Khatiwala S. Fast spin up of ocean biogeochemical models using matrix-free Newton-Krylov[J]. Ocean Modelling, 2008, 23: 121—129.
[2]
Burns W C G. Anthropogenic carbon dioxide emissions and ocean acidification: The potential impacts on ocean biodiversity[A]//Robert A. Askins, Glenn D. Dreyer, Gerald R. Visgilio, Diana M. Whitelaw. Saving Biological Diversity[C]. Berlin: Springer Science and Business Media, 2008:187—202.
[3]
Pelletier G J, Lewis E, Wallace D W R. CO2SYS.XLS: A calculator for the CO2 system in seawater for Microsoft Excel/VBA. Version 16. Olympia (Washington): Washington State Department of Ecology, 2011 (available at : http://www.ecy.wa.gov/programs/eap/models.html).
[4]
Zeebe R E, Zachos J C, Caldeira K, et al. Carbon emissions and acidification[J]. Science, 2008, 321: 51—52.
[5]
Hall-Spencer J M, Rodolfo-Metalpa R, Martin S, et al. Volcanic carbon dioxide vents show ecosystem effects of ocean acidification[J]. Nature, 2008, 454: 96—99.
[6]
Baumann H, Talmage S C, Gobler C J. Reduced early life growth and survival in a fish indirect response to increased carbon dioxide[J]. Nature Climate Change, 2012, 2: 38—41.
[7]
Domenici P, Allan B, McCormick M I, et al. Elevated carbon dioxide affects behavioural lateralization in a coral reef fish[J]. Biology Letters, 2012, 8: 78—81.
Gazeau F, Quiblier C, Jansen J M, et al. Impacts of elevated CO2 on shellfish calcification[J]. Geophysical Research Letters, 2007, 34: L07603, doi:10.1029/2006GL028554.
[10]
Fraga F, Ríos A F, Pérez F F,et al. Theoretical limits of oxygen: carbon and oxygen: nitrogen ratios during photosynthesis and mineralization of organic matter in the sea[J]. Scientia Marina, 1998, 62(1/2):161—168.
Dickson A G. Standard potential of the reaction: AgCl(s)+1/2 H2(g)=Ag(s)+HCl(aq), and the standard acidity constant of the ion HSO-4 in synthetic sea water from 273.15 to 318.15 K[J]. Journal of Chemical Thermodynamics, 1990, 22: 113—127.
[14]
Waldbusser G G, Steenson R A, Green M A. Oyster shell dissolution rates in estuarine waters: effects of pH and shell legacy[J]. Journal of Shellfish Research, 2011, 30(3): 659—669.
[15]
Suzuki A, Nakamori T, Kayanne H. The mechanism of production enhancement in coral reef carbonate system: model and empirical results[J]. Sedimentary Geology, 1995, 99: 259—280.
[16]
沈同, 王镜岩. 生物化学[M]. 第2版. 北京: 高等教育出版社, 1991:1—1090.
[17]
Gao K S, Aruga Y, Asada K, et al. Calcification in the articulated coralline alga Carollina pilulifera, with special reference to the effect of elevated CO2 concentration[J]. Marine Biology, 1993, 117: 129—132.
[18]
Talmage S C, Gobler C J. Effects of elevated temperature and carbon dioxide on the growth and survival of larvae and juveniles of three species of Northwest Atlantic bivalves[J]. PloS ONE, 2011, 6(10): e26941. doi:10.1371/journal.pone.0026941
[19]
Bibby R, Cleall-Harding P, Rundle S, et al. Ocean acidification disrupts induced defences in the intertidal gastropod Littorina littorea[J]. Biology Letters, 2007, 3: 699—701.
[20]
Munday P L, Dixson D L, McCormick M I, et al. Replenishment of fish populations is threatened by ocean acidification[J]. Proceeding of the National Academy of Sciences of the United States of America, 2010, 107: 12930—12934.
[21]
Caldeira K, Wickett M E. Anthropogenic carbon and ocean pH[J]. Nature, 2003, 425:365.
[22]
Kleypas J A, Feely R A, Fabry V J. et al. Impacts of ocean acidification on coral reefs and other marine calcifiers: A guide for future research[R]. Boulder, Colorado: Institute for the Study of Society and Environment (ISSE) of the University Corporation for Atmospheric Research (UCAR), 2006, 1—88.
[23]
Kelly R P, Foley M M, Fisher W S, et al. Mitigating local causes of ocean acidification with existing laws[J]. Science, 2011, 332: 1036—1037.
[24]
Gruber N, Hauri C, Lachkar Z, et al. Rapid progression of ocean acidification in the California current system[J]. Science, 2012, 337: 220—223.
[25]
Zhai W D, Zheng N, Huo C, et al. Subsurface low pH and carbonate saturation state of aragonite on China side of the North Yellow Sea: combined effects of global atmospheric CO2 increase, regional environmental changes, and local biogeochemical processes[J]. Biogeosciences discussion, 2013, 10: 3079—3120.
[26]
Dickson A G. The development of the alkalinity concept in marine chemistry[J]. Marine Chemistry, 1992, 40: 49—63.
[27]
Smith S V, Key G S. Carbon dioxide and metabolism in marine environments[J]. Limnology and Oceanography, 1975, 20: 493—495.
Millero F J, Graham T B, Huang F, et al. Dissociation constants of carbonic acid in seawater as a function of salinity and temperature[J]. Marine Chemistry, 2006, 100: 80—94.
[31]
Mucci A. The solubility of calcite and aragonite in seawater at various salinities, temperatures, and one atmosphere total pressure[J]. American Journal of Science, 1983, 283: 780—799.
[32]
Yamamoto S, Kayanne H, Terai M, et al. Threshold of carbonate saturation state determined by CO2 control experiment[J]. Biogeosciences, 2012, 9: 1441—1450.
[33]
Michaelidis B, Ouzounis C, Paleras A,et al. Effects of long-term moderate hypercapnia on acid–base balance and growth rate in marine mussels Mytilus galloprovincialis[J]. Marine Ecology Progress Series, 2005, 293: 109—118.
[34]
Le Quéré C, Raupach M R, Canadell J G, et al. Trends in the sources and sinks of carbon dioxide[J]. Nature Geoscience, 2009, 2: 831—836.
[35]
Fabry V J, Seibel B A, Feely R A, et al. Impacts of ocean acidification on marine fauna and ecosystem processes[J]. ICES Journal of Marine Science, 2008, 65: 414—432.
[36]
Shamberger K E F, Feely R A, Sabine C L, et al. Calcification and organic production on a Hawaiian coral reef[J]. Marine Chemistry, 2011, 127: 64—75.