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Showing 1–2 of 2 results
Advanced filters: Author: A. Lourantou Clear advanced filters

  • Glacial Termination II was marked by a rise in atmospheric CO2 concentrations and global temperature. An analysis of air bubbles from an Antarctic ice core suggests that during the first phase of deglaciation, Antarctic temperature and atmospheric CO2 concentrations increased together, whereas CO2 lagged behind temperature rise during the second phase.

    • A. Landais
    • G. Dreyfus
    • G. Teste
    Research
    Nature Geoscience
    Volume: 6, P: 1062-1065

  • Atmospheric carbon dioxide levels rose at the end of the last glacial period, but the sources of this carbon are uncertain. Ice-core data and carbon-cycle modelling suggest that the disappearance of a terrestrial inert carbon pool may have contributed to the rise.

    • P. Ciais
    • A. Tagliabue
    • S. L. Piao
    Research
    Nature Geoscience
    Volume: 5, P: 74-79