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 …

In an attempt to find potential interglacial analogues of our present interglacial and its
natural future, five interglacials (MIS-1, 5, 9, 11 and 19) are studied in terms of their …

Abstract The European Project for Ice Coring in Antarctica Dome ice core from Dome C
(EDC) has allowed for the reconstruction of atmospheric CO2 concentrations for the last …

Over the past eight hundred thousand years, glacial–interglacial cycles oscillated with a
period of one hundred thousand years ('100k world'). Ice core and ocean sediment data …

Climate during the last glacial period was marked by abrupt instability on millennial
timescales that included large swings of temperature in and around Greenland (Daansgard …

The recovery of a 1.5 million yr long ice core from Antarctica represents a keystone of our
understanding of Quaternary climate, the progression of glaciation over this time period and …

When five Matuyama‐Brunhes (M‐B) boundary records from the North Atlantic are placed
on isotope age models, produced by correlation of the δ18O record directly or indirectly to …

Climatic variabilities on millennial and longer time scales with a bipolar seesaw pattern have
been documented in paleoclimatic records, but their frequencies, relationships with mean …

We compare the present and last interglacial periods as recorded in Antarctic water stable
isotope records now available at various temporal resolutions from six East Antarctic ice …

For about 50 yr, ice cores have provided a wealth of information about past climatic and
environmental changes. Ice cores from Greenland, Antarctica and other glacier-covered …