Gases trapped in polar ice sheets provide a means of obtaining samples
of Earth's atmosphere from times in the past. We describe geochemical
processes affecting gases trapped in ice and discuss how these mechan
isms affect the composition of gas extracted from polar ice cores. We
review the methods for recovering samples of paleo-atmospheres from ic
e cores and discuss the suitability of each method in different applic
ations. We conclude that extracting gas by mechanical disintegration (
e.g., crushing, grinding, shaving, or milling) is most easily performe
d on relatively young ice in which the content of the bubbles is still
representative of the original atmosphere. For ice recovered from gre
ater depth, where some or all of the gases have been driven into the i
ce matrix itself, more care must be taken in interpreting the analysis
of the extracted gases.