Constraint of the CO2rise by new atmospheric carbon isotopic measurements during the last deglaciation-Reference-Cited by-同舟云学术

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Constraint of the CO2rise by new atmospheric carbon isotopic measurements during the last deglaciation

Published:2010-06 Issue:2 Volume:24 Page:n/a-n/a
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Lourantou Anna¹,Lavrič Jošt V.,Köhler Peter²,Barnola Jean-Marc¹,Paillard Didier³,Michel Elisabeth³,Raynaud Dominique¹,Chappellaz Jérôme¹

Affiliation:

1. Laboratoire de Glaciologie et Géophysique de l'Environnement; Université Joseph Fourier-Grenoble, CNRS; St Martin d'Hères; France

2. Alfred Wegener Institute for Polar and Marine Research; Bremerhaven; Germany

3. Laboratoire des Sciences du Climat et de l'Environnement, IPSL; Université Versailles-St Quentin, CNRS; Gif-sur-Yvette; France

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Link

http://www.agu.org/journals/gb/gb1002/2009GB003545/2009GB003545.pdf

Reference92 articles.

1. A record of atmospheric CO2 during the last 40,000 years from the Siple Dome, Antarctica ice core;Ahn;J. Geophys. Res.,2004

2. The Greenland ice core chronology 2005, 15-42 ka. Part 1: Constructing the time scale;Andersen;Quat. Sci. Rev.,2007

3. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2;Anderson;Science,2009

4. Processes affecting the CO2 concentrations measured in Greenland ice;Anklin;Tellus, Ser. B,1995

5. Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration;Archer;Nature,1994

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