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response to long- and short-term paleoclimatic change.
Earth-Science Reviews , 90 , 71-102.
Sheehan, P.M. (2001). The Late Ordovician mass extinction.
Annual Review of Earth and Planetary Sciences , 29 , 331-64.
Smith, R. and Botha, J. (2005). The recovery of terrestrial
vertebrate diversity in the South African Karoo Basin
after the end-Permian extinction. Comptes Rendus Palevol ,
4 , 623-36.
Soetaert K., Hofmann, A.F., Middelburg, J.J., Meysman,
F.J.R., and Greenwood J. (2007). The effect of biogeo-
chemical processes on pH. Marine Chemistry , 105 , 30-51.
Svensen, H., Planke, S., Malthe-Sørenssen, A. et al . (2004).
Release of methane from a volcanic basin as a mechanism
for initial Eocene global warming. Nature , 429 , 542-5.
Thomas, E. (2007). Cenozoic mass extinctions in the deep
sea: what perturbs the largest habitat on Earth? Geological
Society of America Special Paper , 424 , 1-24.
Veron, J.E.N. (2008). Mass extinctions and ocean acidii ca-
tion: biological constraints on geological dilemmas.
Coral Reefs , 27 , 459-72.
Walker, J.C.G., Hays, P.B., and Kasting, J.F. (1981). A nega-
tive feedback mechanism for the long-term stabilization
of Earth's surface temperature. Journal of Geophysical
Research , 86 , 9776-82.
Widdicombe, S. and Spicer, J.I. (2008). Predicting the
impact of ocean acidii cation on benthic biodiversity:
what can animal physiology tell us? Journal of
Experimental Marine Biology and Ecology , 366 , 187-97.
Wignall, P.B. (2001). Large igneous provinces and mass
extinctions. Earth-Science Reviews , 53 , 1-33.
Wignall, P.B. and Twitchett, R.J. (1996). Oceanic anoxia and
the end Permian mass extinction. Science , 272 , 1155-8.
Wing, S.L., Harrington, G.J., Smith, F.A., Bloch, J.I., Boyer,
D.M., and Freeman, K.H. (2005). Transient l oral change
and rapid global warming at the Paleocene-Eocene
boundary. Science , 310 , 993-6.
Wood, R. (1999). Reef evolution , 414 pp. Oxford University
Press, Oxford.
Zachos, J.C., Lohmann, K.C., Walker, J.C.G., and Wise,
S.W. (1993). Abrupt climate change and transient cli-
mates during the Paleogene: a marine perspective.
Journal of Geology , 101 , 191-213.
Zachos, J.C., Wara, M.W., Bohaty, S. et al. (2003). A tran-
sient rise in tropical sea surface temperature during the
Paleocene-Eocene thermal maximum. Science ,
302 ,
1551-54.
Zachos, J.C., Rohl, U., Schellenberg, S.A. et al . (2005). Rapid
acidii cation of the ocean during the Paleocene-Eocene
thermal maximum. Science , 308 , 1611-15.
Zhuravlev, A.Y. and Wood, R.A. (1996). Anoxia as the
cause of the mid-early Cambrian (Botomian) extinction
event. Geology , 24 , 311-14.
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