-destructive analytical capability, have now
been used for two decades in the analysis of marine sediments. Initially they were used to …

Fire activity has varied globally and continuously since the last glacial maximum (LGM) in
response to long-term changes in global climate and shorter-term regional changes in …

During glacial periods of the Late Pleistocene, an abundance of proxy data demonstrates
the existence of large and repeated millennial-scale warming episodes, known as …

Abstract Changes in the magnitude of millennial-scale climate variability (MCV) during the
Late Pleistocene occur as a function of changing background climate state over tens of …

Magnesium/calcium data from Southern Ocean planktonic foraminifera demonstrate that
high-latitude (∼ 55° S) southwest Pacific sea surface temperatures (SSTs) cooled 6° to 7° C …

Changes in the strength and position of Southern Hemisphere westerly winds during the
Last Glacial cycle have been invoked to explain both millennial and glacial–interglacial …