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DOIhttps://doi.org/10.1594/PANGAEA.728699
Carbon isotopic record of CO2 from the Holocene of the Dome C ice core
Elsig; Joachim; Schmitt; Jochen; Leuenberger; Daiana; Schneider; Robert; Eyer; Marc; Leuenberger; Markus C; Joos; Fortunat; Fischer; Hubertus; Stocker; Thomas F
发布日期2009-10-22
数据集类型dataset
英文简介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.
空间范围Latitude: -75.100000 * Longitude: 123.350000
语种英语
国家国际
学科大类气候变化
学科子类冰冻圈
文献类型数据集
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/213826
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GB/T 7714
Elsig,Joachim,Schmitt,et al. Carbon isotopic record of CO2 from the Holocene of the Dome C ice core.2009-10-22.https://doi.org/10.1594/PANGAEA.728699.
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