These data describe the 18O of O2, 15N of N2, 18Oatm, and O2/N2 ratios of trapped gases in the Vostok ice core from East Antarctica. The investigator used a mass spectrometer to measure gas concentrations and isotopic compositions. Data extend to approximately 420,000 years ago. Two different age models are included.
Data are available in tab-delimited ASCII format via ftp.
Please cite these data as follows:
Bender, M. 2002. Vostok ice core trapped gas concentrations and isotopic compositions. Boulder, CO: National Snow and Ice Data Center. http://dx.doi.org/10.7265/N5862DCW.
|parameter(s)||oxygen and nitrogen isotopes in trapped gases|
|spatial coverage||ice core obtained at Vostok Station, East Antarctica|
|temporal coverage||data extend to approx. 420,000 years ago|
|data format||tab-delimited ASCII|
|file size||files sizes range from 9 KB to 132 KB|
|procedures for obtaining data||data are available via ftp|
Dr. Michael Bender
Department of Geosciences
Princeton, NJ USA
NSIDC User Services
National Snow and Ice Data Center
CIRES, 449 UCB
University of Colorado
Boulder, CO 80309-0449 USA
phone: +1 303.492.6199
fax: +1 303.492.2468
form: Contact NSIDC User Services
Todd Sowers, Joseph Orchardo, Bruno Malaize, and Mary-Lynn Dickson helped with sample analysis.
Data consist of four tab-delimited ASCII files. For a description of these files, see Sample Data Records.
File sizes range from 9 KB to 132 KB.
"Vos_O2-N2_isotope_data_all" contains all data for the 4G, 3G, and 5G cores:
Core Depth del 15N del 18O del 18Oatm del O2/N2 5G 174.5 0.49 1.09 0.11 -28.2 5G 174.5 0.56 1.14 0.01 -35.2 5G 185.2 0.58 0.97 -0.19 -26.4 5G 185.2 0.58 0.99 -0.18 -30.5"Vos_O2-N2_isotope_data_avg" contains average values of the properties at given depths:Core Depth del 15N del 18O del 18Oatm del O2/N2 5G 174.5 0.53 1.11 0.06 -31.7 5G 185.2 0.58 0.98 -0.19 -28.4 5G 205.7 0.56 0.94 -0.18 -34.0"Vostok_EGT20_chronology" contains gas ages and ice ages assigned to each depth according to the EGT20 chronology (see Temporal Coverage). Gas age-ice age differences are included under the header "EGT20 *age."Depth EGT20 ice age EGT20 *age EGT20 gas age 150 5.721 3.319 2.402 151 5.769 3.307 2.462 152 5.816 3.306 2.51 153 5.863 3.315 2.548"Vostok_d18Oatm_chronology" contains gas ages and ice ages assigned to each depth according to the 18Oatm chronology (see Temporal Coverage). Gas age-ice age differences are included under the header "EGT20 *age."Depth 18Oatm ice age EGT20 *age 18Oatm gas age 150 5.68 3.32 2.36 151 5.72 3.31 2.42 152 5.77 3.31 2.47 153 5.82 3.32 2.50
Sampled ice cores came from Russia's Vostok Station in East Antarctica, located at 72.28 degrees south latitude, 106.48 degrees east longitude.
Vostok Station is indicated on the map below by the letter "V." Crosshairs mark the position of the south pole.
Data extend to 3623 meters depth, or approximately 420,000 years ago (i.e., 420 ka).
Isotopic data are presented along with two proposed chronologies. The first is the Extended Glaciological Timescale (EGT20), a minimally tuned glaciological chronology utilized by Petit et al. (1999). The second is an orbitally tuned chronology that exploits the strong relationship between 18Oatm and insolation changes. This chronology, described by Petit et al. (1999), is enhanced by control points that assume correspondence between insolation maxima and the midpoints of decreases in 18Oatm. An additional control point at 385 ka gas age has been added here. The 18Oatm chronology utilizes gas age-ice age differences from the EGT20 timescale.
Data describe the 18O of O2, 15N of N2, 18Oatm, and O2/N2 ratios of trapped gas samples from the Vostok ice cores. All results are reported with respect to the standard of late twentieth-century air.
Data are available via ftp.
18Oatm is a useful variable for correlating ice cores, and for inferring information about past climate and ice extent. At any given time, 18O is approximately constant throughout the atmosphere, but this value varies over time due to changes in the hydrologic cycle, ice sheet volume, and worldwide patterns of plant growth. The 18O of O2 in the past atmosphere (18Oatm) is calculated by subtracting 2x15N from 18O, thus correcting for gravitational fractionation, a process that occurs while air is trapped within the firn prior to being isolated from the atmosphere.
Another effect results from how gases are retained within an ice core. The ratio of O2 to N2 trapped within the core is typically less than the original ratio of the trapped air because O2 is a smaller molecule than N2, and thus escapes more readily from the core as bubbles form and during core storage. 15N of N2 has a constant value of zero in the atmosphere, but is greater than zero in firn air due to gravitational fractionation. 18O of O2 is also enriched by gravitational fractionation.
The investigator collected trapped gases by melting ice samples in a vacuum, refreezing them, and condensing the headspace gases into a stainless steel tube immersed in liquid helium. Trapped gases were admitted to the mass spectrometer and analyzed versus a dry air standard to determine the isotopic composition of N2, the isotopic composition of O2, and the O2/N2 ratio. Methodology followed that of Sowers et al. (1989), except that the investigator did not remelt and refreeze samples after the initial collection. This change in methodology caused loss of O2, which is more soluble than N2, and thus lowered the measured O2/N2 ratios slightly.
Petit, J. R., J. Jouzel, D. Raynaud, N. I. Barkov, J.M. Barnola, I. Basile, M. Bender, J. Chappellaz, M. Davis, G. Delaygue, V. M. Kotlyakov, M. Legrand, V. Y. Lipenkov, C. Lorius, L. Pepin, C. Ritz, E. Saltzman, and M. Stievenard. 1999. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399: 429-436.
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.
30 January 2002
14 February 2002