IEDA
Dataset Information
Carbon-Isotopic Composition of Atmospheric CO2 since the Last Glacial Maximum
Data DOI:
https://doi.org/10.7265/N54F1NN5
Cite as
Wahlen, M. (2002) "Carbon-Isotopic Composition of Atmospheric CO2 since the Last Glacial Maximum" U.S. Antarctic Program (USAP) Data Center. doi: https://doi.org/10.7265/N54F1NN5.
AMD - DIF Record(s)
Abstract
These data describe the concentration and carbon-isotopic composition (d13CO2) of atmospheric CO2 from air trapped in ice between 27,000 and 1,300 years before present from Taylor Dome, Antarctica. Data are used to investigate the causes of the CO2 concentration increase that occurred during the transition between the last glacial maximum (LGM) and the Holocene. Data are in tab-delimited ASCII and Excel formats, and are available via ftp.
Creator(s):
Wahlen, Martin
Date Created:
2002-01-01
Repository:
USAP-DC (current) - NSIDC (original)
Spatial Extent(s)
West: 158.71, East: 158.71, South: -77.8, North: -77.8
Award(s)
Version:
1
References
  1. Craig, H., Y. Horibe, and T. Sowers. 1988. Gravitational separation of gases and isotopes in polar ice caps. Science 242:1675-1678. (doi:10.1126/science.242.4886.1675 )
  2. Indermuhle, A., T. Stocker, H. Fischer, H. Smith, F. Joos, M. Wahlen, B. Deck,, D. Mastroianni, J. Tschumi, T. Blunier, R. Meyer, and B. Stauffer. 1998., Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome,, Antarctica. Nature 398:121-126. (doi:10.1038/18158)
  3. Leuenberger, M. and U. Siegenthaler. 1988. Ice-age atmospheric concentration of nitrous oxide from an Antarctic ice core. Nature 360:449-451. (doi:10.1038/360449a0)
  4. Schwander, J. 1989. The environmental record in glaciers and ice sheets, eds. H. Oeschger and C. C. Langway, Jr. John Wiley and Sons, Ltd., pp. 53-67.
  5. Smith, H. J., H. Fischer, D. Mastroianni, B. Deck, and M. Wahlen. 1999. Dual, modes of the carbon cycle since the Last Glacial Maximum. Nature 400:248-250. (doi:10.1038/22291)
  6. Smith, H., M. Wahlen, D. Mastroianni, and K. Taylor. 1997. The CO2 concentration, of air trapped in GISP2 ice from the LGM-Holocene transition. Geophysical, Research Letters 24(1):1-4. (doi:10.1029/96GL03700)
  7. Steig, E., E. Brook, J.W.C. White, C. Sucher, M. Bender, S. Lehman, D. Morse, E., Waddington, and G. Clow. 1998. Synchronous climate changes in Antarctica and the, North Atlantic. Science 282(5386):92-95. (doi:10.1126/science.282.5386.92 )
  8. Sucher, C. 1997. Trapped gases in the Taylor Dome Ice Core: Implications for, East Antarctic climate change. Master's Thesis, University of Rhode Island.
  9. Sowers, T., M. Bender, and D. Raynaud. 1989. Elemental and Isotopic Composition of Occluded O2 and N2 in Polar Ice. Journal of Geophysical Research 94: 5137-5150. (doi:10.1029/JD094iD04p05137)
  10. Wahlen, M., D. Allen, B. Deck, and A. Herchenroder, Initial measurement of CO2 concentrations (1530 to 1940 AD) in air occluded in the GISP2 ice core from central Greenland, Geophysical Research Letters, 18, 1457-1460, 1991. (doi:10.1029/91GL01724)
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nsidc0108_UG.pdf
Data Files
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nsidc-0108_fgdc.xml

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TDdata.xls

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