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Upper-ocean-to-atmosphere radiocarbon offsets imply fast deglacial carbon dioxide release
Rose, K.A.; Sikes, E.L.; Guilderson, T.P.; Shane, P.; Hill, T.M.; Zahn, R.; Spero, H.J. (2010). Upper-ocean-to-atmosphere radiocarbon offsets imply fast deglacial carbon dioxide release. Nature (Lond.) 466(7310): 1093-1097. https://dx.doi.org/10.1038/nature09288
In: Nature: International Weekly Journal of Science. Nature Publishing Group: London. ISSN 0028-0836; e-ISSN 1476-4687, meer
Peer reviewed article  
Beschikbaar in  Auteurs 
Trefwoorden
    Chemical compounds > Carbon compounds > Atmospheric gases > Carbon dioxide
    Cycles > Chemical cycles > Geochemical cycle > Biogeochemical cycle > Nutrient cycles > Carbon cycle
    Ocean-atmosphere system
    Marien/Kust
Auteurs  Top 
  • Rose, K.A.
  • Sikes, E.L.
  • Guilderson, T.P.
  • Shane, P.
  • Hill, T.M.
  • Zahn, R.
  • Spero, H.J.
Abstract
    At the end of the last ice age, rising atmospheric CO2 levels coincided with a decline in radiocarbon activity, suggesting the release of highly radiocarbon-depleted CO2 from the deep ocean to the atmosphere. These authors present radiocarbon records of surface and intermediate-depth waters from two sediment cores and find an decrease in radiocarbon activity that precedes and roughly equals in magnitude the decrease in the atmospheric radiocarbon signal during the early stages of the glacial–interglacial climatic transition.
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