Due to their outstanding resolution and well-constrained chronologies, Greenland ice-core
records provide a master record of past climatic changes throughout the Last Interglacial …

We present a synchronization of the NGRIP, GRIP and GISP2 ice cores onto a master
chronology extending back to 104 ka before present, providing a consistent chronological …

This report is the first complete assessment of the science of climate change since Working
Group I (WGI) of the IPCC produced its second report Climate Change 1995: The Science of …

Surface winds and surface ocean hydrography in the subpolar North Atlantic appear to have
been influenced by variations in solar output through the entire Holocene. The evidence …

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 …

MANY tropical soils are poor in inorganic nutrients and rely on the recycling of nutrients from
soil organic matter to maintain fertility. In undisturbed rainforests such nutrients are recycled …

Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

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 …

Changes in the East Asian paleomonsoon reflect interactions between the global
atmosphere, ocean, land and ice systems, and are also an expression of their combined …

Oxygen isotope variations spanning the last glacial cycle and the Holocene derived from ice‐
core records for six sites in Greenland (Camp Century, Dye‐3, GRIP, GISP2, Renland and …