Articles | Volume 8, issue 1
https://doi.org/10.5194/cp-8-251-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.Glacial CO2 cycle as a succession of key physical and biogeochemical processes
Related subject area
Subject: Carbon Cycle | Archive: Ice Cores | Timescale: Milankovitch
Cited articles
Adkins, J. F., McIntyre, K., and Schrag, D. P.: The salinity, temperature, and δ18O of the glacial deep ocean, Science, 298, 1769–1773, 2002.
Ahn, J., and Brook, E. J.: Atmospheric CO2 and climate on millennial time scales during the last glacial period, Science, 322, 83–85, https://doi.org/10.1126/science.1160832, 2008.
Amiotte-Suchet, P., Probst, J. L., and Ludwig, W.: Worldwide distribution of continental rock lithology: Implications for the atmospheric/soil CO2 uptake by continental weathering and alkalinity river transport to the oceans, Global Biogeochem. Cy., 17, 1038, https://doi.org/10.1029/2002gb001891, 2003.
Anderson, R. F., Fleisher, M. Q., Lao, Y., and Winckler, G.: Modern CaCO3 preservation in equatorial Pacific sediments in the context of late-Pleistocene glacial cycles, Mar. Chem., 111, 30–46, https://doi.org/10.1016/j.marchem.2007.11.011, 2008.
Anderson, R. F., Ali, S., Bradtmiller, L. I., Nielsen, S. H. H., Fleisher, M. Q., Anderson, B. E., and Burckle, L. H.: Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO2, Science, 323, 1443–1448, https://doi.org/10.1126/science.1167441, 2009.