Articles | Volume 13, issue 7
https://doi.org/10.5194/cp-13-943-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-943-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
20 Jul 2017
Research article |
| 20 Jul 2017
Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle
Daniel Baggenstos
CORRESPONDING AUTHOR
Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
current address: Climate and Environmental Physics, University of Bern, Bern, Switzerland
Thomas K. Bauska
College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Jeffrey P. Severinghaus
Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
James E. Lee
College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Hinrich Schaefer
National Institute of Water and Atmospheric Research Ltd, P.O. Box 14901, Kilbirnie, 301 Evans Bay Parade, Wellington, New Zealand
Christo Buizert
College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Edward J. Brook
College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Sarah Shackleton
Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
Vasilii V. Petrenko
Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA
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Cited
15 citations as recorded by crossref.
- Evaluating the Duration and Continuity of Potential Climate Records From the Allan Hills Blue Ice Area, East Antarctica L. Kehrl et al. 10.1029/2018GL077511
- Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- An 83 000-year-old ice core from Roosevelt Island, Ross Sea, Antarctica J. Lee et al. 10.5194/cp-16-1691-2020
- Global ocean heat content in the Last Interglacial S. Shackleton et al. 10.1038/s41561-019-0498-0
- Millennial‐Scale Changes in Terrestrial and Marine Nitrous Oxide Emissions at the Onset and Termination of Marine Isotope Stage 4 J. Menking et al. 10.1029/2020GL089110
- Chronostratigraphy of the Larsen blue-ice area in northern Victoria Land, East Antarctica, and its implications for paleoclimate G. Lee et al. 10.5194/tc-16-2301-2022
- A preliminary study for blue ice in Victoria Land, East Antarctica Y. Jang et al. 10.14770/jgsk.2017.53.4.567
- A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale D. Baggenstos et al. 10.1029/2017PA003297
- Using ice core measurements from Taylor Glacier, Antarctica, to calibrate in situ cosmogenic 14C production rates by muons M. Dyonisius et al. 10.5194/tc-17-843-2023
- Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier J. Menking et al. 10.5194/cp-15-1537-2019
- Controls on Millennial‐Scale Atmospheric CO2 Variability During the Last Glacial Period T. Bauska et al. 10.1029/2018GL077881
- Evolution of mean ocean temperature in Marine Isotope Stage 4 S. Shackleton et al. 10.5194/cp-17-2273-2021
- Is the Noble Gas‐Based Rate of Ocean Warming During the Younger Dryas Overestimated? S. Shackleton et al. 10.1029/2019GL082971
- A 156 kyr smoothed history of the atmospheric greenhouse gases CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O and their radiative forcing P. Köhler et al. 10.5194/essd-9-363-2017
14 citations as recorded by crossref.
- Evaluating the Duration and Continuity of Potential Climate Records From the Allan Hills Blue Ice Area, East Antarctica L. Kehrl et al. 10.1029/2018GL077511
- Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- An 83 000-year-old ice core from Roosevelt Island, Ross Sea, Antarctica J. Lee et al. 10.5194/cp-16-1691-2020
- Global ocean heat content in the Last Interglacial S. Shackleton et al. 10.1038/s41561-019-0498-0
- Millennial‐Scale Changes in Terrestrial and Marine Nitrous Oxide Emissions at the Onset and Termination of Marine Isotope Stage 4 J. Menking et al. 10.1029/2020GL089110
- Chronostratigraphy of the Larsen blue-ice area in northern Victoria Land, East Antarctica, and its implications for paleoclimate G. Lee et al. 10.5194/tc-16-2301-2022
- A preliminary study for blue ice in Victoria Land, East Antarctica Y. Jang et al. 10.14770/jgsk.2017.53.4.567
- A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale D. Baggenstos et al. 10.1029/2017PA003297
- Using ice core measurements from Taylor Glacier, Antarctica, to calibrate in situ cosmogenic 14C production rates by muons M. Dyonisius et al. 10.5194/tc-17-843-2023
- Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier J. Menking et al. 10.5194/cp-15-1537-2019
- Controls on Millennial‐Scale Atmospheric CO2 Variability During the Last Glacial Period T. Bauska et al. 10.1029/2018GL077881
- Evolution of mean ocean temperature in Marine Isotope Stage 4 S. Shackleton et al. 10.5194/cp-17-2273-2021
- Is the Noble Gas‐Based Rate of Ocean Warming During the Younger Dryas Overestimated? S. Shackleton et al. 10.1029/2019GL082971
Latest update: 19 Nov 2024
Short summary
We present measurements of the gas composition in trapped air bubbles in ice samples taken from Taylor Glacier, Antarctica. We can show that ice from the entire last glacial cycle (125 000 years ago to the present) is exposed at the surface of this glacier and that the atmospheric record contained in the air bubbles is well preserved. Taylor Glacier therefore provides an easily accessible archive of ancient ice that allows for studies of trace components that require large ice volumes.
We present measurements of the gas composition in trapped air bubbles in ice samples taken from...
