Tschumi, T., Joos, F., Gehlen, M., & Heinze, C. (2011). Deep ocean
ventilation, carbon isotopes, marine sedimentation and the deglacial
CO 2 rise. Climate of the Past, 7, 771–800. https://doi.org/10.5194/
cp-7-771-2011.
Vadsaria, T., Ramstein, G., Dutay, J. C., Li, L., Ayache, M., & Richon,
C. (2019). Simulating the occurrence of the last sapropel event (S1):
Mediterranean basin ocean dynamics simulations using Nd isotopic
composition modeling. Paleoceanography and Paleoclimatology.
http://doi.org/10.1029/2019PA003566.
Valdes, P. J., Beerling, D. J., & Johnson, C. E. (2005). The ice age
methane budget. Geophysical Research Letters, 32, L02704. https://
doi.org/10.1029/2004GL021004.
WAIS Divide Project Members. (2015). Precise interpolar phasing of
abrupt climate change during the last ice age. Nature, 520, 661–668.
https://doi.org/10.1038/nature14401.
Walker, J. C. G. (1980). The oxygen cycle. In O. Hutzinger (Ed.), The
natural environment and the biogeochemical cycles (pp. 87–104).
Berlin, Heidelberg: Springer.
Wang, W., Yung, Y., Lacis, A., Mo, T., & Hansen, J. (1976).
Greenhouse effects due to man made perturbations of trace gases.
Science, 194(4266), 685–690.
Weber, S. L., Drury, A. J., Toonen, W. H. J., & van Weele, M. (2010).
Wetland methane emissions during the Last Glacial Maximum
estimated from PMIP2 simulations: Climate, vegetation, and
geographic controls. Journal Geophysical Research, 115,
D06111. https://doi.org/10.1029/2009JD012110.
Wolff, E. W., Fischer, H., Fundel, F., Ruth, U., Twarloh, B., Littot, G.
C., Mulvaney, R., Röthlisberger, R., de Angelis, M., Boutron, C. F.,
Hansson, M., Jonsell, U., Hutterli, M. A., Lambert, F., Kaufmann,
P., Stauffer, B., Stocker, T. F., Steffensen, J. P., Bigler, M.,
Siggaard-Andersen, M. L., Udisti, R., Becagli, S., Castellano, E.,
Severi, M., Wagenbach, D., Barbante, C., Gabrielli P., & Gaspari V.
(2006). Southern Ocean sea-ice extent, productivity and iron flux
over the past eight glacial cycles. Nature 440, 23. https://doi.org/10.
1038/nature04614.
Yin, Q. Z., & Berger, A. (2010). Insolation and CO 2 contribution to the
interglacial climate before and after the Mid-Brunhes Event. Nature
Geoscience, 3, 243–246. https://doi.org/10.1038/ngeo771.
Yin, Q. Z., & Berger, A. (2012). Individual contribution of insolation
and CO 2 to the interglacial climates of the past 800,000 years.
Climate Dynamics, 38(3–4), 709–724.
Yu, J., Menviel, L., Jin, Z. D., Thornalley, D. J. R., Barker, S., Marino,
G., Rohling, E. J., Cai, Y., Zhang, F., Wang, X., Dai, Y., Chen P., &
Broecker W. S. (2016). Sequestration of carbon in the deep Atlantic
during the last glaciation. Nature Geoscience, 9, 319–324.
Ziegler, M., Tuenter, E., & Lourens, L. J. (2010). The precession phase of
the boreal summer monsoon as viewed from the eastern Mediterranean (ODP Site 968). Quaternary Science Reviews, 29, 1481–1490.
300
N. Bouttes et al.
ventilation, carbon isotopes, marine sedimentation and the deglacial
CO 2 rise. Climate of the Past, 7, 771–800. https://doi.org/10.5194/
cp-7-771-2011.
Vadsaria, T., Ramstein, G., Dutay, J. C., Li, L., Ayache, M., & Richon,
C. (2019). Simulating the occurrence of the last sapropel event (S1):
Mediterranean basin ocean dynamics simulations using Nd isotopic
composition modeling. Paleoceanography and Paleoclimatology.
http://doi.org/10.1029/2019PA003566.
Valdes, P. J., Beerling, D. J., & Johnson, C. E. (2005). The ice age
methane budget. Geophysical Research Letters, 32, L02704. https://
doi.org/10.1029/2004GL021004.
WAIS Divide Project Members. (2015). Precise interpolar phasing of
abrupt climate change during the last ice age. Nature, 520, 661–668.
https://doi.org/10.1038/nature14401.
Walker, J. C. G. (1980). The oxygen cycle. In O. Hutzinger (Ed.), The
natural environment and the biogeochemical cycles (pp. 87–104).
Berlin, Heidelberg: Springer.
Wang, W., Yung, Y., Lacis, A., Mo, T., & Hansen, J. (1976).
Greenhouse effects due to man made perturbations of trace gases.
Science, 194(4266), 685–690.
Weber, S. L., Drury, A. J., Toonen, W. H. J., & van Weele, M. (2010).
Wetland methane emissions during the Last Glacial Maximum
estimated from PMIP2 simulations: Climate, vegetation, and
geographic controls. Journal Geophysical Research, 115,
D06111. https://doi.org/10.1029/2009JD012110.
Wolff, E. W., Fischer, H., Fundel, F., Ruth, U., Twarloh, B., Littot, G.
C., Mulvaney, R., Röthlisberger, R., de Angelis, M., Boutron, C. F.,
Hansson, M., Jonsell, U., Hutterli, M. A., Lambert, F., Kaufmann,
P., Stauffer, B., Stocker, T. F., Steffensen, J. P., Bigler, M.,
Siggaard-Andersen, M. L., Udisti, R., Becagli, S., Castellano, E.,
Severi, M., Wagenbach, D., Barbante, C., Gabrielli P., & Gaspari V.
(2006). Southern Ocean sea-ice extent, productivity and iron flux
over the past eight glacial cycles. Nature 440, 23. https://doi.org/10.
1038/nature04614.
Yin, Q. Z., & Berger, A. (2010). Insolation and CO 2 contribution to the
interglacial climate before and after the Mid-Brunhes Event. Nature
Geoscience, 3, 243–246. https://doi.org/10.1038/ngeo771.
Yin, Q. Z., & Berger, A. (2012). Individual contribution of insolation
and CO 2 to the interglacial climates of the past 800,000 years.
Climate Dynamics, 38(3–4), 709–724.
Yu, J., Menviel, L., Jin, Z. D., Thornalley, D. J. R., Barker, S., Marino,
G., Rohling, E. J., Cai, Y., Zhang, F., Wang, X., Dai, Y., Chen P., &
Broecker W. S. (2016). Sequestration of carbon in the deep Atlantic
during the last glaciation. Nature Geoscience, 9, 319–324.
Ziegler, M., Tuenter, E., & Lourens, L. J. (2010). The precession phase of
the boreal summer monsoon as viewed from the eastern Mediterranean (ODP Site 968). Quaternary Science Reviews, 29, 1481–1490.
300
N. Bouttes et al.