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Elsig, Joachim; Schmitt, Jochen; Leuenberger, Daiana; Schneider, Robert; Eyer, Marc; Leuenberger, Markus Christian; Joos, Fortunat; Fischer, Hubertus; Stocker, Thomas F (2009): Carbon isotopic record of CO2 from the Holocene of the Dome C ice core [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.728699, Supplement to: Elsig, J et al. (2009): Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core. Nature, 461, 507-510, https://doi.org/10.1038/nature08393

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Abstract:
Reconstructions of atmospheric CO2 concentrations based on Antarctic ice cores reveal significant changes during the Holocene epoch, but the processes responsible for these changes in CO2 concentrations have not been unambiguously identified. Distinct characteristics in the carbon isotope signatures of the major carbon reservoirs (ocean, biosphere, sediments and atmosphere) constrain variations in the CO2 fluxes between those reservoirs. Here we present a highly resolved atmospheric d13C record for the past 11,000 years from measurements on atmospheric CO2 trapped in an Antarctic ice core. From mass-balance inverse model calculations performed with a simplified carbon cycle model, we show that the decrease in atmospheric CO2 of about 5 parts per million by volume (p.p.m.v.) and the increase in d13C of about 0.25% during the early Holocene is most probably the result of a combination of carbon uptake of about 290 gigatonnes of carbon by the land biosphere and carbon release from the ocean in response to carbonate compensation of the terrestrial uptake during the termination of the last ice age. The 20 p.p.m.v. increase of atmospheric CO2 and the small decrease in d13C of about 0.05% during the later Holocene can mostly be explained by contributions from carbonate compensation of earlier land-biosphere uptake and coral reef formation, with only a minor contribution from a small decrease of the land-biosphere carbon inventory.
Funding:
Fifth Framework Programme (FP5), grant/award no. EVK2-CT-2000-00077: European Project for Ice Coring in Antarctica
Fourth Framework Programme (FP4), grant/award no. ENV4980702: European Project for Ice Coring in Antarctica
German Research Foundation (DFG), grant/award no. 25575884: Integrierte Analyse zwischeneiszeitlicher Klimadynamik
Coverage:
Latitude: -75.100000 * Longitude: 123.350000
Minimum DEPTH, ice/snow: 110.19 m * Maximum DEPTH, ice/snow: 409.64 m
Event(s):
EDC96 * Latitude: -75.100000 * Longitude: 123.350000 * Elevation: 3233.0 m * Location: Antarctica * Campaign: Dome C * Method/Device: Ice drill (ICEDRILL)
Comment:
Dome C ice core covering 0 to 11 kyr BP. The air from polar ice-core samples of about 30g (AWI/Bern) and 5-6g (Bern) is extracted under vacuum with a sublimation methode or via mechanical cracking, respectively, and the extracted gas is then analysed for d13CO2 using gas chromatographic separation and isotopic analyses on two independet mass spectrometers. The mean d13CO2 analytical uncertainty of both methods (1-sigma) is 0.07 per mille.
The age scale used (in ka before 1950 AD) is EDC3 gas age scenario 4 (Loulergue et al., 2007, http://www.clim-past.net/3/527/2007).
Values marked via '/', are outlies, and have not been taken into account for deconvolution calculations. The outlier depths have been measured using both extraction methods and are very likley caused by an ice core break during the drilling (see further details).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, ice/snowDepth ice/snowmGeocode
AGEAgeka BPGeocode
δ13C, carbon dioxide, atmosphericδ13C CO2‰ PDBElsig, JoachimCalculated average/mean valuescorrected for gravitational fractionation using d15N2 data
δ13C, standard deviationδ13C std dev±Elsig, Joachim1-sigma uncertainty
ReplicatesRepl#Elsig, Joachim
Method commentMethod commElsig, Joachimextraction method (mechanical cracking or sublimation of the ice)
Size:
267 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth ice/snow [m]

Age [ka BP]

δ13C CO2 [‰ PDB]

δ13C std dev [±]

Repl [#]

Method comm
110.190.387-6.370.104cracker
118.480.660-6.380.052cracker
129.511.043-6.300.002cracker
129.611.047-6.450.023sublimation
141.171.440-6.380.103cracker
144.001.543-6.361sublimation
144.571.565-6.380.0320cracker
151.071.801-6.310.112cracker
154.221.912-6.381sublimation
162.012.198-6.360.112cracker
170.802.523/-6.820.183sublimation
170.872.525/-6.650.074cracker
172.942.594-6.420.052sublimation
172.972.595-6.430.122cracker
181.372.893-6.280.092cracker
185.513.030-6.300.052cracker
185.653.036-6.331sublimation
192.933.325-6.260.133cracker
196.113.439-6.291sublimation
206.013.778-6.370.062cracker
214.904.088-6.380.093sublimation
216.524.153-6.360.032cracker
220.984.317-6.410.064cracker
231.914.692-6.240.102cracker
231.974.694-6.311sublimation
240.114.992-6.340.132cracker
250.345.350-6.370.113sublimation
250.445.353-6.320.083cracker
260.285.694-6.310.073cracker
260.405.698-6.340.063sublimation
271.906.116-6.360.042cracker
280.256.414-6.281sublimation
280.406.420-6.310.072cracker
283.556.533-6.280.082cracker
291.826.826-6.360.052cracker
294.506.928-6.330.076cracker
294.586.930-6.391sublimation
302.847.221-6.370.084cracker
305.507.300-6.290.132cracker
308.007.389-6.431sublimation
312.717.552-6.410.0219cracker
313.857.582-6.310.142cracker
317.897.721-6.390.054cracker
318.477.737-6.340.032cracker
320.097.800-6.280.052cracker
321.707.853-6.420.053sublimation
324.827.971-6.300.122cracker
326.388.041-6.550.084cracker
330.318.166-6.470.012cracker
338.488.461-6.501sublimation
338.508.462-6.380.082cracker
341.258.561-6.450.094cracker
349.548.852-6.500.032cracker
352.458.968-6.391sublimation
359.879.212-6.480.022cracker
369.359.519-6.461sublimation
369.379.520-6.430.093cracker
374.949.712-6.490.062cracker
379.719.891-6.610.074cracker
382.029.971-6.550.053sublimation
385.2710.086-6.640.023cracker
390.2810.282-6.490.042cracker
396.1810.507-6.572cracker
396.2010.507-6.630.121sublimation
401.7910.721-6.500.074cracker
403.8310.787-6.500.044cracker
406.0510.874-6.580.032cracker
407.2410.919-6.720.094cracker
409.5811.003-6.500.002cracker
409.6411.005-6.631sublimation