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Climate of the Past An interactive open-access journal of the European Geosciences Union
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An ice core from Taylor Glacier, Antarctica, spans a period ~ 70 000 years ago when Earth entered the last ice age. Chemical analyses of the ice and air bubbles allow for an independent determination of the ages of the ice and gas bubbles. The difference between the age of the ice and the bubbles at any given depth, called ∆age, is unusually high in the Taylor Glacier core compared to the Taylor Dome ice core situated to the south. This implies a dramatic accumulation gradient between the sites.
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CP | Articles | Volume 15, issue 4
CP | Articles | Volume 15, issue 4
Clim. Past, 15, 1537–1556, 2019
https://doi.org/10.5194/cp-15-1537-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 15, 1537–1556, 2019
https://doi.org/10.5194/cp-15-1537-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
CP | Articles | Volume 15, issue 4

Research article 08 Aug 2019

Research article | 08 Aug 2019

Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier

James A. Menking et al.

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Short summary
An ice core from Taylor Glacier, Antarctica, spans a period ~ 70 000 years ago when Earth entered the last ice age. Chemical analyses of the ice and air bubbles allow for an independent determination of the ages of the ice and gas bubbles. The difference between the age of the ice and the bubbles at any given depth, called ∆age, is unusually high in the Taylor Glacier core compared to the Taylor Dome ice core situated to the south. This implies a dramatic accumulation gradient between the sites.
Read more
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Climate of the Past

An interactive open-access journal of the European Geosciences Union

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