Skeletons and ocean chemistry: the long view - Ocean Acidification - page 80

Brewer, P.G. and Peltzer, E.T. (2009). Limits to marine life.
Science , 324 , 347-8.
Cao, C.-Q., Love, G.D., Hays, L.E. et al . (2009).
Biogeochemical evidence for euxinic oceans and eco-
logical disturbance presaging the end-Permian mass
extinction event. Earth and Planetary Science Letters , 281 ,
188-201.
Copper, P. (2002a). Ancient reef ecosystem expansion and
collapse. Coral Reefs , 13 , 3-11.
Copper, P. (2002b). Reef development at the Frasnian/
Famennian mass extinction boundary. Palaeogeography,
Palaeoclimatology, Palaeoecology , 181 , 27-65.
Courtillot, V. and Olson, P. (2007). Mantle plumes link
magnetic superchrons to Phanerozoic mass depletion
events. Earth and Planetary Science Letters , 260 , 495-504.
Dickens, G.R., O'Neil, J.R., Rea, D.K., and Owen R.M.
(1995). Dissociation of oceanic methane hydrate as a
cause of the carbon-isotope excursion at the end of the
Paleocene. Paleoceanography , 10 , 965-71.
Doney, S.C., Fabry, V.J., Feely, R.A., and Kleypas, J.A.
(2009). Ocean acidii cation: the other CO 2

Gingerich, P.D. (2006). Environment and evolution
through the Paleocene-Eocene thermal maximum.
Trends in Ecology and Evolution , 21 , 246-53.
Glass, L.M. and Phillips, D. (2006). The Kalkarindji conti-
nental l ood basalt province: a new large igneous prov-
ince in Australia with possible links to end-Early
Cambrian faunal extinctions. Geology , 34 , 461-4.
Gooding, R.A., Harley, C.D.G., and Tang, E. (2009).
Elevated water temperature and carbon dioxide con-
centration increase the growth of a keystone echino-
derm. Proceedings of the National Academy of Sciences
USA , 106 , 9316-21.
Grotzinger, J.P. and Knoll, A.H. (1999). Proterozoic stroma-
tolites: evolutionary mileposts or environmental dip-
sticks? Annual Review of Earth and Planetary Science , 27 ,
313-58.
Harper, D.A.T. (2006). The Ordovician biodiversii cation:
setting an agenda for marine life. Palaeogeography,
Palaeoclimatology, Palaeoecology , 232 , 148-66.
Hautmann, M. (2004). Effect of end-Triassic CO 2 maxi-
mum on carbonate sedimentation and marine mass
extinction. Facies , 50 , 257-61.
Hautmann, M., Benton, M.J., and Tomasovych, A. (2008a).
Catastrophic ocean acidii cation at the Triassic-Jurassic
boundary. Neues Jahrbuch für Geologie und Paläontologie,
Abhandlungen , 249 , 119-127.
Hautmann, M., Stiller, F., Cai, H.W., and Sha, J.G. (2008b).
Extinction-recovery pattern of level-bottom faunas
across the Triassic--Jurassic boundary in Tibet: implica-
tions for potential killing mechanisms. Palaios ,

problem.

Annual Review of Marine Science , 1 , 169-92.
Erwin, D.H. (2006). Extinction: how life on earth nearly ended
250 million years ago , 296 pp. Princeton University Press,
Princeton, NJ.
Evins, L.Z., Jourdan, F. and Phillips, D. (2009). The
Cambrian Kalkarindji Large Igneous Province: extent
and characteristics based on new Ar-40/Ar-39 and geo-
chemical data. Lithos , 110 , 294-304.
Ezaki, Y. (2009). Secular l uctuations in Palaeozoic and
Mesozoic reef-forming organisms during greenhouse
periods: geobiological interrelations and consequences.
Paleontological Research , 13 , 23-38.
Fine, M. and Tchernov, D. (2007). Scleractinian coral spe-
cies survive and recover from decalcii cation. Science ,
315 , 1811.
Ganino, C. and Arndt, N.T. (2009). Climate changes caused
by degassing of sediments during the emplacement of
large igneous provinces. Geology , 37 , 323-6.
Gattuso, J.-P., Allemand, D., and Frankignoulle, M. (1999).
Photosynthesis and calcii cation at cellular, organismal
and community levels in coral reefs: a review on inter-
actions and control by carbonate chemistry. American
Zoologist , 39 , 160-83.
Gili, E., Masse, J.P., and Skelton, P.W. (1995). Rudists as
gregarious sediment dwellers, not reef-builders, on
Cretaceous carbonate platforms. Palaeogeography,
Palaeoclimatology, Palaeoecology , 118 , 245-67.
Gill, B.C., Lyons, T.W., Young, S., Kump, L., Knoll, A.H.,
and Saltzman, M.R. (2011). Geochemical evidence for
widespread euxinia in the later Cambrian ocean. Nature ,
469 , 80-83.

23 ,

711-18.
Higgins, J.A. and Schrag, D.P. (2006). Beyond methane:
towards a theory for the Paleocene-Eocene Thermal
Maximum. Earth and Planetary Science Letters , 245 ,

523-37.
Higgins, J.A., Fischer, W.W., and Schrag, D.P. (2009).
Oxygenation of the ocean and sediments: consequences
for the seal oor carbonate factory. Earth and Planetary
Science Letters , 284 , 25-33.
Hoegh-Guldberg, O., Mumby, P.J., Hooten, A.J. et al . (2007).
Coral reefs under rapid climate change and ocean acidi-
i cation. Science , 318 , 1737-42.
Hough, M.L., Shields, G.A., Evins, L.Z., Strauss, H.,
Henderson, R.A., and Mackenzie, S. (2006). A major sul-
phur isotope event at c. 510 Ma: a possible anoxia- extinc-
tion-volcanism connection during the Early-Middle
Cambrian transition? Terra Nova , 18 , 257-63.
Hurtgen, M.T., Pruss, S.B., and Knoll, A.H. (2009).
Evaluating the relationship between the carbon and sul-
fur cycles in later Cambrian oceans: an example from
the Port au Port Group, western Newfoundland. Earth
and Planetary Science Letters , 281 , 288-97.