Geoscience Reference
In-Depth Information
Atmosphere and climate
Carbon dioxide
Climate
Ocean
Human society
Biology-
biogeochemistry
Chemistry
Fisheries
Tourism
Ecological services
Policies
Higher CO 2
Lower pH
Lower carbonate
Nutrients
Trace metals
Calcification
Dissolution CaCO 3
Nitrogen fixation
Biodiversity
Food chain
Figure 1.4 Highly simplii ed view of the relationships between the atmosphere, ocean, and human activities in the context of ocean acidii cation. For the
sake of clarity, just a few examples are shown. The relationships between the atmosphere and ocean apply in both past and modern times.
1.7 Acknowledgements
Anne-Marin Nisumaa is gratefully acknowledged
for her assistance to draw i gure 1.2 . We thank
Kelvin Boot, Peter Liss and Stephen Smith for com-
ments on an early draft of this chapter. This work
is a contribution to the 'European Project on
Ocean Acidii cation' (EPOCA) which received
funding from the European Community's Seventh
Framework Programme (FP7/2007-2013) under
grant agreement n°211384.
Bates, N.R. (2001). Interannual variability of oceanic CO 2
and biogeochemical properties in the Western North
Atlantic subtropical gyre. Deep-Sea Research (Part II,
Topical Studies in Oceanography) , 48 , 1507-28.
Bates, N.R. and Peters, A.J. (2007). The contribution of
atmospheric acid deposition to ocean acidii cation in
the subtropical North Atlantic Ocean. Marine Chemistry ,
107 , 547-58.
Bibby, R., Cleall-Harding, P., Rundle, S., Widdicombe, S.,
and Spicer, J. (2007). Ocean acidii cation disrupts
induced defences in the intertidal gastropod Littorina
littorea. Biology Letters , 3 , 699-701.
Bijma, J., Barange, M., Brander, L. et al. (2009). Impacts of
ocean acidii cation , 12 pp. European Science Foundation,
Strasbourg, France.
Bouxin, H. (1926a). Action des acides sur le squelette des
larves de l'oursin Paracentrotus lividus . Inl uence du pH.
Comptes Rendus des Séances de la Société de Biologie , 94 ,
453-5.
Bouxin, H. (1926b). Action des acides sur les larves de l'oursin
Paracentrotus lividus . Étude morphologique. Comptes
Rendus des Séances de la Société de Biologie , 94 , 451-3.
Breitbarth, E., Bellerby, R.J., Neill, C.C. et al. (2010).
Ocean acidii cation affects iron speciation during a
coastal seawater mesocosm experiment. Biogeosciences ,
7 , 1065-73.
Brewer, P.G. (1978a). Direct observation of the oceanic CO 2
increase. Geophysical Research Letters , 5 , 997-1000.
Broecker, W. and Clark, E. (2001). A dramatic Atlantic dis-
solution event at the onset of the last glaciation.
References
Agegian, C.R. (1985). The biogeochemical ecology of
Porolithon gardineri (Foslie) , 178 pp. PhD Thesis,
University of Hawaii, Honolulu, HI.
Álvarez, M., Monaco, C.L., Tanhua, T. et al. (2009).
Estimating the storage of anthropogenic carbon in the
subtropical Indian Ocean: a comparison of i ve different
approaches. Biogeosciences , 6 , 681-703.
Andersson, A., Mackenzie, F.T., and Ver, L.M. (2003). Solution
of shallow-water carbonates: an insignii cant buffer
against rising atmospheric CO 2 . Geology , 31 , 513-16.
Anonymous (2009). Monaco Declaration . Prince Albert II of
Monaco Foundation, Monaco.
Barker, S. and Elderi eld, H. (2002). Foraminiferal calcii ca-
tion response to glacial-interglacial changes in atmos-
pheric CO 2 . Science , 297 , 833-6.
 
 
Search WWH ::




Custom Search