Carbon-Isotopic Composition of Atmospheric CO2 since the Last Glacial Maximum, Version 1
Data set id:
NSIDC-0108
DOI: 10.7265/N54F1NN5
Overview
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.
Parameter(s):
CARBON DIOXIDEICE CORE AIR BUBBLESISOTOPES
Platform(s):
GROUND-BASED OBSERVATIONS
Sensor(s):
MASS SPECTROMETERS
Data Format(s):
ASCII, Excel
Temporal Coverage:
Not Specified
Temporal Resolution:
Not Specified
Spatial Resolution:
- Not Specified
Spatial Coverage:
N:
-77.8
S:
-77.8
E:
158.71
W:
158.71
Blue outlined yellow areas on the map below indicate the spatial coverage for this data set.
NSIDC does not archive or provide citation guidance for these data.