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Holocene carbon cycle dynamics

Published:2010-01 Issue:2 Volume:37 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Kleinen Thomas¹,Brovkin Victor,von Bloh Werner²,Archer David³,Munhoven Guy⁴

Affiliation:

1. Max Planck Institute for Meteorology; Hamburg; Germany

2. Potsdam Institute for Climate Impact Research; Potsdam; Germany

3. Department of the Geophysical Sciences; University of Chicago; Chicago; Illinois; USA

4. LPAP, Institut d'Astrophysique et de Geophysique; Universit de Liège; Liège; Belgium

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/gl1002/2009GL041391/2009GL041391.pdf

Reference29 articles.

1. A data-driven model of the global calcite lysocline;Archer;Global Biogeochem. Cycles,1996

2. Foraminiferal calcification response to glacial-interglacial changes in atmospheric CO2;Barker;Science,2002

3. Climate change and Arctic ecosystems: 1. Vegetation changes north of 55°N between the last glacial maximum, mid-Holocene, and present;Bigelow;J. Geophys. Res.,2003

4. Evidence for a reduction in the carbonate ion content of the deep sea during the course of the Holocene;Broecker;Paleoceanography,1999

5. Carbon cycle, vegetation, and climate dynamics in the Holocene: Experiments with the CLIMBER-2 model;Brovkin;Global Biogeochem. Cycles,2002

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