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.
Carbon-Isotopic Composition of Atmospheric CO2 since the Last Glacial Maximum, Version 1
|Spatial Resolution:||Not Specified|
|Temporal Coverage:||Not specified|
|Temporal Resolution:||Not specified|
|Data Contributor(s):||Martin Wahlen|
|Metadata XML:||View Metadata Record|
As a condition of using these data, you must cite the use of this data set using the following citation. For more information, see our Use and Copyright Web page.Wahlen, M. 2002. Carbon-Isotopic Composition of Atmospheric CO2 since the Last Glacial Maximum, Version 1. [Indicate subset used]. Boulder, Colorado USA. NSIDC: National Snow and Ice Data Center. doi: http://dx.doi.org/10.7265/N54F1NN5. [Date Accessed].
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