A methane record from the GISP2 ice core reveals that millennial-scale
variations in atmospheric methane concentration characterized much of
the past 110,00 years, As previously observed in a shorter record fro
m central Greenland, abrupt concentration shifts of about 50 to 300 pa
rts per billion by volume were coeval with most of the interstadial wa
rming events (better known as Dansgaard-Oeschger events) recorded in t
he GISP2 ice core throughout the last glacial period. The magnitude of
the rapid concentration shifts varied on a longer time scale in a man
ner consistent with variations in Northern Hemisphere summer insolatio
n, which suggests that insolation may have modulated the effects of in
terstadial climate change on the terrestrial biosphere.