Meanwhile, this biomarker approach has been used successfully in many studies dealing with the reconstruction of Arctic sea ice
history during the last
glacial to
Holocene time interval, i.e., the last about 30 ka31, 32,33,34,35,36,37.
As the worlds» oldest and most scrutinised instrumental temperature record it usefully covers much of the «Little Ice Age» when the most extensive recent
glacial advances in the
Holocene began, whilst numerous contemporary records make it possible to examine earlier periods in British climatic
history.