Geoscience Reference
In-Depth Information
jected with the NCAR global coupled carbon cycle-cli-
mate model.
Biogeosciences
,
6
, 515-33.
Swift, E. and Taylor, W.R. (1966). The effect of pH on the
division rate of the coccolithophorid
Cricosphaera elon-
gata. Journal of Phycology
,
2
, 121-5.
The Royal Society (2005).
Ocean acidii cation due to increas-
ing atmospheric carbon dioxide
, 60 pp. The Royal Society,
London.
The Royal Society (2009).
Geoengineering the climate: science,
governance and uncertainty
, 82 pp. The Royal Society,
London.
Trivedi, B. and Danforth, W.H. (1966). Effect of pH on the
kinetics of frog muscle phosphofructokinase.
Journal of
Biological Chemistry
,
241
, 4110-12.
Turley, C.M. (1999). Taking research into policy making.
Proceedings of the Third European Marine Science and
Technology Conference
,
Ries, J.B., Cohen, A.L., and McCorkle, D.C. (2009). Marine
calcii ers exhibit mixed responses to CO
2
-induced ocean
acidii cation.
Geology
,
37
, 1131-4.
Rodolfo-Metalpa, R., Martin, S., Ferrier-Pagès, C., and
Gattuso, J.-P. (2010). Response of the temperate coral
Cladocora caespitosa
to mid- and long-term exposure to
p
CO
2
and temperature levels projected for the 2100 AD.
Biogeosciences
,
7
, 289-300.
Rubey, W.W. (1951). Geologic history of sea water: an
attempt to state the problem.
Bulletin of the Geological
Society of America
,
62
, 1111-48.
Sabine, C.L., Feely, R.A., Gruber, N.
et al.
(2004). The oce-
anic sink for anthropogenic CO
2
.
Science
,
305
, 367-71.
Santana-Casiano, J.M., González-Dávila, M., Rueda, M.J.,
Llinás, O., and González-Dávila, E.F. (2007). The inter-
annual variability of oceanic CO
2
parameters in the
northeast Atlantic subtropical gyre at the ESTOC
site.
Global Biogeochemical Cycles
,
6
, pp. 13-19, EU Directorate
21
,
GB1015,
General
Science,
Research
and
Development,
doi:10.1029/2006GB002788.
Shi, D., Xu, Y., Hopkinson, B.M., and Morel, F.M. (2010).
Effect of ocean acidii cation on iron availability to
marine phytoplankton.
Science
,
327
, 676-9.
Silverman, J., Lazar, B., Cao, L., Caldeira, K., and Erez, J.
(2009). Coral reefs may start dissolving when atmos-
pheric CO
2
doubles.
Geophysical Research Letters
,
36
,
L05606, doi:10.1029/2008GL036282.
Smith, S.V. and Pesret, F. (1974). Processes of carbon diox-
ide l ux in the Fanning Island lagoon.
Pacii c Science
,
28
,
225-45.
Sørensen, S.P.L. (1909). Études enzymatiques. II. Sur la
mesure et l'importance de la concentration des ions
hydrogène dans les réactions enzymatiques.
Comptes
Rendus des Travaux du Laboratoire Carlsberg
,
8
, 1-168.
Spivack, A.J., You, C.-F., and Smith, H.J. (1993).
Foraminiferal boron isotope ratios as a proxy for surface
ocean pH over the past 21 Myr.
Nature
,
363
, 149-51.
Steinacher, M., Joos, F., Frölicher, T.L., Plattner, G.-K., and
Doney, S.C. (2009). Imminent ocean acidii cation pro-
Brussels.
Widdicombe, S. and Needham, H.R. (2007). Impact of
CO
2
-induced seawater acidii cation on the burrowing
activity of
Nereis virens
and sediment nutrient l ux.
Marine Ecology Progress Series
,
341
, 111-22.
Wright, R.F. (2003). Predicting recovery of acidii ed fresh-
waters in Europe and Canada.
Hydrology and Earth
System Sciences
,
7
, 429-30.
Yu, J.M., Elderi eld, H., and Ho
nisch, B. (2007). B/Ca
in planktonic foraminifera as a proxy for surface
seawater pH.
Paleoceanography
,
22
, PA2202, doi:10.1029/
2006PA001347.
Zeebe, R.E. and Westbroek, P. (2003). A simple model
for the CaCO
3
saturation state of the ocean: the
'Strangelove', the 'Neritan', and the 'Cretan' Ocean.
Geochemistry Geophysics Geosystems
,
4
, 1104, doi:10.1029/
2003GC0000538.
Zeebe, R.E. and Wolf-Gladrow, D.A. (2001).
CO
2
in sea-
water: equilibrium, kinetics, isotopes
, 346 pp. Elsevier,
Amsterdam.
