Carbon Isotope Constraints on the Deglacial CO 2 Rise from Ice Cores

By the Numbers As carbon dioxide is exchanged between the atmosphere, the oceans, and the terrestrial biosphere, its carbon isotopic composition is modified by various processes involved in its transfer between the different reservoirs. The carbon isotopic composition of the carbon dioxide contained...

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Bibliographic Details
Published in:Science
Main Authors: Schmitt, Jochen, Schneider, Robert, Elsig, Joachim, Leuenberger, Daiana, Lourantou, Anna, Chappellaz, Jérôme, Köhler, Peter, Joos, Fortunat, Stocker, Thomas F., Leuenberger, Markus, Fischer, Hubertus
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2012
Subjects:
Antarctic
Antarc*
Online Access:http://dx.doi.org/10.1126/science.1217161
https://www.science.org/doi/pdf/10.1126/science.1217161
Description
Summary:By the Numbers As carbon dioxide is exchanged between the atmosphere, the oceans, and the terrestrial biosphere, its carbon isotopic composition is modified by various processes involved in its transfer between the different reservoirs. The carbon isotopic composition of the carbon dioxide contained in bubbles of air trapped in ice cores thus provides a record of the processes that regulated the composition of the atmosphere in the past. Using data from three Antarctic ice cores, Schmitt et al. (p. 711 , published online 29 March; see the Perspective by Brook ) present a record of the carbon isotopic makeup of atmospheric CO 2 for the past 24,000 years. The findings reveal the dominant role of the oceans during the early part of the deglaciation and the effects of the regrowth of the terrestrial biosphere later in the deglacial transition. Before the deglaciation, during the Last Glacial Maximum, the carbon cycle was essentially at equilibrium.

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